School of Environmental and Municipal Engineering, Lanzhou Jiaotong University, Lanzhou 730070, China; Cryosphere Research Station on the Qinghai-Tibetan Plateau, State Key Laboratory of Cryospheric Science, Northwest Institute of the Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China.
School of Environmental and Municipal Engineering, Lanzhou Jiaotong University, Lanzhou 730070, China.
Sci Total Environ. 2018 Jul 15;630:314-322. doi: 10.1016/j.scitotenv.2018.02.152. Epub 2018 Feb 24.
The Qinghai-Tibetan plateau (QTP) stores a large amount of soil organic carbon and is the headwater region for several large rivers in Asia. Therefore, it is important to understand the influence of environmental factors on river water quality and the dissolved organic carbon (DOC) export in this region. We examined the water physico-chemical characteristics, DOC concentrations and export rates of 7 rivers under typical land cover types in the Three Rivers Headwater Region during August 2016. The results showed that the highest DOC concentrations were recorded in the rivers within the catchment of alpine wet meadow and meadow. These same rivers had the lowest total suspended solids (TSS) concentrations. The rivers within steppe and desert had the lowest DOC concentrations and highest TSS concentrations. The discharge rates and catchment areas were negatively correlated with DOC concentrations. The SUVA values were significantly negatively correlated with DOC concentrations. The results suggest that the vegetation degradation, which may represent permafrost degradation, can lead to a decrease in DOC concentration, but increasing DOC export and soil erosion. In addition, some of the exported DOC will rapidly decompose in the river, and therefore affect the regional carbon cycle, as well as the water quality in the source water of many large Asian rivers.
青藏高原(QTP)储存了大量的土壤有机碳,是亚洲几条大河的源头。因此,了解环境因素对该地区河流水质和溶解有机碳(DOC)输出的影响非常重要。我们在 2016 年 8 月检查了三江源地区典型土地覆盖类型下 7 条河流的水理化特性、DOC 浓度和输出率。结果表明,高山湿地和草甸集水区的河流记录的 DOC 浓度最高。这些河流的总悬浮物(TSS)浓度最低。草原和沙漠地区的河流的 DOC 浓度最低,TSS 浓度最高。径流量和流域面积与 DOC 浓度呈负相关。SUVA 值与 DOC 浓度呈显著负相关。结果表明,植被退化(可能代表永冻层退化)可能导致 DOC 浓度降低,但会增加 DOC 输出和土壤侵蚀。此外,一些输出的 DOC 会在河流中迅速分解,从而影响区域碳循环以及亚洲许多大河的水源水质。