Groundwater & Lake Interactions: Science, Policy and Tools

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Groundwater & Lake Interactions:
Science, Policy and Tools
Bob Nauta
Nauta, RSV Engineering
Chuck Dunning & Herb Garn, USGS
Tim Asplund, WDNR
Wisconsin Lakes Convention
Workshop: April 17, 2008
Introductions
Wisconsin is water rich
rich…
‹
‹
‹
‹
‹
32 inches of rainfall
per year
15,000+ lakes
44,000 miles of
streams and rivers
1 2 quadrillion gallons
1.2
of ground water
2 Great Lakes and
Mississippi River
Why are we here?
Low lake levels!
‹ Increased demand for water and uncertain
implications of changing climate
‹ Concerns about proposed and existing
high capacity wells near lakes, wetlands,
and springs
‹ Cumulative impacts of wells on regional
water table
‹ Ignorance about how groundwater
“works”
‹ Regulatory Limitations
‹
Huron Lake, Waushara County
Twin Lake, Marquette County
Gilbert Lake, Waushara County
Plainfield Lake, Waushara County
R. Lathrop
Fallison Lake, Vilas County
F. Koshere
Tomahawk Lake, Bayfield County
Tomahawk Lake, Bayfield County
Implications of low water levels
‹ Navigational
issues
‹ Exposure of lake beds to disturbance
‹ Water quality/clarity changes
‹ Shift in aquatic plant community
‹ Reduced
R d
d fi
fish
h cover
‹ Potential for spread of invasives (e.g.
EWM,
EWM Phragmites
Ph
Phragmites)
agmites)
agmites)
‹ Increased likelihood of winterkill
Recent Climate Trends
Projected Climate Changes in
the Great Lakes Region by 2100
‹
Temperature
–
–
–
–
‹
*http://www
http://www.ucsusa.org/greatlakes
ucsusa org/greatlakes
Winter 55-12 °F (3
(3--7 °C)
Summer 55-20 °F ((3(3-11 °C))
Extreme heat more common
Growing season several weeks longer
Precipitation
– Winter, spring increasing
– Summer,
Summer fall decreasing
– Drier soils, more droughts
‹
More extreme events – storms,, floods
– Could be 5050-100% more frequent than now
‹
Ice cover decline will continue
S
Source:
B b All
Bob
Allan, NREL
Moving States - Going to Arkansas?
UCS/ESA 2003
Water Levels – Scenario #1
‹
‹
‹
‹
‹
Warmer, wetter
winters increases
recharge
More recharge
increases baseflow and
groundwater levels
More storms increases
summer runoff and
flooding
More CO2 in
atmosphere
h
makes
k
plants more water
efficient, decreasing ET
Lakes may go up
Source: John Magnuson, 2007
Water Levels – Scenario #2
‹
‹
‹
‹
‹
Shorter duration of
ice cover increases
time for evaporation
Warmer air
temperatures
increase evapo
evapo-transpiration rates
Lower precipitation in
summer decreases
soil moisture
Extended
d d dry
d periods
i d
between storm events
Lakes may
y go
g down
SOURCE: UCS/ESA 2003
Changing water level regime
Source: USGS Circular 1186
Anvil Lake (Vilas Co) Stage
(1936 – 2006)
Anvil Lake
Lake, Vilas County
County, WI
8
Stage
e, in feet
7
6
5
4
3
2
1
0
1/1/30
1/1/40
1/1/50
1/1/60
1/1/70
1/1/80
1/1/90
1/1/00
1/1/10
S
Source:
USGS
Source: USGS
Anvil Lake – Regime shift?
