BUKU KETERANGAN
PETA SATUAN LAHAN DAN TANAH
LEMBAR TOBOALI, SUMATERA
EXPLANATORY BOOKLET OF THE LAND UNIT AND SOIL MAP
OF THE TOBOALI SHEET, SUMATRA
Oleh/By :
A. Hidayat, Junus Dai, H. Darul SWP, H.Y. Sumulyadi, A. Hermawan, Hendra S.,
Yayat AH, P. Buurman, T. Balsem
SEKAIA/SCALE
60
o
1 : 250.000
LEMBAR/SHEET : 1112
99°
105°
-
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1211
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PROYEK PERENCANAAN DAN EVALUASI SUMBER DAYA LAHAN
PENGELOLAAN DATA BASE TANAH
PUSAT PENELITIAN TANAH
BADAN PENELITIAN DAN PENGEMBANGAN PERTANIAN
LAND RESOURCE EVAL UA TION AND PLANNING PROJECT
SOIL DATA BASE MANAGEMENT
CENTER FOR SOIL RESEARCH
AGENCY FOR AGRICULTURAL RESEARCH AND DEVELOPMENT
1989
-
Penanggung jawab
Head of the Project
DR. M. SUDJADI
Kepala Pusat Penelitian Tanah
Badan Penelitian dan Pengembangan Pertanian
Departemen Pertanian
The Director of the Center for Soil Research
Agency for Agricultural Research and Development
Department of Agriculture
Urusan mengenai publikasi ini hams dialamatkan kepada:
Kepala Pusat Penelitian Tanah
Jalan H. Juanda 98, Tilpon 23012
Bogor 16123, Indonesia
Correspondence concerning this publication should be addressed to:
The Director of the Center for Soil Research
Jalan H. Juanda 98, Phone 23012
Bogor 16123, Indonesia
BUKU KETERANGAN
PETA SATUAN LAHAN dan TANAH LEMBAR TOBOALI (1112), SUMATERA
Explanatory booklet of the
LAND UNIT and SOIL map of the TOBOALI Sheet (1112), Sumatra
Sekala/Scale
1 : 250.000
Oleh/By:
A.Hidayat, Junus Dai, H. Darul SWP, H.Y. Sumulyadi, Adi Hermawan,
Hendra S., Yayat A.H., P.Buurman dan/and T.Balsem
Buku Keterangan Peta Satuan Lahan dan Tanah ini dihasilkan oleh Tim
Pengelolaan Data Base Tanah dari Proyek Perencanaan dan Evaluasi
Sumber Daya Lahan, program kerja sama teknis antara Pemerintah
Republik Indonesia dan Bank Pembangunan Asia, dilaksanakan oleh
Pusat Penelitian Tanah (Badan Penelitian dan Pengembangan Pertanian, Departemen Pertanian) dan dikoordinasikan oleh Badan Koordinasi Survei dan Pemetaan Nasional (BAKOSURTANAL). Survei dan
pemetaan dilaksanakan
oleh Pusat Penelitian Tanah
bekerjasama
dengan konsultan dari HASKONING Royal Dutch Consulting Engineers
and Architects.
This Explanatory Booklet and the accompanying Land Unit and Soil
map have been produced by the Soil Data Base Management Team of the
Land Resource Evaluation and Planning Project (LREP, part II), a
technical cooperation programme between the Government of the
Republic of Indonesia and the Asian Development Bank, executed by
the Center for Soil Research (part of the Agency for Agricultural
Research and Development of the Department of Agriculture) and supervised by the National Coordination Agency for Surveys and Mapping (BAKOSURTANAL). The survey and mapping were carried out by
the Center for Soil Research, in cooperation with the consultants
of HASKONING Royal Dutch Consulting Engineers and Architects.
PUSAT PENELITIAN TANAH
BADAN PENELITIAN DAN PENGEMBANGAN PERTANIAN
DEPARTEMEN PERTANIAN
CENTER for SOIL RESEARCH
AGENCY for AGRICULTURAL RESEARCH and DEVELOPMENT
DEPARTMENT of AGRICULTURE
Hak cipta dilindungi. Tidak sebahagianpun dari publikasi ini dapat direproduksi
kembali, disimpan dalam suatu sistim penyirapanan dan penarikan data,
atau
dipindahkan kedalam bentuk apapun atau dengan alat/cara seperti : elektronik,
elektrostatik, pita magnetik, mekanik, fotokopi, direkam atau sejenisnya tanpa
adanya ijin secara t e r t u l i s dari penerbit.
Edisi pertam? , 1989.
All Rights Reserved. No part of chis publication may be reproduced, stored in a
retrieval
system or transmitted
in any form or by any means:
electronic,
electrostatic,
magnetic tape, mechanical, photocopying, recording or otherwise,
wit'iout permission in writing from the publishers.
First edition,
1989.
Cara merujuk buku i n i :
A . H i d a y a t , Junus D a i , H. Darul SWP, H.Y. Sumulyadi, Adi Hermawan, Hendra S . ,
Yayat A . H . , P.Buurman d a n T.Balsem, 1989. Buku K e t e r a n g a n P e t a S a t u a n Lahan d a n
T'anah lembar T o b o a l i ( 1 1 1 2 ) , S u m a t e r a . P u s a t P e n e l i t i a n Tanah. Bogor.
•How to cite
this
book:
A.Hidayat,
Junus Dai, H. Darul SWP, H.Y. Sumulyadi,
Adi Hermawan, Hendra S.,
Yayat A.H., P.Buurman and T.Balsem,
1989. Explanatory
booklet
of
the Land
Unit and Soil
map of the Toboali
Sheet
(1112),
Sumatra.
Center
for
Soil
Research,
Bogor.
Scanned from original by ISRIC - World Soil Information, as ICSU
World Data Centre for Soils. The purpose is to make a safe
depository for endangered documents and to make the accrued
information available for consultation, following Fair Use
Guidelines. Every effort is taken to respect Copyright of the
materials within the archives where the identification of the
Copyright holder is clear and, where feasible, to contact the
originators. For questions please contact soil.isric@wur.nl
indicating the item reference number concerned.
1112 - i i
PENUNTUN UNTUK PEMAKAI
USER MANUAL
Buku keterangan ini adalah penjelasan
dari Peta Satuan Lahan dan Tanah lembar Toboali (1112), Sumatera, sekala
1:250.000.
This booklet is an explanation of the
1:250,000 scale Land Unit and Soil map
of the Toboali
mapsheet
(1112),
Sumatra.
Legenda peta berisikan satuan lahan
yang merupakan satuan geomorfik dan
dibatasi dengan cara menginterpretasi
foto udara, citra satelit dan citra
Radar. Isi dari tiap satuan lahan
diperiksa di lapangan dan kemudian
dicatat. Hanya sebahagian dari semua
informasi ini disajikan dalam peta,
sedangkan sebahagian lagi diberikan
secara ringkas dalam Buku Keterangan
ini ; informasi yang lebih lengkap
dapat tersedia jika diminta.
The legend of the map consists of Land
Units, which are geomorphic units,
delineated by interpretation of images
such as aerial photographs, satellite
imagery and Synthetic Aperture Radar.
The contents of each of the units is
checked in the field and recorded.
Only part of this information can be
represented in the map; the remainder
is briefly documented in the present
explanatory notes, and more complete
information is available upon request.
Simbol peta menunjukan grup fisiografi
(huruf besar), tipe batuan (huruf
kecil), dan pembagian lebih Ianjut
berdasarkan atas lereng dan tingkat
torehan (pada daerah berlereng dan
angkatan) atau berdasarkan lingkungan
pengendapan/hidrologinya (pada daerah
aluvial resen dan marin), yang ditunjukan oleh angka. Huruf kecil yang
berada dimuka kode grup fisiografi
menunjukan adanya tutupan dari bahan
lain, seperti tutupan abu volkan pada
perbukitan dari batuan sedimen atau
lapisan bahan organik tipis pada
dataran aluvial.
Hap symbols indicate physiographic
group (capital letter),
rock type
(lower case letter), and subdivisions
according to slope and dissection (in
sloping and uplifted areas) or to
sedimentary/hydrological environment
(in recent alluvial and marine areas),
indicated with numbers. Lower case
letters preceding the physiographic
group code are used to indicate covers
of material with differing composition, such as volcanic ash covers on
hills of sedimentary rocks, or thin
peat on alluvial plain units.
Grup fisiografi tersebut adalah :
Kubah Gambut, Aluvial, Marin, Teras
Marin, Dataran Tuf Masam, Dataran, Tuf
Masam Toba, Volkan, Karst, Perbukitan,
Pegunungan/Plato dan Aneka Bentuk.
Grup Dataran Tuf Masam, Tuf Masam
Toba, Volkan, Kubah Gambut dan Karst
pembagiannya didasarkan pada tipe
batuan dan morfologi yang spesifik
yang hubungannya erat dengan sifat
tanah yang spesifik. Grup yang lainnya
sebahagian besar hanya berdasarkan
pada morfologi.
The physiographic groups are : Peat
Domes, Alluvial, Marine, Marine Terrace, Acid Tuff Plains, Plains, Toba
Acid Tuff, Volcanic, Karst, Hill,
Mountain/Plateau and Miscellaneous.
The Acid Tuff Plain, the Toba Acid
Tuff, the Volcanic, the Peat Domes and
the Karst group are based on rock type
and specific morphology, with a close
link to specific soil characterestics.
The other groups are largely morphological .
Untuk semua sàtuan lahan, data keadaan
tanah dan hubungan tanah dengan bentang alam disajikan pada Uraian Satuan
For all land units, data on soils and
soil/landscape relations are presented
in the Land Unit Descriptions. These
1112 - iii
Lahan. Uraian satuan lahan ini
merupakan bagian terpenting dari Buku
Keterangan ini sebab semua
informasi
yang diperlukan untuk mengevaluasi
setiap satuan lahan untuk penggunaan
tertentu ada disini.
descriptions form an essential part
of the Explanatory Notes, because all
information
that is necessary to
evaluate a land unit for specific uses
is listed here.
Semua informasi geografik dapat
diperoleh dalam format komputer
(didigitasi ) . Semua data utatna dari
tanah (dari profil yang dianalisis)
juga disimpan dalam komputer dan dapat
tersedia bagi para pemakai yang memerlukan.
Pada tahap selanjutnya,
perangkat lunak untuk evaluasi lahan
yang mempergunakan parameter parameter
yang ada pada uraian satuan lahan akan
segera disediakan oleh Proyek Pengelolaan Data Base Tanah (PDBT).
All geographic information is available in computer (digitized) format.
All primary soil information (analyzed
profiles) is also computerized and can
be made available to the user. At a
later stage, land evaluation software
which uses the parameters listed in
the Land Unit Descript ions will be
made available by the Soil Data Base
Management Project (SDBM).
Permintaan untuk penilaian Kesesuaian
Lahan dari tiap satuan lahan untuk
berbagai keperluan dapat diajukan ke
Pusat Penelitian Tanah, Bogor.
Requests for suitability ratings of
the land units for various purposes
can be submitted to the Center for
Soil Research, Bogor.
1112 - iv
DAFTAR ISI
Hal aman
1
1
1
2
1. Pendahuluan
1.1. Latar belakang
1.2. Konsepsi legenda
1.3. Struktur legenda satuan lahan
2 . Metodologi
2.1. Peta dasar
2.2. Interpretasi citra
2.3. Survei dan data lapangan
2.4. Uraian satuan lahan
2.5. Data base dan pengolahan data
2.6. Relaibilitas peta
3
3
4
4
5
6
9
3. Lokasi daerah peta dan sumber informasi
3.1. Lokasi dan batàs administrasi
3.2. Sumber informasi
10
10
10
4. Keadaan umum fisik daerah
4.1. Fisiografi
4.2. Geologi
4.3. Hidrologi
10
10
16
17
5. Satuan lahan
5.1. Satuan lahan dan tanah
5.2. Isi uraian satuan lahan
18
18
20
6 . Daf tar pustaka
Laporan pemetaan tanah
•
21
22
Daftar Gambar
Gambar
Gambar
Gambar
Gambar
Gambar
Gambar
Gambar
1.
2.
3.
4.
5.
6.
7.
Lokasi peta dan bâtas administrasi
Relaibilitas peta
Indeks peta topografi dan jalur terbang potret udara
Indeks citra radar STAR-1 dan Landsat
Indeks laporan survei dan pemetaan tanah
Grup fisiograf i
•
Satuan lahan, blok diagram dan penampang mellntang
7
8
11
12
13
14
19
Daftar Tabel
Tabel 1. Grup fisiograf i
Tabel 2. Analisis tanah standar dan tambahan PDBT
Tabel 3. Nomor dan nama lembaran peta topografi skala 1:50.000
2
5
10
Lampiran
Lampiran 1. Uraian satuan lahan
23
1112 - v
CONTENTS
Page
2
2
2
2
2 . Introduction
1.1. Background
1.2. Legend concept
1.3. Structure of the land unit legend
2. Methodology
2.1. Base maps
2.2. Image interpretation
2.3. Field survey and field data
2.4. Land unit description
2.5. Data bases and data processing
2.6. Map reliability
3
3
4
4
5
6
9
3. (Map location and sources of information)
3.1. (Location and administrative boundaries)
3.2. (Sources of information)
4. (General physiography of the area)
4.1. (Physiography)
4.2. (Geology)
4.3. (Hydrology)
10
10
10
:
10
10
16
17
5. (Land units)
5.1. (Land units and soils)
5.2. (Contents of a land unit description)
18
18
20
6. (References)
(Soil survey reports)
21
22
List of Figures
Figure
Figure
Figure
Figure
Figure
Figure
Figure
1.
2.
3.
4.
5.
6.
7.
Location and administrative boundaries
7
Map reliability
8
Index of topographic maps and flight lines of aerial photos .. 11
Index of STAR-1 radar and Landsat imagery
12
Index of soil survey reports
13
Physiographic groups
24
Land units, block diagram and cross section
19
List of Tables
Table 1. Physiographic groups
:
Table 2. Standard and additional SDBM soil analyses
Table 3. Numbers and names of 1:50,000 topographic map sheets
2
5
10
Appendix
Appendix 1. Land unit descriptions
23
1112 - vi
1. PENDAHULUAN
1. INTRODUCTION
1.1.Latar belakang
1.1.Background
Buku Keterangan dan Peta Satuan Lahan
& Tanah ini merupakan sebaglan has il
akhir survëi tanah tinjau Sumatra yang
dilaksanakan untuk Proyek Perencanaan
dan Evaluasi Sumber Daya Lahan dan
diprakarsai tahun 1988 oleh Pemerintah
Indonesia serta dibiayai oleh Bank
Pembangunan Asia.
Pelaksanaan survei dilakukan antara
bulan Februari dan Maret 1989 oleh Tim
Survei Tanah dari Pusat Penelitian
Tanah (PPT), sedangkan korelasinya
dilakukan pada bulan Januari
Februari 1989.
This explanatory booklet and the included maps are part of the final
results of the reconnaissance soil
survey of Sumatra, which was carried
out for the Land Resources Evaluation
and Planning Project (LREP), initiated
in 1988 by the Goverment of the
Republic Indonesia and financed by the
Asian Development Bank.
The sheet was surveyed
between
February and March 1989, by teams of
the Center for Soil Research (CSR).
Hap correlation was carried out in
January - February 1989.
1.2.Konsepsi legenda
1.2.Legend concept
Legenda untuk survei ini didasarkan
pada pendekatan satuan lahan. Pendekatan ini dlanggap paling sesuai untuk survei ini , sebab pada sekala
1:250.000 dengan intensitas pengamatan
lapangan yang kurang, semua batas
satuan dapat ditarik dengan cara
menginterpretasi citra. Legenda satuan
lahan memungkinkan adanya pembatasan
setiap satuan dengan sembarang ukuran
yang masih dapat dipetakan (tergantung
skala peta) dengan memanfaatkan namanama morfologi sederhana
dan
berulang. Pendekatan ini menunjang
Struktur hirarki dan merupakan sistem
terbuka sehingga dapat diperbaharui
sesuai dengan penerapannya
di Indonesia; ia tidak memuat parameter
iklim (parameter iklim disimpan dalam
data base terpisah dan dapat digabung
dengan data base satuan lahan).
Tambahan pula legenda satuan lahan
erat hubungannya dengan legenda terdahulu di Indonesia mengenai
bentuk
lahan, sistem lahan dan satuan lahan
tanpa k e l i r u
penggunaannya
(Desaunettes, 1977; RePPProT, 19851988; Kips et al. , 1981) .
The legend for this survey is based on
the Land Unit approach. This approach
is considered most suitable for this
survey,
because
at a scale of
1:250,000 , with low-density field
checks, all unit boundaries are obtained by image interpretation. The
land unit legend allows the delineation of mappable units of any size
(depending on map scale), it makes use
of morphologic'.j. names which are
simple and recurrent, it supports an
hierarchical structure, it is an open
system that can be amended for use
anywhere in Indonesia, and it does not
contain climatic parameters
(the
climatic parameters are stored in a
separate data base which can be combined with the land unit data base).
Satuan Lahan ini diberi batasan berupa
lahan dimana satu atau lebih komponennya mempunyai ciri-ciri khusus dan
merupakan satuan lingkungan dengan
sembarang ukuran yang dapat dibatasi
pada peta. Satuan terkecil yang masih
A Land Unit is defined here as an area
of land of which one or more attributes have special characteristics,
and it refers to an environmental unit
of any size that can be delineated.
The smallest unit that can be
Furthermore, the land unit legend is
closely related to previous Indonesian
land form, land system, and land unit
legends (Desaunettes, 1977; RePPProT,
1985-1988; Kips et al., 1981) without
being confusing.
1112 - 1
dapat d i b a t a s i tanpa menghiraukan
sekalanya berukuran 2 mm lebarnya bila
bentuk memanjang dan kurang lebih 3
sampai 4 mm bila berbentuk bulat. Pada
sekala 1:250.000, suatu satuan yang
membulat dengan diagonal 4 mm meliputi
kurang lebih 80 ha.
Satuan lahan dikelompokkan dalam
grup-grup
f i s i o g r a f i dan kadangkadang dibagl lagi kedalam sub-grup.
Untuk informasi lebih lengkap, lihat
pada Buurman et al (1988) dan Balsem
et a l . (1989)
delineated on any map, irrespective of
scale is about 2 mm wide if it is a
linear feature and about 3 to à mm
across if it is a circular feature.
At a scale of 1:250,000, a circular
unit of 4 mm across has a surface of
nearly 80 ha.
Land units are grouped together
in
Physiographic Groups and, in some
cases, in Sub-Groups.
For more detailed informat ion, see
Buurman et a l . , (1988) and Balsem et
a l . , (1989)
1.3.Struktur legenda satuan lahan
1.3.Structure of the land unit legend
Semua satuan lahan diberi kode berupa
huruf dan angka/dijit; masing-masing
dengan konotasi khusus tergantung
tingkat klasifikasinya.
All mapping units are coded by means
of a sequence of characters and
digits, each with its specific connotation which depends on its level in
the classification.
Contoh:Au.1.1.3- Dataran aluvial luas,
tanggul sungai/alur-alur drainase.
Example: Au.l.1.3 -Broad Alluvial
Plain; levee/spillway.
Grup Fisiografi
Relief, ukuran besarnya
_Physiographic
Group
f.
Relief magnitude
Au.
Au.1.1.31.1.3~Bentuk lahan/torehan/vegetasi
Âu.1.1.3 --Landfon/dissection
/vegetation
JL
Litoloqi
•Sub-grup: Morfologi
Litholoqy
|
Subgroup : morphology
Tabel 1 menyajikan Grup Fisiografi
yang d i i d e n t i f i k a s i di Sumatra dan
pulau-pulau di luarnya. Contoh-contoh
pembagian lanjut hanya disajikan untuk
grup Kubah Gambut dan grup Dataran.
Table 1 lists the Physiographic Groups
which have been identified in Sumatra
and the outer islands.
Examples of
subdivisions
are given for the Peat
Dome and Plain groups only.
Tabel 1. Grup Fisiografi
Table 1 : PhysiographicGroups
A.
B.
D.
H.
I.
K.
M.
P.
Q.
T.
V.
X.
A. Alluvial
B. Marine
ALUVIAL
MARIN
KUBAH GAMBUT
PERBUKITAN
DATARAN TUF MASAM
KARST
PEGUNUNGAN/PLATO
DATARAN
TUF MASAM TOBA
TERAS MARIN
VOLKAN
ANEKA BENTUK
D. Peat Domes
Hilly
Acid Tuff Plain
Karst
Mounta in/PI ateau
Plain
Toba Acid Tuff
T. Marine Terrace
V. Volcanic
X. Miscellaneous
H.
I.
K.
M.
P.
Q.
*)
*)
*)
*)
*)
*)
*) Tidak dijumpai pada lembar peta
ini.
*)
1112 - 2
Not present
in this
*)
*)
*)
*)
*)
*)
mapsheet.
Pembagian lanjut grup Kubah Gambut dan
Dataran adalah sebagai berikut.
Subdivision of the Peat
Plain groups :
Domes and
thin <0,5m
fresh water medium 0,5-2m
thick >2o
tipis <0,5m
air tawar- sedang 0,5-2i
itebal >2m
eutrophic—
eutrofik —
tidal/saline fringes
of domes—|ditto
pasang surut/bagian tepi
kubah bergaram |sda
Kubah Gaibut -
Peat D o u e s —
air tawar
fresh water-|ditto
-|Sda
oligotrophic
oligotrofik-
tidal/saline fringes
of domes—|ditto
pasang surut/bagian tepi
kubah bergaram — | S d a
Bentuk vilayab
datar-
Land form
Penorehan
tanpa
sedikit
sedang
sangat
ekstrim
flat-
Dissection
none
slight
moderate
strong
extreme
Sda
datar - berombakSda
berombak
Dataran—litologi--[berombak - bergelombang- Sda
Sda
bergelombang—
datar berbukit kecil — Sda
berombak berbukit kecil- Sda
flat to undulating
ditto
undulating
ditto
Plain—lithology—[undulating to rolling— ditto
rolling
ditto
ditto
flat with hillocks
undulating with hillocks ditto
Struktur legenda disusun demikian rupa
sehingga lanskap datar, melandai, tertoreh, bergunung, dsb. dengan mudah
dapat dipilih oleh komputer. Struktur
ini langsung berkaitan dengan potensi
lahan untuk pertanian.
The legend structure
is such,
that
flat,
sloping, dissected, mountainous
landscapes, e t c . , are easily selected
by computer. The structure is directy
related to agricultural
potential of
the land.
2.
2.
METODOLOGI
METHODOLOGY
2.1.Peta dasar
2.1.Base maps
Peta dasar untuk keperluan pencetakan
Peta Satuan Lahan & Tanah disediakan
oleh BAKOSURTANAL. Untuk lembar peta
ini, peta dasar yang digunakan adalah
peta JOINT OPERATIONS GRAPHICS (JOG),
Lembar SB48-15, Seri 1501, Edisi 2,
Toboali yang dikeluarkan oleh Royal
Australian Survey Corps, 1982.
Base maps for the printed Land Unit
and Soil map were provided by BAKOSURTANAL. For the present sheet, the base
map was the Joint Operations Graphics
(JOG), Sheet S348-15, Series 1501,
Edition 2, Toboali, published by The
Royal Australian Survey Corps 1982.
1112 - 3
2.2.Interpretasi citra
2.2.Image interpretation
Survei tinjau ini sebahagian besar
didasarkan pada interpretasi citra dan
batas-batas satuan sesungguhnya
ditarik berdasarkan citra. Macam citra
yang digunakan adalah sebagai berlkut:
The surveys are extensively based on
image interpretation and virtually all
unit boundaries are imagery-based. The
following imagery was used:
-potret udara hitam/putih sekala
1:100.000, Angkatan Udara Australia
1976 (umumnya kualitas rendah karena
dicetak berulang kali dan pemrosesan
yang kurang baik).
-LANDSAT komposit warna (band 4-5-6)
sekala 1:250.000 tahun 1985 yang
diperoleh dari LAPAN (kualitas bervariasi, sekala kurang teliti).
-citra Radar stereo STAR-1,
1988
(cetakan hitam putih, kualitas tak
optimal).
- 1:100 000 scale black/white aerial
photography, Australian Airforce,
1976, (usually poor quality due to
recopying and poor processing).
- 1:250,000 LANDSAT colour composites
(bands 4-5-6), 1985, obtained from
LAPAN (varying quality, inacurate
scale).
- 1:250,000 STAR-1 stereo Radar imagery, 1988 (black/white positive
prints, quality not optimal).
2.3.Survei dan data lapangan.
2.3.Field survey and field data
Pelaksanaan survei tinjau dapat dibagi
dalam beberapa tahapan kerja:
The implementation of the reconnaissance survey can be split up into a
number of essential steps :
1. penelaahan data dan informasi dari
peta dan laporan tersedia.
2. interpretasi citra dan penetapan
daerah kunci
3. pengamatan lapangan dan pemasukan
data ke komputer
4.penyusunan satuan lahan dan
pemasukan data ke komputer.
5.analisis contoh tanah
6.melengkapi uralan
satuan
lahan
dengan data analisis.
7. korelasi/verifikasi lapangan
8. produksi peta akhir
9.dijitasi peta dan pemrosesan data
base lainnya.
Semua pengamatan di lapangan (pemboran
dan profil) dicatat, diberi kode dan
dimasukan sesuai dengan prosedur standar PDBT, seperti diuraikan dalam
Laporan Tehnis PDBT No.5 (Balsem et
al., 1988). Kode ini terutama diadaptasi dari standar FAO dan USDA (FAO,
1977; SCS, 1978; Gallup, 1978).
Contoh tanah yang représentatif
dianalisis sifat-sifatnya seperti yang
disajikan pada Tabel 2 .
1. perusal of existing maps and reports
2. image interpretation and selection
of sample/key areas
3 . field observations and computer data
entry
4. preliminary land unit descriptions
and computer data entry
5. soil sample analyses
6. completion of land unit descriptions
with analytical data
7. correlation/field verification
8 . final map production
9. map digitizing and other data base
operations.
All observations
in the
field
(auger ings and profile pits) were
described, coded and entered according
to standard
SDBM procedures
as
described in SDBM Technical Report
No.5 (Balsem et al., 1988).
These
codes are mainly adapted from standard
FAO and USDA codes
(FAO,
1977;
SCS,1978; Gallup, 1978).
Representative soils were analyzed for
the properties listed in Table 2.
1112 - 4
Tabel 2. Analisis tanah standar dan
tambahan PDBT.
Table 2. Standard and additional SDBH
soil analyses.
Analisis
1. tekstur
2. karbon organik
3. KTK NH40Ac pH 7
4. basa dapat ditukarkan dalam NH40Ac
5. Al dalam KC1 IM
6. kerapatan lindak pF 2,5
7. kadar air pF 4,2
8. pH (H20, KC1 , 1:2,5)
"9. N total
10.K tersedia
11.P tersedia
Standard Analyses
1. texture
2. organic Carbon
3. CEC NHAOAc pH 7
4. exchangeable Bases in NHAOAc
5. Al in 1 M KC1
6. bulk density pF 2.5
7. water content pF 4.2
8. pH (H20, KC1, 1:2.5
9. Total N
10.available K
11.available P
Analisis tambahan
untuk tanah volkanik:
-kemasaraan terekstraksi dalam
^
TEA (pH 8.2)
- Al, Fe dan Si terekstraksi oksalat
- mineralogi pasir
- retensi fosfat
untuk Oksïsol:
- Mineralogi pasir
untuk Spodosol:
- Fe, Al,C terekstraksi pirofosfat
- Fe, Al terekstraksi ditionit
untuk endapan marin:
- garam terlarut
- kadar sulfur
- kadar air lapangan (tanah belum
matang)
untuk tanah berkapur:
- kadar karbonat
untuk tanah gambut:
- kadar serat
- kadar abu
- kerapatan lindak
Additional Analyses
for volcanic soils:
- extractable acidity in BaC12-TEA
2.4.
