On ecological and geochemical significance of evapotranspiration

On ecological and geochemical significance of evapotranspiration ISSN 1067-4136, Russian Journal of Ecology, 2008, Vol. 39, No. 5, pp. 371–374. © Pleiades Publishing, Ltd., 2008. Original Russian Text © Yu.L. Mel’chakov, 2008, published in Ekologiya, 2008, No. 5, pp. 390–393. SHORT COMMUNICATIONS On Ecological and Geochemical Significance of Evapotranspiration Yu. L. Mel’chakov Ural State Pedagogical University, pr. Kosmonavtov 26, Yekaterinburg, 620219 Russia; e-mail: gbf_uspu@mail.ru December 21, 2007 DOI: 10.1134/S106741360805010X Key words: ecosystem functioning under natural conditions, atmospheric transfer, evapotranspiration products. Geochemical ecology is a major research field deal- Ba, Zn, and Cu, n kg; Ti, Br, Cr, Pb, Se, and Ni, 100 × n g; ing with migration of chemical elements in the phyto- Li, Zr, Sc, V, Sb, Ag, Cd, Sn, As, Ga, Hg, and Co, cenosis–environment system. Long-term interest in this 10 × n g. Rare earth metals and some other elements problem is indicated by the number of monographs are transferred in amounts of about 0.1–10 × n g/km published in different countries (Duvigneaud and per year. This type of element migration is an important Tanghe, 1962; Odum, 1971; Biogeochemistry…, component in biogeochemical cycles of almost all ele- 1992), including Russia (Koval’skii, 1974; Kovalevskii, ments occurring in nature. In the aggregate, evapotrans- 1991). http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Russian Journal of Ecology Springer Journals

On ecological and geochemical significance of evapotranspiration

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