Double-diffusive deep water circulation in an iron-meromictic lake-Reference-Cited by-同舟云学术

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Double-diffusive deep water circulation in an iron-meromictic lake

Published:2009-06 Issue:6 Volume:10 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Boehrer Bertram¹,Dietz Severine²,von Rohden Christoph³,Kiwel Uwe¹,Jöhnk Klaus D.⁴,Naujoks Sandra¹,Ilmberger Johann³,Lessmann Dieter²

Affiliation:

1. Helmholtz Centre for Environmental Research; Brueckstrasse 3a,; D-39114; Magdeburg; Germany

2. Department of Freshwater Conservation; Brandenburg University of Technology; D-03013; Cottbus; Germany

3. Institute of Environmental Physics; University of Heidelberg; D-69120; Heidelberg; Germany

4. Department of Limnology of Stratified Lakes; Leibniz Institute of Freshwater Ecology and Inland Fisheries; Neuglobsow,; D-16775; Stechlin; Germany

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference37 articles.

1. Transport processes of copper and zinc in a highly eutrophic and meromictic lake;Baccini;Aquat. Sci.,1981

2. Stratification of lakes;Boehrer;Rev. Geophys.,2008

3. Stratification of very deep, thermally stratified lakes;Boehrer;Geophys. Res. Lett.,2008

4. Numerical prognosis for salinity profiles of future lakes in the open cast mine Merseburg-Ost;Böhrer;Int. J. Salt Lake Res.,1998

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