西部典型煤矿区含水层水化学差异及其水害防治指示意义

    Hydrochemical differences of aquifers in western typical coal mine areas and their significance for water hazard control

    • 摘要: 煤矿水害防治对保障安全生产与国家能源稳定供给至关重要。水化学分析是识别矿井水源、判断含水层水力联系的关键技术手段,在防治水害中具有重要作用。以西部典型煤矿曹家滩为研究区,综合运用数理统计、Durov图、Gibbs图、Pearson相关性分析及离子比例系数等方法,系统分析了煤系地下水化学特征,定量表征了含水层间的水力联系,并揭示了其在水害防治中的应用价值。研究结果表明:从浅层到深层地下水,K++Na+、SO42−、Cl−和HCO3−质量浓度呈逐渐增加趋势,溶解性总固体(TDS)质量浓度和 pH 值也随埋深增加而逐渐升高;水化学类型发生显著变化,阴离子由HCO3型逐渐变成HCO3和SO4型,阳离子由多元的Na、Ca、Mg型转化为单一的Na型,这一变化过程反映出水化学形成作用由浅部向深部趋于复杂。进一步分析发现:随着地下水埋深的增加,阳离子交换作用和溶滤作用不断增强;阳离子交换导致深部地下水中K++Na+的质量浓度增加,而溶滤作用促使煤层中的石膏与黄铁矿溶解,造成SO42−质量浓度增加。不同含水层水化学特征的差异及其之间的水力联系,对于准确识别矿井水水源至关重要,也有助于厘定垮落带或导水裂隙带对地层的影响,为煤矿水害的防治提供精准的科学依据,以保障煤矿安全生产。

       

      Abstract: The prevention and control of coal mine water disaster is of great significance to ensure the safety of coal mine production and the stable supply of national energy. The water chemical analysis can identify the mine water source and judge the hydraulic connection of aquifers, providing the key scientific basis for the prevention and control of water damage. This study employs mathematical statistics, Durov, Gibbs, Pearson correlation analysis, and ion ratio coefficient methods to ascertain the hydrochemical characteristics of Caojiatan Coal Mine, subsequently analyzing their implications for effective water hazard prediction and control. The results indicate a progressive increase in the mass concentrations of K++Na+, SO42−, Cl−, HCO3−, and total dissolved solids (TDS) mass concentration in groundwater from shallow to deeper strata, accompanied by a gradual increase in pH; the hydrochemical type has undergone a significant change: the anionic hydrochemical type transitioned from HCO3− dominance to a mixed HCO3− and SO42− type, while the cationic hydrochemical type evolved from a combination of Na+, Ca2+, and Mg2+ to a predominately Na+ type. This variation process reflects that the hydrochemical formation mechanism tends to be complex from shallow to deep strata. Further analysis reveals that cation exchange and leaching effects are continuously enhanced with the increase in groundwater depth; cation exchange contributed to elevated K++Na+ mass concentrations in deeper groundwater, while leaching processes led to the oxidation of sulfide minerals within the coal seams, resulting in heightened SO42− mass concentration. The differences of water chemical characteristics of different aquifers and the hydraulic connections between them are crucial for the accurate identification of mine water sources. At the same time, it is also helpful to determine the impact of the fall zone or water conduction fracture zone on the formation, and provide more accurate information and scientific basis for the prevention and control of coal mine water damage, so as to effectively ensure safety production.

       

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