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A worldwide view of organic carbon export from catchments

机译:流域有机碳出口的全球视角

摘要

Growing interest in the effects of global change on the metabolism, stoichiometry and cycling of carbon in aquatic ecosystems has motivated research on the export of organic carbon (OCE) from catchments. In this article, quantitative and functional features of the annual export rates of total, particulate and dissolved organic carbon (TOC, POC and DOC) were reviewed, and the stoichiometry of export (OC:N, OC:P and N:P) from 550 catchments worldwide was reported. TOC export ranged 2.1-92,474 kg C km-2 year-1, POC export ranged 0. 4-73,979 kg C km-2 year-1 and DOC export ranged 1.2-56,946 kg C km-2 year-1. Exports of TOC and DOC were strongly linked, but POC export was unrelated to DOC. The DOC fraction comprised on average 73 ± 21% of TOC export. The export rates of organic carbon were poorly related to those of total nitrogen and total phosphorus. Discrete and continuous environmental variables failed to predict TOC export, but DOC export was influenced by discharge and catchment area worldwide. Models of OCE in different catchment types were controlled by different environmental variables; hydrological variables were generally better predictors of OCE than anthropogenic and soil variables. Elemental ratios of carbon export in most catchments were above the Redfield ratio, suggesting that phosphorus may become the limiting nutrient for downstream plant growth. These ratios were marginally related to environmental data. More detailed hydrological data, consideration of in-stream processes and the use of quasi-empirical dynamical models are advocated to improve our knowledge of OCE rates and those of other nutrients. © 2010 Springer Science+Business Media B.V.
机译:人们越来越关注全球变化对水生生态系统中碳的代谢,化学计量和碳循环的影响,这促使人们对流域有机碳(OCE)的出口进行研究。在本文中,回顾了总量,颗粒和溶解有机碳(TOC,POC和DOC)的年出口率的定量和功能特征,并从中计算出出口的化学计量(OC:N,OC:P和N:P)据报道,全球有550个集水区。第一年的TOC出口量为2.1-92,474 kg C km-2,第一年的POC出口量为0。4-73,979kg C km-2一年,DOC的出口量为1.2-56,946 kg C km-2一年。 TOC和DOC的出口紧密相关,但POC出口与DOC无关。 DOC份额平均占TOC出口的73±21%。有机碳的出口率与总氮和总磷的关系不大。离散和连续的环境变量无法预测TOC的出口量,但是DOC的出口量受到全球排放量和集水面积的影响。不同流域类型的OCE模型受不同环境变量控制;与人为和土壤变量相比,水文变量通常是OCE的更好预测指标。大多数流域的碳出口元素比率都高于Redfield比率,这表明磷可能成为下游植物生长的限制养分。这些比率与环境数据略有相关。提倡更详细的水文数据,考虑河流过程以及使用准经验动力模型,以提高我们对OCE速率和其他营养素速率的了解。 ©2010 Springer Science + Business Media B.V.

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