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• W1567790969 abstract "An interdisciplinary research program (Geology and Chemistry) at Colby College, Waterville, Maine, is developing a model for surface and groundwater interactions in the Belgrade Lakes watershed. The watershed is a system of seven glacially formed, interconnected lakes in central Maine. Surface and groundwater discharges from the area to the Kennebec River, which empties into the Gulf of Maine. The present study focuses on East Pond, the head of the lake-chain system. East Pond is roughly oval in shape with several coves along the margins; it has an average depth of 4.5 m, a maximum depth of 7.3 m, and a total volume of 26.35 x 10 m. The lake is surrounded by North temperate hardwood forest and a marshy outlet to the other lakes exists in the northwest corner. East Pond has suffered severe yearly algal blooms during the late summer and into the fall since 1993. This project aims to develop a baseline for the geological, geochemical, and hydrochemical parameters through spatial and temporal scales to better understand the lake’s dynamics. It is suspected that changes in water chemistry over the summer may prohibit or promote phosphorus release from the lake bottom, leading to the observed algal bloom. Analyses included: characterization of the lake-bottom sediments, measurement of water-chemistry parameters, and water-quality monitoring throughout the summer. Sediment analysis revealed a substrate that is characterized as an organic rich (mean TOC = 5.42%), moderately well sorted silt (mean grain-size = 4.51 Φ). Total phosphorus concentration in the sediments was elevated with a mean of 0.048%. Total phosphorus" @default.
• W1567790969 created "2016-06-24" @default.
• W1567790969 creator A5081666147 @default.
• W1567790969 date "2004-01-01" @default.
• W1567790969 modified "2023-09-26" @default.
• W1567790969 title "SEDIMENTOLOGICAL AND GEOCHEMICAL CHARACTERIZATION OF EAST POND, BELGRADE LAKES WATERSHED, CENTRAL MAINE" @default.
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• W1567790969 hasPublicationYear "2004" @default.
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