爱沙尼亚Võrtsjärv湖流入和流出的碳和营养物通量

P. Pall, S. Vilbaste, T. Kõiv, A. Kõrs, K. Käiro, Alo Laas, P. Nõges, T. Nõges, K. Piirsoo, L. Toomsalu, M. Viik
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引用次数: 15

摘要

测定了总有机碳(TOC)、溶解无机碳(DIC)和有机碳(DOC)、氮、磷和硅在2008-2009年间通过4个主要入海口进入沃尔茨贾夫湖的通量,并将其与湖泊出海口通量进行了比较。2008年,仅这四条主要河流所研究的物质的排放量和负荷就高于该湖泊的排放量。2009年,流出水量大于流入水量,TOC、DIC和DOC的数量也是如此。但养分输入负荷持续高于输出负荷。无论持水量是正的还是负的,湖泊都积累了氮、磷和硅等营养物质,但碳积累和碳排放的平衡取决于湖泊的水收支。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Fluxes of carbon and nutrients through the inflows and outflow of Lake Võrtsjärv, Estonia
We determined the incoming fluxes of total organic carbon (TOC), dissolved inorganic (DIC) and organic carbon (DOC), nitrogen, phosphorus, and silicon via four main inflows into Lake Vortsjarv and compared these with the outgoing fluxes from the lake during 2008-2009. The discharge and loads of the studied substances from the four main rivers alone were higher than the amounts carried out of the lake in 2008. In 2009, the outflow of water exceeded the inflows and this was the case with the amounts of TOC, DIC, and DOC as well. However, the incoming load of nutrients was continuously higher than the outgoing load. The lake accumulated nutrients (nitrogen, phosphorus, and silicon) irrespective of whether water retention was positive or negative, but the balance between carbon accumulation and carbon emission depended on the lake's water budget.
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