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Jared RogersIRWIN PRAIRIE
GROUNDWATER FLOW
REGIME AND DRAINAGE
 World groundwater supply = .61% (Fetter 2001)
Groundwater accounts for >98% of available fresh
water globally
 Relationship to wetlands
Water filtration and storage
Nutrient cycling and transport retention
Flood attenuation
 Better knowledge = Better management
INTRODUCTION:
HYDROLOGY SIGNIFICANCE
 Irwin Prairie State Nature Preserve
Seasonal wetland
Sub-ecotones
wet prairie
Sedge meadow
Swamp forest
Peat layer (confining unit)
Unconfined sand aquifer
Clay aquitard beneath
INTRODUCTION: SITE DESCRIPTION
Photo by: Dr. Todd Crail 12/1/2011
Wet Period
Standing Water
 Measure heads in piezometers and the wetland
 Determine Surface-water and groundwater
interactions
Recharge and discharge
 Plot potentiometric map to determine GW flow
directions
OBJECTIVE
Standing Water
METHODS
Bancroft Avenue
IrwinRoad
Dorr Street
Installation
by Kirk
Zmijewski
METHODS
ELECTRONIC SOUNDING TAPE
WeeklyPrecipitation(inches)
From wunderground.com (2013)-0.5
0.5
1.5
2.5
3.5
4.5
Date
Precipitation
Wetland
bottom
elevation
Pole-E
RESULTS
Sept. 15, 2013
ft. amsl
Weekly measurements
Drawdown rate
B-North and Pole W too far
DISCUSSION
GW flow direction
Divergent and convergent flow
GW and surface-water interaction
GW discharges to the wetland
Wetland recharges GW in Sept.
CONCLUSION
 Dr. James Martin-Hayden
 Dr. Todd Crail
 Mr. Kirk Zmijewski
 Mr. Ryan Schroeder
 Ohio Department of Natural Areas and Preserves
ACKNOWLEDGEMENTS
 Fetter, C.W. Applied Hydrogeology 4th Ed. New Jersey:
Prentice-Hall, Inc. 2001. Text.
REFERENCES

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Irwin Prairie gw flow regime and drainage pp

Editor's Notes

  1. Wetland is a great buffer for water and nutrient (fertilizer N-P) surges: but it cannot withstand chronic pulses of nutrients and or water pumping into our out without forever changing the wetland instrumental functions and intrinsic value N-P-K
  2. Relevant Geologic characteristics are…