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高原金属矿区地下水与地表水时空演变规律及交互作用

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高原矿区地下水与地表水交互作用研究对高原矿山生态环境保护具有重要意义.文章以普朗铜矿为研究对象,对不同海拔、不同埋深处土体湿度进行了长期的原位监测,结合降雨量和地下水位变化数据,分析了高原矿区地下水与地表水时空演变规律及其交互作用机理.结果表明:不同深度的土体湿度变化趋势基本一致;海拔高度会显著影响土体湿度水平,但土体湿度随时间的演化规律并不受海拔高度影响;土体湿度曲线与降雨量曲线变化趋势基本相同;土体湿度变化超前于钻孔水位变化10~20 天.
Study on Spatiotemporal Evolution Rule and Interaction of Groundwater and Surface Water in Plateau Metal Mining Areas
The study on the interaction between groundwater and surface water in plateau mining areas is of great significance for the ecological environment protection of plateau mines.This paper takes the Pulang Copper Mine as the research object,conducting long-term in-situ monitoring of soil moisture at different altitudes and depths.By combining data on rainfall and fluctuations in groundwater levels,it analyzes the temporal and spa-tial evolution patterns of groundwater and surface water in the plateau mining area,as well as the mechanisms of their interaction.The results show that the change trends of soil moisture at different depths are fundamentally consistent.The altitude significantly affects the level of soil moisture;however,the temporal evolution of soil moisture is not influenced by altitude.The trends of the soil moisture curves are generally similar to those of the rainfall curves.Additionally,changes in soil moisture precede changes in borehole water levels by 10 to 20 days.

Metal mineGroundwaterSurface waterSpatiotemporal evolution

冯兴隆、董桥峰、沈啟武、沙有财、孔垂爱、贺勇

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云南迪庆有色金属有限责任公司,云南 香格里拉 674400

中南大学有色金属成矿预测与地质环境监测教育部重点实验室,湖南 长沙 410083

金属矿山 地下水 地表水 时空演变

云南省科学技术厅科技人才与平台计划云南迪庆有色金属有限责任公司科研项目

202205AD160063DQYS-ZYB-09-2021001

2024

有色金属设计
昆明有色冶金设计研究院

有色金属设计

影响因子:0.184
ISSN:1004-2660
年,卷(期):2024.51(3)