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An Analysis of Terrestrial and Aquatic Environmental Controls of Riverine Dissolved Organic Carbon in the Conterminous United States

机译:美国本土河流溶解有机碳的陆地和水生环境控制分析

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Analyses of environmental controls on riverine carbon fluxes are critical for improved understanding of the mechanisms regulating carbon cycling along the terrestrial-aquatic continuum. Here, we compile and analyze riverine dissolved organic carbon (DOC) concentration data from 1402 United States Geological Survey (USGS) gauge stations to examine the spatial variability and environmental controls of DOC concentrations in the United States (U.S.) surface waters. DOC concentrations exhibit high spatial variability in the U.S., with an average of 6.42 ± 6.47 mg C/L (Mean ± Standard Deviation). High DOC concentrations occur in the Upper Mississippi River basin and the southeastern U.S., while low concentrations are mainly distributed in the western U.S. Soil properties such as soil organic matter, soil water content, and soil sand content mainly show positive correlations with DOC concentrations; forest and shrub land have positive correlations with DOC concentrations, but urban area and cropland demonstrate negative impacts; and total instream phosphorus and dam density correlate positively with DOC concentrations. Notably, the relative importance of these environmental controls varies substantially across major U.S. water resource regions. In addition, DOC concentrations and environmental controls also show significant variability from small streams to large rivers. In sum, our results reveal that general multi-linear regression of twenty environmental factors can partially explain (56%) the DOC concentration variability. This study also highlights the complexity of the interactions among these environmental factors in determining DOC concentrations, thus calls for processes-based, non-linear methodologies to constrain uncertainties in riverine DOC cycling.
机译:对河流碳通量进行环境控制分析对于增进对沿陆-水连续体的碳循环调节机制的了解至关重要。在这里,我们汇总并分析了1402个美国地质调查局(USGS)计量站的河流溶解性有机碳(DOC)浓度数据,以检查美国(美国)地表水中DOC浓度的空间变异性和环境控制。 DOC浓度在美国表现出很高的空间变异性,平均为6.42±6.47 mg C / L(均值±标准差)。 DOC浓度高发生在密西西比河上游流域和美国东南部,而低浓度则主要分布在美国西部。土壤特性如土壤有机质,土壤水分和土壤沙含量主要与DOC浓度呈正相关;森林和灌木地与DOC浓度呈正相关,但城市地区和农田显示出负面影响;总河中磷和大坝密度与DOC浓度成正相关。值得注意的是,这些环境控制措施的相对重要性在美国主要水资源区域之间存在很大差异。此外,DOC浓度和环境控制也显示出从小河到大河的显着变化。总而言之,我们的结果表明,二十种环境因素的一般多线性回归可以部分解释(56%)DOC浓度变异性。这项研究还强调了确定DOC浓度时这些环境因素之间相互作用的复杂性,因此需要基于过程的非线性方法来限制河流DOC循环中的不确定性。

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