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鄂尔多斯盆地本溪组煤岩气含气性主控因素及其实践意义

Key controlling factors of coal-rock gas of Benxi Formation in Ordos Basin and its practical significance

  • 摘要: 鄂尔多斯盆地煤岩气资源丰富,多个区块勘探开发取得重大突破,然而煤岩气的含气性主控因素尚未明确,制约整体勘探开发进程。基于含气量、煤岩煤质、煤岩地化、孔隙结构等大量实测资料,系统分析了本溪组煤岩气地质条件,厘定了含气性主控因素,并开展了煤岩气资源条件分区评价。研究表明:沉积、煤阶、埋深奠定了深层煤岩含气量的整体格局。① 沉积环境制约着煤岩生烃物质基础(包括煤层厚度、煤层结构及煤岩煤质)、煤岩气原始赋存空间及保存条件的平面分布。成煤环境演化则决定了煤岩煤质的纵向差异分布,进而影响含气量的纵向非均质性。② 煤阶不仅控制了煤岩生气强度,还通过影响孔裂隙结构从而影响煤岩气的赋存空间及储集性能。随着变质程度提高,煤岩的吸附性能得到了强化。③ 现今埋深主要影响吸附气和游离气的比例,常压储层在临界深度以下,随着埋深的增加,游离气的比例有所增加,3000 m以深总气量呈减小趋势。④ 微幅构造对发育于缓坡带的煤岩气起到了局部富气的作用。⑤ 综合考虑生、储、保有利条件,明确了盆地煤岩气富集带为榆林到宜川的南北条带,平均含气量高达23 cm3/g。⑥ 依据煤岩气的内涵及含气性主控因素,结合煤层展布,构建了煤岩气资源条件评价体系,将盆地本溪组煤岩划分为4大类13个小区,Ⅰ类区主要分布在榆林地区、大宁—吉县地区和延安地区,Ⅱ类区主要分布在乌审旗一带。研究成果以期为鄂尔多斯盆地煤岩气有序勘探开发提供借鉴与参考。

     

    Abstract: The Ordos Basin is rich in coal-rock gas resources, and significant breakthroughs have been made in exploration and development in many blocks. However, the key controlling factors for the gas content of coal have not yet been clarified, which restricts the overall exploration and development process. Based on a large amount of measured data such as gas content, coal rock and coal quality, coal geochemistry,and pore structure, the geological conditions of coal-rock gas in Benxi Formation were systematically analyzed, the main controlling factors of gas content were determined, and the coal-rock gas resource conditions were evaluated by zoning. The results show that sedimentation, coal rank and buried depth have laid the overall pattern of gas content of coal. ① The sedimentary environment restricts the hydrocarbon material base (including coal seam thickness, coal seam structure and coal quality), the original occurrence space of coal-rock gas and the plane distribution of preservation conditions. The evolution of coal-forming environment determines the longitudinal difference distribution of coal quality, which in turn creates the longitudinal heterogeneity of gas content. ② Coal rank not only controls the gas generation intensity of coal, but also affects the occurrence space and reservoir performance of coal-rock gas by affecting the pore structure, and the adsorption performance of coal is strengthened with the increase of metamorphism. ③ The burial depth mainly affects the proportion of adsorbed gas and free gas, and below the critical depth, with the increase of burial depth, the proportion of free gas increases, and the total gas volume decreases after the depth exceeds 3000m. ④ The micro-amplitude structure plays a role in local gas enrichment in the development and gentle slope zone. ⑤ Taking into account the favorable conditions for hydrocarbon generation, storage, and preservation, coal-rock gas enrichment zone is clearly defined as the north-south strip from Yulin to Yichuan, with an average gas content of up to 23 cm3/g. ⑥ According to the connotation and key control factors of coal-rock gas, combined with the distribution of coal seams, the evaluation system of coal-rock gas resource conditions was constructed, and the coal seam of Benxi Formation in the basin were divided into 4 categories and 13 communities. The class I area was mainly distributed in Yulin area, Daning-Jixian area, and Yanan area, and the class II area was mainly distributed in Wushenqi area. The research results are expected to provide reference and guidance for the orderly exploration and development of coal-rock gas in the Ordos Basin.

     

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