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高校地质学报 ›› 2025, Vol. 31 ›› Issue (06): 769-784.DOI: 10.16108/j.issn1006-7493.2025002

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准噶尔盆地滴南凸起西山窑组煤岩孔隙及孔径多尺度联合表征

姚卫江1, 2,胡正舟1,潘 拓1,胡 鑫1,陈中红3,李 雷1,谢俊阳1,靳晓杰3   

  1. 1.中国石油新疆油田分公司 勘探开发研究院,乌鲁木齐 830013;
    2. 怀柔国家实验室新疆基地,乌鲁木齐 830002;
    3. 中国石油大学(华东)地球科学与技术学院,青岛 266580
  • 出版日期:2025-12-20 发布日期:2025-12-20

Multi-scale Joint Characterization of Pore and Pore Size of Coal Rock in the Xishanyao Formation, Dinan Uplift, Junggar Basin

YAO Weijiang1, 2,HU Zhengzhou1,PAN Tuo1,HU Xin1,CHEN Zhonghong3,LI Lei1,XIE Junyang1,JIN Xiaojie3   

  1. 1. Research Institute of Exploration and Development, Xinjiang Oilfield Company,Petrochina, Urumqi 830013, China;
    2. Huairou National Laboratory Xinjiang Base, Urumqi 830002, China;
    3. School of Geosciences, China University of Petroleum (East China), Qingdao 266580, China
  • Online:2025-12-20 Published:2025-12-20

摘要: 相对传统煤层气储层而言,准噶尔盆地腹部滴南凸起煤岩储层普遍较深(>2500 m)。为了解该区西山窑组煤岩孔裂隙结构特征及其对煤岩气赋存与运移的影响,文章以DM-2-101井西山窑组煤岩作为研究对象,在对煤岩进行煤质、煤阶、物性(应力敏感性、密度、孔渗等)及含气性等进行检测分析的基础上,通过铸体薄片、全直径CT扫描、扫描电镜(SEM)、衍射及能谱分析等对煤岩微观孔缝发育特征进行分析,并利用微米级CT扫描、高压压汞、二氧化碳吸附、氮气吸附等多种方法对孔径分布进行了不同尺度地联合定量表征。研究表明:DM-2-101井西山窑组煤岩显微组分以惰质组和镜质组为主,平均含量分别为48.07%和45.82%,具有低水分、特低灰和低挥发分的特点。煤岩储集空间发育有静压裂缝、层间缝、胞腔孔和少量气孔,孔隙发育程度高,以胞腔孔发育为主。比表面积主要是微孔(<10 nm)的贡献,其占比达到95%以上。孔隙体积主要是大孔(>1000 nm)的贡献,其体积占比达到62.97%~65.92%;其次为微孔,体积占比为24.98%~20.39%。覆压对孔隙度和渗透率的影响存在指数递减关系,覆压状态下的孔隙度和渗透率分别能达到8.23%和1.47 mD,说明该煤岩可形成有效储层,但存在一定的非均质性。煤岩孔径分布影响了其吸附性能和含气量,吸附气是煤岩中比较广泛的赋存方式,天然气主要吸附在微孔周围;而游离气主要聚集在一些大孔内。该研究通过多方法对全孔径定量进行联合表征,明确了深层煤岩储层各级孔隙分布特征,为煤岩气赋存状态及产出机理提供了数据及理论支撑,对准噶尔盆地侏罗系西山窑组煤岩气资源潜力评估有一定指导意义。

关键词: 煤岩气, 孔隙结构, 全孔径拼接, 孔缝特征, 吸附气

Abstract: Compared with traditional coalbed methane reservoirs, the coal rock reservoir in the Dinan Bulge of Junggar Basin is generally deeper (>2500 m). In order to understand the pore structure characteristics of the coal rocks in this area and its influence on the occurrence and migration of coal gas, the coal rock of Jurassic Xishanyao Formation in the well DM-2-101 is taken as the research object. The coal quality, coal rank, physical properties (stress sensitivity, density, porosity and permeability) and gas bearing properties of the coal rocks were detected and analyzed. The characteristics of pore development of coal rocks were analyzed by casting sheet, full-diameter CT scanning, scanning electron microscopy (SEM), diffraction and energy spectrum analysis, and the pore distribution was quantitatively characterized by micrometer CT scanning, high pressure mercury injection, carbon dioxide adsorption and nitrogen adsorption. The results show that coal rock in well DM-2-101 has the characteristics of low moisture, extremely low ash and low volatile content. The maceral components of the coal rock are mainly inertinite and vitrinite, with an average content of 48.07% and 45.82%, respectively. There are numerous hydrostatic fractures, interlayer fractures, cell pores and a few pores in reservoir space, with the domination of cell pores. The specific surface area is mainly the contribution of micropores (<10 nm), which accounts for more than 95%. The pore volume is mainly the contribution of large pores (>1000 nm), and its volume proportion reaches 62.97%-65.92%. The second was micropores, which accounted for 24.98%- 20.39% of the volume. The overlying pressure has an exponential decreasing relationship with porosity and permeability, and the porosity and permeability under overlying pressure can reach 8.23% and 1.47 mD respectively, which indicates that the coal rock can form an effective reservoir, but there is a certain heterogeneity. The pore size distribution of coal rock affects its adsorption properties and gas content. Adsorbed gas is widespread in coal rock, which is mainly adsorbed around micropores. The free gas mainly accumulates in some large pores. This study clarified the pore distribution characteristics at multi-scale levels of deep coal rock reservoirs through multi-methods with full-aperture quantitative characterization, which provided data and theoretical support for the occurrence and production mechanism of coal rock gas, and had certain guiding significance for the evaluation of coal rock gas resource potential of the Jurassic Xishanyao Formation in Junggar Basin. 

Key words: coal rock gas, pore structure, full aperture splicing, pore and fracture characteristics, adsorbed gas

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