INTEGRATION OF PROCEDURES AVAILABLE IN LOW COST IMAGE PROCESSING AND G!!:OGRAPHICAL INFORMATION SYSTEMS. An applica-tion on human settlement and landscape ecology in the depression of EI-Fayoum (Egypt). Th.K.Ghabour & M.Antrop Laboratory for Regional Geography and Landscape Science. State University of Ghent - Belgium C: 0 m . V I I - I.JG. 7 1. Introduction Agriculture in Egypt. as in many other countries in the arid and semi-arid regions, is suffering from salinization of the soils. Soil salinity is one of the most serious problems in agriculture under irrigation. A decline of soil productivity of 30% may occur and is attributed largely to difficulties in oPtimi=in~ the cOlnbined irrigation and drainage system. However, this is not a technical problem in the first place, but a social one. The increase of the population during the second half of this century, caused also an increasing demand of water. A more strictly policy of the water supply was needed, causing important social tenses. 2. The depression of EI-Fayouul El-Fayoum ref~rs to the administrative governorate which is located in a deep. near-circular depression in the limestone plateau of the northern part of the Western Desert of Egypt {fi~.l}. It is situated south-west of Cairo at a distance of about 60 km and nearly 35 km to the west of the Nile. The depression is limited at the north-western side by a shallow brackish lake. called Birkst carun, with an area of about 200 km~ and forming the deepest part at about 45 m below the present sea level. The lake is fed by water of the Nile brought into the depression for irrigation. About 1800 km~ of the depression is filled with rich alluvial sediments and more than 1350 km~ is cultivated. This area represents about 5.3% of the total cultivated area of Egypt. EI-Fav0um Governorate is divided into 5 provinces ElFav()um, Ibshat,Jai, It.sa, 5innuris and Tamiya I, fig. 2). Although th~ latest population census dates from 1986. no data are available yet. The census of 1976 gives 1.14 million people living in the governorate. which was about 3% 0f the total population of Egypt. The estimation of the actual population gives 1.44 million inhabitants. The rural population accounts for 76% and is mainly distributed in 140 villages or small towns. Thus the population density increased f'rom 370 inh./km~ in 1947 to an estimated value of a,br:"ut 8 1)(1 inh.,/km;;;' in IS1e-5. The population is not equally distributed allover the depression. but shows a concentration in the central part and on the most fertile soils. Consequently, the population pressure increases here most rapid Iv and most of the fertile soils are affected in the first place. Salini~ation occurs almost generally in the depression and reaches dramatic values. Detailed monitoring of the VU-48 evolu~ion and the tasl:s. of the population pressure, the irrigation system process of salinization become more and more vital 3. The problem.s Many problems do occur to realize this kind of landscape ecological monitoring. Some of them are global - accurate and detailed demographic statistics are not available since the census of 19 7 6; - the detailed demographic data which are necessary for making prognoses of the future growth, refer only to rather large administrative units and do not reflect the real population distribution of the settlements; - inventories of the soil conditions are very general and do not reflect the rapid changes in the environment; - collecting and integrating all necessary information for a regional and local land assessment is very difficult. Clearly, the use of satellite remote sensing and the use of geographical information systems {GIS) seem to offer interesting solutions. Unfortunately, no financial possibilities to develop such operational systems, nor a sufficient number of trained researchers are available. Consequently, the approach should be very pragmatic, using every tool which is available at this moment. The general idea is to integrate any kind of land information on a PC standard, because these are more or less widely available in administration. The sources for the land information system are all existing maps, aerial photographs, statistics as well as remote sensing data from Landsat TH. 4. Population pressure and salinization This contribution presents only as an example one of the first attempts to relate these different sources of data on a regional and local PC-based Land Information System. Basic questions were ll) determine an estimation of the actual population for each settlement site; ~2) make an inventory of the actual situation of the soil conditions related to the process of salinization; ~3) assessment of the human pressure on the land; l4) test if any relation between population pressure and salinization exist. and if any determine 'hazard or highr i8k zc'nes'. VII ... 49 Q...~..........$.~..t.!:.1.