以 "Polkowice-Sieroszowice "矿为重点,对流入 Legnica-Głogów 铜矿区矿井的地下水进行数值预测

IF 0.4 Q4 ENVIRONMENTAL SCIENCES Geology, Geophysics and Environment Pub Date : 2024-01-31 DOI:10.7494/geol.2024.50.1.61
J. Gurwin, M. Wcisło
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引用次数: 0

摘要

本文介绍了波兰莱格尼察-格沃古夫铜矿区(Legnica-Głogów Copper District,LGCD)矿山水文地质数值模型的研究成果。由于排水造成的对岩体和多层凹陷锥体的广泛影响,模型覆盖面积达 3,049 平方公里。由于多含水层水文地质系统的复杂性和相互水力联系,该模型需要覆盖矿区范围以外的区域,并分离出 17 个数值层。研究是在 GMS 软件环境中使用 Modflow 计算模块进行的。由于模型的结构、参数和边界条件会发生变化,因此对模型进行了连续更新。此外,还根据压强计测量的新数据和记录的挖掘流入量的变化对模型进行了校准。通过模拟,可以确定准确的水平衡,重点是西罗佐维采矿区,因为在该地区发现了突如其来的流入量。随后,进行了两次预测模拟,以估算 2020 年和 2025 年矿井的动态进水量。
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Numerical forecast of groundwater inflow to the mines of the Legnica-Głogów Copper District with a particular emphasis on the “Polkowice-Sieroszowice” mine
The paper presents the results of work on the numerical hydrogeological model of the mines of theLegnica-Głogów Copper District (LGCD) in  Poland. Due to the extensive impact on the rock mass and the multi-layer depression cone caused by drainage, the model covers an area of 3,049 km2 . The complicated, mutual hydraulic connections of the multi-aquifer hydrogeological system required the model to cover the area beyond the range of mining areas, and to separate 17 numerical layers. The research was carried out in the GMS software environment using Modflow computing modules. The model was updated successively, since its structure, parameters, and boundary conditions are subject to change. It was also additionally calibrated based on new data from measurements in piezometers and changes recorded in inflows to the excavations. The simulations made it possible to determine the exact water balance, with a particular emphasis on the Sieroszowice mining area, where sudden unexpected inflows were noted. Subsequently, two prognostic simulations were performed to estimate dynamic water inflows to mine workings in the years 2020 and 2025.
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