The depletion of hypolimnetic DO and the upper depth boundary of anoxia for four different years (1978, 1979, 1980 and 1981), and the accumulation of sulfide for a single year (1981), are documented for ionically enriched hypereutrophic Onondaga Lake, NY, USA. The depletion rate, represented as the
โฆ LIBER โฆ
Depletion of epilimnetic oxygen and accumulation of hydrogen sulfide in the hypolimnion of Onondaga Lake, NY, U.S.A.
โ Scribed by Steven W. Effler; John P. Hassett; Martin T. Auer; Ned Johnson
- Publisher
- Springer Netherlands
- Year
- 1988
- Tongue
- English
- Weight
- 898 KB
- Volume
- 39
- Category
- Article
- ISSN
- 0049-6979
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The vertical distributions of C1 in the pore waters of the sediments and in the water column of Onondaga Lake, New York, are documented and used to estimate the diffusion flux of C1 across the sediment-water interface, and establish the reduction in lake concentrations that has occurred as a result