Temporal and spatial characteristics of dissolved organic carbon in the Wujiang River, Southwest China

被引:2
|
作者
Peng X. [1 ]
Wang B. [1 ,2 ]
Zhao Y. [3 ]
机构
[1] State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang
[2] Institute of Surface-Earth System Science, Tianjin University, Tianjin
[3] Key Laboratory of Digital Earth Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing
基金
中国国家自然科学基金;
关键词
Carbon cycle; Dam-building effect; Dissolved organic carbon; The Wujiang River;
D O I
10.1007/s11631-017-0195-x
中图分类号
学科分类号
摘要
River systems play an important role in the global carbon cycle. Rivers transport carbon to the ocean and also affect the carbon cycle in the coastal ocean. The flux from land to the ocean is thought to be a very important part of the land carbon budget. To investigate the effect of dam-building on dissolved organic carbon (DOC) in rivers, three reservoirs of different trophic states in the Wujiang basin, Guizhou Province, were sampled twice per month between May 2011 and May 2012. Temporal and spatial distributions of DOC in the reservoirs and their released waters were studied. It was found that different factors controlled DOC in river water, reservoir water, and released water. DOC in the rivers tended to be affected by primary production. For reservoirs, the main controlling factors of DOC concentration varied by trophic state. For the mesotrophic Hongjiadu Reservoir, the effect of primary production on DOC concentration was obvious. For the eutrophic Dongfengdu Reservoir and the hypereutrophic Wujiangdu Reservoir, primary production was not significant and DOC came instead from soil and plant litter. © 2017, Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany.
引用
收藏
页码:598 / 604
页数:6
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