Spatiotemporal Variability and Sources of DIC in Permafrost Catchments of the Yangtze River Source Region: Insights From Stable Carbon Isotope and Water Chemistry

• Published in: Water Resources Research
• Main Authors: Song Chunlin, Wang Genxu, Mao Tianxu, Huang Kewei, Sun Xiangyang, Hu Zhaoyong, Chang Ruiying, Chen Xiaopeng, Raymond Peter A.
• Format: Article in Journal/Newspaper
• Language: English
• Published: AMER GEOPHYSICAL UNION 2020
• Subjects: Spatiotemporal Variability; DISSOLVED INORGANIC CARBON; TIBETAN PLATEAU; ORGANIC-CARBON; CO2 CONSUMPTION; FLUVIAL GEOCHEMISTRY; EASTERN SIBERIA; CLIMATE-CHANGE; GAS-EXCHANGE; THAW DEPTH; DIOXIDE; Environmental Sciences & Ecology; Marine & Freshwater Biology; Water Resources; Environmental Sciences; Limnology; permafrost; Siberia
• Online Access: http://ir.imde.ac.cn/handle/131551/34143; https://doi.org/10.1029/2019WR025343

Riverine dissolved inorganic carbon (DIC) exports play a central role in the regional and global carbon cycles. Here, we investigated the spatiotemporal variability and sources of DIC in eight catchments in the Yangtze River source region (YRSR) with variable permafrost coverage and seasonally thawed active layers. The YRSR catchments are DIC-rich (averagely 25 mg C L-1) and export 3.51 g m(-2) yr(-1) of DIC. The seasonal changes of temperature, active layer, flow path, and discharge can alter DIC and stable carbon isotope of DIC (delta C-13-DIC). The most depleted delta C-13-DIC values were found in the thawed period, suggesting the soil-respired CO2 during the active layer thaw period can promote bicarbonate production via H2CO3 weathering. Spatially, delta C-13-DIC values increased downstream, likely due to CO2 outgassing and changed permafrost coverage and runoff. We found that evaporite dissolution and silicate weathering in the seasonally thawed active layer contributed 44.2% and 30.9% of stream HCO3-, respectively, while groundwater and rainwater contributed 16.7% and 7.3% of HCO3-, respectively. Pure carbonate rock weathering played a negligible role in DIC production. These results were compatible with delta C-13-DIC source approximation results. Silicate weathering increased from initial thaw to thawed period, reflecting the active layer thaw and subsequent hydrology change impacts. Silicate weathering consumed 1.25 x 10(10) mol of CO2 annually, while evaporite dissolution may produce CO2 and neutralize this CO2 sink. This study provides new understanding of the riverine DIC export processes of the YRSR. As permafrost degrades, the quantity, sources, and sinks of riverine DIC may also change spatiotemporally.