Abstract
The results of daily observations of the vertical distribution of concentrations of different P forms in the Mozhaisk Reservoir in the summer of 1989, 1990, and 1996 are analyzed. The specific features of this distribution are discussed in connection with the conditions of the water vertical mixing in the water body. Variations in the vertical gradients of P forms concentrations are correlated with variations in the surface water temperature that reflects the alternations of synoptic conditions during observation periods.
Similar content being viewed by others
REFERENCES
Datsenko, Yu.S., Vestn. Mosk. Univ., Ser. 5: Geogr., 1992, no. 2, p. 33.
Datsenko, Yu.S., Vodn. Resur., 1998, vol. 25, no. 4, p. 507.
Ershova, M.G., Nemal'tsev, A.S., Puklakov, V.V., and Sakharova, M.I., Problemy gidrologii i gidroekologii (Problems of Hydrology and Environmental Geology), Moscow: Mosk. Gos. Univ., 1999, no. 1, p. 282.
Modelirovanie rezhima fosfora v dolinnom vodokhranilishche (Modeling Phosphorus Regime in a Valley Reservoir), Moscow: Mosk. Gos. Univ., 1995.
Elementy krugovorota fosfora v vodoemakh (Elements of Phosphorus Cycle in Water Bodies), Leningrad: Nauka, 1987.
Eutrophication of Waters: Monitoring, Assesment and Control, Paris: OECD, 1982.
Strickland, J.D.H. and Parsons, T.R., Bull. Fish. Res. Board Can., 1968, vol. 167, p. 1.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Datsenko, Y.S. Vertical Distribution of Phosphorus Concentrations in the Mozhaisk Reservoir in Summer. Water Resources 29, 327–332 (2002). https://doi.org/10.1023/A:1015688531754
Issue Date:
DOI: https://doi.org/10.1023/A:1015688531754