2.4.Land unit
Uraian satuan lahan
Uraian satuan lahan berupa uraian umum
yang dibuat untuk setiap satuan peta.
Uraian yang dibuat i n i merupakan
generalisasi dari beberapa pengamatan.
Atribut satuan lahan (lihat pada 5.2)
digunakan untuk evaluasi lahan ybs.
Struktur
uraian
satuan
lahan
didasarkan pada suatu cara yang telah
dipublikasikan oleh RePPProT (1988)
dengan beberapa tambahan. Disamping
dari pengamatan di lapangan dalam
penyusunan uraian satuan lahan i n i ,
1112
- oxalate extractable Al, Fe and Si
- sand mineralogy
- phosphate retention
for Oxisols:
- sand mineralogy
for Spodosols :
- pyrophosphate extractable Fe, Al, C
- dithionite extractable Fe, Al
for marine deposits:
- soluble salts
- sulphur content
- field moisture content (unripe
soils)
calcareous soils:
- carbonate content
for peat soils:
- fibre content
- ash content
- bulk density
description
Land Unit descriptions
are general
descriptions which are made for each
of the mapping units.
Such descriptions are generalizations of point observations.
The land unit
attibutes
(5.2) are used for land evaluation.
The
s t r u c t u r e of the land
unit
descriptions
is based on those published by RePPProT (1988) with amendments. In addition to the field observations, the following sources were
- 5
juga dipergunakan beberapa
lain terutama dari :
informasi
used in the compilât ion of the land
unit descriptions:
-RePPProT, 1988: Review of Phase I
Results,Sumatra.
-PPPG, 1978: Peta Geologi Lerabar
Toboali, Sumatera, Sekala 1:250.000.
- Semua laporan survei yang tersedia
dari daerah ybs.(Gambar 5).
- RePPProT, 1988 : Review of Phase I
Results, Sumatra'
- GRDC, 1978 : Geologic Hap of the
Toboali Quadrangle, Sumatra, Scale
1:250 000.
- All available survey reports for the
area (see Figure 5) .
2.5. Data base dan pengolahan data.
2.5.Data
Seperti disebutkan diatas, semua data
lapangan dan analisis disimpan dalam
data base. Data base yang utama ialah:
-pengamatan lapangan (pemboran dan
penampang tanah).
-data analisis
-uraian satuan lahan
As mentioned above, all field and
analytical data are stored in computerized data bases. The main data
bases are :
- field observations (auger and pit).
- analytical data
- land unit descriptions
Data base pengamatan lapangan berisi
semua parameter yang dapat diukur di
lapangan dari setiap tempat pengamatan. Yang didiskripsi dan disimpan
adalah nomor tempat/site, tempat,
lereng, vegetasi/penggunaan lahan dan
semua sifat-sifat tanah yang diukur di
lapangan seperti Struktur, porositas,
tekstur, warna, dll. (lihat Laporan
Teknis No 5a, Versi 1.1, (Baisem et
al. , 1988).
The field observations data base contains
all parameters
that
were
measured in the field, for each of the
observations sites. Described and
stored are site number, location,
slope, vegetation/landuse and all soil
properties that are measured in the
field, such as structure, porosity,
texture, colour etc (see Technical
Report No 5 - Balsem et al., 1988)
Data base analisis berisi semua hasil
analisis kimia, fisika dan mineralogi
serta semua data hasil perhitungan
dari analisis ini yang biasanya dipergunakan untuk menilai kesuburan atau
klasifikasi tanah (Lihat Laporan
Teknis No 7a - Buurman, 1988; Laporan
Teknis No 17 - Muslihat et al., 1989).
The analytical data base contains all
results of chemical , physical and
mineralogical
analy ses and
all
properties used for fertility appraisal or class ification, that are
calculated with these analyses (see
Technical Report No 7 - Buurman, 1988;
and Technical Report No 17 - Muslihat
et al., 1989).
Pada data base pengamatan lapangan dan
data base analisis, data dapat
dikeluarkan dengan cara memanggil
/menuliskan nomor pengamatan, nomor
lembar peta, satuan pada legenda, administrasi (kabupaten atau provinsi)
atau dengan yang lainnya yang ditentukan oleh koordinat geografik.
In both the field observations and in
the analytical data base, data can be
retrieved by observations number, mapsheet, legend unit, administrative
area (province, kabupaten), and other
areas defined by geographic coordinates.
Data base uraian satuan lahan berisi
uraian umum dari tiap satuan peta untuk seluruh Pulau Sumatera yang
dikatalogkan menurut lembar peta.
The land unit description data base
contains the general description of
each mapping unit for the whole island
of Sumatra, catalogued by mapsheet.
1112 - 6
bases and data
processing
GAHBAR 1 : LOKASI PETA DAN BATAS ADHINISTRASI
FIGURE 1 : LOCATION AND ADMINISTRATIVE BOUNDARIES
105°00'
3">00'
15'
106°3O'
106°0O'
30'
Toboali
B
Propinsi Sumatera
Selatan
A : Kab. Ogan Komering
Mir
B : Kab.,Musi Banyuasin
LAUT
J A W A
C : Kab. Bangka
Propinsi Lampung
A : Kab. Lampung Utara
4°00 J
Jalan
Sungai
Kota/Pemukiman
Bâtas Propinsi
Bâtas Kabupaten
1 : 1000.000
0.
10
20
30
40km
GAMBAR 2 •.: RELAIBILITAS PETA
FIGURE 2 : HAP RELIABILITY
15'
106°00'
3°60'
106°30'
15'
Toboali
TINGKAT RELAIBILITAS
L A U T J A W A
1 : 1 000 000
Jalan
Sungai/Anak Sungai
Kota/Pemukiman
10
20
30
40km
Uraian umum berasal dari penyederhanaan semua pengamatan pada seluruh
satuan p e t a ,
termasuk
analisis
laboratorium dari profil yang l a i n .
Parameter yang disimpan berisi semua
informasi yang diperlukan untuk
p e n i l a i a n e v a l u a s i lahan ( l i h a t
Laporan Teknis No 13 - Balsem & Buurman, 1989). Uraian satuan lahan dari
semua satuan peta yang terdapat dalam
lembar peta ini disajikan pada Lampi ran 1.
The general description is derived by
generalizing information of all observations within the mapping unit, including
laboratory
analyses of
separate profiles.
The parameters
stored contain all the information
necessary for land evaluation procedures (see Technical Report No. 13 Balsem & Buurman, 1989). The land unit
descript ions of all mapping units
relevant to the present sheet are
listed in Appendix 1.
2.6.Relaibilitas peta
2.6. Map reliability
Relaibilitas dari peta tergantung pada
beberapa faktor seperti: kerapatan
pengamatan, keragaman tanah, kualitas
dari citra penginderaan jauh, lokasi
dari titik pengamatan atau daerah
kunci, ketepatan dari batas tanah
maupun batas satuan lahan, tingkat
pengetahuan dan pengalaman surveyor.
Tidak semua dari faktor faktor ini
dapat diukur dan karena itu harus
diperkirakan.
The reliability of a map depends on
many such factors as observation density, soil homogeneity or complexity,
quality of the remote sensing imagery,
the location of sample/key areas, accuracy of soil units and soil boundaries, the level of education and the
amount of experience of the soil surveyor'. Not all of these can be
measured and so they have to be estimated.
Berdasarkan faktor faktor tersebut
diatas, terutama kerapatan pengamatan,
maka diperkirakan raengenai relaibilitas peta, dan untuk itu dibagi
menjadi 3 grup (Gambar 2).
Based on the above mentioned factors
mainly on observation density, three
classes of map reliability have been
established (Figure 2).
1112 - 9
3 . LOKASI DAERAH PETA DAN SUMBER
INFORMASI
3 . 1 . L o k a s i dan Bâtas A d m i n i s t r a s !
Secara geografik daerah peta Toboali
(1112), t e r l e t a k antara lO5°o' dan
106°30' Bujur Timur dan antara 3° dan
4° Lintang Selatan.
Secara a d m i n i t r a t i f daerah p e t a
sebahagian besar termasuk kedalam
Provinsi Sumatera Selatan yang t e r d i r i
dari Kabupaten Ogan Komering I l i r ,
Musi Banyu Asin dan Kabupaten Bangka,
sedangkan sebahagian k e c i l masuk
Kabupaten Lampung Utara Provinsi Lampung. (Gambar 1).
3.2.Sumber Informasi
Dal am pelaksanaan survei dan pemetaan
tanah tingkat tinjau ini sumber informasi yang telah digunakan adalah peta
topografi, peta geologi, potret udara,
c i t r a landsat,
c i t r a Radar s e r t a
beberapa peta dan laporan survei terdahulu sebagai nara sumber.
Disamping p e t a
topografi
skala
1:250.000 (BAKOSURTANAL, 1986)
digunakan pula peta topografi berskala
1:50.000 (1975) yang diperoleh d a r i
Jantop TNI AD. Lembaran peta dan
nomornya disajikan pada Tabel 3.
Tabel 3 . Honor dan Naia Lembaran Peta
Topografi Skala 1:50.000
11 Penatang Panggang
12 Wiralaga
13 Pulau Panggang
14 Sungai Hanang
21 Gajah Hati
22 Tanjung Lumit
23 Sungai Jeruju
24 Bagan Kuala S.Pasir
31 32 33 34 -
Bandung lembar Toboali tahun 1978.
Potret udara yang dipakai ialah potret
udara hitam/putih skala 1:100.000
(Royal Australian Air Force, 1976)
berkualitas rendah
sampai
sedang
dengan tutupan awan Ik. 10%. Ikhtisar
jalur terbang dan nomor photo disajikan pada Gambar 3. Sumber informasi lain yang dipakai ialah dari
Citra Landsat dan Radar seperti disajikan dalam Gambar 4.
Beberapa laporan survei tanah terdahulu beserta peta tanahnya telah
ditelaah dalam pekerjaan kompilasi
data untuk memperkokoh data base tanah
daerah ybs.
Gambar 5 menyajikan lokasi daerah survei tersebut, sedangkan judul laporan
survei dicantumkan pada daftar pustaka.
4. KEADAAN UMUM FISIK DAERAH
4.1. Fisiografi
Bentang alam daerah lembar peta
Toboali dapat dibedakan kedalam Lahan
Basah (Lowland), Lahan Kering (Upland)
dan Perbukitan. Lahan Basah selanjutnya dibagi lagi menjadi Grup Kubah
Gambut, Grup Marin dan Grup Aluvial,
sedangkan Lahan Kering terdiri dari
Grup Dataran.
Lahan Basah (Lowland f
Lahan. Basah yang termasuk kedalam Grup
Marin menempati daerah sepanjang pantai dengan lebarnya bervariasi antara
2.5 dan 35 km. Daerah lahan basah ini
merupakan hasil dari proses sedimentasi marin dan perimarin (delta dan
kuala) dan secara jelas dapat dibuktikan dengan adanya pelebaran pantai
yang disebabkan oleh penambahan bahan
endapan dan proses angkatan.
41 Sungaibungin
42 Simpangtiga
43 Panpangan
44 Tulung Selapan
51 Huara Tangkallesa
52 Sungai Lumpur
53 Buntuan
54 Bagan Tengah
61 62 63 Tg Jatigombol
64 -
Peta geologi yang digunakan ialah Peta
geologi skala 1:250.000 dari Pusat
Penelitian dan Pengembangan Geologi
Tambahan pelebaran pantai
pada
beberapa tempat di Lampung diperkirakan sekitar 15 meter per tahun.
Semua endapan marin diendapkan pada
lingkungan daerah bergaram atau payau,
dan sebagai hasilnya, umumnya tanahnya
masih mengandung garam, terutama pada
1112 - 10
GAMBAR 3 : INDERS PETA TOPOGRAFI DAN JALUR TERBANG POTRET UDARA
FIGURE 3 : INDEX OF TOPOGRAPHIC HAPS AND FLIGHT'LINES OF AERIAL PHOTOGRAPHY
105°0O'
15'
30'
45'
62/8293
105,123
: Nomor jalur terbang
: Nomor foto udara
106°00'
1O6°3O-
( 6 u : Nomor lembar peta
topografi 1 : 50.000
GAMBAR 4
FIGURE 4
INDEKS CITRA RADAR STAR-I DAN LANDSAT
INDEX OF STAR-I
105°00'
3°00'
RADAR AND LANDSAT IMAGERY
106°30'
106°00'
30'
4°00'
Liputan citra landsat
Liputan radar 1 : 250.000
STAR - 1, 1112- 2, 3, 6
Daerah tidak terliput
/
A : 123-62 II, 23 • 03- 86
B : 123-62 1. 23-03-86
C:: 123-63 1,23-03-83
D :.124-62 I,30-03-85
E : 124-62 II, 30 03-85
Daerah tidak terliput
MÄHBAR 6 : GRUP FISIOGRAFI LEMBAR TOBOALI
FIGURE 6 : PHYSIOGRAPHIC GROUPS OF THE TOBOALI SHEET
105°00'
3°0O'
15'
B.
1O6°3O'
30'
Grup Kubah Gambut/Peaf Dome Group
P.
Grup Dstaran/PlainGroup
Grup Mu\i\a\IAIIuvial Group
H.
Grup Perbukiian/W/7/j/ Group
Grup Marine/Marine Group
X.
Grup Aneka BenXuk/Misscellaneous Group
GAHBAH 5 : IBDEKS LAPORAH SURVE1 DAN PEHETAAN TANAH
FIGURE 5 : INDEX OF SOIL SURVEY REPORTS
lBB a OD'
Tuliua
LAUT
Toboali - Nesu)i
Pusat Peneliüan Tanah, 19S6
, „ -J Propinsi Uipunq,
i i ^ = Penelitian fanah, l « i
Peiatanq Panqqanq «PP XÏII/D
ÜNIUi, 1982
~T^~\
—'•• j
Hesuji Area - Sub PIS
IPB, I960
>^S
Hesuji IA - A
S s ! v l Dept. Transiiqrasj, 1981
Daerah Konerinq l i t
Sub P4S, IPB 1985
J A W A
pakuan Ka tu IXA (1,2,7)
Toboali VIIIBO) Cf5>
dan Hesuji IEI1). Pusat
Penelitian Tanah. 1983
S. Luiipur, Sub P4S
UH1LÀ, 1982
P. Bangka, Pusat
Penelitian Tanah, 1987
daerah yang masih muda. Karena
sebagian besar daerah ini mempunyai
drainase terhambat, tanahnya umumnya
belum matang atau setengah matang
(half ripe). Tergantung vegetasi aslinya dan dimana daerahnya banyak mengandung pirit, maka akan terbentuk
tanah sulfat masam atau potensial sulfat masam.
Daerah-daerah yang dekat dengan pantai
dan sepanjang sungai akan dipengaruhi
oleh pasang surut. Daerah demikian
biasanya ditumbuhi vegetasi nipah atau
mangrove dan tidak tergenang pada
waktu surut. Daerah yang jauh dari
laut menjadi rawa permanen dan bersifat payau, dan umumnya ditumbuhi
oleh hutan gelam atau vegetasi rendah
seperti rumput. Hutan lebat hanya
dijumpai pada daerah marin tua, dimana
semua kadar garam terlarutnya telah
tercuci.
Di bagian selatan peta dijumpai sisa
jalur beting pantai dan cekungan
(beach ridges and swales). Jalur ini
terdapat agak jauh dari laut dan
sebagian tidak memanjang garis pantai
dan telah tererosi. Beting pantai tua
ini umumnya telah kehilangan karbonat
yang turun kebawah sampai permukaan
air tanah, dan tanahnya telah mengalami perkembangan. Perkembangan tanah
ini pada daerah cekungan tidak nyata.
Pada garis pantai, Grup Marin ditandai
oleh adanya dataran mangrove dan
tanahnya belum matang. Daerah rawa
luas antara jalur mangrove dan beting
pantai tua kemungkinan mengandung
bahan organik yang cukup tebal atau
mempunyai tanah-tanah
yang serupa
dengan tanah-tanah pada dataran
mangrove. Daerahnya basah sepanjang
tahun.
Daerah yang termasuk Grup Aluvial
dijurapai disebelah barat dari Grup
Marin, terutama di bagian selatan
peta. Grup Aluvial ditandai oleh
adanya pelembahan aluvial luas dan
pelembahan erosif di daerah Dataran.
Pelembahan aluvial luas (A.1.2)
terutama membentuk rawa belakang yang
luas yang selalu jenuh air. Tanahnya
sebagian belum matang dan kadangkadang ditutupi oleh bahan organik
tebal.
Tanggul sepanjang sungai utama sedikit
lebih tinggi letaknya dari rawa
belakang, dan terbentuk dari bahan endapan halus. Tanah-tanah di daerah ini
hampir serupa dengan tanah pada rawa
belakang, hanya drainasenya lebih baik
sedikit.
Pelembahan aluvial di daerah Dataran
umumnya erosif dan hanya sedikit
mengandung bahan endapan.
Kubah gambut dijumpai pada bagian
utara lembar peta ini dan luasnya
cukup besar. Dibandingkan dengan pantai disebelah utara seperti di Riau
dan Jambi, kubah gambut disini relatif
terbatas penyebarannya dan ketebalan
bahan organiknya lebih tipis. Secara
umum dapat dikatakan bahwa ketebalan
bahan organik bertambah jika makin
jauh dari sungai. Lapisan liât dibawah
lapisan bahan organik umumnya mengandung pirit dan karenanya terbentuk
tanah-tanah potensi sulfat masam.
Lahan Kering (Uplands)
Lahan kering hanya diwakili oleh satu
Grup Fisiografi, ialah Grup Dataran.
Tanah-tanah pada Grup Dataran terbentuk dari bahan bukan volkan dari zaman
Tersier, yang umumnya berasal dari
laut dangkal. Di lapangan tidak selalu
dapat dengan mudah dibedakan dari
bahan Dataran Tuf Masam yang sudah
lapuk, raeskipun sifat kimia dan
mineraloginya berbeda, nyata. Tutupan
bahan ignimbrit Kuarter menipis dari
Teluk Lampung menuju arah utara dan
hanya ditemukan di bagian barat laut
lembar peta ini.
Karena Dataran punya sejarah yang
cukup kompleks, banyak sisa tanda
proses pembentukan tanah dijumpai,
seperti tutupan konkresi besi, lapisan
plintit, dll. Pada beberapa daerah,
dijumpai sisa dari teras sungai.
Di lembar peta ini, kisaran ketinggian
dari Grup Dataran antara 10-70m diatas
1112 - 15
muka laut.
Pembagian lebih lanjut dari Grup
Dataran berdasarkan morfologi bentang
alam dan tingkat torehan. Karena
proses pembentukan tanah jauh lebih
tua dari proses penorehan (erosi),
maka perbedaan adalah antara profil
tanah lengkap (tererosi sedikit) pada
daerah punggung, dan profil tanah
tererosi ringan sampai berat pada
lereng. Tanah hidromorfik terdapat
pada lereng bawah/ perali'han ke lembah.
Tanah umumnya mempunyai perbedaan
tekstur yang nyata antara horison A
dan B dan karenanya diklasifikasikan
sebagal 'Kanhapludults'. Tanah yang
telah tererosi umumnya diklasifikasikan sebagai Dystropepts sedangkan yang
terkena pengaruh genangan air sebagai
Tropaquepts. Sifat-sifat kimia dari
tanah-tanah ini umumnya miskin dan
mempunyai kadar aluminium yang cukup
tinggi pada lapisan bawah.
Pada bagian yang lebih tua dari Grup
Dataran, tanahnya sudah mengalami
perkembangan lanjut dan diklasifikasikan sebagai Oxisols (Hapludox).
Perbukitan
Perbukitan pada lembar peta ini hanya
ditemukan di Pulau Bangka dan
merupakan sisa i n t r u s i sienit yang
terdapat di Batuampar sebelah utara
jalan
antara
Pampangan
dan
Tulungs e 1apan ( b a r a t l a u t Pulau
Bangka). Intrusi batuan plutonik ini
muncul dipermukaan sebagai singkapan
diantara sedimen Palembang.
4.2. Geologi
Formasl geologi didaerah yang dicakup
lembar peta ini termasuk dalam PreTersier, Tersier dan Kuarter.
Pre-Tersier
Formasi batuan plutonik sienit (pTsy)
dan Formasi batuan plutonik granit
(pTgr) serta Formasi batuan metamorfik
skis termasuk dalam Pre-Tersier;
formasi-formasi tersebut masing-masing
terdapat di Batuampar (utara jalan
Tulungselapan-Pampangan dan di utara
dan selatan Toboali (Pulau Bangka).
Ketinggian tempat intrusi sienit dan
granit antara 30m (utara Pampangan)
dan 292m (timurlaut Toboali); skis
Bangka terdapat antara 10 dan 25m dpi.
Batuan sienit menempati inti antiklinal dan tertutup oleh Formasi Palembang bawah. Batuan granit sekitar
Toboali tergolong amfibolgranit berbutir sedang sampai kasar dan tidak
mengandung kasiterit (oxida timah).
Skis Toboali yang umumnya berwarna
hijau muda mengandung mika, khlorit
dan talk.
Tersier
Formasi Palembang Anggota Bawah (Tmpl)
dan Formasi Palembang Anggota Tengah
(Tppp) mewakili sedimen Tersier di
daerah peta ini. Formasi-formasi ini
masing-masing disebut Formasi Air
Benakat dan Formasi Muara Enim.
Bentuk wilayah intrusi sienit terdiri
dari bukit-bukit kecil terpisah
(.isolated
hillocks).
Berdasarkan
adanya singkapan batuan plutonik di
daerah ini dapat diduga bahwa gejala
t e r s e b u t merupakan akibat proses
peneplainasl.
Formasi Palembang Anggota Bawah yang
terdapat di baratlaut terdiri dari
batulempung, serpih- dan batupasir
glaukonitan yang merupakan endapan
lingkungan neritik. Batulempung berselingan dengan batupasir lempungan
glaukonitan. Tmpl di selatan Batuampar
yang mempunyai kemiringan lapisan
keselatan sebesar 1 sampai 7% merupakan sayap antiklinal yang bersumbu
kira-kira timur-barat.
Tanah diatas sienit umumnya mempunyai
perbedaan tekstur yang nyata antara
horison A dan B dan diklasifikasikan
sebagai Ultisol. Tanah yang telah
tererosi diklasifikasikan sebagai Inceptisol.
Formasi Palembang Anggota Tengah
(Miosen Atas - Pliosen) yang sebagian
besar terdapat di tengah dan selatan
terdiri dari batupasir, batulumpur
yang banyak berselingan dengan lapisan
batubara. Tppp di bagian atas umumnya
1112 - 16
terdiri dari endapan air payau dan endapan rawa dengan lapisan batubara
seperti yang terdapat di sekitar Muara
Enim. Tppp terletak selaras pada Tmpl,
sebaliknya Tppp tertutup tak-selaras
oleh Tuf Ranau.
Ketebalan Tppp
diperkirakan berkisar antara 600 dan
800m.
Kuarter
Kuarter terdiri dari formasi Tuf Ranau
dan Aluvium termasuk Holosen.
Formasi Tuf Ranau (Qrv) terdäpat di
utara Pematangsipanggang membujur ke
timurlaut. Formasi Tuf Ranau berupa
tuf lempungan, tuf liparit mengandung
kuarsa, blotit dan plagioklas masam
dan berasal dari pusat erupsi Danau
Ranau (lembar Kotabumi) yang terletak
di baratdaya. Tuf di pusat erupsi
menunjukkan perlapisan dan bersusunan
biotit liparit dengan kandungan yang
sama seperti Qrv di lembar Toboali,
namun dengan kandungan fragmen batuapung, sanidin dan magnetit.
Ketebalan tuf ini di dekat pusat
erupsi ± 150-200 m dan menipis ke
utara dan timurlaut sampal ujungnya
yakni Qrv di daerah ini. Qrv ditutup
tak-selaras oleh endapan Holosen.
Aluvium terdiri dari pasir, debu, liât
dan bahart organik yang merupakan endapan subresen dan muda dengan
penyebaran paling luas di dataran rendah pantai dan pasang surut, pelembahan sungai, rawa belakang dan cekungan.
4.3. Hidrologi
Secara keseluruhan kawasan timur
Sumatera, Pulau Bangka dan P.Belitung
serta pulau-pulau lalnnya menunjukkan
ciri-ciri tenggelamnya dataran rendah
dibawah permukaan pada zaman Kuarter
tua. Maka oleh sebab itu, daerah agak
datar dan keadaan tata air di daerah
datar ini dikendalikan oleh gradient
kecil sehingga
drainase terhambat
dengan akibat penggenangan yang luas
dan bersifat permanen. Keadaan ini
dominan terjadi di rawa belakang dan
cekungan di sekitar Way Mesuji dan
Sungai Lumpur.
Berdasarkan pengaruh pasang surut
dataran rendah dapat diidentifikasi
sebagai daerah yang sedikit atau sama
sekali tanpa pengaruh pasang surut
yakni jalur aliran sungai perenial dan
tawar, dataran banjir musiman, rawa
belakang air tawar bergambut masam;
batas kawasan ini dengan pengaruh
pasang surut sangat ditentukan oleh
jauhhya intrusi pasang besar di musim
kemarau dan desakan balik air- sungai
waktu musim penghujan (NEDECO, 1981).
Oleh sebab itu sungai-sungai yang
relatif pendek dengan desakan air
tawar kurang kuat untuk menekan air
laut, kemungkinan besar pengaruh
pasang surut terasa jauh ke pedalaman,
a.l dapat diamati pada Sungai Mesuji
dan S.Lumpur yang tergolong pendek.
Dataran rendah yang langsung terkena
pasang surut di daerah ini tampak
jelas yakni sejauh alur-alur pasang
surut (tidal kreeks) yang panjangnya
antara 2 sampai 5 km, bahkan ada yang
10 km lebih: dari selatan ke utara
Sungai Siburbesar, S.Jerwu, S.Lebonghitam, S.Riding dan S.Pidada..
Daerah yang relatif kering adalah
dataran Formasi Palembang yang agak
meninggi dibandingkan daerah tergenang
di sekitarnya. Daerah pematang. bagian
selatan merupakan dataran berombak,
didrainase oleh Sungai Mesuji dan
cabangnya a.l. S.Dabukputih, S.Dabukitem, S.Talangbatin, yang berpola
dendritik. Daerah pematang di tengah
dan di utara didrainase a.l. oleh Sungai Jeruju, S.Pasir, S.Selapan dan
S.Belidang (keduanya cabang S.Lumpur)
yang dendritik.
Keadaan tata air dl daerah Pulau
Bangka sekitar Toboall berbeda antara
daerah granit dan skis yang umumnya
berdrainase baik dan dataran rendah
yang berdrainase terhambat dan bahkan
setempat-setempat tergenang permanen
dan musiman serta daerah pantai dengan
pengaruh pasang surut.
1112 - 17
5.SATUAN LAHAN
tetapi sering raengandung pirit. Jenis
tanah yang mendorainasi satuan lahan
ini adalah Tropohemists dan
Sulfihemists.
