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DOI | 10.1016/j.scitotenv.2023.166262 |
Constraining the sources and cycling of dissolved inorganic carbon in an alpine river, eastern Qinghai-Tibet Plateau | |
Wang, Wanfa; Zhong, Jun; Li, Si-Liang; Ulloa-Cedamanos, F.; Xu, Sen; Chen, Sainan; Lai, Manting; Xu, Sheng | |
发表日期 | 2023 |
ISSN | 0048-9697 |
EISSN | 1879-1026 |
卷号 | 901 |
英文摘要 | It is generally acknowledged that riverine dissolved inorganic carbon (DIC) behaviors play a critical role in global carbon cycling and hence have an impact on climate change. However, little is known about the intricate DIC dynamics under various meteorological conditions in the alpine areas. Here, we investigated DIC biogeochemical processes in the Bailong River catchment, eastern Qinghai-Tibet Plateau (QTP), by combining measurements of major ions, stable and radioactive isotopic compositions of DIC (delta(CDIC)-C-13 and Delta(CDIC)-C-14), and physiographic parameters in the Bailong River catchment. Statistics and stoichiometry analyses suggest that multiple biogeochemical processes could affect carbon cycling in the Bailong River catchment. The old DIC with low Delta C-14 values ( 472.4 +/- 127.8 %, n = 3) and stoichiometry analysis of dissolved ions showed clear evidence that carbonate weathering is primarily responsible for water chemistry in the upstream (elevation >2000 m). However, upstream samples showed that d13CDIC increased between 5 % and 11 % from the theoretical mixing line, concomitant with increasing pH and decreasing pCO(2), suggesting that isotopic fractionation of DIC due to CO2 outgassing may be the primary cause of the increased d13CDIC values. Additionally, the higher Delta C-14 values ( 285.4 +/- 123.5 %, n = 12) in the downstream region below 2000 m suggest that allochthonous modern carbon had a great impact on DIC variations. The presence of younger DIC may have important implications for the interpretation of inorganic carbon age in downstream rivers. Our study demonstrates that physiographic conditions can regulate DIC behaviors, which can improve estimations of carbon yield and comprehension of global carbon cycle. |
关键词 | Physiographic conditionsCarbonate weatheringCarbon cyclingRadiocarbonQinghai-Tibet Plateau |
英文关键词 | CO2 CONSUMPTION; BIOGEOCHEMICAL CYCLES; ORGANIC-MATTER; CLIMATE-CHANGE; DIOXIDE; CHINA; BASIN; RATES; LAND; VARIABILITY |
WOS研究方向 | Environmental Sciences |
WOS记录号 | WOS:001069276200001 |
来源期刊 | SCIENCE OF THE TOTAL ENVIRONMENT |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/282828 |
作者单位 | Guizhou University; Tianjin University; Charles Darwin University |
推荐引用方式 GB/T 7714 | Wang, Wanfa,Zhong, Jun,Li, Si-Liang,et al. Constraining the sources and cycling of dissolved inorganic carbon in an alpine river, eastern Qinghai-Tibet Plateau[J],2023,901. |
APA | Wang, Wanfa.,Zhong, Jun.,Li, Si-Liang.,Ulloa-Cedamanos, F..,Xu, Sen.,...&Xu, Sheng.(2023).Constraining the sources and cycling of dissolved inorganic carbon in an alpine river, eastern Qinghai-Tibet Plateau.SCIENCE OF THE TOTAL ENVIRONMENT,901. |
MLA | Wang, Wanfa,et al."Constraining the sources and cycling of dissolved inorganic carbon in an alpine river, eastern Qinghai-Tibet Plateau".SCIENCE OF THE TOTAL ENVIRONMENT 901(2023). |
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