Flux of reduced chemical constituents (Fe2+, Mn2+, NHinf4sup+ and CH4) and sediment oxygen demand in Lake Erie

Author:

Adams Donald D.,Matisoff Gerald,Snodgrass William J.

Publisher

Springer Science and Business Media LLC

Subject

Aquatic Science

Reference35 articles.

1. Berner, R. A., 1980. Early Diagenesis: a Theoretical Approach. Princeton University Press, Princeton, N.J. 241 pp.

2. Blanton, J. O. & Winklhofer, R. A., 1972. Physical processes affecting the hypolimnion of the central basin of Lake Erie. In: Burns, N. M. & Ross, C. (Eds.) Project Hypo — an Intensive Study of the Lake Erie Central Basin Hypolimnion and Related Surface Water Phenomena, pp. 9–38. U.S.E.P.A. Tech. Report TS-05–71–208–24

3. Bouldin, D. R., 1968. Models for describing the diffusion of oxygen and other mobile constituents across the mud-water interface. J. Ecol. 56: 77–87.

4. Bowman, G. T. & Delfino, J. J., 1980. Sediment oxygen demand techniques: A review and comparison of laboratory and in situ systems. Water Res. 14: 491–499.

5. Burns, N. M. & Ross, C., 1972. Oxygen-nutrient relationships within the Central Basin of Lake Erie. In: Burns, N. M. & Ross, C. (Eds.) Project Hypo — an Intensive Study of the Lake Erie Central Basin Hypolimnion and Related Surface Water Phenomena, pp. 85–119. U.S.E.P.A. Tech. Report TS-05–71–208–24

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