Wang,B., Lee,X.-Q., Yuan,H.-L., Zhou,H., Cheng,H.-G., Cheng,J.-Z., Zhou,Z.-H., Xing,Y., Fang,B., Zhang,L.-K., Yang,F.(2012): Distinct patterns of chemical weathering in the drainage basins of the Huanghe and Xijiang River, China: Evidence from chemical and Sr-isotopic compositions. Journal of Asian Earth Sciences, 59, 219-230.【見る→】
『中国の黄河と西江の流域における化学風化の異なるパターン：化学組成およびストロンチウム同位体組成からの証拠』

『Abstract
　Aquatic geochemistry on watershed background helps elucidate the influence of natural processes and anthropogenic activities to the environment. The 87Sr/86Sr ratios and dissolved loads were measured in 35 water samples from the Huanghe and Xijiang River drainage basins. The dissolved loads and 87Sr/86Sr ratios differed considerably between the two drainage basins. The 87Sr/86Sr ratios of the Xijiang River are between 0.70856 and 0.70936, with an average of 0.70894, reflecting weathering of carbonate minerals as the dominant source and anthropogenic pollution as the secondary one, especially in the upper reach tributaries, while the Sr isotopic ratios in the Huanghe River range from 0.70986 to 0.71139 averaging 0.71118 that results primarily from evaporite dissolution. Precipitation contributes to 2.8% and 5.7% to the chemistry of the Xijiang and Huanghe River, respectively. Evaporite dissolution and silicate weathering account for 79.4% and 11.3%, respectively, in the Huanghe River while carbonate dissolution and silicate weathering account for 75.4% and 14.6%, respectively, in the Xijiang River. The chemical weathering rate is 107.6 t/km2/yr in the Xijiang River drainage basin, and 34.2 t/km2/yr in the Huanghe River drainage basin. The CO2 consumption budget is 305.2×109 mol/yr in the Xijiang River drainage basin, and 147.9×109 mol/yr in the Huanghe River drainage basin.

Keywords: Strontium; 87Sr/86Sr; Carbon sequestration; Water pollution; CO2 consumption budget; Water chemistry』

1. Introduction
2. River setting
3. Sampling and analytical procedures
4. Results and discussion
　4.1. Characteristics of the major elements
　4.2. Strontium concentration and strontium isotope composition
　　4.2.1. The Xijiang River
　　4.2.2. The Huanghe River
　4.3. Sources of the dissolved major elements and strontium
　　4.3.1. Anthropogenic activities
　　4.3.2. Atmospheric dry and wet deposition
　　4.3.3. Rock weathering
　4.4. Chemical budget and chemical weathering rate estimation
　　4.4.1. Chemical budget
　　4.4.2. Chemical weathering estimation
5. Conclusions
Acknowledgements
References

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