5.1.Satuan lahan dan tanah.
Seperti telah disebutkan pada bab terdahulu, satuan lahan yang dijumpai
pada lembar peta ini dapat dikelompokkan kedalam 5 grup fisiografi, yaitu
Grup Kubah Gambut, Grup Aluvial, Grup
Marin, Grup Dataran, Grup Perbukitan
dan Grup Aneka Bentuk (Gambar 6). Pada
setiap satuan lahan umumnya ditemukan
lebih dari satu satuan tanah (pada
tingkat Great G r o u p ) , dan agar
memudahkan pembacaannya maka setiap
satuan tanah yang dijumpai pada setiap
satuan lahan ditentukan luas penyebarannya secara kualitatif, yaitu:
-Sangat dominan: apabila penyebarannya
>75% dari luasan satuan lahan.
-Dominan: apabiia penyebarannya antara
50-75% dari luasan satuan lahan.
-Cukup: apabila penyebarannya antara
25-50% dari luasan satuan lahan.
-Sedikit: apabila penyebarannya antara
10-25% dari luasan satuan lahan.
-Sedikit sekali: apabila penyebarannya
<10% dari luasan satuan lahan.
Dibawah ini akan diuraikan mengenai
keadaan tanah yang dijumpai pada
setiap grup fisiografi.
Grup Kubah Gambut
Di daerah ini dijumpai kubah gambut
oligotropik air tawar dan yang terpengaruh air asin, terbentuk di daerah
yang relatif cekung sehingga daerahnya
tergenang sepanjang tahun. Dalam
lingkungan demikian sisa tumbuhan
sukar hancur dan menumpuk sebagai gambut dengan atau tanpa campuran endapan
tanah mineral. Ketebalan gambut bervariasi antara 0,5 dan 4m. Bentuk permukaan seperti kubah dengan perbedaan
tinggi tidak melebihi 10 m.
Bahan organik telah mengalami dekomposisi menjadi hemist dan saprisc
serta diperkirakan komposisi abunya
tidak kaya akan unsur-unsur hara
(oligotrofik). Bahan mineral di bawah
gambut umumnya miskin unsur, khusus
kalau teksturnya kasar. Bahan halus
dari sedimen marin umumnya lebih kaya,
1112
Daerah ini pada umuranya untuk jangka
pendek tidak mempunyai nllai untuk
dikembangkan sebagai daerah pertanian.
Kecuali sesetempat di bagian pinggir
yang ditempati jenis tanah Tropaquents
dapat dijadikan untuk areal persawahan
lebak dalam luasan yang sempit dan
dengan pengendalian air yang baik.
Penghambat utama di daerah ini adalah
kandungan unsur hara/miskin, ketebalan
gambut dan genangan permanen serta
bahaya keracunan pirit (Sulfihemists).
Grup Aluvial.
Tanah tanah pada grup fisiografi ini
umumnya berkembang dari bahan endapan
halus dan Hydraquents merupakan tanah
yang dominan dijumpai pada Dataran
Aluvial Luas (A.1.1), sedangkan tanah
yang lainnya ialah Tropaquents, Fluvaquents, Tropohemist dan Sulfaquents.
Hydraquents merupakan tanah yang belum
matang, kandungan airnya tinggi dan
drainasenya sangat terhambat. Tingkat
kesuburannya tidak begitu menjadi
masalah dimana diantaranya mempunyai
kadar P total dan nllai Kapasitas
Tukar Kation tinggi.
Tanah tanah pada Lembah Aluvial Luas
(A.1.2) cukup bervariasi, yaitu Tropaquepts, Tropaquents, Fluvaquents,
Sulfihemist dan Dystropepts . Juga
berkembang dari bahan endapan halus.
Diantara semua tanah ini maka Sulfihemist yang terutama akan menjadi
masalah bagi pertanian yaitu mengandung kadar pirit cukup tinggi yang
akan membahayakan tanaman. Tanah lainnya yang menjadi masalah hanya persoalan drainase yang termasuk terhambat sampai sangat terhambat, kecuali
Dystropepts mempunyai drainase baik.
18
GAMBAE 7 : SATUAN LAHAN, BLOK DIAGRAM DAN PENAHPANG MELINTANG LEMBAR TOBOALI
FIGURE 7
LAND UNITS, BLOCK DIAGRAM AND CROSS SECTION OF THE TOBOALI SHEET
tsdan
tOftl.l.OI
,8,..„
iPIo.2.11
?«"
Endipin
S u,.J„„„
IUSOA>
t.oPM-.ni.
1112 - 19
!.»—„
Grup Marin.
Pada Grup Marin tanah yang paling
banyak di jumpai adalah Hydraquents,
Sulfaquents dan Sulfihemists sedangkan
yang lainnya adalah Fluvaquent s dan
Tropaquents. Terbentuk dari bahan endapan halus. Sifat s i f a t dan permasalahan tanah Hydraquents saroa
seperti Hydraquents yang di jumpai pada
Dataran aluvial luas. Seperti halnya
pada Dataran aluvial luas, maka tanah
tanah yang terutama menjadi masalah
ialah Sulfo/Sul fihemist dan Sulfaquents yang mempunyai kadar piri t yang
cukup tinggi yang akan membahayakan
tanaman jika daerahnya dibuka dan
didrainase, karena akan memberikan pH
yang sangat rendah.
Grup Dataran.
Tanah tanah didaerah i n i umumnya
berkembang dari batuan ^pHimen halus
maupun kasar yang berasal dari forraasi
Palembang Tengah dan Bawah.
lukan penelitian lebih d e t a i l .
Adanya lapisan kongkresi Fe pada
daerah perakaran pada penampang tanah
akan sangat menganggu pertumbuhan akar
tanaman. Adanya lapisan p l i n t i t juga
kurang baik bagi tanaman, karena jika
lapisan ini kontak dengan udara akan
menjadi sangat keras. Jadi pada tanah
tanah yang mengandung lapisan p l i n t i t
harus diusahakan pengolahan tidak sampai pada lapisan tersebut.
Disebutkan d i a t a s
Kanhapludults
merupakan t a n a h yang mendorainasi
daerah i n i . Perrnasalahan utama dari
t a n a h i n i i a l a h mempunyai n i l a i
Kapasitas Tukar Kation yang rendah.
yaitu <16 cmol(+)/kg l i â t . Tanah-tanah
ini kurang dapat nenyimpan pupuk jika
dilakukan pemupukan. sehingga cara
pemberian pupuk pada tanah ini mtujadi
masalah yang utama. Salah satu caranya
ialah dengan raemberikannya secara bertahap. Salah satu cara mengatasi rendahnya n i l a i Kapasitas Tukar Kation
ini ialah dengan penambahan bahan organik.
Menurut k l a s i f i k a s i USDA tanah yang
banyak dijurapai di daerah Dataran
ialah Kanhapludults, Dystropepts dan
Tropaquepts, dimana tanah yang d i s e but kan pertama mend orai nasi dal ara hal Tanah lainnya yang di jumpai i a l a h
penyebarannya. Kanhapludul t s umumnya Hapludox. Permasalah tanah Hapludox
dijumpai didaerah punggung yang agak hampir saraa dengan K a n h a p l u d u l t s
datar, Dystropepts pada bagian lereng seperti telah diuraikan diatas yaitu
dan Tropaquepts pada daerah pelemmasalah Kapasitas Tukar Kation.
bahannya.
Grup Perbukitan.
Secara morfologis tanah-tanah yang Tanah-tanah yang terdapat pada daerah
berkembang d a r i batuan sedimen i n i
perbukitan berkembang d a r i
batuan
dapat dikelompokkan dalam 3 kelompok.
plutonik intermedier. Umumnya tanahnya
yaitu :
sudah cukup berkembang dan d i k l a s i fikasikan sebagai Hapludults. Pada
1. Tanah tanpa adanya lapisan kongkresi
daerah yang sudah t e r e r o s i dijumpai
Fe diantara kedalaman 120cm dari pertanah Dystropepts. Pada daerah grup
Pertukitan ini banyak dijumpai batumukaan tanah.
batu dipermukaan ( s e k i t a r 40-60%).
2 . Tanah dengan lapisan kongkresi Fe
diantara kedalap'an 120c m dari per- Akibat banyaknya batu-batu i n i maka
daerah i n i kurang berpotensi untuk
raukaan tanah.
di.kembangkan sebagai daerah pertanian.
3. Tanah dengan lapisan p l i n t i t pada
disamping luasannya yang hanya 1 .080
lapisan bawah diantara kedalaman bOha.
120 cm.
Tanah tanah ini umumnya sudah sangat
tua dan 1apuk.
Penyebaran ket iga
kelompok tanah d i a t a s pada t ingka t
peme taan yang sekarang susah un tuk
diketahui penyebarannya karena memer-
5.2. l s i Uraian Satuan Lahan.
Agar memudahkan untuk para pemakai,
maka s e t i a p s a t u a n l a h a n yang
ditemukan pada lembar p e t a
ini
1112 - 20
diuraikän secara mendetil pada Lampiran 1.
Uraian itu antara lain meliputi :
- Luas dan penyebarannya pada tiap
Provinsi yang diliput.
- Citra satelit, foto udara dan Radar
yang meliput satuan lahan tsb.
- Bahan induk yang meliputi tingkat
pelapukannya, litologinya dan formasi menurut peta Geologi.
- Sumber dan kualitas air
- Kemungkinan perikanan
- Bahaya banjir atau genangan
- Vegetasi dan penggunaan lahan
- Tingkat bahaya erosi (yang dipercepat)
- Satuan tanah yang dijumpai (pada
tingkat Great Group)
- Sifat sifat kimia dan morfologi
penting dari tanah lapisan atas
- Ketinggian dari muka laut
- Bentuk profil satuan lahan tsb
- Pola drainase
- Lereng
- Distribusi lereng pada satuan lahan
tsb
- Perbedaan tinggi
- Bentuk wilayah
- Keadaan pelembahannya
- Pembagian lanjut dari satuan lahan
(faset)
- F r a g m e n t a s i l a h a n yang b i s a
diusahakan untuk pertanian, dan
- Tingkat relaibilitas dari unsur unsur diatas
Disamping itu disajikan pula penampang
melintang dari tiap satuan lahan tersebut untuk memudahkan pemakai membayangkan keadaan satuan lahan tersebut.
6. DAFTAR PUSTAKA
Balsem, T., & P. Buurman, 1989.
Guidelines for Land Unit Description. Soil Data Base Management
Project Technical Report No. 13,
Version 2. Soil Data Base Management, Center for Soil Research,
Bogor
Balsem, T., P. Buurman & U. WoodSictira, 1988. Penggunaan kode komputer untuk data lapangan. Proyek
Pengelolaan Data Base Tanah, Laporan
Tehnis No. 5a, Versi 1.1. Pusat
Penelitian Tanah, Bogor
Buurman, P., 1988. Sifat-sifat kimia,
fisika, dan mineralogi untuk data
base tanah. Proyek Pengelolaan Data
Base Tanah, Laporan Tehnis No. 7a,
Versi 2.0. Pusat Penelitian Tanah,
Bogor.
Buurman, P., T. Balsem & H.G.A. van
Panhuys, 1988. Klasifikasi satuan
lahan untuk survey tingkat tinjau
Sumatera. Proyek Pengelolaan Data
Base Tanah, Laporan Tehnis No. 3a,
Versi 1.2. Pusat Penelitian Tanah,
Bogor.
Desaunettes, J.R., 1977. Catalogue of
landforms for Indonesia. FAO/UNDP
Land Capability Appraisal Project
Working Paper No. 13, Soil Research
Institute, Bogor
FAO/UNESCO, 1977. Guidelines for soil
description. Rome
Gallup, D.L., 1981. Proposed coding
system for pedon data for trial by
the Center for Soil Research, Bogor.
AGO/INS/78/006, Manual 3. Bogor
GRDC (Geological Research and Development Center), 1978. Geologic map of
the Toboali quadrangle, Sumatra,
scale 1:250.000.
Kips, P.A.,
D. Djaenudin & Nata
Suharta, 1981. The land unit approach to land resources surveys for
land use planning, with particular
reference to the Sekarapung watershed, Lampung province, Sumatra, Indonesia.
Muslihat, A., U. Wood-Sichra & P.
Buurman, 1989. Soil sample analysis
data base - User Manual and Technical Manual. Soil Data Base Management Project, Technical Report No.
17, Version 1.0. Center for Soil
Research, Bogor.
NEDECO / Euroconsult - BIEC, 1984.
Nationwide study of coastal ands
1112 - 21
near coastal swamp land in Sumatera, .106.Fernetaan tanah semi detail
Kalimantan and Irian Jaya. DirecPenu.tang Panggang WPP XXII/D. UNILA,
torate General of Water Resources
1982.
Development. Ministry of Public
Works.
112.Soil survey and soil mapping,
Mesuji area Sub P4S , South Sumatra.
PPPG - see GRDC
Institut Pertanian Bogor, 1980.
184.Survei dasar dalam rangka pembanRePPProT (Regional Physical Planning
gunan pertanian Lampung. Lembaga
Programme for Transmigration), 1985.
Penelitian Tanah, 1968.
Review of Phase IB results Cenmtral
Kalimantan. Ministry of Transmigra189.Laporan akhir survei dan pemetaan
tion, Jakarta.
tanah semi detail daerah Komering
III Sub P4S-Sumatera Selatan. InRePPProT (Regional Physical Planning
stitut Pertanian Bogor. 1985.
Programme for Transmigration), 1988.
Review of Phase I results Sumatra. 286.Laporan akhir rencana teknis
Ministry of Transmigration, Jakarta.
satuan pemukiman Tahap IIIA, Mesuji
IA-A1.
Departemen Transmigras!,
SCS (Soil Conservation Service), 1978.
. 1984. .
Pedon coding system for the National
Cooperative Soil Survey. USDA, 319. E. Priyatna Praviranegara, Lukman
Washington D.C.
Hakim, Sudradjat. & E. Suparma :
Laporan peninjauan kembali lokasi
Soil Survey Staff, 1987. Keys to Soil
penempatan transmigrasi lokal daerah
Taxonomy. SMSS (Soil Management SupPakuati Ratu IXA(1,2,7), Toboali
port Service) Monograph 6. US Dept.
VIIIB(3), C(5) dan Mesuji IE(1).
of Agriculture.
Pusat Penelitian Tanah, 1983.
Laporan pemetaan tanah
(Nomor adalah nomor laporan dalam file
SUMREP)
84.Laporan 1 updating peta tanah tinjau daerah Toboali - Mesuji. Pusat
Penelitian Tanah, 1986.
338.Laporan survei dan pemetaan tanah
daerah Sungai Lumpur Sub P4S
Sumatera Selatan. P3SP Universitas
Lampung, 1985.
374.Laporan survei dan penelitian
tanah Pulau Bangka, Puslittan, 1987.
1112 - 22
LAMPIRAN 1. URAIAN
SATUAN
LAHAN
APPENDIX 1. LAND UNIT DESCRIPTIONS
1112 - 23
UBIT REFÛBT
LREP-SDBM, CSB-BOGCB
MAP IMAGE:
CSDSS SBCTIOH:
peat
1.
4.
5.
6.
LAHD OMIT: D.2.1.2
2. MAP SHEET: 1112
3. AREA: 1820 km2
OCCURESCE by PSOPIBCE: Sumatera Selatan: 99X
STATUS IDEOTIFIERS
: 'Updated by: AH
edit date: 30/03/89
Status: Final
IAHD OHIT DE3CKIFTI0H: Freshwater peat domes, organic sediment thickness 0.5 - 2.0 m,
flat to slightly convex.
7. SATELLITE SCEHES
: 123/62/23/03/86, 124/62/23/03/85
8. A£BIAL PHOTOGRAPHS
: 1:100.000
059 /8316-111, 060 /8341-069, 058 /8316-057
9. BADAR
: START1/250/88/1112-3
10. ISRERI MATERIAL
11. BOCK OUTCROP:
%
a. Weathering :
b. Lithology : peat
c. Formation : Qal
12. HAIER
a. Quality : Freshb. Source : Rain
13 _ FISHERIES
: Rawa (swamp)
14. RIVERS a. Floodrisk : None
b. Iromiafcion: Permanent
15. VEGEIATICB/LAHD USE : peat swamp forest (gambut), alang-alang
Area used
: 0 X
16. ACCELERATED EROSIOS
a. Occorence : None
b. Evidence :
17. SOIL GREAT GROOP
Donnant >SOX
Associated 1
Associated 2
het/
eqt/
/112-91
/
Classification
tropohemists
-ulfihemists
tropaquents
/79/P /1112/14/
/88/UA/1112/13/
Z of area
60 X
30 X
10 X
/91 /
/169/
1112 -
hei/
24
Lab. checked
yes
yes
yes
/88/US/1112/22/
/176/
iff snn. n t t w r T B B T S T T C S
Properties
a. Texture:
b.
c.
d.
e.
£.
g.
h.
i.
j.
k.
1.
B.
n.
o.
p.
q.
r.
topsoil
subsoil
Depth:
peatsoil
mineralsoil
Drainage:
Each. K:
topsoil
subsoil
Total K2O: topsoil
subsoil
Avail. P: method
topsoil
subsoil
Total P:
topsoil
subsoil
CBC pH 7
topsoil
subsoil
Soil Reaction:topsoil
subsoil
Al Sat.
topsoil
subsoil
Al toxicity :
Acid sulph. pot.:
Salinity :
Other Toxicity:
Soot obstr. layer :
Organic Matter :
TES :
Total observations:
Dominant. > SOX
organic
organic
very deep
—
Very poorly drained
medium
medium
—
-Bray I
medium
medium
—
—
very high
very high
excessive acid
excessive acid
very low
very low
-moderately deep
--300 cm
91.9
15.1
3
Associated 1
organic
organic
very deep
—
Very poorly drained
low
medium
--Bray I
medium
medium
-~
very high
very high
excessive acid
extreme acid
very low
very low
-shallow depth
—
—
150 cm
37.6
14.9
0
Associated 2
fine
fine
—
very deep
Very poorly drained
very low
very low
very low
very low
Bray I
. medium
medium
very high
high
low
medium
excessive acid
excessive acid
very high
very high
no
—
salt free
—
-3.1
0.1
2
19. ALTITUDE:
Range:
5 m
tünimnm:
2 m
5m
Dominant: No pronounced highs/lows
20. PLAH/PBDFILE:
Included:
a. Pattern: none
b. density: Very low
21. L.Ü. DRAŒAGE: c. Variability:
a. Steepness:flat
b. Variability: Low
22. SLOPE:
d. Variability:
c. Length:
e. Curvature: convex
23. SLOPE DISTR.:
Valleybottoms: 100 X
Interfluves : 0-81:0 X, 9-25Z: 0 X, 25-55X: 0 %
24. BELIEF AHPLI.: a. Amplitude: very low
b. Variability: Low
25. TEBBAIH:
Flat, slope <ZX, 0-50 m
26. CBEST/BIDGES:
a. Shape: no crests
b. Length:
c. Variability:
d. Width:
e. Variability:
27. VALLEI FLOOR:
a. Width:
b. Variability:
-1- Domes, tropohemists, 60X
28. LASD FACETS:
-2- Domes, sulfihemists, 30Z
-3- Domes, tropaquents, 10%
-42 9 . FBAGMEHTATIGH: Valleys:
Interfluves:
30. RELIABILITY:
1= reliable, 2= probable, 3- tenable, 4= plausible
lO.b : 1 12.a: 2
14.a: 2
14.b: 2
17: 1 18.a: 1 18.b: 1 18.c: 1
18.d-q: 2
19: 1
22: 2
23: 2 24: 1
28: 2
29: 2
31. ADOITIGHAL HOTES: Representative profile for Sulfihemists is extrapolated from other
landunit.
1112 - 25
LAHD WUT REPORT
LREP~SD9M, CSR'BOSOR
MAP OMGE:
CS06S SBCTIÛH:
D.2.1.2/3
(undiff)
2.1.1
Pfq.3.1 -'
1. LAHD UHIT: D.2.1.2/3
4.
•»jj>fft'ja:i{
by
5 . SUIDS IDEHTIFIERS
:
6. LAID IfflIT DESCRIPTICS:
7. SATELLITE
8. AEPTÀT. PHOTOGRAPHS
:
9. RADAR
:
10. PARER M*TEPTAT.
2. Map SBEET: 1112
3. AREA: 954 km2
Sumatera Selatan: 99Ï
Updated by: AH
edit date: 31/03/89
Status: Final
Freshwater peat domes, organic sediment thickness 0.5 - > 2.0
m, flat to slightly convex.
124/62/23/03/85
1:100.000
058 /8316-63
START1/250/88/1112-3
11. BOCK COTCSOF:
%
a. Weathering :
12.
13.
14.
15.
16.
b. Lithology :
c. Foraaation :
HEXES
a. Quality :
b. Source :
FISHERIES
:
RIVERS a. Floodriak :
b. Inondation:
VBGEIéTICB/LAIID OSE :
Area axed
:
ACCELERATED EROSIGH
a. Occnrence :
b . Evidence :
peat
Qal
Fresh
Rain
Rawa (swamp)
None
Permanent
secondary forest, bush, swamp (rawa) including sedges
0 %
None
17. SOIL GREAT GROUP
Dominant >50I
Associated 1
Classification
tropohemists
sulfihemists
Associated 2
tropaquents
22. REPRESERTATIVE PROFILES:
het/
/
/88/HK/1112/41/
eqt/
/
/88/US/1112/22/
Z of area
70 X
25 X
5X
hei/
/158/
/156/
1112 - 26
Lab. checked
yes
yes
yes
/189-1
/84/P /1112/41/
/19 /
18. SOU. CHARACTERISTICS
Properties
a. Texture:
topsoil
subsoil
b. Depth:
peatsoil
alsoil
c. Drainase:
d. Exch. K:
topsoil
subsoil
0. Total K2O: topsoil
subsoil
t. avail. F:
aethod
topsoil
subsoil
8- Total P:
topsoil
subsoil
h. CBC pH 7
topsoil
subsoil
1. Soil Réaction:topsoil
subsoil
j. Al Sat.
topsoil .
subsoil
k. âl toxicity :
1. Acid snlpb. pot.:
•. Salinity :
n. Other Taxicity:
o. Boot, obstr. layer :
p. Organic Matter :
q. TUB :
r. Total observations:
Dominant > SOX
organic
organic
extremely deep
—
Very poorly drained
high
high
medium
medium
Associated 1
organic
organic
extremely deep
—
Very poorly drained
medium
medium
—
Associated 2
fine
fine
—
very deep
Very poorly drained
medium
low
medium
medium
high
low
very high
very high
excessive acid
excessive acid
low
low
—
-very high
very high
excessive acid
extreme acid
—
—
very high
very low
high
medium
very strong acid
very strong acid
low
very low
not relevant
salt free
very shallow
salt free
very slightly
300 cm
69.5
5.3
1
170 cm
94.1
9.0
1
120 cm
7.3
18.1
1
19. ALTITUDE:
20.
21.
22.
23.
24.
25.
26.
27.
28.
29.
6 m
Minim»2
Drainant: No pronounced highs/lows
PLUI/PBOnLE:
Included:
b.
a. Pattern: none
L.O. OBADttGE: c. Variability:
b.
a. Steepness:flat
SLOPE:
d.
c. Length:
e. Curvature:
SLOPE DISTR. :
ValleybottoBs: 100 %
Interfluves : 0-81:0 X, 9-251: 0 %, 25-551: 0
b.
RELIEF «MPU.: a. Aavlitade: very low
TFHBATHFlat, slope <2%, 0-50 m
CHEST/RIDGES:
a. Shape: no crests
b. Length:
e. Variability:
d. Width:
b. Variability:
VALLEY FLOOR:
a. Width:
LAO) FACETS:
-1- Domes, tropohemists,.70X
-2- Domes, sulfihemists, 25Ï
-3- Domes, tropaquents, 5Ï
-*Interlluves:
FBABHERTATIOH: Valleys:
--
5 m
density:
Variability: Low
Variability:
i
Variability: Low
c. Variability:
30. RELIABILITÎ:
l- reliable, 2° probable, 3= tenable, 4« plausible
lO.b : 1 12.a: 1
14.a: 2
14.b: 2
17: 2
18.a: 2
18.b: 2
18.c:
18.d*q: 2
19: 1
22: 1
23: 2
24: 1
28: 2
29: 2
31. AODITICSaL BOTES:
1112 - 27
LREP-S0BM, CSB-BOSOB
u m ran BEFCKT
MAP IMAGE:
CSOSS SBCnOH:
l-:-' : -I «ineral soil
1 . LATO OMIT: D . 2 . 2 . 2
2. IMF SHEET: 1112
3. AREA: 196 km2
4 . OCCflSEfiCE b y S8UVXICK: Sumatera Selatan: 992
5 . SZAIOS
Updated by: AB
edit date: 31/03/89
Status: Final
6. LABD OHIT DESCSIPTIOH: Saline peat dome fringes,organic sediment thickness 0.5 2.0 m, flat.
7. SATELLITE «rums
: 123/62/23/03/86
8. ABUTAT- PHOTOGRAPHS : 1:100.000
62 /8293-123
9. RADAR
: STAR 1/250/88/1112-3
10. PAREHT MATERIAL
11. ROCK OUTCROP:
%
a. Weathering :
b. Litbology : peat
c. Foxaation : Qal
12. HATER
a. Qaallty : Fresh
b. Source : Rain
13. FISHERIES
: Rawa (swamp)
14. RIVERS a. Floodrisk : Low
b. Inundation: Permanent
15. VBGEIATIOB/IjUn) OSE : swamp forest (rawa), bush
Area used
: 0 I
16. *fT*Ff WPATMI EROSIO0
a. Occarence : None
b. Evidence :
17. SOU. GSEAT GROUP
Dcaûoant >SOX
Associated 1
Associated 2
Classificatie
sulfohemists
tropohemists
X of area
80 Z
20 X
Lab. checked
yes
yes
3 2 . PICHtiCKIMTATl VK PROFILES:
heo/
/338-18 /82/P /1112/52/
het/
/12 /
1112 - 28
/88/HK/1112/41/
/158/
FEopsrti.es
a. Texture:
b.
c.
d.
e.
f.
8h.
i.
j.
k.
1.
