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中国西南巴布地下河流域水体中溶解态硫酸根的双同位素分布及来源识别

Distribution and source identification of dissolved sulfate by dual isotopes in waters of the Babu subterranean river basin, SW China.

作者信息

Ren Kun, Pan Xiaodong, Zeng Jie, Jiao Youjun

机构信息

Institute of Karst Geology, Chinese Academy of Geological Sciences, No. 50, Qixing Road, Guilin, 541004 Guangxi People's Republic of China.

Karst Dynamics Laboratory, Ministry of Land and Resources, Guilin, 541004 Guangxi China.

出版信息

J Radioanal Nucl Chem. 2017;312(2):317-328. doi: 10.1007/s10967-017-5217-y. Epub 2017 Mar 16.

DOI:10.1007/s10967-017-5217-y
PMID:28458410
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5387059/
Abstract

Sulfur and oxygen isotopes were employed to identify SO sources in surface water and groundwater in the Babu subterranean river basin (BSRB). Our study revealed SO enrichment in the BSRB waters compared with adjacent areas. The SO in some samples originated mainly from precipitation; in others, it was derived mainly from sulfide dissolution in coal seams or from gypsum dissolution. In the water at the subterranean river exit, 13% of SO originated from precipitation, 40% from sulfide oxidation in coal seams, and 47% from gypsum dissolution.

摘要

采用硫和氧同位素来识别八步地下河流域（BSRB）地表水和地下水中的硫氧化物（SO）来源。我们的研究表明，与相邻区域相比，BSRB水体中存在硫氧化物富集现象。一些样品中的硫氧化物主要源自降水；而在其他样品中，它主要来自煤层中硫化物的溶解或石膏的溶解。在地下河出口处的水体中，13%的硫氧化物源自降水，40%源自煤层中的硫化物氧化，47%源自石膏溶解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/73611221a3fb/10967_2017_5217_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/0817396e9ced/10967_2017_5217_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/e6eeab4b82a5/10967_2017_5217_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/e07232061c1f/10967_2017_5217_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/ec57e048196c/10967_2017_5217_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/3a4aabac714d/10967_2017_5217_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/be2475efd353/10967_2017_5217_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/bba7729895cd/10967_2017_5217_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/73611221a3fb/10967_2017_5217_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/0817396e9ced/10967_2017_5217_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/e6eeab4b82a5/10967_2017_5217_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/e07232061c1f/10967_2017_5217_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/ec57e048196c/10967_2017_5217_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/3a4aabac714d/10967_2017_5217_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/be2475efd353/10967_2017_5217_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/bba7729895cd/10967_2017_5217_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6caa/5387059/73611221a3fb/10967_2017_5217_Fig8_HTML.jpg

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