Chemical weathering and CO2 consumption rates of rocks in the Bishuiyan subterranean basin of Guangxi, China
Open Access
- 15 July 2020
- journal article
- research article
- Published by Springer Science and Business Media LLC in Scientific Reports
- Vol. 10 (1), 1-12
- https://doi.org/10.1038/s41598-020-68572-4
Abstract
To investigate the influence of chemical weathering on CO2 consumption, an analysis was performed of water chemistry by applying water chemistry equilibria methods in the Bishuiyan subterranean basin, SW China. The average value of total ion concentrations (TZ+) was 1,854.97 μEq/L, which was significantly higher than the global average value (TZ+ = 1,250 μEq/L). Ca2+ and HCO3− were the main ionic constituents in the waters. SO42− and NO3− concentrations were relatively higher than other anion concentrations, and Cl− concentrations were consistently the lowest. Dissolved load balance models result showed that carbonate weathering, silicate weathering, and atmospheric input were the primary ionic contributors, wherein the effects of carbonate weathering > silicate weathering > atmospheric input for the whole catchment, with the exception of Taiping, where silicate weathering was prominent over carbonate weathering. In addition, these analyses indicated that the erosion via rock weathering was also affected by atmospherically derived CO2 and allogenic acids. The estimated yield by quantitative calculation for the carbonate weathering rate was 59.7 t/(km2 year), which was 4.40 times higher than that of silicate weathering rate. Further, the carbonate and silicate weathering components of the carbon sink accounted for 71.2% and 28.8%, respectively, of the total basin rock weathering carbon sink.This publication has 46 references indexed in Scilit:
- Chemical weathering and atmospheric/soil CO2 uptake in the Andean and Foreland Amazon basinsChemical Geology, 2011
- Atmospheric CO2 sink: Silicate weathering or carbonate weathering?Applied Geochemistry, 2011
- Response of silicate weathering to monsoon changes on the Chinese Loess PlateauCATENA, 2008
- Solute generation and CO2 consumption during silicate weathering under subtropical, humid climate, northern Okinawa Island, JapanChemical Geology, 2007
- Worldwide distribution of continental rock lithology: Implications for the atmospheric/soil CO2 uptake by continental weathering and alkalinity river transport to the oceansGlobal Biogeochemical Cycles, 2003
- Role of mixing corrosion in calcite‐aggressive H2O‐CO2‐CaCO3 solutions in the early evolution of Karst Aquifers in limestoneWater Resources Research, 2000
- Global silicate weathering and CO2 consumption rates deduced from the chemistry of large riversChemical Geology, 1999
- Chemical weathering and lithologic controls of water chemistry in a high‐elevation river system: Clark's Fork of the Yellowstone River, Wyoming and MontanaWater Resources Research, 1999
- Fluvial geochemistry of the eastern slope of the northeastern Andes and its foredeep in the drainage of the Orinoco in Colombia and VenezuelaGeochimica et Cosmochimica Acta, 1996
- Major element chemistry of the Huanghe (Yellow River), China - weathering processes and chemical fluxesJournal of Hydrology, 1995