A multiple isotope (S, H, O and C) approach to estimate sulfate increasing mechanism of groundwater in coal mine area

被引：8

作者：

Huang, Pinghua ^{[1
,2
]}

Zhang, Yanni ^{[1
]}

Li, Yuanmeng ^{[1
]}

Gao, Hongfei ^{[1
]}

Cui, Mengke ^{[1
]}

Chai, Shuangwei ^{[1
]}

机构：

[1] Henan Polytech Univ, Sch Resources & Environm Engn, Jiaozuo 454000, Peoples R China

[2] Collaborat Innovat Ctr Coalbed Methane & Shale Gas, Jiaozuo 454000, Peoples R China

来源：

SCIENCE OF THE TOTAL ENVIRONMENT | 2023年 / 900卷

基金：

中国博士后科学基金; 中国国家自然科学基金;

关键词：

Groundwater; Limestone aquifer; Coal mining; Multi-isotope; Sulfate increasing mechanism; AQUIFER SYSTEM; SURFACE-WATER; BASIN; IDENTIFICATION; GEOCHEMISTRY; EVOLUTION; DRAINAGE; TRACK; FLOW;

D O I：

10.1016/j.scitotenv.2023.165852

中图分类号：

X [环境科学、安全科学];

学科分类号：

08 ; 0830 ;

摘要：

Groundwater in North China type coal mine area is an important source of domestic, industrial and agricultural water. To explore the sulfate increasing mechanism of groundwater in mining area and identify key influencing factors. In this paper, hydrochemistry and multi-isotope tracer techniques such as 634SSO4, 618OSO4, 62HH2O, 618OH2O and 613CDIC were used to study the groundwater circulation law and the migration and transformation mechanism of sulfate and carbonate in coal mine area. The results show that: the hydrochemical types of groundwater in the coal mine area are mainly HCO3  and SO42  anions, while the cations are mainly Ca2+ and Mg2+. The sulfate content is significantly increased, and the pH shows weak alkalinity; the relationship between 618OH2O and 618HH2O shows that the dynamic field of groundwater changes significantly after coal mining or closure, and limestone water mainly comes from surface water recharge through 'skylight' infiltration. The re-lationships between 618OSO4 and 618OH2O, 634SSO4 and 618OSO4 show that the sulfate in groundwater of coal mine area is mainly derived from sulfide oxidation. The A618OSO4-H2O value of groundwater in coal mine area is greater than 8 & PTSTHOUSND;, and the oxygen content in sulfate is 25 %-75 % from oxygen in water, indicating that coal mining has disturbed the groundwater in the study area from reducing environment to oxidizing environment, promoted sulfide oxidation, and accelerated the dissolution of carbonate minerals. The 613CDIC value and 634SSO4 value in the coal mine area are inversely proportional. The 613CDIC of groundwater in the coal mine area is affected by the 634SSO4 value to a certain extent. Sulfuric acid participates in the dissolution of carbonate minerals, making the pH value weak and alkaline as a whole. This paper expounds the migration and trans-formation law of sulfate in groundwater in coal mine area, which has practical significance for groundwater quality management. The research results can provide theoretical support for the rational development and utilization of groundwater resources in coal mine areas.

引用

页数：10