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采空区破碎煤岩体溶蚀作用及净水机理实验研究

王方田 郝文华 张村 孙暖 熊集兵 范常浩

王方田, 郝文华, 张村, 孙暖, 熊集兵, 范常浩. 采空区破碎煤岩体溶蚀作用及净水机理实验研究[J]. 矿业科学学报, 2023, 8(4): 464-473. doi: 10.19606/j.cnki.jmst.2023.04.003
引用本文: 王方田, 郝文华, 张村, 孙暖, 熊集兵, 范常浩. 采空区破碎煤岩体溶蚀作用及净水机理实验研究[J]. 矿业科学学报, 2023, 8(4): 464-473. doi: 10.19606/j.cnki.jmst.2023.04.003
Wang Fangtian, Hao Wenhua, Zhang Cun, Sun Nuan, Xiong Jibing, Fan Changhao. Experimental study on dissolution effect and water purification mechanism of broken coal and rock mass in goaf[J]. Journal of Mining Science and Technology, 2023, 8(4): 464-473. doi: 10.19606/j.cnki.jmst.2023.04.003
Citation: Wang Fangtian, Hao Wenhua, Zhang Cun, Sun Nuan, Xiong Jibing, Fan Changhao. Experimental study on dissolution effect and water purification mechanism of broken coal and rock mass in goaf[J]. Journal of Mining Science and Technology, 2023, 8(4): 464-473. doi: 10.19606/j.cnki.jmst.2023.04.003

采空区破碎煤岩体溶蚀作用及净水机理实验研究

doi: 10.19606/j.cnki.jmst.2023.04.003
基金项目: 

国家自然科学基金 51974297

国家自然科学基金 52104155

北京市自然科学基金 8212032

徐州市重点研发计划(社会发展)-社会事业 KC22283

详细信息
    作者简介:

    王方田(1985—),男,河南永城人,博士,教授,博士生导师,主要从事煤岩力学响应及煤系资源智能绿色开采等方面的研究工作。Tel:13605202425,E-mail:wangfangtian111@163.com

    通讯作者:

    张村(1990—),男,江苏海门人,博士,副教授,博士生导师,主要从事矿山压力控制与煤矿绿色开采方面的研究工作。Tel:15810194127,E-mail:cumt-zc@cumtb.edu.cn

  • 中图分类号: TD745

Experimental study on dissolution effect and water purification mechanism of broken coal and rock mass in goaf

  • 摘要: 开展地下水库采空区破碎煤岩体溶蚀作用及净水机理研究,是实现矿井地下水库安全高效运行的关键。本文以锦界煤矿31409工作面开采形成的地下水库为工程背景,选取采空区破碎煤岩体及去离子水进行污染物释放规律实验研究,分析了采空区破碎煤岩体溶蚀作用规律,探究了破碎煤岩体对水体特征影响机理,获得了破碎煤岩体在不同温度、风化条件下污染物释放规律,并分析了地下水库净水过程中的沉淀溶蚀作用。溶蚀作用及岩体中黏土矿物表面对可溶性有机质的吸附、沉淀作用等水岩作用决定了地下水库净水特征,在不同的时间范围里,溶蚀作用和吸附沉淀作用各自占主导作用,影响矿井水质。
  • 图  1  煤矿地下水库净水机理示意图

    Figure  1.  Schematic diagram of water purification mechanism of underground reservoir in coal mine

    图  2  破碎后的煤岩体样品

    Figure  2.  Broken coal and rock samples

    图  3  水浴锅试验装置及浸泡装置示意图

    Figure  3.  Water bath pot test device and soaking device

    图  4  不同温度及风化程度下浸泡液Na+含量变化曲线

    Figure  4.  Change curve of Na+ content in soaking solution under different temperature and weathering degrees

    图  5  不同温度及风化程度下浸泡液K+含量变化曲线

    Figure  5.  Change curve of K+ content in soaking solution under different temperature and weathering degrees

    图  6  不同风化程度下浸泡液Ca2+含量变化曲线

    Figure  6.  Change curve of Ca2+ content in soaking solution under different weathering degrees

    图  7  不同风化程度下浸泡液NO3-含量变化曲线

    Figure  7.  Change curve of NO3- content in soaking solution under different weathering degrees

    图  8  不同风化程度下浸泡液SO42-含量变化曲线

    Figure  8.  Change curve of SO42- content in soaking solution under different weathering degrees

    图  9  不同时间下矿井水总碱度和总硬度变化曲线

    Figure  9.  Variation curves of total alkalinity and total hardness for mine water at different times

    表  1  矿井水主要离子浓度分析

    Table  1.   Analysis of main ion concentration in mine water mg/L

    水样 Fe3+ Al3+ NH3/NH4+ Na+ Ca+ Cl- SO42- HCO3-
    离子浓度 0.51~0.66 0.04~0.05 0.387~0.439 172.65~184.94 210.5~278.2 42.1~52.1 475.1~495.1 141.3~160.4
    下载: 导出CSV

    表  2  破碎煤岩体主要化学成分组成

    Table  2.   Main chemical composition of broken coal and rock mass %

    化学组分 SiO2 Al2O3 Fe2O3 CaO MgO Na2O K2O TiO2 P2O5
    风化煤岩体 52.34 12.32 1.05 0.08 0.54 0.25 1.73 0.45 0.12
    新鲜煤岩体 44.27 9.43 1.58 1.21 0.82 0.37 0.54 0.52 0.16
    下载: 导出CSV

    表  3  金属离子沉淀pH值

    Table  3.   Metal ions precipitation boundary pH

    金属离子 pH值
    开始沉淀 完全沉淀
    Fe3+ 2.7 3.7
    Al3+ 3.7 4.7
    Cu2+ 4.4 6.4
    Zn2+ 6.0 8.0
    Fe2+ 7.6 9.6
    Mg2+ 9.3 10.8
    Ca2+ 8.0 12.0
    下载: 导出CSV
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  • 收稿日期:  2022-11-23
  • 修回日期:  2023-02-06
  • 刊出日期:  2023-08-31

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