司家营铁矿南区是正在开发建设中的大型铁矿床.矿区地处冀东平原,矿体上富含第四系含水层,是一复杂水文地质条件的大水矿床.借助地质和水文勘察资料,总结分析矿区水文地质概况,在研究矿区地层渗透特性基础上,建立了南区水文地质模型.通过对该模型的平、剖面的分析,揭示了矿区地层的水文地质特征和隔透水层的空间展布,为矿床开采设计提供依据.
Southern area of sijiaying Iron Mine is part of a large-scale iron deposit under development and construction. The mining area lies to the eastern of Hebei plain, and there is quaternary system aquifer above the orebody. This deposit is a water-rich deposit with complex hydrogeologic condition. The hydrogeologic model was established on the basis of studying the geological and hydrologic exploration data,hydrogeologic general situation,and permeability of strata. Through the analysis of plane and section of this model,the hydrogeologic characteristics and impermeable and permeable bed spatial distribution of the mining area were revealed. These results provided basis for the deposit mining design.