摘要
本文分析了矿床的水文工程地质特征,研究表明:黄山东铜镍矿床的水文地质条件较为简单,属于简单—中等裂隙充水矿床类型,矿区所在区域属于大陆性干燥气候区,少雨蒸发量大,导致地表洪流水系不能形成地下水的补给来源,矿体的顶底板均受基岩裂隙水充水在矿床开采早期涌水量相对较大,随着开采的进行,涌水量逐渐减少直至干涸。
This paper analyzes the hydrogeological characteristics of the ore deposit, and shows that the hydrogeological conditions of the copper and nickel deposit in Huang Cave are simple, belonging to the simple-medium fractured water deposit type, the area of the mining area belongs to the continental dry climate zone, the evaporation of less rain is large,The surface torrent water system can not form the source of groundwater recharge, the top bottom plate of the orebody is relatively large water inrush in the early stage of the deposit mining, and with the mining, the water inrush decreases gradually until it dries up.
引文
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