吐哈盆地艾丁湖三区煤炭地下气化地质评价与有利区预测

Geological evaluation and prediction of favorable areas of underground coal gasification in the Third Area of Aiding Lake in Tuha Basin

  • 摘要: 以吐哈煤田艾丁湖三区煤储层为研究对象,从煤岩煤质特征、煤层赋存特征、水文特征、围岩特征、地质构造特征等角度进行了系统分析,采用层次分析法、变异系数法和TOPSIS法等数学分析方法,构建了煤炭地下气化地质选层资源评价体系,探究了吐哈煤田艾丁湖三区煤炭地下气化的可行性,并优选了有利区。研究结果表明:研究区呈缓倾斜的单斜构造,断层不发育,煤层结构简单,属于稳定的中厚煤层,灰分水分含量较低,埋深适中;顶底板多为细砂岩、粉砂岩及泥岩,适宜进行煤炭地下气化工作。在此基础上进一步优选出煤层厚度、煤层埋深和煤层倾角等19个地质影响因素作为二级评价指标,计算了其综合权重并进行了分级处理,并确定了各二级指标的组合权重,通过利用模糊数学综合评价法对三区6号煤层进行了定量评价与地质选区,优选出2个有利区和2个较有利区,为该区后续的地下气化工作实施提供科学依据和有力保障,也对其他地区煤炭地下气化地质选区具有借鉴意义。

     

    Abstract: Taking the coal reservoir in the Aiding Lake Area of the Tuha Coalfield as the research object, the characteristics of coal, rock, coal quality, coal seam occurrence, hydrological features, surrounding rock properties, and geological structural characteristics are systematically analyzed. Mathematical analysis methods such as the analytic hierarchy process, coefficient of variation method, and TOPSIS method are adopted to establish a geological layer-selection resource evaluation system for underground coal gasification. The feasibility of underground coal gasification in the Third Area of Aiding Lake in the Tuha Coalfield is investigated, and favorable zones are identified. The results show that the study area has a gently inclined monoclinic structure with undeveloped faults; the coal seams have a simple structure, stable medium thickness, low ash and moisture content, and moderate burial depth; the roof and floor are mostly composed of fine sandstone, siltstone, and mudstone. Overall, the area is suitable for underground coal gasification. On this basis, 19 geological influencing factors—including coal seam thickness, burial depth, and inclination—are further selected as secondary evaluation indices. Their comprehensive weights are calculated and graded, and the combined weights of each secondary index are determined. The fuzzy mathematical comprehensive evaluation method is applied to conduct quantitative evaluation and geological selection for the No. 6 coal seam in the Third Zone. Two favorable areas and two more favorable areas are identified, which provides a scientific basis and strong support for the subsequent implementation of underground gasification work in this area, and also has reference significance for geological site selection of underground coal gasification in other regions.

     

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