Hydrograph for Anvil Lake, Vilas Co
8
Stage height (ft)
S
7
6
1985 2007
1985-2007
1936-1981
5
4
3
2
1
0
100%
80%
60%
40%
20%
% of time lower than stage height
0%
Implications of low water levels
Source: USGS Circular 1186
Human water use
Source:UWSP
Source:UWSP
NW Waushara County Lakes
‹
‹
‹
‹
‹
‹
Landlocked lakes,, no
outlet
Sandy soils
Lakes near major
regional groundwater
divide
Recent
R
td
declines
li
after
ft
unusually high period
in the 1990s
Short--term drought in
Short
Central WI
Major pumping center
Overpumping of the deep sandstone aquifer:
650
ALTITUDE, IN FEET ABOVE S
SEA LEVEL
CA-6
600
OU-326
Slope of line is
3 feet per year
550
BN-154
50 feet
BN-76
500
450
3-4 feet per year
400
350
300
1949
1958
1968
1978
1988
1998
Max
drawdown
> 300 feet
650
ELEVA
ATION, IN FEET ABOVE SEA LEVEL
600
Max
drawdown
<60 feet
Kenosha County
550
Slope of line is 7 feet /year
Milwaukee County
500
450
400
350
300
1940
50 feet
Racine County
7 feet per year
1949
1959
1969
Waukesha
County
1979
1989
1999
10 feet
Source: US Geological Survey and
Wisconsin Geological and Natural History Survey
and, adding
Chicago…
Increased pressure on shallow
sand and gravel aquifer
New Shallow Aquifer Municipal Well
q
Municipal
p Well
New Sandstone Aquifer
Planned Shallow Aquifer Municipal Well
Planned Sandstone Aquifer Municipal
Well
Areas of Recent Conflict over Groundwater
Use
Slide courtesy of John Jansen
Recent conflicts in the Mukwonago
Ri
River
watershed
t
h d
‹
‹
‹
‹
‹
Lake residents
concerned about new
municipal well sitings
Communities
C
iti needing
di
new sources of water
Downstream flows,
water budgets, water
quality concerns
Conflicts
C fli t also
l spurred
d
by urban sprawl and
development
p
patterns
p
Litigation/cooperation
Role of Climate Change
Exacerbation of Existing Problems
Increased flooding and erosion
‹ Pressure to increase water
extraction from the Great Lakes
‹ Mining
g of deep
p aquifers
q
increases
pressure on shallow groundwater
‹ More reliance on irrigation
g
to g
grow crops
p
‹ Anthropogenic impacts may
enhance or counter long term
regional trends
‹
Source: Dave Hansen, MN Extension Service
Which one is the future?
M b b
Maybe
both!
th!
Wisconsin Water Law
‹ Riparian
Ri
i
rights
i ht
‹ Reasonable/
beneficial use
‹ Navigable
g
waters
‹ Public Trust
Doctrine
‹ Statutory
authority
DNR’s
DNR
’s
s Statutory Authority
‹ “The
The
purpose of this subchapter is to
grant necessary powers and to
organize a comprehensive
program…for the enhancement of the
quality management and protection
of all waters of the state, ground and
surface public and private.
surface,
private.” Wis.
Wis
Stats Ch. 281.11
Surface Water Withdrawals
For any agricultural
or irrigation
purpose
‹ 2 million gpd level
for other uses
‹ 10
10--year permits
‹ Riparian rights &
beneficial uses
‹ Cumulative
impacts
‹ Public rights flows
‹
Groundwater Withdrawals
‹
‹
‹
‹
Over 100,000 gpd
subject
bj t tto state
t t
approval
Over 2 million gpd,
th
then
mustt nott impair
i
i
public water rights
Over 5 million gpd in
Great Lakes basin
require approval from
all states & provinces
Great Lakes Compact
negotiations currently
underway
So what are we worried about?
