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Simulating dissolved organic carbon dynamics at the swedish integrated monitoring sites with the integrated catchments model for carbon, INCA-C.利用碳综合集水区模型 INCA-C 模拟瑞典综合监测站点的溶解有机碳动态。
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本文引用的文献

1
Recovery of soil water, groundwater, and streamwater from acidification at the Swedish integrated monitoring catchments.瑞典综合监测集水区酸化后土壤水、地下水和河流水的恢复。
Ambio. 2011 Dec;40(8):836-56. doi: 10.1007/s13280-011-0207-8.
2
Decreased DOC concentrations in soil water in forested areas in southern Sweden during 1987-2008.1987-2008 年间瑞典南部森林地区土壤水中 DOC 浓度降低。
Sci Total Environ. 2011 Apr 15;409(10):1916-26. doi: 10.1016/j.scitotenv.2011.02.017. Epub 2011 Mar 5.
3
Decreasing DOC trends in soil solution along the hillslopes at two IM sites in southern Sweden--geochemical modeling of organic matter solubility during acidification recovery.在瑞典南部的两个 IM 站点的山坡上,土壤溶液中的 DOC 趋势下降——酸化恢复过程中有机质溶解度的地球化学模拟。
Sci Total Environ. 2010 Dec 1;409(1):201-10. doi: 10.1016/j.scitotenv.2010.09.023.
4
Increased dissolved organic carbon (DOC) in Central European streams is driven by reductions in ionic strength rather than climate change or decreasing acidity.中欧河流中溶解有机碳(DOC)的增加是由离子强度降低驱动的,而非气候变化或酸度降低。
Environ Sci Technol. 2009 Jun 15;43(12):4320-6. doi: 10.1021/es803645w.
5
Dissolved organic carbon trends resulting from changes in atmospheric deposition chemistry.大气沉降化学变化导致的溶解有机碳趋势
Nature. 2007 Nov 22;450(7169):537-40. doi: 10.1038/nature06316.
6
Temperature sensitivity of soil carbon decomposition and feedbacks to climate change.土壤碳分解的温度敏感性及其对气候变化的反馈
Nature. 2006 Mar 9;440(7081):165-73. doi: 10.1038/nature04514.
7
Long-term increases in surface water dissolved organic carbon: observations, possible causes and environmental impacts.地表水溶解有机碳的长期增加:观测结果、可能原因及环境影响
Environ Pollut. 2005 Sep;137(1):55-71. doi: 10.1016/j.envpol.2004.12.031.
8
Chemical response of lakes in the Adirondack Region of New York to declines in acidic deposition.纽约阿迪朗达克地区湖泊对酸性沉降减少的化学反应。
Environ Sci Technol. 2003 May 15;37(10):2036-42. doi: 10.1021/es020924h.

瑞典综合监测点河岸带区域对溪流水中溶解有机碳浓度的影响。

Riparian zone influence on stream water dissolved organic carbon concentrations at the Swedish integrated monitoring sites.

机构信息

Department of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences, P.O. Box 7050, 750 07 Uppsala, Sweden.

出版信息

Ambio. 2011 Dec;40(8):920-30. doi: 10.1007/s13280-011-0199-4.

DOI:10.1007/s13280-011-0199-4
PMID:22201006
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3357875/
Abstract

Short-term variability in stream water dissolved organic carbon (DOC) concentrations is controlled by hydrology, climate and atmospheric deposition. Using the Riparian flow-concentration Integration Model (RIM), we evaluated factors controlling stream water DOC in the Swedish Integrated Monitoring (IM) catchments by separating out hydrological effects on stream DOC dynamics. Model residuals were correlated with climate and deposition-related drivers. DOC was most strongly correlated to water flow in the northern catchment (Gammtratten). The southern Aneboda and Kindla catchments had pronounced seasonal DOC signals, which correlated weakly to flow. DOC concentrations at Gårdsjön increased, potentially in response to declining acid deposition. Soil temperature correlated strongly with model residuals at all sites. Incorporating soil temperature in RIM improved model performance substantially (20-62% lower median absolute error). According to the simulations, the RIM conceptualization of riparian processes explains between 36% (Kindla) and 61% (Aneboda) of the DOC dynamics at the IM sites.

摘要

短期河川水中溶解性有机碳(DOC)浓度的变化受水文学、气候和大气沉降的控制。利用河岸带水流-浓度综合模型(RIM),我们通过分离出对河川 DOC 动态的水文效应,评估了瑞典综合监测(IM)流域中控制河川水中 DOC 的因素。模型残差与气候和沉积相关驱动因素相关。DOC 与北部集水区(Gammtratten)的水流关系最密切。南部的 Aneboda 和 Kindla 集水区具有明显的季节性 DOC 信号,与水流关系较弱。Gårdsjön 的 DOC 浓度增加,可能是由于酸沉降减少所致。土壤温度与所有站点的模型残差密切相关。在 RIM 中纳入土壤温度可大大提高模型性能(中位数绝对误差降低 20-62%)。根据模拟结果,RIM 对河岸带过程的概念化解释了 IM 站点中 36%(Kindla)到 61%(Aneboda)的 DOC 动态。