•.
n.
o.
p.
q.
r.
topsoi-1
subsoil
Depth:
peatsoil
•ïneralsoil
Drainage:
Euch. K:
topsoil
subsoil
Total K2O: topsoil
subsoil
Avail. F:
Method
topsoil
sid>soil
Total F:
topsoil
subsoil
CBC pH 7 topsoil
subsoil
Soil Reaction:topsoil
subsoil
Al Sat.
topsoil
subsoil
Al taxicity :
Acid solpb. pot.:
Salinity :
Other Taxicity:
Boot obstx. layer :
Organic Matter :
TEB :
Total observations:
19. ALTITUDE:
2 0 . FLAB/TKQFILE:
2 1 . L.O. WATMCR2 2 . SLOPE:
2 3 . SLOPE D I S K . :
2 4 . BELIEF AMPLI.:
2 5 . TBgttATW-
26. uussi/BIDSffiS:
27. VALLET FLOOR:
28. LAHD FACETS:
2 9 . FBaOfERIATiai:
Dominant > 501
organic
organic
very deep
-
-
•
Very poorly drained
high
high
------very high
very high
strong acid
extreme acid
very low
medium
—
very shallow
saline
—
75 cm
44.9
74.4
0
Associated 1
organic
organic
very deep
-Very poorly drained
high
high
medium
medium
Bray I
—
-high
low
very high
very high
excessive acid
excessive acid
Associated 2
low
low
—
-
•
-
salt free
-300 cm
69.5
9.0
0
0.0
0.0
0
5 m
MinimoB:
2
Bange:
3m
Dominant: No pronounced highs/lows
Included:
a. Pattern: none
b. density:
c. Variability:
a. Steepness:flat
b . V a r i a b i l i t y : Low
d. Variability:
c. Length:
e. Curvature: convex
ValleybottoBs: 100 X
InterCLoves : 0-81:0 X, 9-25X: 0 % 25-551: 0 X
a.fliiii I mlii very low
b. Variability: Low
Flat, slope <2X, 0-50 m
a. Shape: no crests
b. Length:
c. Variability:
d. Width:
e. Variability:
a. Width:
b. Variability:
-1- Domes, sulfohemists, 80Ï
-2- Domes, tropohemists, 20Ï
-3-*Valleys:
Interflows:
30. BKI.TABTT.TTt:
1° reliable, 2- probable, 3> tenable, 4- plausible
lO.b : 1 12.a: 2 14.a: 2 14.b: 2
17: 2 18.a: 2 18.b: 2 18.c: 1
18.d-q: 2
19: 2
22: 1
23: 2 24: 1
28: 2
29: 2
31. ADDXTIOHAL HOTES: All representative profiles are extrapolated from other landunit.
1112 - 29
LAHD u u x REFOBT
IBEF-SDEH, CSR-BOBCB
MAP HUGE:
SECHG0:
P
À.l.1.2 à.i.i.i IA.1.1.3 'mi
1.3
P
— ><— — ,
Y
X1
A.l.2.1
Wllllll A.l.2.2
2. MAF SHEET: 1112
3. AREA: 437 km2
LAHD IMIT Af. 1 . 1 . 1
« « T H i n y y b y ÏHtWUCE: Sumatera Selatan: 79Ï, Lampung: 21Z
edit date: 04/03/89
Status: Final
SXUDS IDEKIXFTEBS
: Updated by: AH
Uffl) OBIT DESŒIPTICH: Marshes of broad alluvial plains with open low vegetation, fine
sediments, slopes 0-3X.
7. ^ATF^-^rITV- nt-Vfit&i
; 123/63/23/03/83, 124/62/30/03/85
8. ABPTAT- FB0T0G8APBS
: 1:100.000
59 /8316-097, 59 /8316-105, 58 /8316-63
9. BADAR
: START1/250/88/1112-2
10. PâBBBI MATERIAL
11. ROCK OOTCSOP:
%
a.. Weathering : Slight
b. Litfcology : clay
c. Formation : Qal
1.
4.
3.
6.
12. HATES
a. Quality :
b. Source :
13. fTSHEBIBS
:
14. RIVERS a. Floodrisk :
b. Inondation :
15. VEGETAHOB/LAHD USE :
Area used
16 . AH TKI -FPATMI E80SIGH
Brackish
Shallow wells
Rawa (swamp)
Medium
Permanent
mangrove forest (bakau), bush, swamp (rawa) including sedges
0 X
a. Occurence : None
b. Evidence :
1 7 . SOIL GREAT GROUP
Da>inant >SOZ
Associated 1
Classification
hydraquents
fluvaquents
Associated 2
tropohemists
32. H
eqw/
het/
/112-82
/
PROFILES:
/79/P /1112/12/
/88/HJ/1112/14/
Z of area
80 X
15 Z
Lab. checked
yes
yes
yes
5Z
/82 /
/170/
1112 -
eqv/
30
/185-23
/84/F /1111/51/
/24 /
18. SOU. CHARACTERISTICS
Properties
a. Texture:
topsoil
subsoil
b. Depth:
peatsoil
•ineralsoil
c. Drainage:
d. Exch. K:
e.
f.
g.
b.
i.
j.
k.
1.
a.
n.
o.
p.
q.
r.
topsoil
subsoil
Total K2O: topsoil
subsoil
Avail. P:
method
- topsoil
subsoil
Total P:
topsoil
subsoil
CEC pH 7
topsoil
subsoil
Soil Reaction:topsoil
subsoil
Al Sat.
topsoil
subsoil
Al toxicity :
Acid sulph. pot. :
Salinity :
Other Toxicity:
Root obstr. layer :
Organic Matter :
TEB :
Total observations:
Donnant > 501
fine
fine
-very deep
Very poorly drained
low
low
—
-—
--—
high
high
very strong acid
excessive acid
medium
low
Associated 1
fine
fine
-very deep
Very poorly drained
high
medium
very low
very low
Bray I
very low
very low
very high
very low
very high
high
very strong acid
excessive acid
—
—
-—
very deep
salt free
120 cm
16.5
7.3
6
150 cm
7.8
9.0
1
Associated 2
organic
organic
extremely deep
—
Very poorly drained
high
medium
high
medium
Olsen
very high
high
very high
medium
very high
very high
excessive acid
extreme acid
medium
low
—
salt free
170 cm
8.4
8.3
2
Range:
1 m
2 m
5m
Minium:
Dominant: No pronounced highs/lows
PLffl/FBOFILE:
Included:
b. density:
a. Pattern: none '
L.U. DBAIBAGE: c. Variability:
b. Variability: Low
a. Steepness:flat
SLOPE:
d. Variability:
c. Length:
e. Curvature: concave
SLOPE DISTR.:
Valleybottoms: 100 X
Interduves : 0-8Z:0 X 9-251: 0 X, 25-55X: 0 Ï
b. Variability: Low
RELIEF AMPLI.: a. Amplitude: very low
TPBPATMFlat, slope <2X, 0-50 m
c. Variability:
a. Shape: no crests
CHEST/RIDGES:
b. Length:
d. Width:
e. Variability:
b. Variability:
VALLEY FLOCK:
a. Width:
-1- Marshes, hydraquents, 80X
LAID FACETS:
-2- Marshes, fluvaquents, 15X
-3- Marshes, tropohemists, 5X
-4FRAGHEWTATIGB: Valloys:
Interfluves:
19. ALTITuDE:
20.
21.
22.
23.
24.
25.
26.
27.
28.
29.
30. RELIABILITY:
10.b : 1 12.a: 2
U.d-q: 2
19: 2
» reliable, 2- probable, 3» tenable, 4= plausible
18.b: 2
18.c: 1
14.a: 2
14.b: 2
17: 1
18.a: 1
29: 2
22: 2
23: 2
24: 2
28: 3
31. ADDITIONAL •DIES: Locally Sulfaquents may occur
1112 - 31
L A D OBIT REPORT
LREP~SDBM, GSR~BOGGR
MAP IMAGE:
p
A.I.1.2 A.l.1.1 IA.1.1.3 i A.l.1.1 X.3
-. -
*^^
A.I.1.1
A.I.1.2
A.1.1.3
P
r
EHS3 A.l.2.1
Ulllllll
A.1.2.2
1.
4.
5.
6.
LARD OBIT: Af.1.1.2
Z. MAP SHEET: 1112
3. AREA: 293 kœ2
U3UIKrjl.as by PROVBBCE: Sumatera Selatan: 99Ï
SIAIDS IDENTIFIERS
: Updated by: AH
edit date: 04/03/89
Status: Final
LAND OBIT DESCRIPTICH: Marshes of broad alluvial plains with mixed vegetation, fine
sediments,slopes 0-3%.
123/63/23/03/83, 123/62/23/03/86
7 . SATELLITE
60 /8341-079, 59 /8316-099, 60 /8341-071
8. AEBTAT. PHOTOGRAPHS
: 1:100.000
9. RADAR
: START1/250/88/1112-2.3
11. ROCK ODIC8OP:
X
10. FASERT MATERIAL
a. Heatfaering : Slight
b. Lithology : clay
c. Formation : Qal
12. HATES
13.
14.
15.
16.
a. Quality :
b. Source :
FISHERIES
:
RIVERS a. FLoodxisk :
b. Inondation:
VBSETATIOR/LARD OSE :
Area used
:
ACCELERATED EKOSIGH
a. Occurence :
b. Evidence :
Brackish
Medium wells
Rawa (swamp)
Medium
Permanent
, bush, swamp (rawa) including sedges
0 %
None
17. SOIL GREAT GROUP
Donnant >50Z
Associated 1
Associated 2
Z of area
60 X
30 X
5 X
Classification
hydraquents
tropaquents
tropohemists
32. RlEPRESERIATIV1! PROFILES:
eqw/
/11Z-87 /79/F /1112/12/
het/
/88/HJ/1112/14/
/
/97 /
/170/
eqt/
1112 -
32
Lab. checked
yes
yes
yes
/88/AF/1112/41/
/179/
1« «sryn, nuatftmmrsmrs
Properties
a. Textare:
topsoil
subsoil
b. Depth:
peatsoil
niiumlltnil
c. Drainage:
d. Exch. K:
topsoil
subsoil
e. Total K2O: topsoil
subsoil
£. Avail. F:
method
topsoil
subsoil
g. Total F:
topsoil
subsoil
h. CEC pH 7
topsoil
subsoil
i. Soil Reaction:topsoil
subsoil
j. Al Sat.
topsoil
subsoil
k. Al toxicity :
1. Acid sulph. pot.:
<a. Salinity :
n. Other Toxicity:
o. Boot obstr. layer :
p. Organic Matter :
q. TEB :
r. Total observations:
1 9 . ALTITUDE:
2 0 . PLÄH/PROFILE:
Dominant > SOX
organic
fine
-very deep
Very poorly drained
medium
low
--—
-—
—
high
high
strong acid
very strong acid
very low
very low
—
very deep
salt free
-92 cm
17.1
12.1
0
Associated 1
fine
fine
-very deep
Very poorly drained
low
low
very low
very low
Olsen
medium
medium
medium
medium
high
medium
excessive acid
excessive acid
low
low
—
-salt free
-120 cm
11.1
0.7
1
Associated 2
organic
organic
very deep
Very poorly drained
high
medium
high
medium
Olsen
very high
high
very high
medium
very high
very high
excessive 'acid
extreme acid
medium
low
-—
salt free
-170 cm
83.7
8.3
0
2 9 . FfiAGMEHIATIQS:
10 m
Minimum:
3
Dominant: No pronounced highs/lows
Included:
a. Pattern: none
b.
c. Variability:
a. Steepness:flat
b.
d.
c. Length: long
e. Curvature: concave
Valleybottoas:
%
Interfluves : 0-81:0 X, 9-25%: 0 Ï 25-55%: 0
a. Amplitude: very low
b.
Flat, slope <ZX, 0-50 m
a. Shape: no crests
b. Length:
d. Width:
e. Variability:
a. Width:
b. Variability:
-1- Marshes, hydraquents, 60X
- 2 - Marshes, tropohemists, 5%
-3- Transitional, tropaquents, 30Ï
-4Valleys:
Interfluves:
30. RELIABILITY:
lO.b : 1 12.a: 1
18.d-q: 2
19: 1
« reliable, 2= probable, 3° tenable, 4= plausible
18.b: 2
18.c:
14.a: 1
14.b: 1
17: 1
18.a: 2
29: 2
22: 1
23: 2
24: 1
28: 2
2 1 . L.U.
2 2 . SLOPE:
2 3 . SLOPE DISTR.:
2 4 . BELIEF AMPLI.:
2 5 . TERRAIN:
2 6 . CHEST/RIDGES:
2 7 . VALLEI FLOCK:
2 8 . LAKD FACETS:
density:
Variability: Low
Variability: Low
%, >55Z:
%
Variability: Low
c. Variability:
31. ADDITIONAL BOXES: Representative profiles for Hydraquents and Tropohemists are extra
polated from other landunit. In this l.u.is alsofound Sulfaquents
1112 -
33
LAHD OHIT REFCBT
LBEP~SDBM, CSR~BOGGR
MAP DOGE:
CSOSS SECTIGH:
P
1. LAHD 0HIT: Af.1.1.3
A.l.1.2 4.1.1.1 .4.1,1.3 iA.1.1.1 1.3
P
2. KâP SHEET: 1112
3. AREA: 261 km2
Lampung: 8X
updated by: AH
edit date: 04/03/89
Status: Final
Levees and flooded areas of broad alluvial plains, fine sediments,
slopes
0-3%.
123/62/23/03/86, 123/63/23/03/83
1:100.000
60 /8341-069, 61 /8293-023, 60 /8341-079
START1/250/88/1112-2.3
11. BOCK OOTCBQP:
%
Slight
clay
Qal
4. OCCORESCE by FSLWUHUE: Sumatera Selatan: 92%,
5. STATOS IDENTIFIERS
:
6. LAHD OOIT DESCHIFTIOS:
7. SATELLITE SCEHES
8. AERIAL PH0K0G8APHS
:
:
9. RADAR
10. PAREN MATERIAL
a. Weathering
b. Lithology
c. Formation
12. HATER
a. Quality
b. Source
13. FISHERIES
14. RIVERS a. Floodrisk
:
:
:
:
:
:
:
:
Brackish
Shallow wells
Rawa C swamp)
High
b. Inundation: None
15. VBGETATICH/LA8D USE : lowland wetland forest, bush
Area used
: 0 %
16.
a. Occurence
b. Evidence
17. SOIL G8EAT GSOOP
Dominant >SOZ
Associated 1
Associated 2
32.
iqt/
het/
/1.4-2
/
Classification
tropaquepts
hydraquents
tropohemists
/75/DR/1111/12/
/88/HK/1112/42/
Z of area
60 X
35 %
5 %
/08 /
/167/
eqw/
1112 - 34
Lab. checked
yes
yes
yes
/185-2
/83/A /1111/53/
/10 /
SOTÎ
topsoil
sabsoil
peatsoil
Depth:
Deralsoil
Drainage:
Each. K:
topsoil
sabsoil
Total K2O: topsoil
sabsoil
Avail. P:
method
topsoil
sabsoil
Total P:
topsoil
sabsoil
CEC pH 7
topsoil
sabsoil
Soil Reaction:topsoil
sabsoil
Al Sat.
topsoil
sabsoil
Al toxicity :
Acid salph. pot.:
Salinity :
Other Toxicity:
Boot obstr. layer :
Organic Matter :
TEB :
Total observations:
Tartare:
b.
c.
d.
e.
£.
g.
h.
i.
j.
k.
1.
m.
n.
o.
p.
q.
r.
Donnant > SOZ
moderately fine
moderately fine
Associated 1
moderately coarse
moderately coarse
very deep
Very poorly drained
low
low
low
very low
very deep
Very poorly drained
medium
low
very low
very low
Bray I
very low
medium
low
low
very high
very high
extreme acid
excessive acid
very low
very low
medium
very low
low
low
very strong acid
strong acid
very low
very low
Associated 2
organic
organic
very deep
Very poorly drained
high
high
high
high
Olsen
very high
very high
low
low
very high
very high
excessive acid
excessive acid
very low
very low
not relevant
salt free
105 cm
1.4
1.1
0
110 cm
4.9
6.0
0
19. ALTITUDE:
2 0 . PLAH/EBOFILE:
Bfcnrinam:
10 m
Minimum:
3m
Dominant: No pronounced highs/lows
Included:
b.
a. Pattern: meandering
21. L.D.
c. Variability: low
b.
a. Steepness:flat
22. SLOPE:
d.
c. Length: short
e. Curvature: not recorded
23. SLOPS DISTR.:
Valleybotttras: 100 %
Interleaves : O-8X:0 X, 9-25X: 0 X 25-55X: 0
b.
24. BELIEF AMPU.: a. Amplitude: very low
Flat, slope <ZX, 0-50 m
25. TEBBAXB:
26. CBEST/BIDSES:
a. Shape: no crests
b. Length:
d. Hidth:
e. Variability:
27. VALLEY FLOOR:
a. Hidth:
b. Variability:
-1- Levees, tropaquepts, 60X
28. LAKD FACETS:
~Z~ Flooded areas, hydraquents, 35Ï
-3- Flooded areas, tropohemists, 5%
-42 9 . FBA9ŒSTATIGH: Valleys:
Interfloves:
200 cm
91.9
13.3
1
10 m
density: Very low
Variability: Low
Variability: Medium
%
Variability: Medium
c. Variability:
30. «El.TABTT.TTY:
1- reliable, 2= probable, 3= tenable, 4° plausible
10-b : 1 12.a: 2
14.a: 2
14.b: 2
17: 2
18.a: 2
18.b: 2
18.c:
18.d-ti: 2
19: 1
22: 2
23: 3
24: 1
28: 2
29: 2
31. ADDITIONAL ROTES: Representative profiles for Tropaquepts and Hydraquents are extrapolated from other landunit. In this l.u is also found Sulfaquents
1112 - 35
LAID
REPORT
L8EP-SDBM, CSB-BOBCB
MAP IMAGE:
CROSS SECTIOS:
A.1.2.1
A.1.2.2
neander scar
backsvanp.
A.1.2.2
present river
svacp
X'.
Y/ / \ oldei subsoil
I alluvial' sediients
1. LAMD nHIT: Af.1.2.1
2. MAP SHEET: 1112
3. AREA: 356 km2
4. OCCQBEBCE by PROVHKE: Sumatera Selatan: 85Ï, Lampung: 15Z
5. SUIOS IDERIFIERS
: Updated by: AH
edit date: 04/03/83
Status: Final
6. LAB) U n i DESCKIPTIOH: Meanderbelts of broad alluvial valleys, fine sediments, slopes
0-3X.
7. SATELLITE
8. AERIAL PBDT0G8APBS
9. RADAR
10. PAREHT M»TKBTAI.
12.
13.
14.
13.
16.
124/62/23/03/85, 123/62/23/03/86
: 1:100.000
58 /8316-073, 61 /8293-027, 60
: START1/250/88/1112-2
/8341-077
11. ROCK OUTCROP:
a. Weathering : Slight
b. Litbology : clay
c. Foxnatian : Qal
HATER
a. Quality : Fresh
b. Source : Perennial River
FISHERIES
: Sungai (river)
RIVERS a. Floodrisk : High
b. Inundation: None
VHJKIATIOB/LAHD OSE ; secondary forest, bush, mixed gardens of fruit trees
Area used
: 30 X
ACCELERATED EROSION
X
a. Occurence :
b. Evidence :
17.
SOIL G8EAT G800P
Dominant >50Z
Associated 1
Associated 2
Classification
tropaquepts
fluvaquents
dystropepts
32. REPBESERIATIVE PROFILES:
iqt/
/184-1
/68/IS/1112/12/
ity/
/83-2
/64/X /1112/11/
Z of area
65 X
30 X
5X
/041/
/02 /
eqv/
1112 -
36
Lab. checked
yes
yes
yes
/112-86
/79/P /1112/12/
/86 /
<
IA «arm rtutaurTvarsTTm
ProperU.es
a. Texture:
topsoil
sobsoil
b. Depth:
peatsoil
•ôneralsoil
c. Drainage:
d. Erch. K:
topsoil
subsoil
e. Total K2O: topsoil
subsoil
t. Avail. F:
method
topsoil
subsoil
g. Total P:
topsoil
sobsoil
h. CEC pH 7
topsoil
subsoil
i. Soil Reaction:topsoil
subsoil
j. Al Sat.
topsoil
subsoil
k. Al taxicity :
1. Acid salph. pot.:
B . Salinity :
n. Other Toxicity:
o. Boot obstr. layer :
p. Organic Matter :
q. TES :
x. Total observations:
Dominant > 501
fine
fine
-very deep
Poorly drained
--medium
low
Associated 1
fine
fine—
very deep
Poorly drained
low
low
---
—
--
-----
medium
low
--very strong acid
excessive acid
—
-—
not relevant
—
—
120 cm
7.0
0.0
1
medium
medium
excessive acid
. excessive acid
low
low
—
moderately deep
salt free
-120 cm
3.7
4.3
2
Associated 2
medium
medium
—
very deep
Well drained
very high
very high
high
high
—
-medium
high
very high
very high
slightly acid
strong acid
very low
very low
—
—
-120 cm
1.3
0,0
0
19. ALTITUDE:
20 m
Minimum:
5 m
Dominant: No pronounced highs/lows
20. PLAI/PBOFILE:
Included:
b. density: Very low
a. Pattern: meandering
21. L.Ü. DRAIBASE: c. Variability: low
b. Variability: Low
a. Steepness:flat
22. SLOPE:
c. Length: short
d. Variability: Medium
e. Curvature: not recorded
23. SLOPE DISTK.: Valleybottoms: 100 %
Interflaves : 0-8Z:0 %, 9-25Z: 0 X 25-55X: O X
b. Variability: Medium
24. BELIEF AMPLI.: a. Amplitude: very low
25. TEBBAIB:
Flat, slope <2X, 0-50 m
c. Variability:
26. CREST/RIDGES:
a. Shape: no crests
b. Length:
d. Width:
e. Variability:
27. VALLEY FLOOR:
a. Width:
b. Variability:
-1- Levees, tropaquepts, 65X
28. LAID FACETS:
- 2 - Spillways, fluvaquents, 30Ï
-3- Old meander, dystropepts, 5Ï
-4Interflaves:
29. FfiAGMERAn«: Valleys: None
30. RELIABILITY:
lO.b : 2 12.a: 1
18.d-q: 2
19: 2
= reliable, 2= probable, 3= tenable, 4= plausible
18.b: 1
18.c: 1
14.a: 2
14.b: 2
17: 1
18.a: 1
22: 1
23: 2
24: 2
28: 3
29: 2
31. ADOITIOBAL BOIES: Representative profile for Dystropepts is extrapolated from other
landunit.
1112 -
37
um
ran
IREP-SDBM, CSR-BOGOR
REPORT
CSOSS SECTION:
CROSS SECTION
A
1.2.2
A.1.2.1
A.1.2.2
savah
V
2. mP SHEET: 1112
3. AREA: 198 km2
LAHD OBIT: Af . 1 . 2 . 2
m i m n ' i 1 by PROVINCE: Sumatera Selatan: 80Ï, Lampung: 20Ï
edit date: 04/03/89
Status: Final
STATUS IDEKTIFTERS
: Updated by: AH
LAHD UHIT DESCRIPTIGB: Seasonally flooded areas of broad alluvial valleys, fine sediments,
slopes 0-3Ï.
7. SATELLITE SCEHES
: 124/62/23/03/85, 123/62/23/03/86
8. AERIAL PHOTOGRAPHS
: 1:100.000
58 /8316-071, 61 /8293-025
9. RADAR
: START1/250/88/1112-2
10. PAREHT MATERIAL
11. BOCK OOTCSOP:
X
a. Weathering : Slight
b. Lithology : clay
c. Formation : Qal
12. HfilER
a. Quality : Fresh
b. Source : Perennial River
13. FISHERIES
: Sungai (river)
14. RIVERS a. Floodrisk : Medium
b. Inundation: Seasonal
1.
4.
5.
6.
15. VBGETATIQS/LAHD OSE : lowland wetland forest, bush, swamp (rawa) including sedges,
wetland rice (sawah)
Area used
: 10 X
16. ACCELERATED ERÛSIQS
a. Occorence :
b. Evidence :
17. SOIL GBEAT GROUP
DoBinant >SOZ
Associated 1
Associated 2
Classification
tropaquepts
tropaquents
sulfihemists
32. SEPBESERTATIVE PROFILES:
iqt/
/184-1
/68/IS/1112/12/
hei/
/189-4
/84/P /1112/41/
Z of area
70 X
25 X
5X
/041/
/30 /
eqt/
1112 -
38
Lab. checked
yes
yes
yes
/88/AF/1112/43/
/195/
is. aan. ca
isncs
ri ii|wi 11 uw
a. Texture:
topsoil
subsoil
b. Depth:
peatsoil
•ineralsoil
c. Drainage:
d. Exch. K:
g.
h.
i.
j.
k.
1.
•.
n.
o.
p.
q.
x.
very deep
Poorly drained
very deep
Very poorly drained
low
very low
very low
very low
Olsen
very low
very low
very high
high
medium
medium
very strong acid
very strong acid
very low
very low
very high
very high
extreme acid
extreme acid
very low
very low
120 cm
9.0
20.0
2
140 cm
51.6
8.7
3
medium
low
netted
topsoil
sobsoil
medium
Total F:
topsoil
subsoil
low
CSC pH 7
topsoil
subsoil
Soil Reaction:topsoil very strong acid
sobsoil excessive acid
Al Sat.
topsoil
sobsoil
Al taxicity :
Acid snlph. pot.:
not relevant
Salinity :
Other Taxicity:
Boot obstr. layer :
120 cm
Organic Matter :
7.0
TES :
0.0
Total observations:
0
19. ALTITUDE:
2 0 . FLftH/PHCFILE:
2 1 . L.O. DBADUGE:
2 2 . SLOPE:
2 3 . SLOPE DISTR.:
2 4 . BELIEF AMPLI.:
25.
TFEPATW-
26.
CBEST/BIDSES:
2 7 . VALLET FLOOR:
2 8 . LARD FACETS:
29.
Associated 1
fine
fine
topsoil
subsoil
e. Total K2O: topsoil
subsoil
f. Avail. F:
Dominant > 501
fine
fine
FfiflGMERTATICH:
Associated 2
organic
organic
extremely deep
Very poorly drained
medium
low
Bange:
2 m
3 m
5 m
Damnant: No pronounced highs/lows
Included:
a. Pattern: none
b. density: Very low
c. Variability:
a. Steepness:flat
b. Variability: Low
d. Variability:
c. Length:
e. Curvature: concave
Valleybottons:
%
Interfiles : O-8X:0 %, 9-251: 0 Z, 25-55X: 0 X, >55X:
%
a. Amplitude: very low
b . Variability: Low
Flat, slope <2I, 0-50 m
c. Variability:
a. Shape: no crests
b. Length:
d. Width:
e. Variability:
a. Width:
b. Variability:
-1- Depressions, tropaquepts, 70Ï
-2- Depressions, sulfihemists, 5!
-3- Transitions, tropaquents, 25X
-4Valleys:
Interfluvos: Large blocks
30. R E U A B r U T T :
1- reliable, 2 - probable, 3= tenable, *- plausible
10.b : 1 12.a: 1
14.a: 2
14.b: 2
17: 2
18.a: 2
18.b: 2
18.c: 2
18.d-q: 2
19: 1
22: 1
23: 2
24: 1
28: 3
29: 2
31. ADDITIOBAL BOIES: Representative profile for Tropaquepts is extrapolated from other
landunit.
1112 - 39
LAHD UBIT
LREP-SDBM, CSR-BOSOR
MAP IMAGE:
CROSS
IA.1.1.1
jPfq.3.1
».1.3
Pfq.2.1
/:
. . . ".-.-
X «..it».*.*;
1.
4.
5.
6.
7.
8.
9.
10.
12.
13.
14.
IS.
IK
LAHD UHIT: A£.1.3
2. MAP SHEET: 1112
3. *»FJ> 650 km2
«»junKHW.ir. by PROVINCE: Sumatera Selatan: 902, Lampung: 10Z
STATUS WtriÏÂjflxiss : Updated by: AH
edit date: 04/03/89
Status: Final
LAHD UHIT DESCRIPTIGB: Narrow valley bottoms , fine sediments, slopes 0-3X.
SATELLITE mi-EMMK
: 123/63/23/03/83
AERIAL PaOTOGRAPBS
: 1:100.000
59 /8316-099, 60 /8341-079
RADAR
: START1/250/88/1112-2
BAREST MATERIAL
11. ROCK OUTCROP:
Z
a. Weathering : Slight
b. Litbology : clay
c. Formation : Qal
HATES
a. Quality : Fresh
b. Source : Medium wells
FISHERIES
: Rawa (swamp)
RIVERS a. Floodrisk : Medium
b. Inundation: Seasonal
VEGEIATIOH/LAHD USE : , bush, swamp (rawa) including sedges
Area used
: 20 *
«rrantATEn rareira
a. Occnxonce :
b. Evidence :
17.