~.m.~n t.;.,~., ..,. .g..n~;.L . . ,.P.Q.P.V..b,.Q,.!:.,;!'.Q,.H The population is mainly concentrated in about 140 villages about 200 to 3000 inhabitants. Each district has also a town or even a small city. The villages are almost randomly distributed allover the depression. They can be detected and delineated easily upon Landsat TM imagery \on band 3 black & white and false color composites with bands 2.3.4). Visual interpretation proved to be rapid and accurate because of the natural capability of the human percePtion in dealing with complex contextual information and because most localizations are approximately known. Shape and size could be determined and compared with the aerial photographs dated 1956. Figures 4 and 5 show the image ot El Minva (about 13000 inhabitants) on the aerial photograph and on the Landsat TM (band 3). The new extension of the town can be seen clearly. Thus, a complete and updated settlement mapping could be achieved and which is presented in figure 2 where the administrative boundaries are added also. No changes occurred in the territories and sites of the settlements during the last 40 years, only their sizes changed. rangin~ from A population census on a communal level is only available for 1947. From the census of 1976 only data on the district level are generally available. Both have been use to make an estimation of the population of each village in 1985, the year of the Landsat TM registration. A logistic growth model was used. The carrying capacity was estimated using the territorial size. Determining the carrying capacity is not easy because of lack of appropriate ground data. especially in the past. Simulation of the logistic model was used to find the best fit of the predicted population with the general sensus data. This resulted in a rural population density of about 800 inhabitants/km~. Such an approach is only valid for rural settlements in which is initially physical isotropic. The results are strongly biased for cities and large territories containing heterogeneous land qualities. Another estimation of the carrying capacity can be based upon the village sizes. The correlation between the population in 1947 and the sizes of the villages interpreted upon the Landsat TM imagery, proved to be highly significant. Consequently, most of the population growth seems to be absorbed in the larger towns and not in the rural villa;2,es. t~!, ..~.",..."I. h.§!.,.,... I;~..LQ.::;.§,§..;'~"L" . ,9..t . . . .~,.§l,.l.~h.D..i..?'.9..1j~.9,n,.:... Several field surveys showed a rapid increase of the salt affected soils in the depression. The soils have been classified as Aridisols, Entisols and Vertisols. Most important physical factors for developing soil salinity are the basin like topography. the severe aridity, the high evaporation rate. the shallow ground water table. Most important human factors are the inadequate drainage system and the social stress at some locations were the human pressure is high and the amount of available water is somewhat restricted. This clearly shows that only a holistic approach may result in some kind of success. Landscape as a VIl . . 50 whole, with its natural and human components should be considered as valuable resource which can only be managed in a integrated and ecological way (M.AntroP 1983). j I Accurate mapping of the different degrees of salinization could be carried out in a very satisfactory manner using Landsat MSS (6th July 1981) and TM (12 July 1985, imagery and the most simple interpretation techniques (Th.Ghabour & L.Daels,1986). Photographic images of different spectral bands were combined producing diazo color composites. The scenes were optical enl to a scale of 1:100,000 and interpreted visually, Additional information was collected from the stereos when necessary. The resulting map is presented in 3 and shows clearly the increasing salinization in the per ieal zone of the depression as well as some 'high risk' spots in the central part between some settlements. 5. The use of a GIS MAP2 is the PC version of the Map Analysis Package (MAP) adapted by De Dorschkamp (The Netherlands) tsee A.Van den Berg et.al. ,1984,1985). It is a low cost GIS and runs on any PC XI or AI having at least 640 kb of RAM memory. It is a raster based GIS which has a large set of procedures for map comparison and spatial analysis. Although the package was primary developed for educational purposes and has therefore a limited capacity, it became widely used in landscape ecological research, in landscape assessment and land evaluation. The main drawbacks are the input and output procedures which are not users friendly. Data must be entered in raster format and no facility is available for vector to ras~er conversion. Output of the maps is only possible on a matrixprinter and not on the screen, which gives a serious limitation for a fast interactive