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新余市曹坊庙硅灰石矿矿坑涌水量预测研究OACHSSCD

Study on the Prediction of Mine Water Inflow in Caofangmiao Wollastonite Mine in Xinyu City

中文摘要英文摘要

以新余市曹坊庙硅灰石矿为研究对象,详细查明其水文地质条件、矿床充水因素,采用适宜的方法进行矿坑涌水量预测.研究结果表明:大气降水是矿床充水的主要充水水源,溶洞及顶板导水裂隙是主要充水通道;预测-70 m 中段矿坑正常涌水量为 464 m3/d,暴雨工况下最大涌水量为 1 110.068 m3/d.研究结果可为矿山未来的排水方案修正、矿山安全生产建设提供科学依据.

This paper focuses on the Caofangmiao Wollastonite Mine in Xinyu city.It involves a detailed investigation of its hydrogeological conditions and the water-filling factors of the ore deposit.Appropriate methods were employed to forecast the mine water inflow.The research results indicate that atmospheric precipitation is the primary water source for filling the deposit,with solution cavities and water-conducting fractures in the roof serving as the main water conduits.The predicted normal water inflow at the-70 m level is 464 m3/d,with a maximum inflow of 1 110.068 m3/d under storm conditions.The findings of this study contribute to providing a scientific basis for revising future mine drainage plans and ensuring safe production and construction in the mine.

张云涛

江西省核工业地质调查院,江西 南昌 330038

矿业与冶金

硅灰石矿矿床充水因素矿坑涌水量

wollastonite minewater-filling factors of ore depositmine water inflow

《中国资源综合利用》 2026 (8)

119-121,3

10.3969/j.issn.1008-9500.2026.08.038

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