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1
Identity and yields of major halogenated products of aquatic fulvic acid chlorination.水生富里酸氯化主要卤化产物的特性与产率
Environ Sci Technol. 1983 Oct 1;17(10):625-8. doi: 10.1021/es00116a012.
2
Riparian zone influence on stream water dissolved organic carbon concentrations at the Swedish integrated monitoring sites.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。
Ambio. 2011 Dec;40(8):920-30. doi: 10.1007/s13280-011-0199-4.
3
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.
4
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.
5
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.
6
The importance of the relationship between scale and process in understanding long-term DOC dynamics.理解长期 DOC 动态中规模与过程之间关系的重要性。
Sci Total Environ. 2010 Jun 1;408(13):2768-75. doi: 10.1016/j.scitotenv.2010.02.046. Epub 2010 Apr 15.
7
Quantifying the drivers of the increasing colored organic matter in boreal surface waters.量化北方地区地表水中有色有机物增加的驱动因素。
Environ Sci Technol. 2010 Apr 15;44(8):2975-80. doi: 10.1021/es903179j.
8
Aluminium concentrations in Swedish forest streams and co-variations with catchment characteristics.瑞典森林溪流中的铝浓度及其与集水区特征的共同变化。
Environ Monit Assess. 2010 Jul;166(1-4):609-24. doi: 10.1007/s10661-009-1027-1. Epub 2009 Jun 20.
9
Testing seasonal and long-term controls of streamwater DOC using empirical and process-based models.使用基于经验和过程的模型测试溪水溶解有机碳的季节性和长期控制因素。
Sci Total Environ. 2008 Dec 15;407(1):698-707. doi: 10.1016/j.scitotenv.2008.10.002. Epub 2008 Oct 30.
10
Long-term increase in dissolved organic carbon in streamwaters in Norway is response to reduced acid deposition.挪威河流水体中溶解有机碳的长期增加是对酸沉降减少的响应。
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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。

Simulating dissolved organic carbon dynamics at the swedish integrated monitoring sites with the integrated catchments model for carbon, INCA-C.

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):906-19. doi: 10.1007/s13280-011-0203-z.

DOI:10.1007/s13280-011-0203-z
PMID:22201005
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3357881/
Abstract

Surface water concentrations of dissolved organic carbon ([DOC]) are changing throughout the northern hemisphere due to changes in climate, land use and acid deposition. However, the relative importance of these drivers is unclear. Here, we use the Integrated Catchments model for Carbon (INCA-C) to simulate long-term (1996-2008) streamwater [DOC] at the four Swedish integrated monitoring (IM) sites. These are unmanaged headwater catchments with old-growth forests and no major changes in land use. Daily, seasonal and long-term variations in streamwater [DOC] driven by runoff, seasonal temperature and atmospheric sulfate (SO₄(2-)) deposition were observed at all sites. Using INCA-C, it was possible to reproduce observed patterns of variability in streamwater [DOC] at the four IM sites. Runoff was found to be the main short-term control on [DOC]. Seasonal patterns in [DOC] were controlled primarily by soil temperature. Measured SO₄(2-) deposition explained some of the long-term [DOC] variability at all sites.

摘要

由于气候、土地利用和酸沉降的变化，北半球地表水溶解有机碳（DOC）浓度正在发生变化。然而，这些驱动因素的相对重要性尚不清楚。在这里，我们使用综合流域碳模型（INCA-C）来模拟瑞典四个综合监测（IM）站点的长期（1996-2008 年）河流水 DOC。这些是无人为管理的源头集水区，拥有原始森林，土地利用没有重大变化。所有站点均观测到径流量、季节性温度和大气硫酸盐（SO₄(2-))沉积驱动的河流水 DOC 的日变化、季节变化和长期变化。利用 INCA-C，可以重现四个 IM 站点河流水 DOC 观测到的变化模式。径流量被认为是 DOC 的主要短期控制因素。DOC 的季节性模式主要受土壤温度控制。测量的 SO₄(2-)沉积解释了所有站点的部分长期 DOC 变异性。