Hydrogeological feasibility of mine water deep geological storage in Baotashan coarse sandstone: A case study in Ordos Basin

Ge Chen, Yajun Sun, Zhimin Xu, Xin Li
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引用次数: 3

Abstract

For the sake of mine water drainage and sustainable groundwater protection, the new approach of mine water deep geological storage (MWDGS) is highly necessary to save water resources in the semi-arid region of China. However, up to now, little academic research has been done on mine water geological storage. Given this situation, the hydrogeological feasibility of MWDGS was explored in Baotashan coarse sandstone (BCS) of Jurassic measure in Ordos Basin. The results show that the white-gray BCS with a fragile skeleton of quartz (41.4%), feldspar (21.1%), and clay minerals (16.4%) provides the potential variable-void for mine water; and its hydro-chemical type of BCS aquifer is CO3-Na and Cl-Na. As the burial depth increases, the strong alkaline groundwater is in stagnant and poor recharge-runoff-discharge condition. The lab test shows that the pores whose diameter is over 10 μm could be treated as the main storage of mine water; and the effective porosity varies from 1.36% to 3.46%. When mine water is injected, the strong hydrodynamics of mine water storage would change the permeability significantly and about 0.201% soluble solids would be dissolved. Partial clay minerals obstruct the pores and induce the saturated phase of high permeability to evolve into steady phase of lower permeability. Under the condition of nonhydraulic fracturing during continuous storage, the heterogeneous anisotropic medium obtained by Transition PRObability GeoStatistics (TPROGS) shows that the capacity of BCS aquifer is 0.455 to 1.226 Mm3 for 1 km2 in the study area. The simulation shows that the groundwater mound in well-scale and mine-scale would be formed. The groundwater quality characteristics of “Three Zone” would occur around and gradually drop to approximate the original brine within 10 years. The hydrogeological feasibility reveals that this approach is useful for the well design and groundwater environment management during the mine water deep geological storage project in the Ordos basin.

Abstract Image

宝塔山粗砂岩矿井水深储水文地质可行性——以鄂尔多斯盆地为例
为了矿井水的排水和地下水的可持续保护,在中国半干旱区,采用矿井水深层地质蓄水新方法节约水资源是十分必要的。然而,迄今为止,学界对矿井水地质蓄水的研究还很少。在此基础上,对鄂尔多斯盆地宝塔山侏罗系粗砂岩(BCS)进行了水文地质可行性研究。结果表明:以石英(41.4%)、长石(21.1%)和粘土矿物(16.4%)为脆弱骨架的白灰色BCS为矿井水提供了潜在的可变孔隙;BCS含水层水化学类型为CO3-Na和Cl-Na。随着埋深的增加,强碱性地下水处于停滞状态,补给-径流-排放状况较差。室内试验表明,孔径大于10 μm的孔隙可以作为矿井水的主要储集层;有效孔隙度为1.36% ~ 3.46%。注入矿井水时,矿井储水的强水动力作用使渗透率发生明显变化,约0.201%的可溶性固形物被溶解。部分粘土矿物堵塞孔隙,导致高渗透饱和阶段向低渗透稳定阶段演化。在非水力压裂连续储层条件下,利用过渡概率地质统计(Transition PRObability GeoStatistics, TPROGS)获得的非均质各向异性介质表明,研究区BCS含水层1 km2的储层容量为0.455 ~ 1.226 Mm3。模拟结果表明,井尺度和矿山尺度的地下水丘将形成。“三带”地下水水质特征将在10年左右出现,并逐渐下降到接近原盐水的水平。水文地质可行性表明,该方法可用于鄂尔多斯盆地矿井水深层地质蓄水工程的井设计和地下水环境管理。
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