analysis. Because only text screens are used the package can be used on any PC configuration. The price and the flexibility determined this choice for the development of GIS on scales of the governorate, district and communal level. Thus, information from image interpretations maps. field surveys and statistics could be combined. The procedures for spatial analysis proved to be particularly useful. As an example, distance zoning was carried out from the drainage and irrigation channels, using terrain elevation data in a Digital Terrain Model (DTM) based upon the topographical map lfig.6). Spatial association with the interpreted salinity map (fig.7) and with field survey maps proved to be significant in most cases. This analysis supported the hypothesis that salinization increases with the distance from the water channels and is more severe for drainage channels than for irrigation channels. 6. Perspectives Although d ital imagery contains more precise information. it is still very difficult to use this to practical 1 work because 0f the restricted availability of the hardware in developing countries. This is particularly true for many small scale projects. Fortunately. low cost software for ciigi tal image processing becomes available for P(~ t()O, as the PCIPS tMyers~ 1985). Most procedures of image enhancement can hardly be used for more ecological ways of spatial analysis. Nevertheless, this kind of software may be interesting for a more easy input of information in a raster GIS. Also. output of the GIS can be improved using digital image software to produce coloured maps of better readabili than matrixprinted maps. 7. Conclusions In the field land evaluation and landscape assessment any type of remote sensing imagery is an important and even fundamental source of information. Many enhancement and interpretation techniques (analog as well as digital) treat that information with a very loose link with the complex and holistic reality on the terrain. The main reason seems to t'e t.hat t.he necessary terrai.n i.nformation is not always available and if so, it has seldom the expected perfection. Meaningful interpretation with really practical use for the local and regional planning authorities, can seldom be achieved without an integrated landscape ecological approach. Techniques for spatial analysis available in GISpackages are even more useful then enhancement procedures. Although an integration of both is required. Anyhow, the skilled human interpreter remains indispensable. 8. Literature Ant.rop M. \. 1982,\ - The "natural way" of visual image interpretation for land classification and landscape plannin~. Toulollse,GOTA.Proc.lnt.Symp.ISPRS,Com.VII/l. Archives vol.24-Vll/l,897-907 Antrop M. (1983) - Inventoring and monitoring of landscape as a natural and cultural resource. Paris.ESA,Proc.EARSel/ESA Symp. on Remote Sensing Applications for Environmental Studies. 26-28 April 1982, Brussels,105-113 Antrop M. {1986> - Structural information of the landscape as ground truth for the interpretation of satellite imagery. In: Damen. Sicco-Smit & Verstappen led.) : Remote Sensing for Resources Development and Environmental Management. Enschede,ITC,Proc. 7th Int. Symp.ISPRS.Com.VII,3-8 Ghabour Th. & Daels L. (1986) - Visual interpretation of Landsat MSS images for the detection of salt-affected soils <EI-Favourn. Egypt) Myers H. & Bernstein R. (1985) - Image Processing on the IBM Personal Computer. Proc.IEEE.vol.73,n~6,1064-1070. Van den A .. Lith J. & Roos J. (1984) - MAP: A set of computer programs that for input, ou t and transformation of cartogr c data. Roskilde Universitv.Proc. Ith Int.Seminar on Methodology in Landscape Ecol cal Research and Planning, theme I11,101-113 Van den Berg A., Lentjes P .. Lith J. & Roas J. (19854) MAP2 User Manual. Wageningen, Research Institute for F()rl-.::strv and Larv:iscaJ:'e Planning HDe Dorsch~:amp". PROCESSED AT FUCINO ON 17/04/86 KM 15 NASA Fig.1. The Ju ID:50497080~2 S/W ID. :011 TM5 3 177 040 2 sion of El Fayoum on Landsat TM band 3 (12 1985) , Lt) co ~ ~-- ...... Lt) ....ra {J c: ra ...... ~ ~ ~ ffi ~ 0 (!) ~ :;j c: 0 1:J Cat VI ra ..Q VI ~ :1 ra ....c: Cat ~ ~ ...... ....~ .... ~~ Fig.2 Administrative divisions of El Fayoum Governorate and the settlement shapes and sizes interpreted upon Landsat TM. 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"od DIll ~-~.5k .. non " .. 1 , 3 k .. mod .... 1 • 3 Ie .. very .... 1 ) 3 Ie" 1511 13;< 602 437 489 92 99 15 ~23 41.97 3.67 16.72 12.14 13.58 2.56 2.75 .42 6.19 .00 6.32 ~11.82 ~0.92 23.41 4.40 4.74 .72 10.67 Fig.7 .6 Part of the MAP2 GIS of El Fayoum : commune El nya. Distance zoning around the main drainage channels, related to the topography. Part of the MAP2 GIS of El Fayoum commune El Minya. Combination of the interpreted salinity map (Landsat TM, 1985) and the distance zoning around the main drainage channels.