Title: Southeastern Wisconsin Regional Water Supply Issues and Regional Planning Program Overview and Chall
1Southeastern WisconsinRegional Water Supply
Issuesand Regional Planning Program Overview and
Challenges
- Waukesha County Action Network
- June 28, 2006
118893
2 A Cooperative Program
SE Wisconsin Water Utilities
Seven Southeastern Wisconsin Counties
3Presentation Overview
- Regional Setting
- Water Supply Issues
- Regional Water Supply Planning Program
Background and Status Report - Water Supply Planning Challenges
4- Areas Served by Public and Private Water Supply
Systems in Southeastern Wisconsin 2000
- 2,700 Square Miles (62 west of Divide)
- 2.0 Million People
- Public Water Supply
- Lake Michigan
- Nine Plants (30 systems)
- 1.2 Million People
- 210 mgd
- Groundwater
- 50 Systems
- 400,000 People
- 55 mgd
- Private Water Supply
- 400,000 People
- 40 mgd
5Trends in Water Use in Southeastern Wisconsin
1979-2000(in million gallons per day)
6Trends in Water Use for the Region 1979-2000(in
million gallons per day)
Excludes thermoelectric power generation uses
7Historic Per Capita Water Use in the Southeastern
Wisconsin Region 1979-2000 (gallons per person
per day)
NOTE Figure represents total water use.
Residential water uses among counties is very
similar 60 to 70 gpd.
8General Hydrogeology of Southeast Wisconsin
20 miles
Unconfined aquifer
Lake Michigan
Milwaukee
2200 feet
Maquoketa shale confining unit
Confined sandstone aquifer
Resource assessment requires knowing recharge
and inflows
Source USGS
9Sand and Gravel Aquifer Present as Lenses or
Channel Deposits in Bedrock Valleys
- Sand not present as uniform layer
- Thickness and permeability of sand changes with
location
10Dolomite Aquifer -Silurian dolomite -Fracture-
dominated flow -Only present in east -Important
for municipal and domestic wells
11Sandstone Aquifer -Sandstone,
dolomite -Regionally extensive -Excellent
aquifer -Porous flow -Most high-capacity
wells -Occurs beneath shale in east
Exposure of Sandstone in the Wisconsin Dells
12Relative well depths
tallest buildings 600 ft high
most municipal wells 200-800 ft deep
dolomite
shale
sandstone
granite
13Major Issues
- Groundwater Supply Demand is Rising
- Overuse of the Deep Sandstone Aquifer Has Caused
Large Cone of Depression Up to 500 Feet of
Drawdown - Current Radium Exceedance Issues (22 systems in
Southeastern Wisconsin and 53 in State) - Quality of Deep Sandstone Aquifer Water Is
Declining in Some Wells - Potential for Contamination and Surface Water
Impacts with Increased Use of the Shallow Aquifer
(Conflicts between Water Suppliers and Surface
Water Advocates)
14Regional Water Supply Planning Program
- Three Elements (Coordinated with and Designed to
Complement Local Actions) - Conduct Basic Groundwater Inventories (Completed
in 2001 with PartnersWGNHS and WDNR) - Collect Additional Inventory Data and Develop
Regional Aquifer Simulation Model (Completed with
PartnersUSGS, WGNHS, UW-Milwaukee, WDNR, and SE
Wisconsin Water Utilities) - Prepare Regional Water Supply System Plan
(Planning is Underway with Support from Seven
Counties in Southeastern Wisconsin)
15Second Element Groundwater Model Objectives
- Understand Present GW System
- Study Current and Future Impacts of Groundwater
Use - Water Supply Plan--Simulate Alternative
Management Options - Delineate Contributing Areas for Wellhead
Protection - Provide a Framework for Site-Specific Models and
Studies
16Well Locations and Pumping Rates
Water Levels in the Sandstone Aquifer (feet above
sea level)
Mixed or Intermediate Depth
Shallow
Deep
1880-1900
17Well Locations and Pumping Rates
Water Levels in the Sandstone Aquifer (feet above
sea level)
Mixed or Intermediate Depth
Shallow
Deep
1920-1930
18Well Locations and Pumping Rates
Water Levels in the Sandstone Aquifer (feet above
sea level)
Mixed or Intermediate Depth
Shallow
Deep
1950-1961
