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    义桥煤矿矿井水水文地球化学成因及灌溉适宜性评估

    Hydrogeochemical genesis and irrigation suitability evaluation of mine water in Yiqiao Coal Mine

    • 摘要: 为了解汶上义桥煤矿有限责任公司(以下简称“义桥煤矿”)矿井水水文地球化学特征、形成机制及水质适宜性,选取了砂岩矿井水(SMW)、灰岩矿井水(LMW)和混合矿井水(MMW)共138个水样,综合运用统计分析、水文地球化学方法、钠吸附比(SAR)与钠含量百分比(Na/%)等进行了相关研究。研究结果表明,义桥煤矿矿井水整体呈弱碱性,矿井水中主要的阳离子和阴离子分别为Na+和HCO3,SMW、LMW、MMW中阳离子浓度均值存在Na+>Ca2+>Mg2+>K+的关系,阴离子浓度均值则遵循HCO3>SO42−>Cl>NO3的顺序,矿井水的水化学类型主要划分为HCO3−Na型和SO4•Cl−Na型。矿井水水文地球化学特征主要受到岩石风化和蒸发结晶作用控制,但阳离子交换是影响矿井水水化学特征的一个重要的水文地质化学过程,且以正向交换作用为主导。

       

      Abstract: In order to understand the hydrogeochemical characteristics, formation mechanism and water quality suitability of mine water in Wenshang Yiqiao Coal Mine Co., Ltd. (hereinafter referred to as "Yiqiao Coal Mine"), a total of 138 water samples of sandstone mine water (SMW), limestone mine water (LMW) and mixed mine water (MMW) were selected, and statistical analysis, hydrogeochemical methods, sodium adsorption ratio (SAR) and sodium content percentage (ω(Na)/%) were comprehensively used for related research. The results show that the mine water in Yiqiao Coal Mine is weakly alkaline as a whole. The main cations and anions in mine water are Na+ and HCO3, respectively. The average concentration of cations in SMW, LMW and MMW has the relationship of Na+>Ca2+>Mg2+>K+, and the average concentration of anions follows the order of HCO3>SO42−>Cl>NO3. The hydrochemical types of mine water are mainly divided into HCO3-Na type and SO4•Cl-Na type. The hydrogeochemical characteristics of mine water are mainly controlled by rock weathering and evaporation crystallization, but cation exchange is also an important hydrogeological chemical process that affects the chemical characteristics of mine water, and is dominated by positive exchange.

       

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