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RIVERINE INORGANIC CARBON DYNAMICS: OVERVIEW AND PERSPECTIVE
作者姓名:YAO  Guan-rong  GAO  Quan-zhou
作者单位:School of Geographical Science and Planning,SUN Yat-Sen University,Guangzhou 510275,P. R. China
基金项目:Under the auspices of the National Natural Science Foundation of China (No. 40471120), the Specialized ResearchFund for the Doctoral Program of Higher Education (No. 20040558025), the '985 Project' of GIS and Remote Sensing for Geo-sciences from the Ministry of Education of China (No. 105203200400006), and the Guangdong Provincial Natural Science Founda-tion (No. 031548)
摘    要:1INTRODUCTION River systems are the major linkage between the land and the ocean, not only transporting carbon from terres- trial environment to the ocean, but also exchanging CO2 with the atmosphere, actively involved in the global car- bon biogeochemical cycle (RICHEY et al., 2002; COLE and CARACO, 2001). The inorganic carbon, mainly o- riginating from soil CO2, carbonate minerals and atmo- sphericCO2,constitutedthegreatpart(about 60%) ofthe riverine carbon exported to the ocean…

关 键 词:河流  无机成分    溶解气体  气候变化
文章编号:1002-0063(2006)02-0183-09
收稿时间:2005-09-16

Riverine inorganic carbon dynamics: overview and perspective
YAO Guan-rong GAO Quan-zhou.Riverine inorganic carbon dynamics: overview and perspective[J].Chinese Geographical Science,2006,16(2):183-191.
Authors:Guan-rong Yao  Quan-zhou Gao
Institution:(1) School of Geographical Science and Planning, SUN Yat-Sen University, 510275 Guangzhou, P. R. China
Abstract:Inorganic carbon, the great part of the riverine carbon exported to the ocean, plays an important role in the global carbon cycle and ultimately impacts the coupled carbon-climate system. An overview was made on both methods and results of the riverine inorganic carbon researches. In addition to routine in situ survey, measurement and calculation, the direct precipitation method and the gas evolution technique were commonly used to analyze dissolved inorganic carbon in natural water samples. Soil CO2, carbonate minerals and atmospheric CO2 incorporated into riverine inorganic carbon pool via different means, with bicarbonate ion being the dominant component. The concentration of inorganic carbon, the composition of carbon isotopes (δ13C and Δ14C), and their temporal or spatial variations in the streams were controlled by carbon input, output and changes of carbon biogeochemistry within the riverine system. More accurate flux estimation, better understanding of different influential processes, and quantitative determination of various inputs or outputs need to be well researched in future. Foundation item: Under the auspices of the National Natural Science Foundation of China (No. 40471120), the Specialized Research Fund for the Doctoral Program of Higher Education (No. 20040558025), the ‘985 Project’ of GIS and Remote Sensing for Geosciences from the Ministry of Education of China (No. 105203200400006), and the Guangdong Provincial Natural Science Foundation (No. 031548) Biography: YAO Guan-rong (1980–), female, a native of Jiaocheng of Shanxi Province, Ph.D. candidate, specialized in carbon cycle and the global change. E-mail: yaoguanrong@yahoo.com.cn
Keywords:riverine inorganic carbon  dissolved inorganic carbon  dynamics  flux
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