“There’s a gap in Wisconsin’s
water llaw…”
‹ No
limits on groundwater
withdrawals unless exceeding 2
million gallons per day
‹ No explicit authority to deny
approval of high capacity well if
impacts surface waters
‹ No
N requirements
i
t ffor water
t
conservation
‹ No consideration of cumulative
impacts
The “New” Groundwater Law 2003 Wi
Wisconsin
i A
Actt 310
Requires
equ es notification
ot cat o of
o all
a new
e well
e
construction and water use reporting
‹ Expanded DNR authority to consider
environmental
i
l impacts
i
iin iissuing
i
hi
high
h cap
approvals in certain situations
‹ Established Groundwater Management
Areas in 2 parts of state
‹ Created Groundwater Advisory Committee
to advise department and make
recommendations for future legislation
‹
Environmental reviews of high
capacity wells – acute impacts
‹ Groundwater
(GPAs)
Protection Areas
– within 1200 feet of critical surface water
resources
‹ High
water loss
– withdrawals that result in water loss of
>95%
‹ Potential
impact to a spring
– defined
d fi d as >1
1 cfs
f att least
l
t 80% off the
th
time
GPAs:
ORW =
Outstanding
Resource Water
ERW =
Exceptional
Resource Water
Trout Streams
include Class I,
II and III
II,
ORW Lakes
‹
‹
‹
‹
105 out of 15,082
,
lakes
ORW designation
intended
i t d d tto protect
t t
against point source
discharges
Mostly pristine lakes
in forested areas
Recent
R
t petition
titi
tto add
dd
waters to list
Groundwater Management Areas –
Ch i IImpacts
Chronic
Areas of significant
drawdowns and overoverpumping
‹ 150
150--ft drawdown
contour
‹ Water quality
problems (arsenic,
radium,
d
salinity)
l
)
‹ Need for a
coordinated
di t d
management strategy
‹
Groundwater Advisory Committee
Began
ega meeting
eet g in April
p 2005
005
‹ Members appointed by
Governor and Legislature
‹ Municipal, industrial,
agricultural, &
environmental interests
represented
‹ Staffed by DNR
‹ Science and policy advisors
‹ Advise on rule development
p
and further legislation
‹
Groundwater Advisory Committee
‹ Wrapped
up work in Dec.
Dec 2007
‹ Reports delivered to legislature on
schedule
‹ Recommendations did not include
f t
future
legislation,
l i l ti
b
butt offered
ff
d severall
alternative regulatory frameworks
Goals of Workshop
‹
‹
‹
‹
‹
Better understanding
g of lake and
groundwater interactions
How to sort out climate from human
impacts on lake levels?
Predicting potential impacts of proposed
wells as well as determining if impacts
are already
l
d occurring
i
Tools and Resources from a lake scale to
a watershed scale
What can one lake do (AKA when do you
need to bring in the experts)?
Workshop Overview
‹ Science
of groundwater/surface
water interactions
‹ Tools for Understanding Groundwater
and Lake Interactions
‹ Case
C
studies
t di ffrom Wisconsin
Wi
i
‹ Future Opportunities, Policy
Directions, and General Discussion
Science of groundwater and lakes
( f
(surface
water)) interactions
i
i
Tools for Understanding
G
Groundwater
d
and
dL
Lake
k IInteractions
i
