临沂方城盆地白垩纪潜火山岩蓄水构造富水特征分析
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Analysis on Water Rich Characteristics of Cretaceous Subvolcanic Rocks in Fangcheng Basin in Linyi City
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    摘要:

    通过水文地质调查、地质钻探、抽水试验、水化学分析等手段,对临沂方城盆地白垩纪火山岩地下水富集规律及水化学特征进行综合研究,发现方城盆地潜火山岩与周围火山碎屑岩构成具有供水意义的岩脉型潜火山岩蓄水构造。潜火山岩蓄水构造富水性中等,钻孔单位涌水量18.7~310.7m3/(d·m),地下水溶解性总固体一般<1g/L,水化学类型以HCO3Ca型、HCO3Ca·Mg型、HCO3·ClCa型、HCO3·ClCa·Mg型为主,水质良好,可以作为火山岩贫水地区抗旱打井的目标含水层之一。该发现对解决沂蒙山火山岩贫水区农村集中供水水源问题具有重要意义。

    Abstract:

    Through hydrogeological investigation, geological drilling, pumping tests, hydrochemical analysis and other methods, a comprehensive study has been conducted on the enrichment law and hydrochemical characteristics of groundwater in Cretaceous volcanic rocks in Fangcheng basin in Linyi city. It is found that volcanic rocks in Fangcheng basin and the surrounding volcanic debris rocks constitute a vein type volcanic rock water storage structure with water supply significance. The water storage structure of Qianhuoshan rock has moderate water richness, with a unit water inflow of 18.7~310.7m3/(d · m) for drilling. The total dissolved solids in groundwater are generally less than 1g/L. The hydrochemical types are mainly HCO3 Ca type, HCO3 Ca · Mg type, HCO3 · Cl Ca type, and HCO3 · Cl Ca · Mg type. The water quality is good, and it can be used as one of the target aquifers for drought resistant well drilling in areas with poor water in volcanic rocks. This discovery is of great significance for solving the problem of centralized water supply sources for rural areas in Yimeng Mountain volcanic rock poor water area.

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纪汶龙,徐建国,王玮,徐华,刘春华,刘治政,刘华峰,张卓,刘中业.临沂方城盆地白垩纪潜火山岩蓄水构造富水特征分析[J].山东国土资源,2025,41(7):

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  • 在线发布日期: 2025-07-22