E3S Web Conf.
Volume 98, 201916th International Symposium on Water-Rock Interaction (WRI-16) and 13th International Symposium on Applied Isotope Geochemistry (1st IAGC International Conference)
|Number of page(s)||6|
|Section||Geochemistry of Natural Waters: From Atmospheric Precipitations to Deep Brines|
|Published online||07 June 2019|
Arsenic in the hot springs in the Yunnan-Sichuan-Tibet Geothermal Province, China
State Key Laboratory of Biogeology and Environmental Geology & School of Environmental Studies, China University of Geosciences, 430074 Wuhan, Hubei, P. R. China
* Corresponding author: firstname.lastname@example.org
The Yunnan-Sichuan-Tibet Geothermal Province (YST) in China is characterized by extremely high terrestrial heat flow and widely distributed hydrothermal systems, which are discharging geothermal waters with a wide range of arsenic concentrations. In this paper, the distribution of arsenic in the YST geothermal waters are presented, the general hydrochemistry of these waters is described, and the primary geochemical processes controlling the concentrations and speciation of geothermal arsenic in YST is considered.
© The Authors, published by EDP Sciences, 2019
This is an open access article distributed under the terms of the Creative Commons Attribution License 4.0 (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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