SOIL CHEAT GROUP
Damnant >SOZ
Associated 1
Associated 2
:
Classification
fluvaquents
tropaquepts
32. REEBESEHTATT7E PROFILES:
eqv/
/84-5
/86/WD/1112/11/
Z of area
65 %
35 Z
'
/016/
iqt/
1112 -
40
Lab. checked
yes
yes
/88/UA/1112/21/
/183/
isncs
Dominant > 501
fine
fine
-b. Depth:
•imralitnil
deep
Poorly drained
c. Drainage:
very low
d. Exch. K:
topsoil
very low
subsoil
very low
e. Total K20: topsoil
subsoil
very low
Bray I
f. Avail. P:
Batted
very low
topsoil
very low
sobsoil
very high
g. Total P:
topsoil
subsoil
very low
high
h. CEE pH 7
topsoil
subsoil
medium
i. Soil Reaction:topsoil very strong acid
subsoil excessive acid
very high
j. Al Sat.
topsoil
subsoil
very high
no
k. Al taxicity :
moderately deep
1. Acid sulpta. pot. :
salt free
•. Salinity :
—
n. Other Taxicity:
100 cm
o. Boot obstx. layer :
5.8
p. Organic Matter :
1.0
q. TEB :
r. Total observations:
1
ProjwrU.es
a. Texture:
Associated 1
moderately fine
moderately fine
—
very deep
Very poorly drained
low
low
very low
very low
Olsen
medium
very low
very low
very low
low
low
excessive acid
excessive acid
very high
very high
no
—
-—
110 cm
A.8
0.9
1
topsoil
subsoil
peatsoil
19. ALTITUDE:
2 0 . PLAB/rBOFILE:
2 1 . L.O. DBAIBflCE:
2 2 . SLOPE:
5 m
Miiriw:
2 m
Dominant;: No pronounced highs/lows
Included:
a. Pattern: meandering
c. Variability:
a. Steepness:flat
c. Length:
e. Curvature:
Associated 2
0.0
0.0
0
3 m
b. density: Very low
b. Variability: Low
d. Variability:
Valleybottoos: 100 Z
Interfloves : 0-8X:0 X, 9-25X: 0 %, 25-55X: 0 %
b. Variability: Low
2 4 . RELIEF AMPLI.: a. taplitode: very low
2 5 . TEBRAIH:
Flat, slope <2%, 0-50 m
2 3 . SLOPE DISTR-:
26. CREST/RIDGES:
a. Shape: no crests
b. Length:
d. Width:
e. Variability:
2 7 . VALLEI FLOOR:
a. Width: wide
b. Variability: Low
2 8 . LAID FACETS:
-1- Flood plains, fluvaquents, 65%
-2- Levee, tropaquepts, 35Ï
-3-429. FftAGMERTATI«: Valleys: Medium blocks
Interfluves:
c. Variability:
30. RELIABILITY:
1= reliable, 2= probable, 3- tenable, *= plansible
10-b : 2 12.a: 1
14.a: 2
14.b: 2
17: 2
18.a: 2
18.b: 1
18.c: 1
18.d-q: 2
19: 1
22: 1
23: 1
24: 1
28: 3
29: 2
31. ADDITIONAL BOTES: Repesentative profile
landunit.
•
for Fluvaquents is extrapolated from other
1112 - 41
LAID WUT REPORT
MF
B.5
IBEP-SDBM. CSR-BOSOB
IMAGE:
CROSS SECTIOR:
.••;ïi'«
WIAM
B.1.2!/ B.4.2
/•jB.l.lJ
f'
B.1.2
B.4.2
B.l.l
Sea
4.1
_^7 sea
/.••
?.i_:2i^ B.4.2 i j j ^ :
U:D'."'():)
rlh&iU
(old)
1. Laffl) OMIT: Bfq.1.2
5. S1AIDS IDEHTIFIEBS :
6 . Lam> OTII DESCRIPTICM:
7 . S&TEtXITE SCESES
8 . ABRTAf. fBQTOGSAfBS
:
:
9 . JUDAS
:
10.
(old, flattened
eroded)
(young)
IMKERT MAT1HTAT.
(young)
X'
2. MAP SHEET: 1112
3. AREA: 109 km2
Sumatera Selatan: 92%, Lampung: 8%
Updated by: AH
edit date: 31/03/89
Status: Final
Complex of eroded beach ridges and fill-in swales, fine and
coarse sediments (partly ripened)
123/63/23/03/83
1:100.000
62 /8293-111, 65 /8284-S9
START1/250/88/1112-2
11. ROCK OUTCROP:
X
a. Weathering :
12.
13.
14.
15.
16.
17.
b. Litbology :
c. Formation :
MATES
a. Quality :
b. Source :
BUSHHII HK
;
RIVERS a. Floodrisk :
b . TtwrrM^?it-i on :
VBOTIATIOH/LÄHD OSE :
Area u s e d
:
ACCELERATED EROSIGS
a. Occurenco :
b. Evidence :
sand, clay
Qal
Brackish
Medium wells
Rawa (swamp)
None
None
secondary forest, bush, alang-alang, mixed gardens of fittit trees
20 X
None
SOIL GBEAT GROUP
Dominant >SOZ
Associated 1
Associated 2
Classification
quartzipsamments
tropaquepts
psammaquents
32. REPRESEHTATIVE PROFILES:
esz/
/84-3 /86/Dd/lllO/Sl/
eqs/
/i84-3
/68/IS/1111/51/
Z of area
65 X
30 %
5X
/03 /
/28 /
iqt/
1112 - 42
Lab. checked
yes
yes
yes
/84-4
/86/Dd/lllO/Sl/
/04 /
1« SOTT, r P » P A r ™ I T S T T r s
Properties
a. Texture:
topsoil
subsoil
b. Depth:
peatsoil
•dnaralsoil .
c. Drainage:
d. Exch. K: topsoil
subsoil
e. Total K2O: topsoil
subsoil
t. Avail. P: method
topsoil
subsoil
g. Total P: topsoil
subsoil
h. CBC pH 7
topsoil
subsoil
i. Soil Reaction:topsoil
subsoil
j. Al Sat.
topsoil
subsoil
k. Al toxicity :
1. Acid sulph. pot.:
m. Salinity :
n. Other Toxicity:
o. Root obstr. layer :
p. Organic Matter :
q. TEB :
r. Total observations:
Dominant > 501
coarse
coarse
-very deep
Excessively drained
very low
very low
low
very low
Bray I
very low
very low
very low
very low
very low
very low
neutral
neutral
very low
very low
—
—
—
-125 cm
1.3
1.7
0
Associated 1
fine
fine
—
very deep
Poorly drained
medium
very low'
medium
low
Bray I
medium
medium
high
medium
medium
high
moderately acid
very strong acid
very low
very low
—
—
—
-125 cm
7.7
13.9
0
Associated 2
coarse
coarse
—
deep
Excessively drained
—
-low
very low
—
-low
very low
--very strong acid
very strong acid
--—
-—
-75 cm
0.1
0.0
0
19. ALTITUDE:
Maximum:
20. FLAB/PROFILE:
Dominant: non-linear and parallel > 60Ï of area flat-topped
Included:
10 m
Minimum:
3 m
Range:
5m
a. Pattern: parallel
b. density: Very low
c. Variability:
a. Steepness:flat
b. Variability: Low
22. SLOPE:
c. Length: short
d. Variability: Low
e. Curvature: convex
23. SLOPE DISTK. : Valleybottams: 35 %
Interfluves : 0-8Z:65 X, 9-251: 0 X, 25-551: 0 %
24. RELIEF AMPLI.: a. Amplitude: very low
b. Variability: Low
25. TFPPATHUndulating 2- 8%, Ó-50 m
26. CSEST/RIDSES:
c. Variability: Low
a. Shape: Irregular
b. Length:Short
d. Width: narrow
e. Variability: Low
27. VALLEY FLOOR:
a. Width: narrow
b. Variability: Low
-1- Ridges, quartzipsamments, 65X
28. LAND FACETS:
-Z~ Swales, tropaquepts, 30X
-3- Transition, psammaquents, 5%
-42 9 . FRAGMESTATHS: Valleys:
Interfloves: Small blocks
21. L.O. DRAIHAGE:
30. RELIABILITY:
1= reliable, 2= probable, 3= tenable, 4= plausible
lO.b : 1 12.a: 2
18.b: 1 18.c:
14.a: 2
14.b: 2
17: 2
18.a: 2
18.d-q: 2
19: 1
29: 2
22: 2
23: 2
24: 1
28: 1
31. ADDITIONAL HOTES: All representative profiles are extrapolated from other landunits
1112 - 43
LBEP-SBBM, CSR-BOBOR
LAID EBTT REPORT
MAP D U G S :
1WTSS SECTIOH:
B.5.1
1.3
B.4.4
B.4.2
3.4.3
B.4.1 'Sea
I»
3 . AREA: 48 km2
1. LAID DHIT: Bf.4.1
2. MAP SHEET: 1112
4. OOCOREKE by PROVINCE; Sumatera Selatan: 99X
Status: Final
Updated by: AH
edit date: 31/03/89
5 . STATUS
6 . LAHD u r i l l n i c w i t n ^ n M Tidal mud flats, fine sediments (unripe).
123/62/23/03/86, 123/63/23/03/83
7 . SATELLITE MliMlKW
1:100.000
63 /8284-173, 65 /8284-11
8 . AERIAL PHOTOGRAPHS
START1/250/88/1112-2.3
9 . RADAR
11. ROCK OUTCROP.
1 0 . P A R E « HATKRTAT.
a. Weathering
b. Idthology
c. Fonatian
12. HATER
a. Quality
b. Source
13. FISHERIES
14. RIVERS a. Floodrisk
b. Inundation
15. VBGETATICa/LAHD USE
Area used
16. ACCELERATED EBOSIOH
clay
Qal
Saline
Rain
Laut (sea)
None
Medium Tidal Range
swamp forest (rawa), swamp (rawa) including sedges
0 X
None
b. Evidence
17. SOIL GREAT GBODP
Donnant >SOZ
Associated 1
Associated 2
Classification
hydraquents
sulfaquents
X of area
65 X
35 X
Lab. checked
yes
yes
3 2 . REPBESBRATIVE PROFILES:
eqw/
/338-3
/82/P /1112/52/
/58 /
eqi/
1112 - 44
/338-1
/82/P /1112/
/
/55 /
18. SOIL CHARêCTERISnCS
Daninant > 501
Properties
fine
a. Tartare:
topsoil
fine
subsoil
deep
b. Depth:
peatsoil
__
Very poorly drained
c. Drainage:
very high
d. Exch. K:
topsoil
very high
subsoil
-e. Total K2O: topsoil
-subsoil
t. avail. P:
method
-topsoil
—
subsoil
—
g. Total P:
topsoil
—
subsoil
h. CEC pH 7
topsoil
very high
subsoil
very high
i. Soil Reaction:topsoil strong acid
subsoil excessive acid
very low
j. Al Sat.
topsoil
subsoil
very low
k. Al taxicity :
moderately shallow
1. Acid sulph. pot.:
•. Salinity :
moderately
-n. Other Taxicity:
110 cm
o. Root obstr. layer :
p. Organic Matter :
1.9
61.3
q. TEB :
r. Total observations:
0
Associated 1
fine
--deep
Very poorly drained
very high
very high
---
Associated 2
-•
—
—
low
high
strong acid
very strong acid
very low
very low
-shallow depth
saline
-110 cm
2.3
71.5
0
0.0
0.0
0
Range:
1m
2 m
Minimum:
0 m
Dominant: No pronounced highs/lows
20. PIAB/PSOFILE:
Included:
a. Pattern: none
b. density:
21. L.Ü. DBAIBAGE: c. Variability:
b. Variability: Low
a. Steepness:flat
22. SLOPE:
d. Variability:
c. Length:
e. Curvature: not recorded
23. SLOPE DISTR.:
Valleybottons: 100 X
Interfluves : 0-81:0 X, 9-251: 0 X, 25-55X: 0 X
b. Variability: Low
24. RELIEF AMPLI-: a. Aagtlitode: very low
25. TPPBATBFlat, slope <2X, 0-50 m
a. Shape: no crests
c. Variability:
26. CREST/RIDGES:
b. Length:
d. Width:
e. Variability:
a. Width:
27. VALLEY FLOOR:
b. Variability:
-1- Tidal flats, hydraquents, 65%
28. LAB) FACETS:
- 2 - Tidal flats, sulfaquents, 35Z
-3-4Interfluves:
2 9 . FRACMERATIOS: Valleys:
19. ALTITUDE:
30. RELIABILITT:
1= reliable, 2= probable, 3= tenable, 4» plausible
lO.b : 1 12.a: 1
14.a: 1
14.b: 2
17: 2
18.a: 2
18.b: 1
18.c: 1
18.d-q: 2
19: 1
22: 1
23: 2
24: 1
28: 2
29: 2
31. ADDITIOXAL BOTES: All representative profiles are extrapolated from other landunit.
1112 -
45
IAHD
REPORT
LBEP-SDBM, CSR-BOSGR
SECTIGH:
M&P DOGE:
B.5.1
B.4.4
Ï.3
B.4.2
3.4.3
B.4.H Sea
•M
1.
4.
5.
6.
7.
8.
IAHD OBIT: Bf.4.2
OCCÜiREHCE by PROVINCE:
STAIOS IDKHTIFIERS
:
IAHD OBIT DESCRIPTICH:
SATELLITE SCEHES
:
AERIAL PBOTOGBAPBS :
2. MftP SHEET: 1112
3. AREA: 294 km2
Sumatera Selatan: 99%
Updated by: AH
edit date: 03/03/89
Status: Final
Marshy tidal flats behind shore, fine sediments (unripe).
123/62/23/03/86, 123/62/23/03/83
1:100.000
63A /8284-155, 63 /8284-173, 65 /8284-09
: START1/250/88/1112-2.3
11. ROCK OUTCROP:
9. RADAR
10. PARBBT MATERIAL
a. Weathering :
b. Lithology :
c. Formation :
12. MATER
a. Quality :
b. Source :
13. FISHERIES
:
14. RIVERS a. Floodrisk :
b. Inundation:
15. VESETATIOg/IAKD USE :
Area used
:
16. AfTTlfT fy A T « ' EROSIQH
a. Occurence :
b. Evidence :
X
clay
Qal
Saline
Rain
Laut (sea)
None
Medium Tidal Range
swamp forest (rawa), bush, swamp (rawa) including sedges
0 X
None
17. SOU. GBEA.T GSOOP
Donnant >SOZ
Associated 1
Associated 2
Classification
hydraquents
sulfaquents
Z of area
65 X
35 X
Lab. checked
yes
yes
3 2 . REIBESEHTAT1VE PROFILES:
eqw/
/
/88/ES/1112/52/
/154/
eqi/
1112 - 46
/338-1
/82/P /1112/54/
/55 /
18. SOIL CHARACTERISTICS
Properties
a. Texture:
topsoil
subsoil
b. Depth:
poatsoil
•ïneralsoil
c. Drainage:
d. Excta. K:
topsoll
subsoil
e. Total K2O: topsoll
subsoil
£. Avail. P:
method
topsoil
subsoil
E- Total P:
topsoil
subsoil
h. CEE pH 7
topsoil
subsoil
i. Soil Reaction:topsoil
subsoil
j. Al Sat.
topsoil
subsoil
k. Al taxicity :
1. Acid solpta. pot.:
B. Salinity :
n. Other Tenacity:
o. Root obstr. layer :
p. Organic Hatter :
q. TEB :
r. Total observations:
1 9 . ALTITUDE:
2 0 . PLAH/P8QFILE:
2 1 . L.O. DRAIHAGE:
2 2 . SLOPE:
2 3 . SLOPE DISTft.:
2 4 . BELIEF AMPLI.:
2 5 . TEBRAIH:
2 6 . CHEST/RIDGES:
2 7 . VALLEY FLOOR:
2 8 . LAHD FACETS:
2 9 . FRACMEBTAXIOI:
Dooinant > SOX
fine
fine
Associated 1
fine
—
very deep
Very poorly drained
very high
medium
very high
very high
Olsen
low
low
very high
medium
very high
medium
moderately acid
extreme acid
very low
very low
deep
Very poorly drained
very high
very high
—
--
very deep
very slightly
shallow depth
very slightly
140 cm
13.6
50.9
2
100 cm
23.3
71.5
2
Associated 2
-—
—
-low
high
strong acid
very strong acid
very low
very low
0.0
0.0
0
Range:
1m
5 m
Minimum:
Dominant: No pronounced highs/lows
Included:
b. density:
a. Pattern: none
c. Variability:
b. Variability: Low
a. Steepness:flat
d. Variability: .
c. Length:
e. Curvature: not recorded
Valleybottaras: 100 %
Interfluves : 0-81:0 %, 9-251:
X, 25-551: 0 %
a. Amplitude: very low
b. Variability: Low
Flat, slope <2%, 0-50 m
a. Shape:
c. Variability:
b. Length:
d. Width:
e. Variability:
a. Width:
b. Variability:
-1- Marshes, hydraquents 65X
-2- Marshes, sulfaquents 35Ï
-3-4Interfluves:
Valleys:
30. BEUABILITi:
1= reliable, 2= probable,
lO.b : 2 12.a: 1
14.a: 1
14.b: 2
17: 1
18.d-q: 2
19: 2
22: 1
23: 2
24: 1
e
tenable, 4= plausible
18.a: 1
18.b: 2
18.c: 1
28: 2
29:
31. ADOITIOHAL KITES:
1112 -
47
I-ÄWH m i T 8BHIIT
LHEP-SDBM, CSR-BOBGR
MAP IMAGE:
CHOSS SECTIOH:
B.5.1 1.3
B.4.4
B.4.2
3.4.3
B.4.1 'Sea
HD
w
X'
1.
4.
5.
6.
LAND UBIT: Bf. 4.3
2. MSP EHEET: 1112
3. AREA: 215 km2
naaikrjuu*. by PROSTBCE: Sumatera Selatan: 99%
STATDS IDEHTIFIERS
: Updated by: AH
edit date: 03/03/89
Status: Final
LAHD IDHIT DESCRIPTION: Tidal flats with mangrove vegetation, fine sediments (uripe).
7. SATELLITE SCENES
: 123/62/23/03/86, 123/63/23/03/83
8. AERIAL PBOTOG8APHS
: 1:100.000
9. RADAR
: START1/250/88/1112-2 . 3
10. PARENT MATERIAL
a. Weathering :
b. Lithology : clay
c. Formation : Qal
12. HATER
a. Quality : Saline
b. Source : Rain
13. FISHERIES
: Laut (sea)
14. RIVERS a. Floodrisk :
b. Inundation: Medium Tidal Range
15. VEGEIATIOH/LAHD USE : mangrove forest (bakau)
Area used
: 0 %
16. ACCELERATED EROSION
a. Occurence : None
b. Evidence :
11. B O X COTCKQP:
17. SOIL GHEAT GSOOP
Dominant >SOZ
Associated 1
Associated 2
Classification
hydraquents
sulfaquents
32.' REPRESEHTA7TVE PROFILES:
eqw/
/
/88/US/1112/61/
Z of area
90 %
10 X
/184/
eqi/
1112 -
48
Lab. checked
yes
yes
/338-1
/82/P /1112/52/
/55 /
18. SOIL CHARACTERISTICS
Properties
a. Texture:
topsoil
subsoil
b. Depth:
peatsoil
mineralsoil
c. Drainage:
d. Exch. K:
topsoil
subsoil
e. Total K2O: topsoil
subsoil
£. Avail. P:
method
topsoil
subsoil
g. Total P:
topsoil
subsoil
b. CEC pH 7
topsoil
subsoil
i. Soil Reaction:topsoil
subsoil
j. Al Sat.
topsoil
subsoil
k. Al toxicity :
1. Acid sulph. pot.:
a. Salinity :
n. Other Taxicity:
o. Boot obstr. layer :
p. Organic Matter :
q. TEB :
r. Total observations:
Dominant > SOZ
moderately fine
fine
Associated 1
fine
--
very deep
Very poorly drained
very high
very high
medium
medium
Olsen
medium
medium
very high
very high
medium
medium
neutral
slightly alkaline
very low
very low
deep
Very poorly drained
very high
very high
---
very deep
saline
shallow depth
very slightly
120 cm
100 cm
23.3
71.5
0
it.O
10.2
2
Associated 2
----low
high
strong acid
very strong acid
very low
very low
0.0
0.0
0
Minimn:
Bange:
0 m
2 m
3 m
Dominant: No pronounced highs/lows
Included:
b. density:
L.D. DRAHttGE: a. Pattern: none
c. Variability:
SLOPE:
b. Variability: Low
a. Steepness:flat
d. Variability:
c. Length:
e. Curvature: not recorded
Valleybottoms: 100 %
SLOPE DISTR.:
Interfluves : 0-81:0 %, 9-25t: 0 %, 25-551: 0 X
b. Variability: Low
BELIEF AMPLI. : a. Amplitude: very low
TEBBAIH:
Flat, slope <2%, 0-50 m
CREST/RIDGES:
c. Variability:
a. Shape: no crests
b. Length:
d. Width:
e. Variability:
VALLET FLOOR:
a. Width:
b. Variability:
-1- Tidal flats, hydraquents, 90%
LAHD FACETS:
- 2 - Tidal flats, sulfaquents, 10%
-3-*FBAGMERTATICH: Valleys:
Interfluves:
19. ALTITUDE:
20. PLAH/PROFILE:
21.
22.
23.
24.
25.
26.
27.
28.
29.
30. RELIABILITY:
1= reliable, 2= probable, 3= tenable, 4= plausible
lO.b : 1 12.a: 1
14.a: 1
14.b: 2
17: 2
18.a: 2
18.b: 1
18.c: 1
18.d-ti: 2
19: 1
22: 1
23: 2
24: 1
28: 2
29:
31. ADDITIONAL BOTES: Representative frofile for Sulfaquents is extrapolated from other
L.U.
1112 - 49
LR£P~SDBM, CSR~BO80R
LAID UBJ.X
MAP IMAGE:
CSDSS SECTIOH:
B.5.1 1.3
B.4.4
B.4.2
3.4.3
B.4.1 Sea
X1
1. LARD OBIT: Bf.4.A
5. STATUS UMÜfTlPlERS
6. LAHD UBJ.X DESCBIFTTC»
7. SATELLITE ?3'pilfCK
8. AERIAL FB0TDG8AEBS
9. BAOAR
10. PAREOT mTERTAI.
a. Weathering
2. SAP SHEET: 1112
3. AREA: 242 km2
Sumatera Selatan: 99X
Updated by: AH
edit date: 03/03/89
Status: Final
Estuarine flats along rivers with nipa vegetation, fine sediments
(unripe).
123/62/23/03/86, 123/63/23/03/83
1:100.000
63 /8284-169, 62 /8293-121, 62 /8293-117
START1/250/88/1112-2.4
11. ROCK OOTCSOF:
clay
Qal
Saline
Rain
Sungai (river)
13. FISHERIES
High
14. RIVERS a. Floodrisk
b. Tmnvi^itri on Medium Tidal Range
nipah forest (nipah), bush
15. VEGETATIGH/LAgD OSE
0 %
Area used
16. »nr-FjTO*TFn rajriKTni
I
b. Litbology
c. Formation
a. Quality
12. M&TES
b. Source
a. Occareoce
b. Evidence
,
•
•
None
17. SOIL G8EAI O O D P
Dominant >SOZ
Associated 1
Associated 2
Classification
hydraquents
fluvaquents
sulfaquents
32. REfBESERATTVE rSQFXLES:
eqw/
/
/88/ES/1112/52/
eqi/
/338-2
/82/P /1112/52/
Z of area
80 X
15 I
•
/155/
/01 /
5
X
eqv/
1112 - 50
Lab. checked
yes
yes
yes
/184-1
/68/IS/1111/52/
/034/
18. SOIL CHARACTERISTICS
Properties
Daainant > 50Z
fine
a. Tartare:
topsoil
fine
subsoil
b. Depth:
peatsoil
very deep
•ineralsoil
Very poorly drained
c. Drainage:
very high
d. Erch. K:
topsoil
very high
subsoil
very high
e. Total K2O: topsoil
very high
subsoil
Olsen
£. Avail. P:
method
low
topsoil
low
subsoil
low
g. Total F:
topsoil
medium
subsoil
medium
h. CEC pH 7
topsoil
subsoil
high
i. Soil Reaction:topsoil excessive acid
subsoil extreme acid
very low
j. Al Sat.
topsoil
subsoil
very low
k. Al toxicity :
1. Acid snlph. pot.:
very deep
m. Salinity :
saline
n. Other Toxicity:
110 cm
o. Root obstr. layer :
8.6
P- Organic Matter :
27.4
q1
r. Total observations:
Associated 1
fine
fine
Associated 2
fine
fine
very deep
Very poorly drained
low
low
high
high
very
Very
very
very
--medium
low
—
-strong acid
strong acid
-—
—
deep
poorly drained
high
high
---
--—
-very high
low
strong acid
strong acid
very low
very low
saline
very shallow
saline
120 cm
3.4
0.0
1
110 cm
20.2
54.4
7
19. ALTITUDE:
Range:
2 m
4 m
Minimal:
0 m
Dominant: No pronounced highs/lows
20. PLAB/ÎBDFILE:
Included:
a. Pattern: none
b. density:
21. L.D. EBAIBAGE: c. Variability:
a. Steepness:flat
b. Variability: Low
22. SLOPE:
c. Length:
d. Variability:
e. Curvature:
23. SLOPE DISTR.:
ValleybottOBS: 100 X
Interfiles : 0-81:0 X. 9-251: 0
25-55X: 0 X
b. Variability: Low
24. RELIEF AMPU.: a. Anplitude: very low
25. TERRAIS:
Flat, slope <ZX, 0-50 m
26. CREST/RIDGES:
c. Variability:
a. Shape: no crests
b. Length:
d. Width:
e. Variability:
27. VALLET FLOOR:
a. Width:
b. Variability:
-1- Flats with nipa, hydraquents, 80X
28. LAID FACETS:
-2- flats with mangrove, fluvaquents, 15X
-3- Flats with mangrove, sulfaquents, 5X
-429. FRAGHEHTATICH: Valleys:
Interfluves:
30. RELIABILITY:
1» reliable, 2° probable, 3> tenable, 4« plausible
lO.b : 1 12.a: 1
18.b: 2
18.c: 1
14.a: 1
14.b: 2
17: 2
18.a: 1
18.d-q: 2
19: 1
29:
22: 1
23: 2
24: 1
28: 2
31. ADDmCHAL HOTES:
1112 -
51
LAHD 'UHIT REFCBT
LREP~SDBM„ CSR~BOGQR
MAP DUGE:
CROSS SECTIO8:
p
B.4.2
B.4.5
r r- f- f f *
•HK
"~ "* *" "
*v
X.
1.
4.
5.
6.
X'
IARD OBIT; Ef.4.5
2. JfeP S5EET: 1112
3. AREA: 39 km2
(IHaiRtWm by PfiUVlKCE: Sumatera Selatan: 99Z
STATUS IDEBTIFIERS
: Updated by: AH
edit data: 03/03/89
Status: Final
LARD OBIT DESCRIPTIGH: Tidal flats above storm level, fine sediments (partly ripened).
