Seepage measurements from Long Lake,Indiana Dunes National Lakeshore |
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| Authors: | S A Isiorho F M Beeching P M Stewart R L Whitman |
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| Institution: | (1) Geosciences Dept., Indiana University – Purdue University Fort Wayne (IPFW), Fort Wayne, IN 46805, USA, IN;(2) National Biological Service, 1100 N. Mineral Springs Raod, Porter, IN 46304, USA, US |
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| Abstract: | Long Lake, located near Lake Michigan within the dune-complexes of Indiana Dunes National Lakeshore, USA, was formed some
time during the Pleistocene and Holocene epochs. A surficial aquifer underlies Long Lake, which is either a source or sink
for the later. The hydrologic processes in the lakeshore and surrounding environs have been significantly altered during the
agricultural, municipal, and industrial development of the region. Limited data suggest that the organisms of Long Lake have
elevated levels of several contaminants. This study attempts to quantify seepage within the lake to assess the potential threat
to groundwater quality. Seepage measurements and minipiezometric tests were used to determine seepage within the lake. Seepage
measurements and minipiezometric tests suggest that water seeps out of Long Lake, thus recharging the groundwater that flows
southwest away from the lake. There is a great deal of variability in the seepage rate, with a mean of 11.5×10–4±11.2×10–4 m d–1. The mean seepage rate of 0.3 m yr–1 for Long Lake is greater than the 0.2 m yr–1 recharge rate estimated for the drainage basin area. The Long Lake recharge volume of 2.5×105 m3 yr–1 is approximately 22% of the volume of the lake and is significant when compared to the total surface recharge volume of 4.8×105 m3 yr–1 to the upper aquifer of the drainage area. There is a potential for contamination of the groundwater system through seepage
from the lake from contaminants derived from aerial depositions.
Received: 16 August 1995 · Accepted: 18 September 1995 |
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| Keywords: | Long Lake Seepage Minipiezometers Indiana Dunes National Lakeshore |
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