The use of groundwater tracers, including {sup 36}Cl, {delta}{sup 18}O, and {delta}{sup 2}JH, in the study fo the Magothy aquifer, Maryland
- Univ. of Maryland, College Park, MD (United States); and others
The recent conclusion of a study of groundwater from the Magothy Formation, Maryland allows for an examination of processes occurring in this aquifer system. Water samples were gathered from a wide area along flow paths estimated from hydrological parameters and analyzed for the major cations and anions, nutrients, and {sup 87}Sr/{sup 86}Sr ratios, in addition to {sup 36}Cl, {delta}{sup 18}O, and {delta}{sup 2}H. Also, three samples that contained anomalously high {sup 36}Cl/Cl ratios were analyzed for {sup 3}H in an attempt to determine possible sources for those readings. A comparison of the results of this study to those of a previous study conducted by this group of the overlying Aquia Aquifer will also be given. The potential of inter-aquifer mixing between the two systems in some areas and of matching {sup 36}Cl and Cl{sup -} values to sea level rise and fall will be discussed.
- OSTI ID:
- 126696
- Report Number(s):
- CONF-950402-; TRN: 95:006086-0706
- Resource Relation:
- Conference: 209. American Chemical Society (ACS) national meeting, Anaheim, CA (United States), 2-6 Apr 1995; Other Information: PBD: 1995; Related Information: Is Part Of 209th ACS national meeting; PB: 2088 p.
- Country of Publication:
- United States
- Language:
- English
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