Coupled control of land uses and aquatic biological processes on the diurnal hydrochemical variations in the five ponds at the Shawan Karst Test Site, China: Implications for the carbonate weathering-
Bo Chen;  Rui Yang;   Zaihua Liu;  Hailong Sun;  Hao Yan;  Qingrui Zeng;   Sibo Zeng;  Cheng Zeng;   Min Zhao
刊名Chemical Geology
2017
卷号456页码:58-71
关键词Diurnal Hydrochemical Variation Bcp Effect Dic Fertilization Effect Rock Weathering-related Carbon Sink LAnd Use And Cover Change
英文摘要

High-resolution hydrochemical data from five spring-fed ponds are presented to demonstrate the effect of different land uses and aquatic biological processes on the carbon cycle at a karst-analog test site. The results show that hydrochemical parameters including pH and the concentrations of HCO3, Ca2 +, NO3, partial pressures of CO2(pCO2) and dissolved O2 (DO) as well as carbon isotopic compositions (δ13C) of HCO3in the pond water all displayed distinct diurnal variations, while those of the spring water itself were rather stable. The coupled dynamic behaviors of pCO2, DO and NO3 indicate a significant influence from the metabolism of submerged plants in the ponds. In the afternoon, when photosynthesis is the strongest, the pCO2 of the five pond waters was lower even than that of the ambient atmosphere, demonstrating the existence of a “biological carbon pumping (BCP) effect”, similar to that in the oceans. It was determined that, in October (autumn), the BCP fluxes in the five spring-fed ponds were 156 ± 51 t C km− 2 a− 1 in P1 (Pond 1 – adjoining a bare rock shore), 239 ± 83 t C km− 2 a− 1 in P2 (adjoining uncultivated soil), 414 ± 139 t C km− 2 a− 1 in P3 (adjoining land cultivated with corn), 493 ± 165 t C km− 2 a− 1 in P4 (adjoining grassland) and 399 ± 124 t C km− 2 a− 1 of P5 (adjoining brushland), indicating the potentially significant role of aquatic photosynthesis in stabilizing the carbonate weathering-related carbon sink. In addition, by comparing the DIC concentrations and fluxes of DIC transformed into autochthonous organic matter (AOC) in the five ponds, the so-called “DIC fertilization effect” was found in which more AOC is produced in pond waters with higher concentrations of DIC. This implies that the carbon cycle driven by aquatic biological processes can be regulated by changing land use and cover, the latter determining the DIC concentrations. Further, the rock weathering-related carbon sink is underestimated if one only considers the DIC component in surface waters instead of both DIC and AOC.

语种英语
内容类型期刊论文
源URL[http://ir.gyig.ac.cn/handle/42920512-1/8335]  
专题地球化学研究所_环境地球化学国家重点实验室
作者单位1.University of Chinese Academy of Sciences, Beijing 100049, China
2.State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, CAS, Guiyang 550081, China
3.School of Geographical Sciences, Southwest University, Chongqing 400715, China
推荐引用方式
GB/T 7714
Bo Chen;Rui Yang; Zaihua Liu;Hailong Sun;Hao Yan;Qingrui Zeng; Sibo Zeng;Cheng Zeng; Min Zhao. Coupled control of land uses and aquatic biological processes on the diurnal hydrochemical variations in the five ponds at the Shawan Karst Test Site, China: Implications for the carbonate weathering-[J]. Chemical Geology,2017,456:58-71.
APA Bo Chen;Rui Yang; Zaihua Liu;Hailong Sun;Hao Yan;Qingrui Zeng; Sibo Zeng;Cheng Zeng; Min Zhao.(2017).Coupled control of land uses and aquatic biological processes on the diurnal hydrochemical variations in the five ponds at the Shawan Karst Test Site, China: Implications for the carbonate weathering-.Chemical Geology,456,58-71.
MLA Bo Chen;Rui Yang; Zaihua Liu;Hailong Sun;Hao Yan;Qingrui Zeng; Sibo Zeng;Cheng Zeng; Min Zhao."Coupled control of land uses and aquatic biological processes on the diurnal hydrochemical variations in the five ponds at the Shawan Karst Test Site, China: Implications for the carbonate weathering-".Chemical Geology 456(2017):58-71.
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