‹ Citizen
work (with limited assistance)
(Nauta)
‹ Expanded watershed studies (Nauta)
‹ Multi
Multi--watershed studies (Nauta or
Dunning)
D
i )
‹ Grants (Asplund)
‹ Technical Assistance (Dunning)
Case Studies for Understanding
G
Groundwater
d
and
dL
Lake
k IInteractions
i
‹ Middle
Genessee
Genessee, Walworth Co
(Dunning or Garn)
‹ Silver Lake,
Lake Waukesha Co (Dunning
or Garn)
‹ Crystal
C
t l Lake,
L k Sh
Sheboygan
b
C
Co (Nauta)
(N t )
‹ Central sand plains (Asplund)
Case Studies for Understanding
G
Groundwater
d
and
dL
Lake
k IInteractions
i
‹
‹
‹
‹
Middle
dd e Ge
Genessee,
essee,
Walworth Co
Silver Lake,
Waukesha Co
Crystal Lake,
Sheboygan Co
Central sand plains
Source:UWSP
Source:UWSP
Source:UWSP
Effects of irrigation
1970 –1/4 of the area irrigated
- normal summer stream loss:
25-30%
- normall summer water
t decline:
d li
½ foot
- drought stream loss:
70-90%
- drought water decline:
2-3 feet
Effects of irrigation
If 50% of area irrigated
-drought
drought stream loss:
100%
- drought water decline:
4 - 5 feet
2007:
50-75% of area irrigated
Waushara County Lakes
Long, Huron
Fish, Pine
Source: UWSP
1950s
1994
99
Spring 2006
July
Ju
y 2006
006
NW Waushara County Lakes
1105
Feet ab
bove sea le
evel
1100
1095
1090
Long
Huron
1085
Pine
Fish
1080
1075
1070
1065
1954 1961 1968 1975 1982 1988 1995 2002 2009
Year
NW Waushara County Lakes
‹
‹
‹
‹
‹
‹
Landlocked lakes,, no
outlet
Sandy soils
Lakes near major
regional groundwater
divide
Recent
R
td
declines
li
after
ft
unusually high period
in the 1990s
Short--term drought in
Short
Central WI
Major pumping center
Relative
e Lake Leve
el (5 Feet Inttervals)
Waushara Co Lakes
Marl
Huron
Pleasant
Beans
Pine
Pi
Witters
Long
Fish
Bughs
1954 1960 1965 1971 1976 1982 1987 1993 1998 2004 2009
Year
Waushara Co.
Co Lakes
At sub-continental divide, near pumping
1105
Feet abov
ve sea levell
1100
1095
2
R = 0.0096
1090
1085
2
R = 0.3949
0 3949
1080
2
R = 0.5418
1075
1070
2
R = 0.7118
1065
Jun- Dec- May- Nov- May- Oct- Apr- Oct- Apr1968 1973 1979 1984 1990 1995 2001 2006 2012
Year
Long
Huron
Pine
Fish
Waushara Co.
Co Lakes
Away from divide, distant from pumping
890
Feet above sea levvel
885
880
2
R = 0.0092
875
870
865
2
R = 0.0908
860
855
850
2
R = 0.0006
845
Jun- Dec- May- Nov- May- Oct- Apr- Oct- Apr1968 1973 1979 1984 1990 1995 2001 2006 2012
Year
Gilbert
Bughs
Witters
Water table well
near Hancock, WI
source: US Geological Survey http://groundwaterwatch.usgs.gov
Down 3 ft
Kraft, 2008
Nelsonville
Amherst Jct.
Down 1 ft
Wild Rose
Down 1 ft
Down 3 ft
Wautoma
Water levels unaffected by
pumping
i
Year
1950
1960
1970
1980
1990
PT0276
WS0105
2000
2010
Depth to wa
D
ater (ft) from
m 1959 reference
-10.0
-8.0
-6.0
-4.0
-2.0
0.0
2.0
4.0
60
6.0
PT0015
Kraft, 2008
Water levels affected by
pumping
i
Year
1950
1960
1970
1980
1990
2000
2010
Depth to wa
D
ater (ft) from
m 1959 refe
erence
-10.0
-8.0
-6.0
-4.0
-2.0
0.0
2.0
4.0
60
6.0
PT376_1464
WS0008
Kraft, 2008
Down 3 ft
Kraft, 2008
Nelsonville
Amherst Jct.
