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DOI10.1016/j.jhydrol.2021.126197
Glaciation enhanced chemical weathering in a cold glacial catchment, western Nyaingentanglha Mountains, central Tibetan Plateau
Yu, Zhengliang; Wu, Guangjian; Li, Fei; Chen, Mengke; Tran, Tuong Vi; Liu, Xiaoming; Gao, Shaopeng
通讯作者Wu, GJ (通讯作者)
发表日期2021
ISSN0022-1694
EISSN1879-2707
卷号597
英文摘要The uplift of the Tibetan Plateau (TP) not only may enhance physical denudation and chemical weathering but also makes this area contain the largest glacier storage outside the polar regions. There is an argument on whether glaciation favours chemical weathering and carbon sequestration. To explore chemical weathering processes and intensities in the cold glacial region of the central TP, hydrochemistry of the river water in two catchments, i.e. the Qugaqiong and Qugaqie, was monitored from April to September 2018 with high-frequency sampling. These two catchments share similar geographical features except there are some cold glaciers in the upper reaches of the Qugaqie. The results of chemical composition show that the river water of the Qugaqie has a lower proportion of Ca2+ and HCO3 but higher SO42- and K++Na+ compared with the Qugaqiong. The seasonal variation of ionic concentration in the Qugaqie is significant but minor in the Qugaqiong. Those differences highlight the glacial impact in the Qugaqie compared with the non-glacierized Qugaqiong. Solutes in the glacial runoff of the Qugaqie mainly derive from sulfide oxidation. Its contribution to cations in the runoff of the Zhadang glacier and the Hanging glacier reaches 39% and 36%. The second most important contribution is carbonate dissolution (32% for both glacial runoffs). Silicate weathering provides fewer solutes and its contribution is only 20% and 11% in the two glacial runoffs, respectively. River water of the Qugaqiong shares similar hydrochemical characteristics with the non-glacial tributaries draining granodiorite/biotite adamellite in the Qugaqie. The contribution of sulfide oxidation to solutes in those rivers decreases to 10% while carbonate dissolution increases to 50%. Glacial comminution exposed trace sulfide minerals, thus made sulfide oxidation became pretty active due to this reaction is much faster than other mineral dissolution. The carbonate weathering rate (CWR) and silicate weathering rate (SWR) in the Qugaqie catchment are 9.7 t/km(2)/y and 6.7 t/km(2)/y. In comparison, values in the Qugaqiong catchment are 6.9 t/km(2)/y and 3.8 t/km(2)/y, respectively, which means CWR and SWR is 1.4 and 1.8 times higher in the Qugaqie catchment, respectively. Higher runoff and physical erosion rates are considered as the main reasons for higher chemical denudation rates in the Qugaqie catchment. The drainage system of the glaciers is dominated by the distributed pattern, which caused longer residences time of water, thus further promoted chemical weathering in the glacierized region. Our observation supports the idea that glaciation in the glacierized catchment of the central TP enhances chemical weathering, especially for SWR. Chemical denudation rates in the Qugaqie catchment remain at a moderate level compared with other glacierized catchments in the world and lithology and runoff are important factors to cause this spatial heterogeneity.
关键词SEASONAL-VARIATIONHIMALAYAN GLACIERWATER CHEMISTRYMASS-BALANCECARBON-CYCLEBASINDENUDATIONCO2RUNOFFROCKS
英文关键词Glaciation; Central Tibetan Plateau; Chemical weathering; Silicate; Carbonate
语种英语
WOS研究方向Engineering ; Geology ; Water Resources
WOS类目Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources
WOS记录号WOS:000652835600073
来源期刊JOURNAL OF HYDROLOGY
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/260156
推荐引用方式
GB/T 7714
Yu, Zhengliang,Wu, Guangjian,Li, Fei,et al. Glaciation enhanced chemical weathering in a cold glacial catchment, western Nyaingentanglha Mountains, central Tibetan Plateau[J]. 中国科学院青藏高原研究所,2021,597.
APA Yu, Zhengliang.,Wu, Guangjian.,Li, Fei.,Chen, Mengke.,Tran, Tuong Vi.,...&Gao, Shaopeng.(2021).Glaciation enhanced chemical weathering in a cold glacial catchment, western Nyaingentanglha Mountains, central Tibetan Plateau.JOURNAL OF HYDROLOGY,597.
MLA Yu, Zhengliang,et al."Glaciation enhanced chemical weathering in a cold glacial catchment, western Nyaingentanglha Mountains, central Tibetan Plateau".JOURNAL OF HYDROLOGY 597(2021).
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