Estimating groundwater inflow and leakage outflow for an intermontane lake with a structurally complex geology: Georgetown Lake in Montana, USA
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- 作者：Glenn D. Shaw ; Katie L. Mitchell ; Christopher H. Gammons
- 关键词：Stable isotopes ; Groundwater/surface ; water relations ; Groundwater recharge/water budget ; Lake ; USA
- 刊名：Hydrogeology Journal
- 出版年：2017
- 出版时间：February 2017
- 年：2017
- 卷：25
- 期：1
- 页码：135-149
- 全文大小：
- 刊物类别：Earth and Environmental Science
- 刊物主题：Hydrogeology; Hydrology/Water Resources; Geology; Water Quality/Water Pollution; Geophysics/Geodesy; Waste Water Technology / Water Pollution Control / Water Management / Aquatic Pollution;
- 出版者：Springer Berlin Heidelberg
- ISSN：1435-0157
- 卷排序：25
文摘
Stable isotopes of the water molecule (δ18O and δD) for groundwater, lake water, streams, and precipitation were coupled with physical flux measurements to investigate groundwater–lake interactions and to establish a water balance for a structurally complex lake. Georgetown Lake, a shallow high-latitude high-elevation lake, is located in southwestern Montana, USA. The lake is situated between two mountain ranges with highlands primarily to the east and south of the lake and a lower valley to the west. An annual water balance and (δ18O and δD) isotope balance were used to quantify annual groundwater inflows of 2.5 × 107 m3/year and lake leakage outflows of 1.6 × 107 m3/year. Roughly, 57% of total inflow to the lake is from groundwater, and 37% of total outflow at Georgetown Lake is groundwater. Stable isotopes of groundwater and springs around the lake and surrounding region show that the east side of the lake contains meteoric water recharged annually from higher mountain sources, and groundwater discharge to the lake occurs through this region. However, springs located in the lower western valley and some of the surrounding domestic wells west of the lake show isotopic enrichment indicative of strong to moderate evaporation similar to Georgetown Lake water. This indicates that some outflowing lake water recharges groundwater through the underlying west-dipping bedrock in the region.