Down 1 ft
Wild Rose
Down 1 ft
Down 3 ft
Wautoma
Future Opportunities, Policy
Di
Directions,
i
and
dG
Generall Di
Discussion
i
‹ Lake
Level Monitoring Network
‹ Groundwater monitoring and
modeling
‹ Statewide and Regional Policy
Di
Directions
ti
– Recent Groundwater Legislation
‹ Question
and Answers
‹ Discussion
PROGRESS: Acute Impacts
451 wells approved
pp
under new statute
since 2005; 369 wells constructed
‹ 56 wells constructed within 2000 feet of
GPA
‹ 26 approvals/14 wells located within GPAs
‹ No wells have required
q
full environmental
analysis, but many rere-located to avoid
GPA
‹ Approved wells in GPAs conditioned to
ensure no significant impact to surface
water resource
‹ New
N
administrative
d i i t ti
rules
l iin effect
ff t as off
Sept. 2007 (NR820)
‹
PROGRESS:: GMAs
PROGRESS
‹
‹
‹
‹
Two Groundwater
Management Areas
designated by rule
Purpose
P
off GMA nott
defined
Process for adding
new GMA or removing
designation subject to
future legislation
Groundwater Advisory
Committee report
p
Groundwater Advisory Committee
Began
ega meeting
eet g in April
p 2005
005
‹ Members appointed by
Governor and Legislature
‹ Municipal, industrial,
agricultural, &
environmental interests
represented
‹ Staffed by DNR
‹ Science and policy advisors
‹ Advise on rule development
p
and further legislation
‹
PROGRESS: Groundwater
PROGRESS:
M
Management
A
Areas (Task
(T k 1)
‹
‹
‹
‹
‹
Groundwater Management
g
Plans should be
developed for each GMA
Additional requirements for new and existing high
cap wells in GMA’s
GMA s after 10 years
2 new Groundwater Attention Areas (GAA)
proposed, but no new GMAs
P
Process
f reviewing
for
i i
and
d recommending
di
new
potential GMA’s, as well as removal of
designation
Increased funding and support for mitigation and
monitoring of groundwater and surface water
Task #2: GPA’s
GPA s – Dec.
Dec 2007
‹ Better
definition of springs
‹ Factors to be considered in
determining “significant
significant adverse
environmental impact”
‹ Changes
Ch
regarding
di
regulation
l ti
off
wells within GPAs, near springs, or
with
ith >95%
95% water
t loss
l
‹ Adaptive management approaches
‹ Potential for use of general permits
PROGRESS: Groundwater
PROGRESS:
P
Protection
i A
Areas - consensus
‹
No
o further
u t e definition
de
t o of
o “significant
sg
ca t
adverse environmental impact”
– criteria identified in rule adequate
No change to regulation of wells with high
water loss
‹ Updated springs inventory for rest of state
‹ Regular review of regulatory framework
every 5 years
‹ Comprehensive statewide water
management policy
‹
NO PROGRESS:
PROGRESS: Groundwater
P
Protection
i A
Areas
‹
No consensus on changing definition of
spring, or regulatory approach
– Need to wait for springs
g inventory
‹
No consensus on changes to Groundwater
Protection Area concept or regulatory
approach
– Several alternatives suggested and voted upon
‹
No further action on general permits or
adaptive management
Groundwater Advisory Committee
‹ Wrapped
up work in Dec.
Dec 2007
‹ Reports delivered to legislature on
schedule
‹ Recommendations did not include
f t
future
legislation,
l i l ti
b
butt offered
ff
d severall
alternative regulatory frameworks
‹ Track GAC activities on DNR website:
http://dnr.wi.gov/org/water/dwg/
A first step…
step
Recognizes
g
that all wells have impact
p
on
quantity
‹ Recognizes connection between surface
and groundwater,
groundwater quality and quantity
‹ Many critical waters remain vulnerable
‹ Retains p
protection of p
public water utility
y
wells
‹ Most areas of state and most well
approvals will be “business
business as usual
usual”
‹ Acknowledged need for further solutions,
including legislation
‹
Future Directions
‹
‹
‹
Better science and understanding
– Lake and g
groundwater level monitoring
g
– Quantify impacts of pumping on regional scale
– Identify lakes vulnerable to pumping
Pursue lakelake-specific management options
– Physical/engineering approaches
– Cooperative
C
i
arrangements among water users
– Mitigation/contingency plans in dry periods
Regional/Statewide regulations and incentives
– Better oversight of individual water extractions
– Coordinated water management
Questions?
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