7. SATELLITE SCEHES
123/62/23/03/86
8. AERIAL PHOTOGRAPHS
1:100.000
61 /8293-29
9. RADAR
Star 1/250/88/1112-3
10. PARE« lttTERIAL
a. Weathering
b. Lithology : clay
c. Formation : Qal
12. HATER
a. Quality
Brackish
b. Soazce : Rain
: None
13. FISHERIES
14. RIVERS a. Floodrxsk
None
b. Inundation: Medium Tidal Range
15. VBSETATICB/LAHD OSE
Area used
16. ACCELERATED EBOSICB
a. Occurence
b. Evidence
11. BOCK OOTCHOT:
: mangrove forest (bakau), bush, swamp (rawa) including sedges
: 0X
: None
:
17. SOIL GREAT GBOOP
Doainant >SOX
Associated 1
Associated 2
Classification
sulfaquents
hydraquents
X of area
65 I
35 Ï
eqv/
/63 /
1112 - 52
Lab. checked
yes
yes
/338-12
/82/P /1112/52/
/61 /
1 8 . SOIL CHARACTEBISTICS
P1.OJMU. L l O S
a. Textare:
topsoil
subsoil
Associated 1
fine
fine
very
Very
very
very
very
Very
very
very
Associated 2
b. Depth:
c.
d.
e.
£.
8.
h.
i.
j.
k.
1.
m.
n.
o.
p.
q.
r.
peatsoil
•ineralsoil
Drainas«:
Exch. K:
topsoil
sobsoil
Total K2O: topsoil
subsoil
Avail. P:
nethod
topsoil
subsoil
Total P:
topsoil
subsoil
CEC pH 7
topsoil
subsoil
Soil Reaction:topsoil
subsoil
Al Sat.
topsoil
subsoil
Al toxicity :
Acid solph. pot.:
Salinity :
Other Toxicity:
Boot obstr. layer :
Organic Matter :
TEB :
Total observations:
INrritiflfnti ^ 50Z
fine
fine
deep
poorly drained
high
high
deep
poorly drained
high
high
very high
very high
strong acid
moderately acid
very low
very low
high
very high
very strong acid
strong acid
very low
very low
shallow depth
saline
very deep
moderately
110 cm
14.9
54.7
0
120 cm
7.7
44.7
0
0.0
0.0
0
Range:
5 m
MinijoaDs:
.3m
4 m
Dominant: No pronounced highs/lows
20. FLAB/PROFILE:
Included:
a. Pattern: none
b. density:
21. L.O. DBAIHAGE: c. Variability:
a. Steepness:flat
b. Variability: Low
22. SLOPE:
c. Length:
d. Variability:
e. Curvature:
Valleybottcms: 100 %
23. SLOPE DISTR.:
Interfluves : 0-81:0 %, 9-251: 0 %, 25-551: 0 %
b. Variability: Low
2*. BELIEF AMPLI.: a. Amplitude: very low
25. TESHAIS:
Flat, slope <2%, 0-50 m
26. CSEST/RIDGES:
a. Shape: no crests
b. Length:
c. Variability:
d. Width:
e. Variability:
a. Width:
b. Variability:
27. VALLEY FLOOR:
-1- Flats, sulfaquents, 65%
28. LAHD FACETS:
- 2 - Depressions, hydraquents, 35%
-3-429. FKAGMEBTATÎOB: Valleys:
Interfluves:
19. ALTITUDE:
30. RELIABILITY:
1= reliable, 2= probable, 3= tenable, 4= plausible
lO.b : 1 12.a: 1
14.a: 1
14.b: 2
17: 2
18.a: 2
18.b: 2
18.c: 1
18.d-q: 2
19: 2
22: 1
23: 2
24: 1
28: 2
29:
,31. ADDITIOBAL BOTES: all representative profiles are extrapolated from other L.U
1112 -
53
'
•
LBEP-SDBM, CSR-BOBGR
IJUHl I H D T MIHMMT
CSGSS SBCTIOB:
MAP IMAGE:
D.
2.1.2
B.5 . 1
•
$
B
5. 1
B. 5 . 3
B.5. 4
%
r
f?
B.
5.4
B. 1 1
1
* x_
- --
S
•
•
Potensiîl acid ulfat
X'
1.
4.
5.
6.
LAM) UBII: Bf.5.1
2. MAF SHEET: 1112
3. «•»• 1100 I;rs2
QCCnBEKE by PBOWUiCE: Sumatera Selatan: 93%, Lampung: 7Z
SUIDS 1DEHTIFIEKS
: updated by: AH
edit date: 03/03/89
States: Final
LAHD D M T DESCRTPTICH: Saline back swamps with grass vegetation, fine sediments (unripe).
7. SATELLITE SCEHES,
8. AERIAL CBDTOGSAFHS
9. BADAR
10. BABERT iOTBBTAt-
12.
13.
14.
15.
: 123/62/23/03/86, 123/63/23/03/83
: 1:100.000
63 /8284-160, 62 /8293-119, 61 /8293-011
: START1/250/88/1112-2.3
11. HOCK ODTCBOP:
X
a. Neatfaaxins :
b. Litbology : clay
c. Foxmatian : Qal
HATER
a. Quality : Saline
b. Source : Rain
FISHERIES
: Tambak (estuary)
RIVERS a. Floodrisk : None
b. Inondation: Medium Tidal Range
WHGEIATIOH/LAHD OSE : , bush, swamp (rawa) including sedges
Area used
:0 X
16. ACCELERATED EBGSIGH
a. Occnrence : None
b . Evidence :
17. SOIL flPFftT GROUP
Damnant >50Z
Associated 1
Associated 2
eqw/
eqi/
/
/338-16
:
X of area
Classification
hydraquents
sulfohemists
sulfaquents
/88/ER/1112/ / /140/
/82/P /1112/52/
/48 /
1112 -
Lab. checked
60 X
yes
30 X
yes
5 X
yes
heo/
/338-18
/82/P /1112/52/
/12 /
18. SOIL CHARACTERISTICS
Properties
a. Textare:
topsoil
subsoil
b. Depth:
peatsoil
•ineralsoil
c. Drainage:
d. Exch. K:
topsoil
subsoil
e. Total K2O: topsoil
subsoil
f. Avail. P:
method
topsoil
subsoil
g. Total P:
topsoil
subsoil
h. CBC pH 7
topsoil
subsoil
i. Soil Reaction:topsoil
subsoil
j. Al Sat.
topsoil
subsoil
k. al tozicity :
1. Acid sulph. pot. :
•. Salinity :
n. Other Tozicity:
o. Boot obstx. layer :
p. Organic Matter :
q. TUB :
r. Total observations:
Donnant > SOX
fine
fine
Associated 1
organic
organic
deep
very deep
Very poorly drained
medium
medium
medium
medium
Olsen
very low
very low
medium
very low
medium
high
strong acid
strong acid
very low
very low
Very poorly drained
high
high
Associated 2
fine
fine
very deep
Very poorly drained
high
very high
high
very high
strong acid
strong acid
very low
very low
not relevant
saline
very high
very high
strong acid
excessive acid
very low
medium
no
shallow depth
saline
110 cm
2.6
19.4
2
100 cm
44.9
74.4
1
110 cm
13.6
53.3
5
very shallow
saline
19. ALTITUDE:
12 m
Minium:
3
5 m
Dominant: No pronounced highs/lows
20. FLAB/PROFILE:
Included:
b. density: Low
a. Pattern: deranged
21. L.D. DRAIHAGE: c. Variability: low
b. Variability: Low
a. Steepness:flat
22. SLOPE:
d. Variability:
c. Length:
e. Curvature:
Valleybottoms: 100 %
23. SLOPE DISTR.:
InterCluves : 0-8X:0 X, 9-25X: 0 X 25-55X: 0 X
b. Variability: Low
24. RELIEF AMPLI.: a. Amplitude: very low
Flat, slope <2%, 0-50 m
25. TEKRAIH:
a. Shape: no crests
c. Variability:
26. CHEST/RIDGES:
b. Length:
d. Width:
e. Variability:
a. Width:
27. VALLET FLOOR:
b. Variability:
-\- Swamps, hydraquents, 60%
28. LAHD FACETS:
- 2 - Swamps, sulfohemists 30Z
-3- Swamps, sulfaquents, 10X
-4Interfluves:
2 9 . FRAGMERATIGB: Valleys:
30. RELIABILITY:
1= reliable, 2= probable, 3= tenable, 4= plausible
lO.b : 1 12.a: 1
14.a: 2
14.b: 3
17: 1
18.a: 1
18.b: 2
18.c: 1
18.d-q: 1
19: 2
22: 1
23: 2
24: 1
28: 2
29:
3 1 . ADDITICHAL BOTES :
1112 - 55
IAEP-S0B4, CSR'BGGOR
KAP SttfGS:
1.
4.
5.
6.
U B D EBIT: Bf.5.2
2. M&P SSEEÏ: 1112
3. AREA: 629 km2
««jumnmuiii by FROTH5CE: Sumatera Selatan: 84%, Lampung: 162
STATUS IDEHTIFTEHS
: Updated by: AH
edit date: 18/04/89
Status: Final
leSD OBIT DESCBIPnCH. Saline backswamps with mixed forest, fine sediments (unripe).
7. SATELLITE SCEHES
8. &EBIAL FBOTOGBAPHS
9. BâDâB
10. PAHBJT MUraBTAt.
a. Weathering
b. Lithology
c. Formation
12. H&TEB
a. Quality
b. Source
13.
14.
15.
16.
:
:
:
:
FISHERIES
:
RIVERS a. Floodrisk :
b. Inundation:
VEGETATTOH/LAHD USE :
Area used
:
ACCELERATED EROSICH
a. Occurence :
b. Evidence :
123/63/23/03/83, 123/62/23/03/83
1:100.000
62 /8293-187, 63A /8284-157, 62 /8293-117
STAR-I/250/88/1112-2,3
11. BOCK GO7CSQP:
clay
Qal
Saline
Rain
Rawa (swamp)
None
Medium Tidal Range
swamp forest (rawa), bush, swamp (rawa) including sedges
0X
None
17. SOIL GREAT GROUP
Dominant >50I
Associated 1
Associated 2
Classification
tropohemists
Z of area
65 %
hydraquents
32. REPRESENTATIVE PROFILES:
het/
/112-57 /79/F /1112/21/
35 X
/67 /
eqw/
1112 -
56
Lab. checked
yes
yes
/87/ES/1112/21/
/160/
isncs
Properties
a. TmlJiire:
b.
c.
d.
e.
t.
g.
h.
i.
j.
k.
1.
m.
n.
o.
p.
q.
r.
topsoil
subsoil
Depth:
peatsoil
•im uralsoil
Drainage:
topsoil
Erch. K:
subsoil
Total K2O: topsoil
subsoil
•ethod
Avail. P:
topsoil
subsoil
topsoil
Total P:
subsoil
topsoil
CBC pH 7
subsoil
Soil Reaction:topsoil
subsoil
topsoil
Al Sat.
subsoil
Al taxicity :
Acid salpta. pot.:
Salinity :
Other Toxicity:
Soot obstr.. layer :
Organic Matter :
TEB :
Total observations:
Dominant > 501
organic
organic
very deep
__
Very poorly drained
high
very high
—
-----very high
very high
very strong acid
strong acid
very low
very low
—
very deep
saline
-130 cm
22.0
44.4
0
Associated 1
fine
fine
-very deep
Very poorly drained
high
medium
very high
high
Olsen
medium
low
high
medium
high
high
very strong acid
very strong acid
very low
very low
-—
saline
-110 cm
14.9
17.7
0
Associated 2
0.0
0.0
0
IS. ALTITUDE:
2 0 . FLAB/PROFILE:
8 m
Minimus:
1m
Range:
5 m
Dominant: No pronounced highs/lows
Included:
b. density:
2 1 . L.n. DBADUGE: a. Pattern: none
c. Variability:
b. Variability: Low
2 2 . fff A fm *
a. Steepness:flat
c. Length:
d. Variability:
e. Curvature:
2 3 . SLOPE DISTH. :
Valleybottons: 100 X
Interfluves : 0-81:0 X, 9-251: 0 X, 25-551: 0 X
2 4 . RELIEF AMPLI.: a. Amplitude: very low
b. Variability: Low
2 5 . TBPPATT»Flat, slope <2X, 0-50 m
2 6 . CSEST/RIDSES:
a. Shape: no crests
b. Length:
c. Variability:
d. Width:
e. Variability:
a. Width:
b. Variability:
2 7 . VALLEY FLOOR:
-1- Swamps, tropohemists, 65X
2 8 . LAID FACETS:
- 2 - Swamps, hydraquents, 35X
-3-429. FRAGMEaTATIGH: Valleys:
Interfluves:
30. RELIABILITY:
1- reliable, 2- probable, 3- tenable, 4- plausible
lO.b : 1 12.a: 1
14.a: 1
14.b: 2
17: 2
18.a: 2
18.b: 2
18.c: 1
18.d-q: 2
19: 1
22: 2
23: 2
24: 1
28: 3
29:
31. ADDITIONAL BOTES: All representative profiles are extrapolated from other L.U
1112 - 57
I ATI HUIT REFOBT
LR£P~SQBH, GSR~B060R
MAP HUGE:
CSOSS SECTIGH:
B,5. 2
D.2.1.2
B.4.2
B.5.3
B.I.I
tidal creed!
X
X'
tv:-::y,,i icoarse'terture
Ij-g-"^! fine teiture
1. LAHD tffllT: Bf.5.3
2. M&P SHEET: 1112
3. AREA: 104 km2
4. «»JJIKHK-E by FBOVIBCE: Sumatera Selatan: 55%, Lampung: 45!
5. SI&IOS nJEHTIFIERS
: Updated by: AH
adit data: 04/03/89
Status: Final
6. LAUD UBIT DESCKIFTICB: Forested tidal levees along tributaries, fine sediments (unripe).
7.
8. AFBTAT. PBOIOGBAFBS
9. RADAR
10. EAREWT MOTBPTAT.
12.
13.
14.
15.
a. Haathering
b. Lithology :
c. Faxaatian :
HATER
a. QnaUty :
b. Source :
FISHERIES
:
RIVERS a. Floodrisk :
b. Inundation
VBSETATIOB/LABD BSE
Area used
16. ACCELERATED EROSICB
123/63/23/03/83
1:100.000
61 /8293-11
START1/250/88/1112-2
11. ROCK OUTCROP:
clay
Qal
Saline
Rain
Rawa (swamp)
None
Permanent
riparian forest of meander belt, bush
0!
a. Occnrence
None
b. Evidence .:
17. SOIL GREAT GROUP
DoB±nant >50Z
Associated 1
Associated 2
Classification
sulfaquents
hydraquents
fluvaquents
X of area
60 X
30 X
10 X
32. REPRESENTATIVE PROFILES:
eqi/
/112-32 /79/F /1112/21/ /042/
eqv/
/112-66 /79/F /1112/21/
/76 /
1112 - 58
eqw/
Lab. checked
yes
yes
yes
/112-43
/79/F /1112/21/
/043/
1« «cm, rm»*rna»TRTTrs
Properties
a. Texture:
topsoil
subsoil
b. Depth:
peatsoil
miitw*! *ni l
—
extremely deep
c. Drainage:
d. Exch. K:
Very poorly drained
high
topsoil
subsoil
very high
---
e. Total K2O: topsoil
subsoil
f. Avail. P:
method
topsoil
g. Total P:
h. CEC pH 7
Associated 1
fine
fine
--
Associated 2
fine
fine
—
very deep
Very poorly drained
very deep
high
medium
high
Poorly drained
medium
---
---
subsoil
—
--
—
--
---
topsoil
subsoil
---
---
—
--
topsoil
high
high
high
subsoil
very high
high
very strong acid
strong acid
high
very low
very low
very low
—
i. Soil Reaction:topsoil
subsoil
j. Al Sat.
Dominant > 501
fine
fine
topsoil
subsoil
excessive acid
extreme acid
very low
low
excessive acid
excessive acid
k. Al toxicity :
no
very low
—
1. Acid sulph. pot.:
m. Salinity :
very shallow
moderately deep
moderately deep
n. Other Toxicity:
salt free
—
salt free
—
salt free
--
o. Boot obstr. layer :
p. Organic Matter :
216 cm
31.A
120 cm
12.8
120 cm
5.6
q. TEB :
17.5
4
31.2
12
13.5
4
r. Total observations:
19. ALTITUDE:
2 0 . FLAM/PROFILE:
21.
a.
c.
a.
c.
L.O.
2 2 . SLOPE:
23.
SLOPE DISTK.:
2 4 . BELIEF AHPLI.:
2 5 . ram ATM 2 6 . C8EST/BTXJGES:
2 7 . VALLET FLOOR:
28.
12 m
LAID FACETS:
8m
10 m
Dominant: No pronounced highs/lows
Included:
b . density:
Pattern: meandering
Variability:
Steepness:flat
Length:
b . Variability: Low
d. Variability:
e. Curvature:
Valleybottoms: 100 %
Interfluves : 0-81:0 X 9-251: 0 X, 25-551: 0 X
a. Amplitude: very low
b . Variability: Low
Flat, slope <2%, 0-50
a. Shape: no crests
b . Length:
c. Variability:
e. Variability:
d. Width:
a. Width:
b . Variability:
- 1 - Levees, sulfaquents, 60%
~Z~ Backswamps, hydraquents, 30Ï
- 3 - Backswamps, fluvaquents, 10X
29. FBAGMEHTATIOH:
30. RELIABILITY:
lO.b
-4Valleys:
1- reliable,
Interfluves:
2 - probable,
3= tenable,
:1
12.a: 1
14.a: 1
14.b: 2
17: 1
18.a: 1
18.d-q: 2
19: 1
22: 1
23: 2
24: 1
28: 2
31. ADDITIOKAL BOIES:
1112 - 59
4= plausible
18.b: 2
29:
18.c: 1
LREP-SDBM. CSB-BOQGR
u m m t REPORT
MftP DttGE:
D.
B.5 .1
B.5.4
B.5.3
2 1.2
$
>
ni
9M
B
B.
5.1
5.4
B .1. 1
^>»
Potensial acid sulfît
1.
LAHD
raiT:
Bf.5.4
2. HUP SHEET: 1112
3. AREA: 391 km2
4 . OCCnREBCE b y HttJVJÜUE: Sumatera Selatan: 99Z
5 . SX&IDS | l^fflfT| yI ^ P S
• Updated by: AH
edit date: 04/03/89
Status: Final
6 . LAND OBIT DESCRIPTIOH: Mixed open swamps vegetation with gelarn trees, fine sediments
(unripe).
7. SATELLITE «-HM ist
8. AffBTAf. WinijPAPHg
9. BADAR
10. FAREST HUTERTAf.
a. Heathering
b. Lithology
c. Fomatian
HATER
a. Quality
12.
b. Source
:
;
:
:
:
:
:
:
123/62/23/03/86, 123/63/23/03/83
1:100.000
062 /8293-105, 061 /8293-27 , 061 /8293-17
START1/250/88/1112-2.3
11. SOCK OUTCROP:
X
Slight
clay
Qal
Saline
Rain
Rawa (swamp)
None
Permanent
gelam forest (brackish, bush, swamp (rawa) including sedges
0 %
13. FISHERIES
:
1*. RIVERS a. Floodriak :
b. Inundation :
15. VEGEIATICB/LAHD USE :
Area used
:
16. ** ' "Kl JtRAT*1-1 ' U M IM I'fW
a. Occorence : None
b. Evidence :
17.
SOIL GSEAT GBODP
DoBinant >50I
Associated 1
Associated 2
:
Classification
hydraquents
sulfihemists
tropaquents
32. ItWItlgtBfTATIWH EBUF1LES:
eqw/
/112-7 /79/P /1111/53/
eqt/
/112-12 /79/P /1111/53/
X of area
80 X
15 Z
5 Z
/07 /
/12 /
hei/
1112 -
60
Lab. checked
yes
yes
yes
/112-15
/79/P /1111/53/
/15
isncs
18.
Properties
&. Tttztnx9:
b. Depth:
topsoil
subsoil
peatsoil
•dn n > T »l «>{ 1
c. Drainage:
topsoil
d. Exch. K:
subsoil
e. Total K20: topsoil
subsoil
•ethod
£. Avail. F:
topsoil
subsoil
topsoil
g. Total F:
subsoil
h. CEC pH 7
topsoil
subsoil
i. Soil Reaction: topsoil
subsoil
topsoil
j. Al Sat.
subsoil
k. Al taxicity :
1. Acid sulph.. pot.:
•. Salinity :
n. Other Tazicity:
o. Boot obstr . layer :
p. Organic Hatter :
q. TEB :
r. Total observations:
Donnant > SOX
moderately fine
moderately fine
—
very deep
Very poorly drained
high
medium
—
Associated 1
organic
organic
extremely deep
Very poorly drained
very low
medium
----—
--
—
—
__
-very high
high
strong acid
excessive acid
—
—
—
not relevant
--—
8.3
13.7
0
high
high
excessive acid
excessive acid
—
—
—
shallow depth
•
-—
15.7
3.2
0
Associated 2
moderately fine
medium
-very deep
Very poorly drained
high
high
--—
---very high
very high
very strong acid
excessive acid
—
—
—
-—
-—
4.7
40.6
0
Bange:
3 m
7 m
Minima:
1 m
Doninant: No pronounced highs/lows
PLAR/PBOFILE:
Included:
a. Pattern: none
b. density:
L.O. DBAIBAGE: c. Variability:
b. Variability: Low
a. Steepness:flat
c. Length:
d. Variability:
e. Curvature:
Valleybottons: 100 %
SLOPE DISTR.:
Interfluves : 0-81:0 %, 9-25Ï: 0 X, 25-55X: 0
BELIEF AMPLI.: a. Amplitude: very low
b. Variability: Low
TBBPÄTWFlat, slope <2I, 0-50 m
CREST/RIDGES:
b. Length:
c. Variability:
a. Shape: no crests
e. Variability:
d. Width:
b. Variability:
VALLET FLOOR:
a. Width:
-1- Swamps, hydraquents, BOX
LAID FACETS:
-2- Swamps, sulfihemists , 15*
-3- Swamps, tropaquents, 5X
-4Interfluves:
FBAGMBBIATICH: Valleys:
19. ALTITUDE:
20.
21.
22.
23.
24.
25.
26.
27.
28.
29.
30. RELIABILITY:
1= reliable, 2= probable, 3» tenable, 4- plausible
lO.b : 1 12.a: 1
14.a: 2
14.b: 3
17: 2
18.a: 2
18.b: 2
18.c: 2
18.d-q: 2
19: 1
22: 2
23: 2
24: 1
28: 2
29:
31. AUDITIUHAL KITES: All representative profiles are extrapolated from other L.U
1112 -
61
LREP-SDBM, CSB-BOGOB
TJHTO
C80SS SECnOH:
MAP WEGE:
Mq.1.0
.»alley bottoi
valleybottn
]
inter
flure
ioterflure
'iaterflute
] cous« saüienUry rocks
1 fine sediientiry rocks
2. MAP SHEET: 1112
3. AREA: 154 km2
1. LAUD ORIT: Pfq.1.0
4. urmiuiu»;« by EBOTIBCE: Sumatera Selatan: 97%, Lampung: 3%
edit date: 06/03/89
Status: Final
5. STATUS IDENTIFIERS
: Updated by: AH
6. LAHD OBIT DESCRIPTICH: Not dissected flat plain fine and coarse felsic sedimentary rocks,
7. SATELLITE
8. AERIAL PHOTOGRAPHS
9. RADAR
10. BAREST MATERIAL
a. Weathering
b. Lithology
c. Formation
slopes
0-3%
123/63/23/03/83, 124/62/23/03/85
59 /8316-97 , 61 /8293-15 , 59 /8316-99
: 1:100.000
: STAR-1/250/88/1010-2,3
11. RGCK OUTCROP:
: High
: claystone, sandstone,
: Tppp , Qal
t
12. HATER
a. Quality : Fresh
b. Source : Shallow wells
13. FISHERIES
: None
1«. RIVERS a. Floodrisk : None
None
IS. VBEETATIOB/LABD OSE : swamp forest (rawa), secondary forest, bush, alang-alang, upland
crops, rubber (karet), towns, villages
Area used
: 60 %
ACCELERATED EROSICH
a. Occurence : Localised
b. Evidence : Various
17. SOIL GREAT GBOOP
Doainant >50I
Associated 1
Associated 2
37.
udh/
ity/
/
/
:
Classification
kanhapludults
tropaquepts
Z of area
55 %
30 I
15 %
dystropepts
/88/HJ/1112/23/
/88/HK/1112/43/
iqt/-
/185/
/134/
1112 - 62
Lab. checked
yes
yes
yes
/84-4
/86/SR/1112/12/
/10 /
xsncs
is. son. c
Pi upti Li. o
«. Tartare:
Dcsdnant > 501
moderately fine
fine
topsoil
sabsoil
peatsoil
b . Depth:
sdneralsoil
c. Drainage:
d. Each. K:
topsoil
sabsoil
e. Total K2O: topsoil
sabsoil
£. Avail. F:
snthod
topsoil
sabsoil
g. Total F:
topsoil
sabsoil
h. CBC p H 7
topsoil
sabsoil
i. Soil Reaction:topsoil
sabsoil
j. A l Sat.
topsoil
sabsoil
k. A l taxicity :
1. Acid salph. pot.:
•. Salinity :
n. Other Toxicity:
o. Boot obstr. layer :
p . Organic Matter :
q. TEB :
r. Total observations:
Associated 1
fine
fine
very deep
deep
Well drained
associated 2
moderately fine
moderately fine
very deep
Well drained
low
Very poorly drained
low
very low
low
very low
very low
low
very low
Bray I
low
very low
Bray I
very low
very low
Bray I
low
very low
very low
very low
very low
medium
very low
very low
very low
very low
very low
high
very low
very low
medium
excessive acid
very strong acid
high
very low
very high
no
very high
no
not relevant
not relevant
excessive acid
excessive acid
high
high
no
not relevant
low
very low
excessive acid
excessive acid
high
salt free
140 cm
1.6
0.5
0
100 cm
5.6
0.8
0
30 m
19. ALTITUDE:
Mini—-
io m
60 cm
1.5
0.7
0
Bange:
15 m
D a n s a n t : No pronounced highs/lows
20. FLAI/FBOFILE:
21. L.0. DBAIHAGE:
22. SLOPE:
23. SLOPE DISTR.:
24. RELIEF AMPLI.:
25. TPmtATM26. C8EST/BIDGES:
27. VALLEY FLO0B:
28. T-*"n FACETS:
Included: non-linear and random > 60Z of area flat-topped
b . density: Very low
a. Pattern: dendritic
c. Variability: low
b . Variability: Low
a. Steepness:flat
d. Variability: Low
c. Length: extremely
e. Curvature: convex
ValleybottOBS: 30 X
InterCLuves : 0-81:70 i, 9-251: 0 Ï, 25-551: 0 Z
b . Variability: Low
a. »ill il ml«: very low
Flat, slope <2X, 0-50 m
c. Variability:
a. Shape: no crests
b. Length:
d. Width:
a. Width: very narrow
e. Variability:
b. Variability: Low
- 1 - Interfluves, kanhapludults, 55Ï.
