Open AccessHydro‐Geochemical and Sr Isotope Characteristics of the Yalong River Basin, Eastern Tibetan Plateau: Implications for Chemical Weathering and Controlling Factors
Author(s) -
Zhang Xuan,
Xu Zhifang,
Liu Wenjing,
Moon Seulgi,
Zhao Tong,
Zhou Xiaode,
Zhang Jiangyi,
Wu Yao,
Jiang Hao,
Zhou Li
Publication year - 2019
Publication title -
geochemistry, geophysics, geosystems
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.928
H-Index - 136
ISSN - 1525-2027
DOI - 10.1029/2018gc007769
Subject(s) - weathering , geology , carbonate , silicate , drainage basin , plateau (mathematics) , geochemistry , carbonate rock , silicate minerals , radiogenic nuclide , hydrology (agriculture) , earth science , geomorphology , sedimentary rock , geotechnical engineering , cartography , mathematics , chemical engineering , mantle (geology) , geography , engineering , metallurgy , mathematical analysis , materials science
Abstract Major ions and Sr isotope compositions of waters in the Yalong River basin in the eastern Tibetan plateau were investigated to explore the sources of dissolved loads and the controls on chemical weathering rates. Measured radiogenic 87 Sr/ 86 Sr ratios of water samples are most likely derived from the weathering of metamorphic carbonates or the Precambrian silicate rocks. Quantitative analysis of water geochemistry shows that carbonate weathering dominates the chemical characteristics of the river water. The chemical weathering rate of the whole Yalong River basin is calculated to be 7.6 ton·km −2 ·year −1 by silicate weathering and 44.7 ton·km −2 ·year −1 by carbonate weathering, which consumes 158.5 × 10 3 and 885.0 × 10 3 mol·km −2 ·year −1 of atmospheric CO 2 , respectively. The highest carbonate weathering rate (116.3 ton·km −2 ·year −1 ) in the Yalong River basins is observed from the basin with the steepest catchment average slope. This highest magnitude of carbonate weathering is comparable to the rates from catchments in the southern Himalayas. Positive relationships are observed between silicate weathering rates and both climatic (precipitation and temperature) and topographic (relief and slope) controls. The combined climatic and tectonic effects increase silicate weathering and counterbalance the dilution effect. However, the relationship between silicate weathering rate and climatic and topographic controls varies with hydrologic conditions. The rate for low‐discharge catchments is more closely related to climatic parameters, while the rate for high‐discharge catchments is more closely related to local topography.