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Studies of Adirondack Mountain (N. Y. ) lakes: limnological characteristics and sediment diatom - water chemistry relationships

Thesis/Dissertation ·
OSTI ID:6134713
The author investigated the limnology of six small lakes located along an elevational gradient in the Adirondack Mountains (N.Y.). The lakes are all dilute, poorly buffered, and unproductive. Summer lake average pH (7.1 to 4.6) and alkalinity (73 to -32 ..mu..eg/L) decrease continuously with increasing elevation as do concentrations of Ca (142 to 68 ..mu..eq/L) and Mg (24 to 14 ..mu..eq/L). Total Al concentrations are high (August 1979 values ranged from 31 to 701 ..mu..g/L), and increase toward higher elevations. Differences in chemistry among the lakes appear to be controlled primarily by watershed characteristics, including precipitation, evapo-transpiration, weathering rate, and rates of nutrient uptake by plants. In two lakes, loss of S to the sediment and production of alkalinity appear to be important proceses modifying hypolimnetic chemistry. Trophic status of the lakes ranges from ultraoligotrophic to ligomesotrophic, based on summer lake average concentrations of total P (3.1 to 6.3 ..mu..g/L) and chlorophyll a (0.3 to 2.9 ..mu..g/L). Composition of phytoplankton, zooplankton, aquatic macrophytes, and fish assemblages varies with elevation and lakewater pH. The author also studied the relationships between surface sediment diatom assemblages and lakewater characteristics in a suite of 37 diverse Adirondack lakes. The distribution of diatoms along lake chemical gradients was examined using reciprocal averaging ordination, cluster analysis, and regression techniques. Alkalinity, pH, and concentrations of Ca, Mg, and Na correlated closely with diatom distributions. Total P, chlorophyll a, color, SO/sub 4/, Cl, lake surface area, and mean depth were not important in explaining differences among assemblages.
OSTI ID:
6134713
Country of Publication:
United States
Language:
English