-2~ Depressions, tropaquepts, 25t
- 3 - Interfluves, dystropepts, 15Ï
29. FBAGMBITATiaa:
30. RELIABILITY:
lO.b
- 4 - Valley bottoms, tropaquepts, 5Z
Valleys:
Interfloves: Large blocks
1= reliable,
2 = probable,
3 " tenable,
:2
12.a: 1
14.a: 1
14.b: 2
17: 2
18.a: 2
18.d-q: 2
19: 2
22: 2
23: 2
24: 1
28: 2
4= plausible
18.b: 1 18.c:
29: 2
31. ADDITIOBAL BOTES: All representative profiles are extrapolated from other L.U
1112 - 63
LREP-S0BM, CSR-BQSGR
LAID O U T UKHBIT
CSOSS SECÎTCB:
MAF IMAGE:
PfiJ.2.0
valley bottoi
inUrfluve |
valley bottoi
|
iJiterfluve
interflure
coarse sediaeatary rocks
~^T| fine sediaentary rocfcs
1.
LAB) t H I T :
2. MAF SHEET: 1112
Pfq.2.0
3. AREA: 406 km2
4 . (UJIRMCE b y FBOVIBCE: Sumatera Selatan: 99%
5.
STATDS IDENTIFIERS
:
Updated by: AH
edit date: 15/03/89
Status: Final
6 . LAHD DHIT DESCRIFTHK: Not dissected flat to undulating plain fine and coarse felsic
sedimentary
rocks, slopes 0 - 8%
123/63/23/03/83, 123/62/23/03/86
1:100.000
60 /8341-65 , 60 /8341-73
8 . AERIAL PBOTOGSAFflS
:
9 . BADAR
: STAR-1/250/88/1112-2,6
10. PARERT MATERIAL
11. BOCK GOTCBQP:
Z
a. Heather ing : High
b. Litbology : claystone, sandstone,
c. Fonaaticm : Tppp , Tmpl
12. HATER
a. Quality : Fresh
b. Source : Perennial River
13. FISHERIES
: None
14. RIVERS a. Floodrisk : None
b. Xnnndafcioii: None
15. VBGEIATIOB/LAro OSE : secondary forest, bush, alang-alang, shifting cultivation, upland
crops, rubber (karet), towns, villages
Area used
: 85.X
16. ACCELERATED EROSIGH
a. Occurenco : Localised
b. Evidence : Various
7 . SATELLITE SCEHES
:
17. SOIL GBEAT G8ODP
Daninant >SOZ
Associated 1
Associated 2
Classification
kanhapludults
dystropepts
tropaquepts
Z of area
60 X
30 X
10 X
Lab. checked
yes
yes
yes
32. PFCTIKKMITATIVK PROFILES:
udh/
/
/88/HJ/1112/23/
/185/
iqt/
784-4
/86/SR/1112/12/
/10 /
ity/
1112 ' 64
/88/HK/1112/43/
/134/
Dominant > SOZ
moderately fine
fine
-b. Dapth:
gpf n s r s l «il 1
very deep
Well drained
c. Drainas»:
low
d. Ezch. K:
topsoil
subsoil
very low
very low
e. Total K20: topsoil
very low
sabsoil
Bray I
f. Avail. P:
Method
low
topsoil
very low
sabsoil
very low
g. Total P:
topsoil
sabsoil
very low
h. CEC pH 7
topsoil
very low
very low
sabsoil '
i. Soil Reaction: topsoil excessive acid
sabsoil excessive acid
high
j. Al Sat.
topsoil
high
sabsoil
no
k. Al taxicity :
1. Acid salph. pot.:
not relevant
—
•. Salinity :
-n . O t h e r TaatiLcity:
o. Soot obstr. layer :
140 cm
p. Organic Matter :
1.6
q. TUB :
0.5
0
r. Total observations:
Properties
a. Tartar«:
Associated 1
moderately fine
moderately fine
—
very deep
Well drained
low
very low
low
very low
Bray I
low
very low
very low
very low
very low
very low
excessive acid
excessive acid
high
very high
no
not relevant
--60 cm
1.4
0.7
0
topsoil
sabsoil
psatsoil
Associated 2
fine
fine
—
deep
Very poorly drained
low
low
very low
very low
Bray I
very low
very low
medium
very low
high
medium
excessive acid
very strong acid
high
very high
no
not relevant
salt free
-100 cm
5.6
0.8
0
19. AUITUDE:
50 m
Minima:
10 m
Range:
20 m
Dominant: non-linear and random > 60Ï of area flat-topped
20. PLAI/PBOFILE:
Included: No pronounced highs/lows
a. Pattern: dendritic
b. density: Very low
21. L.O. IKAHUGE: c. Variability: low
a. Steapness:gently sloping
b. Variability: Low
22. SLOPE:
c. Length: extremely
d. Variability: Low
e. Curvature: convex
23. SLOPE DISTR.: ValleybottoBs: 10 !
Interleaves : 0-8Z:85 I, 9-251: 5 X 25-55X: 0 X
24. RELIEF AMPLI.: a. Amplitude: low
b. Variability: Medium
25. TETOAT»Undulating 2- 8Z, 0-50 m
26. CREST/RIDGES:
a. Shape: no crests
b. Length:
c. Variability:
d. Width:
e. Variability:
27. VALLET FLOOR:
a. Width: narrow
b. Variability: Low
28. LAID FACETS:
-1- Interfluves, kanhapludults, 60Ï
- 2 - Interfluves, dystropepts, 30X
-3- Valley bottoms, tropaquepts, 10X
-4Interfluves: Large blocks
29. FRAGMBRATIOB: Valleys: Small blocks
30. Rfg.TAHn.TTT:
lO.b : 1 12.a: 1
U.d-q: 2
19: 2
» reliable, 2= probable, 3- tenable, 4 s plausible
18.b: 1
18.c:
14.a: 1
14.b: 2
17: 2
18.a: 1
29: 2
22: 2
23: 2
24: 1
28: 2
31. ADDITIOBVU. BOTES: All representative profiles are extrapolated from other L.U.
1112 -
65
T-AWl Q8IT
LHEP-SDW, CSR-BOGGB
C80SS SECTIOH:
MAP IMAGE:
Pfq.2.1
interfluve
interfile
valley bottoi
1
I
I
I jcoarse scdiKntjry rocks
1 if b e sedi«entary rocks
2. MAP SHEET: 1112
3. AREA: 1403 km2
1. LAID ÜHIT: Pfq.2.1
4. nrrnnnMTR by PROVINCE: Sumatera Selatan: 94!, Lampung: 6Ï
Updated by: AH
edit date: 13/04/89
Status: Final
5. STATUS
6. LAHD OBIT DESCRIPTICH: Slightly dissected flat to undulating plain fine and coarse felsic
sedimentary rocks, slopes 0 - 8 1
124/62/23/03/85, 123/63/23/03/83
7. SATELLITE
8. AERIAL PBOTOG8APBS
9. RADAR
10. PARERT HATERTAf.
a. Weathering
12.
13.
14.
15.
b. Litbology
c. Formation
HATER
a. Quality
b. Source
FISHERIES
RIVERS a. Floodrisk
b.
VBGETATim/LAHD OSE
1:100.000
60 /8341-75 , 58
STAR-1/250/88/1112-6,3
/8316-59 , 62
/8293-111
11. BOCK OOTC8QP:
I
High
claystone, sandstone
Tppp , Tmpl
Fresh
Shallow wells
None
None
None
secondary forest, bush, alang-alang, shifting cultivation, upland
crops, rainfed wetland rice, rubber (karet), towns, villages
Area axed
16. ACCELERATED EROSIOH
a. Occorence
b. Evidence
85 Ï
Localised
Various
17. SOIL O E A T GSOOP
Associated 1
Classification
kanhapludults
dystropepts
Associated 2
tropaquepts
Damnant >5OI
X of area
60 X
25 Ï
15 X
Lab. checked
yes
yes
yes
32. mtwoMiatTATivg fBOFTLES:
udh/
iqt/
/
/84-4
/88/HJ/1112/23/
/86/SR/1112/12/
ity/
/185/
/10 /
1112 - 66
/88/HK/1112/43/
/134/
18. SOIL CHARACTERISnCS
Properties
Dcadnant > 501
a. Textare:
topsoil
moderately fine
subsoil
fine
b. Depth:
peatsoil
very deep
Well drained
Drainage:
low
Exch. K:
topsoil
very low
subsoil
Total K2O: topsoil
very low
subsoil
very low
Avail. P:
aethod
Bray I
topsoil
low
subsoil
very low
topsoil
very low
8- Total F:
subsoil
very low
topsoil
very low
b. CEC pH 7
subsoil
very low
i. Soil Reaction:topsoil excessive acid
subsoil excessive acid
Al
Sat.
topsoil
high
jsubsoil
high
no
k. Al taxicity :
not relevant
1. Acid sulph. pot.:
Salinity :
n. Other Toxicity:
140 cm
o. Root obstr. layer :
1.6
P- Organic Matter :
0.5
q- TEB :
r. Total observations:
1
Associated 1
moderately fine
moderately fine
Associated 2
fine
fine
very deep
Well drained
low
very low
low
very low
Bray I
low
very low
very low
very low
very low
very low
excessive acid
excessive acid
high
very high
no
not relevant
deep
Very poorly drained
low
low
very low
very low
Bray I
very low
very low
medium
very low
high
medium
excessive acid
very strong acid
high
very high
no
not relevant
60 cm
1.5
0.7
3
100 cm
5.6
0.8
0
50 m
Minima:
10 m
Range:
30 m
Dominant: non-linear and random > 60X of area flat-topped
FLAH/PfiOFIlE:
Included:
a. Pattern: dendritic
b. density: Low
L.O. DBAWGE: c. Variability: low
a. Steepness:gently sloping
b. Variability: Low
SLOPE:
c. Length: extremely
d. Variability: Low
e. Curvature: convex
SLOPE DISTR.:
Valleybottons: 10 %
Interfluves : 0-81:85 % 9-25X: 5 %, 25.-55X: 0 X
b. Variability: Low
RELIEF AMPLI.: a. Amplitude: low
TKHKÀTWUndulating 2- 8%, 0-50 m
c. Variability:
CREST/RIDGES:
a. Shape: no crests
b. Length:
d. Width:
e. Variability:
a. Width: narrow
b. Variability: Low
VALLET FLOOR:
-1- Interfluves, kanhapludults, 60X
LAflD FACETS:
-2- Interfluves, dystropepts, 25%
-3- Valley bottoms, tropaquepts, 15Ï
-4FR6GHEHTATIO8: Valleys: Small blocks
Interflnves: Large blocks
19. ALTITUDE:
20.
21.
22.
23.
24.
25.
26.
27.
28.
29.
30. RELIABILITY:
1= reliable, 2= probable, 3° tenable, 4= plausible
18.b: 1
18.c: 1
lO.b : 1 12.a: 1
14.a: 1
14.b: 2
17: 2
18.a: 2
22: 2
23: 2
24: 1
28: 2
29: 2
18.d-q: 2
19: 2
31. ADDITIOBAL BOTES: The representative profile for Tropaquepts is extrapolated from ot
her L.U.
1112 -
67
, CSR~BOQQR
LARD tnrrr EERST
CSOSS SECTIOH:
MAP IMAGE:
dPfq.2.1
valley bottoi
interfluve
1
interfluve
coarse sediœntary rocks
fine seditentary rocks
1.
4.
5.
6.
7.
8.
9.
10.
12.
13.
14.
LAHD OMIT: dPfq.2.1
2. MAP SHEET: 1112
3. AREA: 227 km2
OOCHREHCE by PB0VXHCE: Sumatera Selatan: 99Z
edit; dat«: 13/04/89
Status: Final
STATES IDEBTIFIERS : Updated by: AH
LAHD DBIT DESCHIPTICH: Slightly dissected flat to undulating plain fine and coarse
sedimentary rocks covered by acid tuffs,slopes 0-8X.
124/62/23/03/85
SATELLITE
58 /8316-71 , 58 /8316-67
AERIAL PBOTOG8APBS : 1:100.000
RADAR
: STAR-1/250/88/1112-2,3'
11. ROCK OTTC80P: %
PARBR MATERIAL
a. Weathering : High
b. Lithology : claystone, sandstone, dacite
c. Fomat-ion : Tpp
, Qrv
HATER
a. Quality : Fresh
' b. Source : Medium wells
FISHERIES
: None
RIVERS a. Floodrlsk : None
b. Immdatxan: None
15.
VEGETATIGH/LAHD OSE : , bush, alang-alang, shifting cultivation, upland crops, rainfed
wetland rice, rubber (karet), banana, towns, villages
Area used
: 80 %
16.
ACCELERATED EROSIGH
a. Occurenc« : Localised
b. Evidence : Various
17.
SOIL G8EAI GROUP
Donnant >SOZ
Associated 1
Associated 2
Z of area
60 2
25 X
15 X
Classification
kanhapludults
dystropepts "
tropaquepts
32. BKWKKETATIUK PROFILES:
udh/
/
/88/UA/1112/13/
iqt/
/106-1
/82/P /1112/11/
/171/
/24 /
ity/
1112 -
68
Lab. checked
yes
yes
yes
/•106-2
/82/P /1112/11/
/6
/
Dominant > SOZ
moderately fine
fine
b. Depth:
—
-—
c. Drainage:
low
d. Exch. K:
topsoil
subsoil
low
very low
a. Total K2O: topsoil
subsoil
very low
Olsen
f. Avail. P:
method
topsoil
medium
subsoil
very low
very low
g. Total P:
topsoil
subsoil
very low
b. CEC pH 7
topsoil
low
subsoil
very low
1. Soil Baactian:topsoil excessive acid
subsoil very strong acid
j. Al Sat.
topsoil
medium
subsoil
high
k. Al toxicity :
no
1. Acid sulph. pot. :
not relevant
-m. Salinity :
-n. Other Toxicity:
120 cm
o. Boot obstr. layer :
0.8
p. Organic Matter :
q. TES :
0.8
3
r. Total observations:
Properties
a. Texture:
topsoll
subsoil
peatsoil
Associated 1
fine
fine
Associated 2
fine
fine
very deep
Imperfectly drained
low
low
very low
very low
Bray I
very low
very low
very low
very low
low
low
excessive acid
excessive acid
high
high
no
not relevant
—
very deep
Poorly drained
medium
medium
low
very low
Bray I
very high
medium
low
very low
medium
low
very strong acid
excessive acid
low
medium
no
not relevant
salt free
120 cm
1.3
0.4
1
120 cm
5.0
1.1
1
19. ALTITUDE:
10 m
Bange:
35 m
55 m
Donnant: non-linear and random > 60% of area flat-topped
20. PLAI/PBOFILE:
Included:
b. density; Low
a. Pattern: dendritic
21. L.O. DBAIHAGE: c. Variability: low
a. Steepness:gently sloping
ng
b. Variability: Medium
22. SlJQPB:
d. Variability: Low
c. Length: extremely
e. Curvature: convex
23. SLOPE DISTR. : Valleybottons: 15 X
Inter£Loves : 0-8Z:80 % 9-25Z: 5 X, 25-55Z: 0 %
24. BELIEF AMPLI.: a. Aaplitode: low
b. Variability: Medium
Undulating 2- SX, 0-50 m
25. TERRAIN:
26. < 3MWÏT/BIIMJMRa. Shape: no crests
c. Variability:
b. Length:
a. Variability:
d. Width:
b. Variability: Low
27. VALLEY FLOOR:
a. Width: narrow
-1- Interfluves, kanhapludults, 60%
28. LAID FACETS:
-2- Interfluves, dystropepts, 25%
-3- Valley bottoms, tropaquepts, 15%
-429. FBAGMEHTAIIGH: Valleys: Small blocks
Intorfloves: Large blocks
30. BEUABILITÏ:
1° reliable, 2» probable, 3» tenable, 4> plausible
18.b: 1
18.c: 1
lO.b : 2 12.a: 1
14.a: 1
l*.b: 2
17: 2
18.a: 1
22: 2
23: 2
24: 1
28: 2
29: 2
U.d-q: 2
19: 1
31. ADDITIGBAL BOTES:
1112 -
69
T-A«n nBIT REPORT
LREP-SDBM. CSR-BOSOR
CBOSS SECTICB:
MAP IMAGE:
Pfq.3.1
(undiff).top
(radiff).top
1
1
I
=n
I coarse sediwntary rocks
I - - - - I fine sediientary roots
l : und. top
2 : slope
3 :valley botton
2. MAP SHEET: 1112
3. AREA: 632 km2
LAND t f f l l T :
Pfq.3.1
4. OCCOREHCE by HtOVIKE Sumatera Selatan: 76%, Lampung: 24%
5. STATUS IDEHTIFIEKS
Updated by: AH
edit date: 18/04/89
Status: Final
6. LAHD nHIT DESCRIPTICH Slightly dissected undulating plain fine and coarse felsic
sedimentary rocks, slopes 3-8Z.
7. SATELLITE SCEHES
123/63/23/03/83, 124/62/23/03/85
8. AERIAL PHOTOGRAPHS
1:100.000
61 /8293-17 , 58 /8316-57 , 60 /8341-79
9. 8ADAR
STAR-I/250/88/1112-3,6
10. BAREST MATERIAL
11. ROCK OUTCROP:
2
a. Heatherins
High
b. tAthology
claystone, sandstone,
c. Formation
Tppp , Tmpl
12. HATER
a. Quality
Fresh
b. Source
Medium wells
13. FISHERIES
None
14. RIVERS a. Floodrisk
None
b. Inundation: None
15. VBGETATIOB/LAHD OSE
secondary forest, moist primary lowland forest, bush, alang-alang,
shifting cultivation, upland crops, mixed gardens of fruit trees,
rubber (karet), towns, villages
Area used
80 X
16. ACCELERATED EROSIGH
Common
a. Occnrence
b . Evidence
Various
1.
17. SOIL GBEAT GROUP
Dominant >50I
Associated 1
Associated 2
Classification
kanhapludults
dystropepts
tropaquepts
32. REPRESERAnVE PROFILES:
udh/
/
/88/NR/1112/11/
iqt/
/84-4
/86/SR/1112/12/
Z of area
65 %
30 %
5X
ity/
/100/
/10 /
1112 -
70
Lab. checked
yes
yes
yes
/88/UA/1112/11/
/191/
18.
a. Textare:
t.
c.
d.
e.
f.
g.
h.
i.
j.
k.
1.
•.
n.
o.
p.
q.
r.
topsoil
subsoil
Depth:
peatsoil
•dnaralsoil
Drainage:
Exch. K:
topsoll
subsoil
Total K2O: topsoil
subsoil
Avail. P:
aethod
topsoil
subsoil
Total P:
topsoil
subsoil
CEC pH 7
topsoil
subsoil
Soil Reaction:topsoil
subsoil
Al Sat.
topsoil
subsoil
Al toxicity :
Acid sulph. pot.:
Salinity :
Other Toxicity:
Boot obstr. layer :
Organic Matter :
TEB :
Total observations:
19. AUITODE:
20. PLAW/PBOFILE:
21. L.O.
22. SLOPE:
23. SLOPE DISTR.:
24. BELIEF AHEU.:
23. TERRAIN:
26.
DoBdnant > 501
moderately fine
fine
-deep
Well drained
very low
very low
very low
very low
Bray I
low
very low
very low
very low
very low
very low
excessive acid
excessive acid
high
high
no
not relevant
-- '
—
—
1.5
0.6
1
Asitoriateri 1
moderately fine
fine
—
deep
Well drained
low
low
low
very low
Bray I
very low
very low
very low
very low
low
low
excessive acid
excessive acid
medium
very high
no
not relevant
-—
—
0.8
1.0
0
Associated 2
fine
fine
—
deep
Very poorly drained
low
low
very low
very low
Bray I
very low
very low
medium
very low
high
medium
excessive acid
very strong acid
high
very high
no
not relevant
salt free
—
—
5.6
0.8
1
10 m
Bange:
30 m
75 m
t: non-linear and random > 60X of area flat-topped
Included:
b. density: Low
a. Pattern: dendritic
c. Variability: low
b. Variability: Low
a. Steepness:gently sloping
d. Variability: Medium
c. Length: long
e. Curvature: convex
ValleybottoBs:
5 X
Interflaves : 0-81:80 Ï , 9-25Z: 15 Z, 25-551: 0 X
a. flpjuiilmin: low
b. Variability: Low
Undulating 2- SX, 0-50 m
b. Langth:Moderately long
a. Shape: Level
c. Variability: Low
e. Variability: Low
d. Hidtb: moderate .
27. VALLET FLOOR:
a. Width: very narrow
b. Variability: Low
28. LAID FACETS:
-1- Flat tops, kanhapludults, 65%
-2- Slopes, dystropepts, 30X
-3- Valley bottoms, tropaquepts, 5X
-429. IBAGMERATIQB: Valleys: Small blocks
Interfloves: Large blocks
30. RELIABILITY:
1» reliable, 2° probable, 3~ tenable, 4- plausible
lO.b : 2 12.a: 1
18.a: 2
18.b: 2
18.c: 2
14.a: 1
14.b: 2
17: 2
18.d-q: 2
19: 1
28: 2
29: 2
22: 2
23: 2
24: 1
31. AUM.I1UW. KOTES: The representative profile for Dystropepts is extrapolated from
other L.U.
1112 -
71
TJfflO UHIT BEFOBT
IMAGE:
tytgy
SECTIOBT:
dPfq.3.1
| dacite
| coarse sediaentary rocks
I
1.
4.
5.
6.
| fine sediiKntary rocks
1 : (undiff) top 2: slope
3 : valley botton
2. MAF SHEET: 1112
3. AREA: 265 km2
U D tartT: dPfq.3.1
OOCflBEHCE b y HHJVINUE Sumatera Selatan: 99Ï
Updated by: AH
edit date: 18/04/89
Status: Final
Slaxust UMÜHltiüüS
LAB) UHiT DESŒIÏTIO» Slightly dissected undulating plain,fine and coarse felsic
sedimentary rocks covered by acid tuffs, slopes 3-8%
7. SATELLITE
8. AERIAL FBOTOGKAPBS
9. RADAR
10. MREHT M>TBBTATa. Weathering
b . lithology
c. Fomation
12.
13.
14.
15.
: 124/62/23/03/85
: 1:100.000
58 /8316-69
: STAR-I/250/88/1112-3
11. BOCK OUTCSOP:
X
: High
: claystone, sandstone, dacite
: Tppp , Qrv
HATER
a. Quality : Fresh
b. Source : Medium wells
PTKHHIIP1
: None
RIVERS a. Floodriak : None
b. Inundation: None
VBSETATIGH/LAfl) USE moist primary lowland forest, bush, alang-alang, shifting cu
ltivation, upland crops, rainfed wetland rice, rubber (karet),
banana, towns, villages
60 X
Area used
16. ACCELE8ATB) ESOSIOH
a. Occorence
b
Common
Varions
17. SOU. GREAT GHCOP
Doannant >SOZ
Associated 1
Associated 2
Classification
hapludox
dystropepts
tropaquepts
32. RKHKKStJUAPVE IBGFILES:
odh/
/
/88/UA/1112/1B/
iqt/
/106-1
/82/P /1112/11/
Z of area
60 X
30 X
10 X
ity/
/150/
/24 /
1112 - 72
Lab. checked
yes
yes
yes
/106-7
/82/P
/32
18. SOIL CHARACTERISTICS
ScopexU.es
Dominant > 501
moderately fine
a. Texture:
topsoil
subsoil
moderately fine
b. Depth:
peatsoil
•inaralsoil
deep
Well drained
c. Drainage:
very low
d. Exch. K:
topsoil
very low
subsoil
very low
e. Total K2O: topsoil
very low
subsoil
£. Avail. P: netfaod
topsoil
subsoil
g. Total F:
topsoil
very low
subsoil
very low
h. CBC pH 7
topsoil
low
subsoil
very low
i. Soil Reaction:topsoil excessive acid
subsoil excessive acid
j. Al Sat.
topsoil
high
subsoil
medium
k. Al tozicity :
no
1. Acid snlph. pot.:
not relevant
m. Salinity :
n. Other Tozicity:
o. Soot obstx. layer :
120 cm
p. Organic Matter :
0.9
q. TEH :
0.8
r. Total observations:
2
Associated 1
moderately fine
fine
Associated 2
fine
fine
very deep
Imperfectly drained
medium
low
very low
very low
Bray I
high
very low
very low
very low
low
low
excessive acid
excessive acid
very high
very high
no
not relevant
—
very deep
Poorly drained
medium
medium
low
very low
Bray I
very high
medium
low
very low
medium
low
very strong acid
excessive acid
low
medium
no
very shallow
salt free
120 cm
1.8
0.6
2
120 cm
5.0
1.1
0
19. ALTITUDE:
20. PIAK/PBOFILE:
21.
22.
23.
24.
25.
26.
27.
28.
29.
Maximal:
60 m
Mi nimm»:
20 m
' Bange:
35 m
Dominant: non-linear and random > 60% of area flat-topped
Included:
b. density: Low
L.O. DBAIHAGE: a. Pattern: dendritic
c. Variability: low
b. Variability: Low
SLOPE:
a. Steepness:gently sloping
d. Variability: Medium
c. Length: long
e. Curvature: convex
SLOPE DISTk.:
Valleybottoms: 10 X
Interflnves : 0-81:75 % 9-251: 15 X, 25-551: 0 X
BELIEF AMPLI.: a. Amplitude: low
'
b. Variability: Low
Undulating 2- 8%, 0-50 m
TEBKASB:
a. Shape: Level
b. Lemgth:Moderately long
CXESX/BUDGES:
c. Variability: Low
e. Variability: Low
d. Width: moderate
VALLET FLOCK:
b. Variability: Low
a. Width: very narrow
LAHD FACETS:
-1- Flat tops, hapludox, 60%
- 2 - Slopes, dystropepts, 30%
-3- Valley bottoms, tropaquepts, 10%
-4FBAGMEBTATIGB: Valleys: Small blocks
Interduves: Large blocks
30. RELIABILITY:
1= reliable, 2= probable, 3 s tenable, 4= plausible
lO.b : 2 12.a: 1
14.a: 1
14.b: 2
17: 2
18.a: 2
18-b: 2
18.c: 2
18.d-q: 2
19: 1
22: 2
23: 2
24: 1
28: 2
29: 2
31. ADOITIOBAL HOTES: The representative profile for Tropaquepts is extrapolated from
other L.U.
1112 - 73
LAHD UH1T REPORT
LREP-SDBM, CSR-BOSOR
MAF IMAGE:
SECTIOH:
Pfq.3.2
(undiff) top
1
coarse sediieaUry rocks
fine sedinenUry rocks
2: slop«
l'-imd.top
1. LAHD UHIT: Pfq.3.2
2. MAP SHEET: 1112
3: »alley bottoi
3. AREA: 135 km2
4.
n r r a i B W l f b y P8OVHCE: Sumatera Selatan: 24%,
5.
STAÏDS IDENTIFIERS
6.
LAHD tJHIT DESCRIPTIGH: Moderatelly dissected undulating plain fine and coarse felsic
7.
SATELLITE SCEHES
: 123/63/23/03/83, 124/62/23/03/85
8.
ABBTAT. PHOTOGRAPHS
: 1:100.000
9.
BADAR
: STAR-I/250/88/1112-2
: Updated by: AH
Lampung: 76%
edit date: 18/04/89
sedimenatry rocks, slopes 3-8Ï.
10.
59
/8316-93 ,58
Status: Final
'
/8316-75
11.
PAREST MATERIAL
BIXX QOTCKDP
%
a. Weathering : High
b.
Lithology
: claystone, sandstone,
c- Formation : Tppp
,
a. Quality : Fresh
12.
