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Isotope Investigations in Wellhead Protection Areas. Jim Walsh MDH. Isotopes Can Tell Us. How old is it? Where did it come from?. Precipitation and Groundwater from Direct Infiltration Plot on Meteoric Water Line. Krabenhoft, 1990. Mass-balance approach to mixing.
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Isotope Investigations in Wellhead Protection Areas Jim Walsh MDH
Isotopes Can Tell Us • How old is it? • Where did it come from?
Precipitation and Groundwater from Direct Infiltration Plot on Meteoric Water Line Krabenhoft, 1990
Steps in Wellhead Protection Wells In Need of Protection
Develop Conceptual Model
Assess Vulnerability Low High
Isotope Techniques Apply To: • Conceptual model development • Model calibration/validation • Vulnerability assessments
It’s A Protected Aquifer, So I Don’t Need To Worry About Surface Water. Right ?
Elevation (Ft. Above Sea Level) Tritium = 18-39 TU Clay-Rich Till Sand and Gravel
~70% lake water ~10 – 20% lake water
The Case of The Likely Lake • Shallow Buried Drift Aquifer • CFC Recharge Age of 15-25 years
15-60% River Water At Wells Located Within 250’ 100’ 250’ 1,200’ Delta18O (per mil) Date
Low High
Little Geologic Cover • Nitrate and Pesticide Contamination OPDC CSLF CJDN
Delta18O (per mil) Date
How About Those Mine Pits? Dewatered Taconite Pits Keewatin, 1996
Keewatin Wellhead Protection Area With Mesabi Chief Pit Dewatered
Differing Isotope Signatures • Also Differing: • Tritium Results • Water Chemistry (Chloride)
TC Positive • Tritium = 11.6 TU Well Casing Uncased Borehole
Well Casing • TC Negative • Tritium = 6.3 TU Uncased Borehole
Isotopes Are Your Friends For: • Conceptual model development • Model calibration/validation • Vulnerability assessments • Well construction investigations
Thick Unsaturated Zones Peat Till Minnesota River