基于电阻率−声波测井联合的顶板砂岩富水性评价方法研究

    Study on roof sandstone water abundance evaluation based on resistivity-acoustic logging combination

    • 摘要: 受河流−三角洲沉积体系影响,鄂尔多斯盆地侏罗系煤层顶板砂岩岩性变化快、泥质含量高,导致其富水性精细预测难度较大。针对这一难题,以内蒙古巴彦高勒矿3号煤层顶板砂岩含水层为例,基于测井资料,采用Simandoux公式定量分析了顶板砂岩的含水饱和度分布;通过λρ−μρ(拉梅常数λ与密度ρ乘积−剪切模量μ与密度ρ乘积)交会分析,对电阻率测井定量预测结果进行了验证;综合砂岩厚度、孔隙度及含水饱和度,构建了富水性评价指数;并在变差函数分析的基础上,采用序贯高斯模拟方法,预测了顶板砂岩平面富水性分布。结果表明:3号煤层顶板砂岩整体具有含水饱和度高、厚度大、孔隙度高的特征,但纵、横向非均质性强;λρ−μρ交会图能够有效区分砂岩孔隙度与含水饱和度的差异,从而侧面验证了电阻率测井富水性预测结果的可靠性;顶板砂岩富水区域主要分布于研究区西北部与东北部,与瞬变电磁法所预测的低阻异常区吻合良好。相较于传统Archie公式,Simandoux公式在预测侏罗系煤层顶板砂岩含水饱和度方面更具适用性。因此,基于电阻率−声波测井联合的富水性评价方法,不仅是对现有技术的有益补充,也为解决该类评价难题提供了有效途径,可为地下水资源保护与矿井顶板水害防控提供可靠的技术支撑。

       

      Abstract: Affected by the fluvial-deltaic sedimentary system, the Jurassic coal seam roof sandstone in the Ordos Basin is characterized by rapid lithological changes and high argillaceous content, resulting in great difficulties in the fine prediction of its water abundance. To address this problem, taking the roof sandstone aquifer of No.3 coal seam in Bayangaole Mine, Inner Mongolia as an example, based on logging data, the Simandoux formula was used to quantitatively analyze the water saturation distribution of the roof sandstone; the quantitative prediction results of resistivity logging were verified through λρ-μρ (product of Lame constant λ and density ρ - product of shear modulus μ and density ρ) crossplot analysis; integrating sandstone thickness, porosity and water saturation, a water abundance evaluation index was constructed; and on the basis of variogram analysis, the sequential Gaussian simulation (SGS) method was adopted to predict the planar water abundance distribution of the roof sandstone. The results show that the roof sandstone of No. 3 coal seam is generally characterized by high water saturation, large thickness and high porosity, but exhibits strong vertical and horizontal heterogeneity; the λρ-μρ crossplot can effectively distinguish the differences between sandstone porosity and water saturation, thereby indirectly verifying the reliability of the water abundance prediction results from resistivity logging; the water-rich areas of the roof sandstone are mainly distributed in the northwest and northeast of the study area, which are in good agreement with the low-resistivity anomaly areas predicted by the transient electromagnetic method. Compared with the traditional Archie formula, the Simandoux formula is more applicable in predicting the water saturation of Jurassic coal seam roof sandstone. Therefore, the water abundance evaluation method based on the combination of resistivity and acoustic logging is not only a useful supplement to the existing technologies, but also provides an effective approach to solving such evaluation problems, and can offer reliable technical support for groundwater resource protection and mine roof water hazard prevention and control.

       

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