皖北矿区地下水化学组成控制因素及水源识别研究进展——基于水岩相互作用和EPA Unmix模型的思考
Research Progresses on Controlling Factors of Chemical Constitution and Water Source Identification of Groundwater in Mining Area, Northern Anhui Province — Consideration of Water-Rock Interaction and EPA Unmix Model
DOI: 10.12677/OJNS.2019.73019, PDF,    科研立项经费支持
作者: 陈凯, 孙林华：安徽理工大学地球与环境学院，安徽 淮南；宿州学院资源与土木工程学院，安徽 宿州
关键词: 地下水；煤矿；水文地球化学；水岩相互作用；Unmix模型；Groundwater； Coal Mine； Hydrochemistry； Water-Rock Interaction； Unmix Model
摘要:

查明皖北煤矿区含水层水岩相互作用机理是进行水源识别的关键所在。本人对前人的工作进行了总结并指出当前研究中存在的一些问题：1) 矿区地下水主要离子的定性分析需要验证及2) 主要离子来源需要进一步定量分析。这些问题可以通过水岩相互作用实验和EPA Unmix模型分析相结合来进行解决：利用水岩相互作用实验得到各种矿物/岩石的溶解谱，而EPA Unmix模型则可以获取离子来源的定量信息，两者的结合可以为今后基于水岩相互作用来识别突水水源提供新的方法和思路。

Abstract: It is a key point to identify the water-rock interaction mechanism in the aquifers of coal mining area in northern Anhui province. This paper summarized the work of the predecessors and pointed out some problems existing in the current research: 1) the qualitative analysis of major ion sources of groundwater in mining area needs to be verified and 2) the major ion sources require further quantitative analysis. These problems can be solved by combining the water-rock interaction experiment with the EPA Unmix model analysis: the dissolution spectra of various minerals/rocks can be obtained by using the water-rock interaction experiment, whereas the EPA Unmix model can obtain quantitative information of ion sources. Their combination can provide new methods and ideas for identifying water inrush sources based on water-rock interactions in the future.
文章引用：陈凯, 孙林华. 皖北矿区地下水化学组成控制因素及水源识别研究进展——基于水岩相互作用和EPA Unmix模型的思考 [J]. 自然科学, 2019, 7(3): 129-136. https://doi.org/10.12677/OJNS.2019.73019

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