HATES
13.
FISHERIES
b.
Source
: Medium wells
14.
: None
RIVERS a. Floodrisk : None
b. Immdation: Hone
15.
VEGEIATtCH/LAHD OSE : secondary forest, bush, alang-alang, shifting cultivation, upland
crops, rubber (karet), towns, villages
16.
Area used
: ÜCJ '.
AIfvy f^}A^Rn mrvïTm
a. Occurence : Common
b.
17.
Evidence : Various
SOU. GREAI GROUP
:
Classification
32.
Z of area
Lab.
checked
Donnant >50I
hapludox
60 %
yes
Associated 1
dystropepts
30 %
yes
Associated 2
tropaquepts
10 %
yes
REPHESEHTATTVE PROFILES:
ity/
odh/
/
/88/HJ/1112/11/
/146/
iqt/
/84-A
/86/SR/1112/12/
/10 /
1112 -
74
/88/UA/1112/11/
/191/
18. S O U CHARACTERISTICS
Proportie»
a. Texture:
topsoil
subsoil
b. Depth:
peatsoil
•ineralsoil
c. Drainage:
d. Each. K:
topsoil
subsoil
e. Total K20: topsoil
subsoil
t. Avail. P:
method
topsoil
subsoil
g. Total P:
topsoil
subsoil
b. CEC pH 7
topsoil
subsoil
i. Soil Reaction:topsoil
subsoil
j. Al Sat.
topsoil
subsoil
k. Al toxicity :
1. Acid sulph. pot.:
m. Salinity :
n. Other Toxicity:
o. Boot obstr. layer :
p. Organic Matter :
q. TEB :
r. Total observations:
1 9 . ALTITUDE:
Dominant > 30X
fine
Associated 1
moderately fine
fine
Associated 2
fine
fine
very deep
Moderately well
medium
low
medium
low
Bray I
low
very low
low
very low
low
low
excessive acid
excessive acid
high
high
no
not relevant
deep
Well drained
low
low
low
very low
Bray I
very low
very low
very low
very low
low
low
excessive acid
excessive acid
medium
very high
no
not relevant
deep
Very poorly drained
low
low
very low
very low
Bray I
very low
very low
medium
very low
high
medium
excessive acid
very strong acid
high
very high
no
not relevant
80 cm
1.8
1.3
0
120 cm
0.8
1.0
2
100 cm
5.6
0.8
0
fine
•
2 9 . F8AGKEHTATIQX:
10 m
Range:
25 m
50 m
60% of area flat-topped
Dominant: non-linear and random
Included:
a. Pattern: dendritic
b. density: Moderate
c. Variability: low
a. Steepness:gently sloping
b. Variability: Low
c. Length: extremely
d. Variability: Low
e. Curvature: convex
ValleybottoBs: 10 X.
Interfiles : 0-81:75 X, 9-25Z: 15 X, 25-55Z: 0 %
a. Amplitude: medium
b. Variability: Low
Undulating 2- 8%, 0-50 m
a. Shape: Level
b. Length:Moderately long
c. Variability: Low
d. Width: moderate
e. Variability: Low
a. Width: very narrow
b. Variability: Low
-1- Flat tops/crest, hapludox, 60%
-2- Slopes, dystropepts, 30%
-3- Valley bottoms, tropaquepts, 10%
-4Valleys: Small blocks
Interfluves: Large blocks
30. RELIABILITY:
lO.b : 2 12.a: 1
18.d-q: 2
19: 1
= reliable, 2= probable, 3= tenable, 4= plausible
14.a: 1
14.b: 2
17: 2
18.a: 1
18.b: 2
18.c:
22: 1
23: 2
24: 1
28: 2
29: 2
2 0 . PLAH/FBQFILE:
2 1 . L.P. DBAZHAGE:
2 2 . SLOPE:
2 3 . SLOPE DISTS.:
2 4 . RELIEF AMPLI.:
2 3 . TERRAIS:
26. CHEST/RIDGES:
27. VALLET FLOOR:
28. LAHD FACETS:
31. ADDITIOBAL BOTES: The representative profile for Hapludox and Tropaquepts are extrapolated from other L.U.
1112 -
75
LAID USIT BEFOBT
LREP-SDBM, CSB-BOGCB
CSD6S SECTIOH:
2: slope
2. M&F SHEET: 1112
3. AKEA: 5 km2
LABO OBIT: Ptn.3.2
" " ' » " ' » by VSOnaCE: Sumatera Selatan: 99Ï
edit date: 18/04/89
Status: Final
STATUS IDEHTIFIERS : Opdated by: AH
LABD HBIT DESCHIPTICB: Moderatelly dissected undulating plain,metamorphic rocks,slopes
3-8%
7. SATELLITE SCEHES
: 123/62/23/03/86
8. AERIAL FBOTOGKAFBS : 1:100.000
3 /8308-106
9. RADAR
: STAR-I/250/88/1112-6
10. BAREST MATBBTA1.
il. BOCK amas»: %
a. Weathering : High
b. Litbology : schists, gneiss
c. Formation : Ptse
12. HATER
a. Quality : Fresh
b. Source : Shallow wells
1 3 . ymmijvi jijt
; None
1*. RIVERS a. Floodrisk : None
b _ TiiMnnifl*'-'* o n : None
15. VEEETATIOH/LAHD DSE : , bush, upland crops, rubber (karet), towns, villages
1.
4.
5.
6.
Area used
: 75 X
16. ACCELERATED EROSICH
a. Occurence : Common
b. Evidence : Various
17. SOIL GREAT GRQOP
Donnant >30Z
Associated 1
Associated 2
Classification
kanhapludults
dystropepts
tropaquepts
32. BERESESTATIVE IBOFTLES:
udh/
/
/87/DA/1112/
/
/I
Z of area
80 Z
10 %
10 X
/
ity/
1112 -
76
Lab. checked
yes
yes
no
/87/DA/1112/
18. SOU. CHARACTERISTICS
Properties
Dominant > 501
moderately coarse
a. Texture:
topsoil
subsoil
moderately fine
b. Depth:
peatsoil
deep
Moderately well
c. Drainage:
very low
d. Exch. K:
topsoil
subsoil
very low
very low
e. Total K2O: topsoil
very low
subsoil
Bray I
netted
£. A v a i l . F:
very low
topsoil
subsoil
very low
topsoil
very low
g. Total P:
subsoil
very low
topsoil
very low
h. CEC pH 7
subsoil
very low
i. Soil Beaction:topsoil strong acid
subsoil very strong acid
high
j. Al Sat.
topsoil
very high
subsoil
k. Al toxicity :
no
1. Acid sulpb. pot.:
not relevant
•. Salinity :
n. Other Toxicity:
o. Boot obstr. layer :
75 cm
1.2 '
p. Organic Matter :
0.4
q. TUB :
r. Total observations:
1
Associated 1
moderately coarse
moderately fine
Associated 2
very deep
Well drained
very low
very low
very low
very low
Bray I
very low
very low
very low
very low
low
very low
strong acid
strong acid
high
high
no
not relevant
120 cm
3.5
0.5
1
0.0
0.0
0
19. ALTITUDE:
Mari mm-
20. PLAH/TBOFILE:
Dominant: non-linear and random > 60% of area flat-topped
Included:
30 m
tUniaaa:
10 m
Bange:
25 m
a. Pattern: dendritic
b. density: Moderate
c. Variability: low
a. Steepness:gently sloping
b. Variability: Low
22. SLOPE:
c. Length: extremely
d. Variability: Low
e. Curvature: convex
Valleybottarns:
5X
23. SLOPE DISTR.:
Interfluves : 0-81:80 %, 9-25Z: 15 %, 25-551: 0 %
24. BELIEF AMPLI.: a. Amplitude: low
b. Variability: Medium
25. TEBRAXB:
Undulating 2- 8%, 0-50 m
26. CREST/HIDSES:
a. Shape: Level
b. Length:Moderately long
c. Variability: Low
d. Width: moderate
e. Variability: Low
27. VALLES FLOOR:
a. Width: narrow
b. Variability: Low
-1- Interfluves, kanhapludults, 80%
28. LAHD FACETS:
-2- Interfluves, dystropepts, 10%
-3- Valley bottoms, tropaquepts, 10%
-•2 9 . FHAGMEHTATICH: Valleys:
Interfluves: Large blocks
21. L.O. DSAIHAGE:
30. REf.TABn.TTi:
1= reliable, 2= probable, 3» tenable, 4= plausible
lO.b : 2 12.a: 1
14.a: 1
14.b: 1
17: 2
18.a: 1
18.b: 1
18.c: 1
18.d-q: 2
19: 1
22: 2
23: 2
24: 2
28: 2
29: 2
31. ADDITIGHAL BOIES:
1112 -
77
o m BERST
IMAGE:
SECTICH:
1-1.3
dPfq.4.1
dPfq.4.1
âacite
coarse se-lioenUry rocks
1 fine sediMntary rocks
|
l: und. top
2 r slope
3 : Valley tnttoi
1.
•.
S.
6.
LAID OUT: d P f q . 4 . 1
2. MAP SHEET: 1112
3. AREA: O km2
OOCOBEBCB by PBUV1HUE: Sumatera Selatan: 991
STATUS
Updated by: AH
edit date: 18/04/89
Status: Final
LAID OBIT DE3C8XPTICH: Slightly dissected undulating to rolling plain fine and coarse
felsic sedimenatry rocks covered by acid tuffs,slopes 3-15Ï.
7 . SATBf J.iTfL
124/62/23/03/85
8. AERIAL PBOTOGBAPHS
1:100.000
58 /8316-71
9 . BAQAR
STAR-I/250/88/1010
10. BAKER HATFKTAÎ.
11. BOCK aOKSOP:
Z
High
a. Weathering
claystone, sandstone, dacite
b. Lithology
Tppp , Qrv
c. Formation
Fresh
12. HATER
a. Quality
Perennial River
b. Source
None
None
1«. HIVERS a. Floodrlsk
None
IS. VBSEIAXIGH/LABD OSE
Area used
IK
, bush, alang-alang, shifting cultivation, upland crops, rainfed
wetland rice, rubber (karet), towns, villages
: 60 Z
«o-mjtVATEn fronen rm
a. Occorence : Conmon
b. Evidence : Various
17.
\
a»
SOIL G8EAI 6BCOP
Dcsdnant >SOX
Classification
hapludox
Associated 1
Associated 2
dystropepts
tropaquepts
X of area
55 Z
35 Z
10 Z
Lab.
checked
yes
yes
yes
up4if.Nl« 1 AT I vg PROFILES-
odh/
/
/88/HJ/1112/13/
/164/
iqt/
/106-1
/82/P /1112/11/
/24 /
.1112 -
ity/
78
/106-7
/82/P /1112/13/
/32 /
18. SOIL CHABACTEBISTICS
Pujperties
a. Texture:
topsoil
subsoil
b. Depth:
peatsoil
•inaralsoil
c. Drainage:
d. Each. K:
topsoil
sobsoil
e. Total K2O: topsoil
subsoil
t. Avail. F: aathod
topsoil
sobsoil
8- Total P:
topsoil
subsoil
h. CEC pH 7
topsoil
subsoil
i. Soil Beaction:topsoil
subsoil
j. Al Sat.
topsoil
subsoil
k. Al toxicity :
1. Acid sulph. pot.:
m. Salinity :
n. Other Toxicity:
o. Boot obstr. layer :
p. Organic Matter :
q. TEB :
r. Total observations:
DoMnant > SOX
fine
fine
Associated 1
moderately fine
fine .
Associated 2
fine
fine
very deep
Moderately well
low
low
low
very low
Bray I
very deep
Imperfectly drained
medium
low
very low
very low
Bray I
high
very low
very low
very low
low
low
excessive acid
excessive acid
very high
very high
no
not relevant
—
very deep
Poorly drained
medium
medium
low
very low
Bray I
very high
medium
low
very low
medium
low
very strong acid
excessive acid
low
medium
no
not relevant
salt free
120 cm
1.8
0.6
0
120 cm
5.0
1.1
0
very low
very low
low
low
excessive acid
excessive acid
high
high
no
not relevant
130 cm
2.0
1.0
1
19. ALTITUDE:
50 m
MünüuB:
10 m
Bange:
40 m
DcKinant: non-linear and random > 60! of area flat-topped
20. PLAB/rBOFILE:
Included:
a. Pattern: dendritic
b. density: Low
21. L.D. DBAIBAGE: c. Variability: low
a. Steepness:sloping
b. Variability: Medium
22. SLOPE:
c. Length: long
d. Variability: Medium
e. Curvature: convex
23. SLOPE DISTR.:
Valleybottoas: 10 X
InterzXuves : 0-81:40 Ï, 9-25X: 50 Ï, 25-551: 0 !
24. BELIEF AMPLI.: a. Amplitude: medium
b. Variability:
25. TFBRAT»Rolling
9-15!, 0-50 m
26. CREST/RIDGES:
a. Shape: Undulating
b. Length:Moderately long
c. Variability: Low
d. Hidth: moderate
e. Variability: Low
27. VALLET FLOCS:
a. Hidth: narrow
b. Variability: Low
28. LAID FACETS:
-1- Crest, hap'ludox, 55!
-2- Slopes', dystropepts, 35!
-3- Valley bottoms, tropaquepts, 10!
-4Intordoves: Large blocks
29. FBAOffiBIATIOa: Valleys: Small blocks
30. BELIABHITT:
10.b : 2 12.a: 1
18.d-q: 2
19: 2
1» r e l i a b l e ,
14.a: 1
22: 2
2 - probable,
14.b: 1 17: 2
23: 2 24: 2
3 - tenable,
18.a: 2
28: 2
4 - plausible
18.b: 2
29: 2
18.c: 2
31. ADDmOKAL BOTES: The representative profiles for Dystropepts and Tropaquepts is ext
rapolated from other L.U.
1112 - 79
LAMD l U l T HEPOBT
LBEP-SDEM, CSR-BOSOR
MAP IMAGE:
GSDSS SECTIGH:
couse sediKnUry n d s
1
1 . LAUD OBIT: P f q . 4 . 2
2. MAP SHEET: 1112
3. AREA: 133 km2
4.
i i i T » - » by PROVIBCE: Sumatera Selatan: 70%, Lampung: 30%
5.
STATUS IDENTIFIERS
: Updated by: KB
J iTalley bott«
1 fine s a l i w t a y racks
edit date: 18/04/89
Status: Final
6 . LAID U U T D E S X I P n C H : Moderatelly dissected undulating to rolling plain fine and coarse
felsic sedimentary rocks, slopes 3 - 15%
7 . SATELLITE SCEBES
8.
AFPTAT
HCTOGSAPHS
: 124/62/23/03/85, 123/63/23/03/83
:
1:100.000
58 /8316-73 , 58 /8316-75 , 59 /8316-93
9 . RADAR
: STAR-I/250/88/1112-2
10. PéSBÊJ MATERIAL
a. Heathartng
b. Lithology
c. Formation
12. HATER
a. Quality
b. Source
13. FISHERIES
:
:
:
:
:
:
11. ROCK OOTCSOP:
%
High
claystone, sandstone,
Tppp
Fresh
Medium wells
None
14. BIVERS a. Floodxisk : None
b . Trmivt*1n%\ on ' None
1 5 . VBSEtAIIGH/LABD USE : , bush, alang-alang, shifting cultivation, upland crops, rubber
(karet), towns, villages
80 %
Area used
16. V»Tg.1
a. Occorenc a
b. Evidence
Common
Various
17. SOU. GREAT GROUP
Doaiiiant >5OI
Associated 1
Associated 2
Classification
hapludox
dystropepts
X of area
55 I
45 %
Lab. checked
yes
yes
32. HHHIiSEFTATIViC WMUf I l.fgg.
odh/
/
/88/HJ/1112/H/
/146/
ity/
1112 - 80
/88/HJ/1112/11/ /155/
18. SOIL CHUUCtEBISnCS
Proparties
Dominant > 501
a. Texture:
b. Depth:
topsoil
subsoil
peatsoil
very deep
Moderately well
medium
topsoil
subsoil
low
Total K2O: topsoil
medium
low
subsoil
Avail. P: aettaód
Bray I
topsoil
low
subsoil
very low
Total P:
topsoil
low
subsoil
very low
CEE pH 7
topsoil
low
subsoil
low
Soil Reaction:topsoil excessive acid
subsoil excessive acid
Al Sat.
topsoil
high
subsoil
high
no
Al tenacity :
Acid sulph. pot.:
not relevant
Salinity :
Other Taxicity:
Root abstr. layer :
100 cm
Organic Matter :
1.8
TEB :
1.3
Total observations:
1
^rJTM^yff|«ni 1
c. Drainage:
d. Exch. K:
e.
£.
g.
h.
i.
j.
k.
1.
m.
n.
o.
p.
q.
r.
fine
fine
Associated 1
fine
fine
very
Well
low
very
very
very
Associated 2
deep
drained
low
low
low
-
-
•
—
very low
very low
very low
low
excessive acid
strong acid
medium
very high
no
—
140 cm
1.1
1.4
0
0.0
0.0
0
19. ALTITUDE:
20.
21.
22.
23.
24.
25.
26.
27.
28.
29.
55 m
Minium:
20 m
Range:
40 m
Dominant: linear and random > 602 of area flat-topped
PUB/PROFILE:
Included:
a. Pattern: dendritic
b. density: Moderate
L.D. DSAESftSB: c. Variability: low
a. Steepness:gently sloping
b. Variability: Medium
SLOPE:
c. Length: long
d. Variability: Medium
e. Curvature: convex
SLOPE DISTR.:
Valleybottoms:
5%
Interfluves' : 0-81:60 %, 9~25Z: 30 X, 25-55Z: 5 %
BBI-TEP AMPLI.: a. Amplitude: medium
b. Variability: Medium
TERRAIS:
Undulating 2- 8%, 0-50 m
c. Variability: Low
C8EST/RH3GES:
a. Shape: Level
b. Length:Moderately long
d. Width: moderate
e. Variability: Low
VALLET FLOOR:
a. Width: very narrow
b. Variability: Medium
IAHD FACETS:
-1- Crests, hapludox, 50%
~2~ Slopes, dystropepts, 45%
-3~ Valley bottoms, 5%
-4FKAGMEHTATIGH: Valleys:
Interrluves: Medium blocks
30. RELIABILITY:
1= reliable, 2= probable, 3= tenable, 4= plausible
lO.b : 2 12.a: 1
14.a: 1
14.b: 1
17: 2
18.a: 1
18.b: 1
18.c: 1
18.d-q: 1
19: 1
22: 2
23: 2
24: 1
28: 2
29: 2
31. ADDITIOBAL BOTES: The representative profile for Dystropepts is extrapolated from ot
her L.U.
1112 - 81
UIJIT 8EFCBT
LKEP-SBEM, CSR-BOGGR
massa
MAP IMAGE:
1 und top
1 . LAHD DHIT:
2 slope
2. MAP SHEET: 1112
Pg.4.2
SECTIGH:
3 valley bottoi
3. AREA: 6 km2
4 . U n i H H r F . b y PKOTIBCE: Svimatera Selatan: 99Ï
5 . STATDS IDEMTIFIERS
: Updated by: AH
edit date: 18/04/89
Status: Final
6 . LAUD OBIT DE3CKIPTICH: Moderatelly dissected undulating to rolling plain, acid plutonic
7. SATELLITE
8. AEBTAT. PHOTDGSAPBS
9. B&D&R
10. PABEHT MATEKUL
a. Weathering
b . Litbology
c. Fomation
12. HATEK
a. Quality
b. Source
13 _ FISHERIES
14. BIVEBS a. Floodrisk
15. VBGETâTIOH/LAHD OSE
Area used
16. ACXELEBATED EKOSIOH
a. Occorence
b. Evidence
rocks, slopes 3-15X.
123/62/23/03/86
1:100.000
3 /8308-106,
STAR-I/250/88/1112-6
11. BOCK CDTCSQP:
Medium wells
None
None
None
, bush, alang-alang, shifting cultivation, upland crops, rubber
(karet), coconut (kelapa), towns, villages
80 X
Common
Various
17. SOU. GSEAT G800P
Dcsinant >SOZ
Associated 1
Classification
dystropepts
hapludox
Z of area
65 X
35 X
Lab. checked
yes
yes
Associated 2
32. BIBJUKSm 1 Aixve ÎBDFILES:
ity/
/
X
High
granite
pTgr
Fresh
/87/JD/1112/ /
odh/
/l /
1112 -
82
/
/87/JD/
18. SOIL CHARACTERISTICS
Proptu-Lies
Dominant > SOZ
moderately coarse
a. Tartare:
topsoil
moderately fine
subsoil
b. Depth:
peatsoil
deep
Imperfectly drained
c. Drainage:
low
d. Exch. K:
topsoil
very low
sabsoil
low
e. Total K2O: topsoil
very low
subsoil
Bray I
t. Avail. P: method
medium
topsoil
sabsoil
very low
g. Total F:
topsoil
low
sabsoil
very low
h. CEC pH 7
topsoil
low
low
subsoil
i . Soil Reaction:topsoil strong acid
subsoil very strong acid
j . Al Sat.
topsoil
low
low
subsoil
k. Al toxicity :
1. Acid sulph. pot.:
not relevant
m. Salinity :
n. Other Toxicity:
o. Boot ebstr. layer :
100 cm
p. Orgaaic Matter :
1.9
q. TEB :
0.6
r. Total observations:
2
Associated 1
fine
fine
Associated 2
deep
Imperfectly drained
high
very low
high
very low
Bray I
very high
very low
very high
low
low
low
strong acid
strong acid
low
very low
not relevant
80 cm
3.5
1.2
2
0.0
0.0
0
19. ALTITtDE:
20. FLA1/ÏW3FILE:
10 m
Bange:
25 m
70 m
Minimum:
Dominant: non-linear and random < 40Ï of area flat-topped
o
Included:
21. L.D. DBAIHAGE: a. 'Pattern: dendritic
b. density: Moderate
c. Variability: low
22. SLOPE:
b. Variability: Medium
a. Steepness:gently sloping
d. Variability: Medium
c. Length: long
e. Curvature: convex
Valleybottoms:
5X
23. SLOPE DISTK.:
Interfloves : 0-81:65 X 9-25Z: 30 X. 25-55Z: 0 X
b. Variability:
24. BELIEF AMPLX.: a. Amplitude: low
Undulating 2- 8%, 0-50 m
25. TESIAIH:
a. Shape: Level
26. CREST/RIDGES:
b. Length:Moderately long
c. Variability: Low
e. Variability: Low
d. Width: moderate
27. VALLEY FLOOR:
b. Variability: Medium
a. Width: very narrow
28. LAHD FACETS:
-1- Slopes, dystropepts, 65Î
-2- Convex tops/crest, hapludox, 35%
-3-42 9 . FRAGKEBTATICH: Valleys:
Interfloves: Large blocks
30. RELIABILITY:
1= reliable, 2— probable, 3= tenable, 4= plausible
lO.b : 2 12.a: 1
14.a: 1
14.b: 1
17: 1
18.a: 1
18.b: 2
18.c: 2
18.d-q: 1
19: 1
22: 2
23: 2
24: 2
28: 2
29: 2
31. ADDITIOHAL KOTES:
1112 - 83
LAID DBTT KEPOBT
LREP-SDBM, CSR-BOGCK
MAP IMAGE:
CBOSS SECTIGH:
Br.1.1.2
2.1.2 1.2,2
äj-' *
Plutonic rods
^'alltnial sedinents
1 . LAID «MIT: Hr. 1 . 8 . 2
It.
2. MAP SHEET: 1112
3. AREA: 11 km2
OCCOREBCE.by PROVUKE: Sumatera Selatan: 99%
: Updated by: AH
edit date: 18/04/89
Status: Final
6. LABD UNIT DESCRIPT1GH: Moderatelly dissected isolated hillocks, intermediate plutonic
rocks, slopes8 - 15 Ï.
7. SATELLITE SCEHES
: 124/62/23/03/85
8. AERIAL PHOTOGRAPHS
: 1:100.000
58 /8316-57
9. BADAR
: STAR-I/250/88/1112-6
10. BAREST MATERIAL
11. ROCK OUTCROP: 20 %
a. Weathering : High
b. Lithology : syenite
c. Formation : pTsy
12. HATER
"a. Quality : Fresh
5 . STAUS IDEHTIFIERS
b. Source :
13. FISHERIES
:
14. RIVERS a. Floodrisk :
b. Inundation:
Medium wells
None
None
None
15. VBSETATICH/LAHD USE : , bush, alang-alang, shifting cultivation, upland crops, rubber
(karet), rock outcrops, mining, mine tailings
60 X
Area used
16.
.UiATFii EROSIOB
a. Occnxence
b. Evidence
Common
Various
17. SOIL GREAT GROUP
DoMinant >50I
Associated 1
Associated 2
Classification
hapludults
dystropepts
Z of area
80 X
20 X
32. REPHESEHTAllvfc PROFILES:
uda/
/
/88/AF/1112/43/
/167/
1112 -
84
Lab. checked
yes
no
18.
Proparties
a. Texture:
b. Depth:
ISTICS
topsoil
subsoil
peatsoil
c. Drainage:
d. Exch. K:
topsoil
subsoil
e. Total K2O: topsoil
subsoil
t. Avail. P: aethod
topsoil
subsoil
g. Total P:
topsoil
subsoil
h. CEE pH 7 topsoil
subsoil
i. Soil Reaction:topsoil
subsoil
j. Al Sat.
topsoil
sobsoil
k. Al toxicity :
1. Acid sulph. pot. :
st. Salinity :
n. Other Taxicity:
o. Root obstr. layer :
p. Organic Matter :
q. TEB :
r. Total observations:
1 9 . ALTITUDE:
2 0 . PLAW/PBOFILE:
2 1 . L.O. fBATWCR2 2 . SLOPE:
2 3 . SLOPE DISTR.:
2 4 . RELIEF AMPLI-:
25. TBBRATM26.
2 7 . VALLET FLOOR:
2 8 . LAD FACETS:
29.
Doadnant > 501
fine
fine
Associated 1
Associated 2
Well drained
very low
very low
low
very low
Bray I
low
low
medium
low
low
low
excessive acid
excessive acid
low
very high
no
not relevant
120 cm
3.1
0.8
1
0.0
0.0
0.0
0.0
0
0
SO m
Minima:
10 m
Range:
40 m
Dominant: non-linear and random < 40X of area crested/peaked
Included:
b. density: Moderate
a. Pattern: dendritic
c. Variability: low
b. Variability: Medium
a. Steepness:sloping
d. Variability: Medium
c. Lengtli: moderate
e. Curvature: convex
ValleybottaBs:
t
Intarfluves : 0-81:20 X 9-251: 70 %, 25-551: 10 %
a. Aaplitode: medium
b. Variability: Medium
hillocKy
>16X, 0-50 m
a. Shape: Irregular
c. Variability: Low
b. Length:Short
d. Width: moderate
e. Variability: Low
a. Width: very narrow
b. VariabiUty: Low
-1- Slopes, hapludults 80X
-2- Crests, hapludults 20X
-3-4Valleys:
Interfluves
30. mg.TAnTT.TTT:
1= reliable, 2 - probable, 3= tenable, 4- plausible
10.b : 1 12.a: 1
14.a: 1 14.b: 1
17: 2
18.a: 2
18.b: 2
18.c: 2
18.d-q: 2
19: 1
22: 2
23: 2 24: 2
28: 2
29: 2
31. AODITIOBAL •OTES:
1112 - 85