19Well Locations and Pumping Rates
Water Levels in the Sandstone Aquifer (feet above
sea level)
Mixed or Intermediate Depth
Shallow
Deep
1990-2000
20The Milwaukee/Chicago cone of depression is one
of the largest areas of groundwater drawdown in
North America
Well Locations and Pumping Rates
Water Levels in the Sandstone Aquifer (feet above
sea level)
Mixed or Intermediate Depth
Shallow
Deep
2010-2020
21Regional Groundwater Modeling Important Initial
Findings
- Pumping Has Altered Groundwater Flow Directions
- Groundwater that Once Flowed Toward Lake Michigan
is Now Intercepted by Pumping and Diverted West
Under the Surface Water Divide Where, After Use,
it is Ultimately Discharged to Surface Water
Within the Mississippi River Basin
1900
2000
22Regional Groundwater Modeling Important Initial
Findings
Water Transferred from Surface Water Within the
SEWRPC Region Accounts for 80 of Combined
Shallow and Deep Pumping
Deep Pumping 33.3mgd
Shallow Pumping 32.5mgd
23Third Element Regional Water Supply Plan
- OVERALL CHALLENGE To Develop a Plan for the
Provision of Long-Term Sources of High-Quality
Water for the Southeastern Wisconsin Region - Determine a Balanced and Efficient Management
Program for Sources of Supply - Lake Michigan
- Shallow Aquifer
- Deep (Regional) Aquifer (with treatment)
- Precipitation
- Infiltration Systems
- Enhanced Precipitation
- Wastewater?
24Third Element Regional Water Supply Plan
Major Plan Components
- Development of water supply service areas and
forecast demand for water use plan year 2035 - Documentation of existing and potential water
supply problems and issues - Development of recommendations for water
conservation efforts to reduce water demand - Development and evaluation of alternative means
of addressing the identified water supply
problems and issues - Selection and documentation of a recommended
plan - Identification of groundwater recharge areas to
be considered for protection - Specification of any new institutional structures
found necessary to carry out the plan
recommendations and - Identification of any constraints to development
levels in subareas of the Region due to water
supply sustainability concerns.
25Planning Challenges
- Study Area Considerations
- Basic Grid Spacing 2,500 feet, or an average of
one-quarter square mile - Includes 18 Layers
- Total of about 600,000 cells
26Planning Challenges
- All Groundwater Use Has Consequences
- Balance Groundwater Water Supply Needs With
Surface Water ImpactsReasonableness
27Planning Challenges
- CHALLENGE Water Conservation
- Determine What Levels Are Achievable and At What
Cost - Balance Conservation and Economic Development
Objectives - Implementation How to Achieve
- Need to Consider Different Situations (Sources of
Supply)
28Water Supply and Comprehensive Planning
Linkages
- Opportunity to Integrate Water Supply and Other
Utility Planning with Land Use and Other
Comprehensive Plan Elements at Regional, County,
and Local Level - Link Reasonably Expected Water Supply Capacities
As One of Several Factors Considered in Future
Land Use Decisions This Requires Water Supply
Facilities Plan - Take Into Account Important Water Supply
Considerations in Establishing Land Use Patterns - Preserve Important Groundwater Recharge Areas
- Protect Existing and Future Well Zone of
Contribution Areas - Promote Local Zoning to Protect Areas Most
Susceptible to Groundwater Contamination
29Water Supply and Comprehensive Planning
Linkages
- Opportunity to Integrate Water Supply and Other
Utility Planning with Land Use and Other
Comprehensive Plan Elements at Regional, County,
and Local Level (contd) - Promote Low Impact and Other Development Patterns
and Stormwater Management Practices Which
Maintain the Natural Hydrology - Potential Limits to Development Density in
Selected Areas to Help Achieve a Safe Water
Supply - Water Conservation?
30Your Turn