Cited by 30Atmospheric and Environmental Gas DynamicsAquatic Ecosystems and Phytoplankton DynamicsPeatlands and Wetlands Ecology

Summer Methane Fluxes and Fall Oxygen Resources of Onondaga Lake

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Addess, Jeffrey M., Effler, Steven W.·1996·Lake and Reservoir Management

Abstract

The sediment release and cycling of CH4 in SO2− 4 – rich hypereutrophic Onondaga Lake, New York, was assessed for the summer/fall interval of 1989 through a program of collection and analysis of ebullitive gas and monitoring of the lake's water column for dissolved CH4. Approximately 1×107 mol of CH4 were released from the lake's sediments, at an average rate of 16 mmol/m2/d, from mid-June to mid-September; two-thirds was dissolved, one-third was in the gas phase. About 75% of the ebullitive release of CH4, or 25% of the total release, was lost from the lake to the atmosphere. Strong temporal variations in ebullitive flux were observed. Oxidation of entrained hypolimnetic accumulations of CH4 contributed importantly to the major depletion of O2 and highly undersaturated conditions observed for the lake's upper layers during the fall mixing period. This water quality problem is a manifestation of the cultural eutrophication of the lake.

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  • The hypereutrophic condition of Onondaga Lake caused subsequent accumulation of reduced byproducts of anaerobic metabolism, including sulfide and methane.

    “subsequent accumulation of reduced byproducts of anaerobic metabolism, including ∑S 2(Effler et al. 1988) and CH4 (Addess and Effler 1996)”
  • The vertical pattern of progressive increases with depth is recurring for the byproducts of the various metabolic pathways, reflecting localization of decomposition processes within the sediments or at the sediment-water interface in combination with limited mixing within the hypolimnion.

    “This vertical pattern is recurring for the byproducts of the various metabolic pathways (Fig. 4b-e), reflecting the localization of these decomposition processes within the sediments (or at the sediment-water interface) in combination with limited mixing within the hypolimnion (Effler et al. 1988, Addess and Effler 1996).”
  • By the onset of fall turnover, CH4 and ∑S 2- were eliminated from the water column as a result of rapid oxidation.

    “By the onset of fall turnover, CH 4 and ∑S 2were eliminated from the water column as a result of the rapid oxidation of these constituents (Effler et al. 1988, Addess and Effler 1996, Gelda and Auer 1996).”

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Research works printed but not linked: 13

  1. Addess, J. M. 1990. Methane cycling in Onondaga Lake, New York. M.S. thesis, College of Environmental Science and Forestry, State University of New York, Syracuse, NY.
  2. Bowie, G. L., W. B. Mills, D. B. Porcella, C. L. Campbell, J. R. Pagenkopf, G. L. Rupp, K. M. Johnson, P. W. H. Chan, S. A. Gherini and C. Chamberlain. 1985. Rates, constants, and kinetic formulations in surface water quality modeling, 2nd edition, EPA/600/3-85/040. U.S. Environmental Protection Agency, Athens, GA. 455 p.
  3. Driscoll, C. T., S. W. Effler and S. M. Doerr. 1996. Anoxic organic carbon decomposition and the distribution of related chemical species (Chapter 5). In S. W. Effler (ed.). Limnological and engineering analysis of a polluted urban lake. Prelude to environmental management of Onondaga Lake, New York. Springer-Verlag, NY (in press).
  4. Effler, S. W. (ed.). 1996. Limnological and engineering analysis of a polluted urban lake. Prelude to environmental management of
  5. Onondaga Lake, New York. Springer-Verlag, NY (in press). Effler, S. W., C. M. Brooksand K. A. Whitehead. 1996. Domestic waste
  6. Effler, S. W., J. P. Hassett, M. T. Auer and N. Johnson. 1988. Depletion of epilimnetic oxygen and accumulation of hydrogen sulfide in the hypolimnion of Onondaga Lake, NY, USA. Wat., Air, Soil Pollut. 39: 59-74. inputs of nitrogen and phosphorus to Onondaga Lake, and water quality implications. Lake and Reserv. Manage. 12(1):127-140.
  7. Effler, S. W. and R. D. Hennigan. 1996. Onondaga Lake, New York: legacy of pollution. Lake and Reserv. Manage. 12(1):1-13.
  8. Effler,S. W. and E. M. Owens. 1996. Densitystratificationin Onondaga Lake: 1968-1994. Lake and Reserv. Manage. 12(1):25-33.
  9. Gelda, R. K. and M. T. Auer. 1996. Development and testing of a dissolved oxygen model for a hypereutrophic lake. Lake and Reserv. Manage. 12(1):165-179.
  10. Kelly, C. A. and D. P. Chynoweth. 1979. Methanogenesis: a measure of chemoorganotrophic (heterotrophic) activity in anaerobic lake sediments. In:J.W. Costerson and R.R. Colwell (eds.). Native aquatic bacteria: enumeration, activity, and ecology, American Society for Testing and Materials, ASTM STP 695:164-179.
  11. Owens, E. M. and S. W. Effler. 1996. Hydrodynamics and transport (Chapter 4). In S.W. Effler (ed.). Limnological and engineering analysis of a polluted urban lake. Prelude to environmental management of Onondaga Lake, New York. Springer-Verlag, NY (in press).
  12. Rowell, H. C. 1995. Paleolimnology of Onondaga Lake: the history of anthropogenic impacts on water quality. Lake and Reserv. Manage. 12(1):35-45.
  13. Tango, P. J. and N. H. Ringler. 1996. The role of pollution and external refugia in structuring the Onondaga Lake fish community. Lake and Reserv. Manage. 12(1):81-90.

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Authors
Addess, J. M., & Effler, S. W.
Affiliations
Upstate Freshwater Institute (US)
Venue
Lake and Reservoir Management
Published
1996-03
Volume
12
Issue
1
Pages
91-101
ISSN
  • 0743-8141 (ISSN-L)
  • 1040-2381
  • 2151-5530
OpenAlex
W2037604090
Cited by
30
References
1
Citations by year
2022: 2 · 2021: 1 · 2016: 1
FWCI
3.72
Type
journal article
Language
en
Open access
Locations
Lake and Reservoir Management (publishedVersion)
Topics
  • Physical Sciences › Environmental Science › Global and Planetary Change › Atmospheric and Environmental Gas Dynamics
  • Physical Sciences › Environmental Science › Environmental Chemistry › Aquatic Ecosystems and Phytoplankton Dynamics
  • Physical Sciences › Environmental Science › Ecology › Peatlands and Wetlands Ecology
Keywords
methane flux, Onondaga Lake, ebullition, dissolved methane, sulfate reduction, hypereutrophic lakes, cultural eutrophication, methane oxidation, hypolimnion, dissolved oxygen depletion

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