湖南锡矿山高锑地下水稳定碳同位素特征及其富锑意义
Characteristics of Stable Carbon Isotopes and Its Significance of Antimony Enrichment in High-antimony Groundwater of Xikuangshan Mines,Hunan
贺凯凯 1朱峰 2王彦堂 1郝春明1
作者信息
- 1. 华北科技学院矿山安全学院,三河 065201
- 2. 兖矿能源(鄂尔多斯)有限公司,鄂尔多斯 017004
- 折叠
摘要
溶解性有机碳是地下水中Sb富集的关键因素,为探明湖南锡矿山高Sb地下水稳定碳同位素特征,揭示有机质氧化分解过程对地下水中Sb富集的影响,对湖南锡矿山高Sb地下水选用碳稳定同位素分馏和水化学相结合的方式进行分析.结果表明:湖南锡矿山高Sb地下水δ13CDIC值在-17.84‰～-2.30‰,δ13CDOC值在-26.87‰～-16.70‰.高Sb地下水中Sb与DOC、HCO3-均呈正相关关系,表明微生物作用对高Sb地下水中Sb的富集具有较大的贡献.高Sb地下水溶解性有机碳相对于溶解性无机碳具有更负的δ13C值,DOC主要受内源有机质的影响;随着813CDIC-δ13CDOC差值的减小,Sb浓度逐渐升高,表明由于微生物的存在,有机质的氧化分解明显促进了高Sb地下水中Sb的富集.
Abstract
DOC(dissolved organic carbon)is a crucial factor for antimony(Sb)enrichment in groundwater.High-Sb groundwater samples were analyzed using hydrochemistry and stable carbon isotope to elaborate the effects of oxidative degradation of organic matter on Sb enrichment in groundwater of Xikuangshan Mines,Hunan.The results indicate that the value of 813CDIC and 813CDOC ranged from-17.84‰ to-2.30‰ and from-26.87‰ to-16.70‰,respectively.An obviously positive correlation between Sb and DOC,as well as HCO3-in high-Sb groundwater,indicating that Sb enrichment may be significantly contributed to microbial activities.Mean-while,DOC had lower values of δ13 C compared with dissolved inorganic carbon,suggesting DOC was mainly controlled by endogenous organic matter.Owing to the Sb concentration showed gradually increased trends with decreasing difference between 813 CDIC andδ13CDOC,the microbial degradation of DOM had a substantial contribution to Sb mobility.
关键词
锑Sb/碳稳定同位素/溶解性有机碳DOC/有机质氧化/Sb富集Key words
Sb/carbon stable isotopes/DOC(dissolved organic carbon)/organic matter oxidation/Sb enrichment引用本文复制引用
基金项目
河北省自然科学基金(D2021508004)
自然资源部冷水江锡矿山生态环境承载力项目(LCG2020009)
出版年
2024
NETL
NSTL
万方数据