Jiří Kopáček1, Jiří Kaňa1, Eva Kaštovská2

  • 1Biology Centre CAS, Institute of Hydrobiology, CZ-370 05 České Budějovice, Czech Republic; University of South Bohemia, Faculty of Science, CZ-370 05 České Budějovice, Czech Republic.

概括

大气中沉积最初增加了塔特拉山脉湖泊中酸盐的泄. 然而,最近的变暖趋势可能会通过增强植被生长和土壤碳可用性来减少和酸盐出口.