安徽地质2025，Vol.35Issue(3)：215-217,223,4.
安徽庐江泥河铁矿水文地质特征及矿坑涌水量预测
Hydrogeological assessment and pit water inflow prediction at the Nihe iron mine,Lujiang,Anhui Province
张骏 1王鹏飞1
作者信息
- 1. 安徽省地质矿产勘查局327地质队,安徽 合肥 230011
- 折叠
摘要
Abstract
The Nihe iron deposit is classified as a porphyritic iron-sulfur deposit with fissure-type water filling,where primary water-bearing lithologies include the Shuangmiao Formation volcanic rocks and secondary quartzite exhibiting low aquifer productivity.Utilizing analytical methods,this study predicts a maximum pit water inflow of 5343 m³/d at the-675 m elevation in the initial mining section,establishing critical benchmarks for early-stage mine drainage system design.关键词
泥河铁矿/水文地质特征/解析法/涌水量预测Key words
Nihe iron deposit/hydrogeology/analytical method/water inflow prediction分类
天文与地球科学引用本文复制引用
张骏,王鹏飞..安徽庐江泥河铁矿水文地质特征及矿坑涌水量预测[J].安徽地质,2025,35(3):215-217,223,4.
