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QIN Jian-hua. Continental chemical weathering flux,chemical denudation rates and net CO2 consumption rates in the Changjiang drainage basins on the eastern Qinghai-Xizang Plateau[J]. Sedimentary Geology and Tethyan Geology, 2008, 28(1): 1-6.
Citation: QIN Jian-hua. Continental chemical weathering flux,chemical denudation rates and net CO2 consumption rates in the Changjiang drainage basins on the eastern Qinghai-Xizang Plateau[J]. Sedimentary Geology and Tethyan Geology, 2008, 28(1): 1-6.

Continental chemical weathering flux,chemical denudation rates and net CO2 consumption rates in the Changjiang drainage basins on the eastern Qinghai-Xizang Plateau

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  • Published Date: March 29, 2008
  • Based on the samples taken from the Changjiang drainage basins on the eastern Qinghai-Xizang Plateau in May and June of 2000,2001 and 2002,the continental chemical weathering flux,chemical denudation rates and net CO2 consumption rates for individual basins are generalized as follows.(1) The chemical denudation rate is highest(2.34×106 mol/yr/km2) for the Qumar River and lowest(1.40×106 mol/yr/km2) for the Tuotuo River.The chemical denudation rates of the other four main tributaries of the Changjiang River in the region are 1.69×106 mol/yr/km2for the Yalong River,1.74×106 mol/yr/km2 for the Jinsha River,1.57×106 mol/yr/km2 for the Dadu River,and 1.88×106 mol/yr/km2 for the Minjiang River,respectively.(2) The net CO2 consumption rates in the tributaries of the Yangtze River,on the other hand,are 101.81×103 mol/yr/km2 for the Dadu River,7.55×103 mol/yr/km21 for the Qumar River,44.38×103 mol/yr/km2 for the Jinsha River,69.64×103 mol/yr/km2 for the Yalong River,81.90×103 mol/yr/km2 for the Minjiang River,and 21.90×103 mol/yr/km2 for the Tuotuo River,respectively.The physical weathering is considered as a most important factor influencing the chemical denudation rates in the study area.
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