Abstract
The paper discusses the results derived from the analysis of the vertical distribution of nitrates in the Black Sea density field during the winter of 1994. It has been shown that in the absence of winter-time convective mixing of waters, the vertical structure of nitrates is isopycnically defined. Maximum nitrates concentration persists throughout the warm period, normally changing from 5 to 9 μmol in the deep-water part of the area, and has not altered, in comparison with the 1980 data.
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References
Sapozhnikov, V.V. and Lukashev, Yu.F. The cause of the variable vertical distribution of nitrogen compounds in suanaerobic and anaerobic waters (Arabian Sea and Black Sea).Okeanologia (1989)29, 423–428.
Sapozhnikov, V.V. Novel views about hydrochemical structure of the Black Sea. In:Variability of the Black Sea Ecosystem. Natural and Anthropogenic Factors. Moscow: Nauka (1991), pp. 34–46.
Vinogradov, M.E. and Nalbandov, Yu.R. The effect of changing density upon the distribution of phsical, chemical and biological characteristics of the Black Sea ecosystem.Okeanologia (1990)30, 769–777.
Eremeev, V.N., Konovalov, S.K. and Romanov, A.S. Investigation of the formation of vertical structure of biogenic elements fields in the Black Sea, using the method of spatial isopycnic analysis.Phys. Oceanogr. (1997)8, 389–402.
Basturk, O., Saydam, S., Salihoglu, I.,et al. Vertical variations in the principal chemical properties of the Black Sea in the autumn of 1991.Mar. Chem. (1994)45, 149–165.
Codispoti, L.A., Friederich, G.E., Murray J.W.,et al. Chemical variability in the Black Sea: implications of continuous vertical profiles that penetrated the oxic/anoxic interface.Deep-Sea Res. (1991)38, 691–710.
Saydam, C., Tugril, S., Basturk, O.,et al. Identification of the oxic/anoxic interface surfaces in the Black Sea.Deep-Sea Res. (1993)40, 1405–1412.
Methods of Hydrochemical Investigations of Ocean. Moscow: Nauka (1978).
Fluid Dynamics and Plankton Productivity in the Black Sea. Moscow: Acad. Sci. USSR (1988).
Murray, J.W., Codispoti, L.A. and Friederich, G.E. Redox environments: the suboxic zone in the Black Sea.Am. Chem. Soc. Advances in Chemistry Series (1995) No. 244, 157–176.
Lukashev, Yu.F., Gusarova, A.N., Nalbandov, Yu.R.,et al. Hydrological-chemical structure of the upper 200-m layer in the Black Sea. In:Current State of the Black Sea Ecosystem. Moscow: Nauka (1987), pp. 13–28.
Sorokin, Yu.I.Black Sea. Moscow: Nauka (1982).
Vinogradov, M.E., Sapozhnikov, V.V. and Shushkina, O.A.Black Sea Ecosystems. Moscow: Nauka (1992).
Krivenko, O.V. The role of biotic circulation of nitrogen in the formation of chemical structure of waters in the coastal and open Black Sea areas. In:Multidisciplinary Ecological Investigations of the Black Sea. Sevastopol: MHI (1995), pp. 121–134.
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Translated by Vladimir A. Puchkin.
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Kirikova, M.V., Gevorgiz, N.S. Analysis of the nitrate distribution in the Black Sea density field. Phys. Oceanogr. 9, 339–346 (1998). https://doi.org/10.1007/BF02522729
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DOI: https://doi.org/10.1007/BF02522729