周淋, 杨文敬, 谢题志, 田国庆, 管岩, 何辉, 朱玉双. 2022: 苏里格气田南区莲102井区盒8段储层微观孔隙结构及气-水渗流特征. 地质通报, 41(4): 682-691. DOI: 10.12097/j.issn.1671-2552.2022.04.012
    引用本文: 周淋, 杨文敬, 谢题志, 田国庆, 管岩, 何辉, 朱玉双. 2022: 苏里格气田南区莲102井区盒8段储层微观孔隙结构及气-水渗流特征. 地质通报, 41(4): 682-691. DOI: 10.12097/j.issn.1671-2552.2022.04.012
    ZHOU Lin, YANG Wenjing, XIE Tizhi, TIAN Guoqing, GUAN Yan, HE Hui, ZHU Yushuang. 2022: Reservoir micropore structure and gas-water percolation in He 8 member of Well Lian 102 in south area of Sulige gas field. Geological Bulletin of China, 41(4): 682-691. DOI: 10.12097/j.issn.1671-2552.2022.04.012
    Citation: ZHOU Lin, YANG Wenjing, XIE Tizhi, TIAN Guoqing, GUAN Yan, HE Hui, ZHU Yushuang. 2022: Reservoir micropore structure and gas-water percolation in He 8 member of Well Lian 102 in south area of Sulige gas field. Geological Bulletin of China, 41(4): 682-691. DOI: 10.12097/j.issn.1671-2552.2022.04.012

    苏里格气田南区莲102井区盒8段储层微观孔隙结构及气-水渗流特征

    Reservoir micropore structure and gas-water percolation in He 8 member of Well Lian 102 in south area of Sulige gas field

    • 摘要: 苏里格气田南区莲102井区盒8段储层孔隙结构复杂,气-水渗流规律不清,因此,运用铸体薄片、图像孔隙、扫描电镜、高压压汞等测试方法对研究区储层孔隙结构进行分析,利用气-水相渗流及可视化渗流实验方法,研究了成藏过程中的气-水渗流特征。研究结果表明,研究区盒8段储层孔隙以岩屑溶孔为主,粒间孔次之,晶间孔及粒间溶孔发育较少,喉道类型以片状喉道和弯片状喉道为主,平均喉道半径0.3 μm。根据孔隙度、渗透率、排驱压力及最大进汞饱和度,将盒8段储层孔隙结构分为3类,从Ⅰ类至Ⅲ类孔隙组合类型分别为粒间孔-溶孔、晶间孔-溶孔、溶孔-晶间孔; 孔喉半径分布由单峰型或左高右低双峰型转变为左低右高双峰型,主流喉道半径逐渐变小; 储层物性由好变差,孔隙连通性也逐渐变差。研究区目的层气驱水类型分为3类,分别为均匀驱替、网状驱替和指状驱替,不同气驱水类型的储层,气-水两相渗流束缚水饱和度及两相渗流区宽度差异较大。气-水渗流特征与物性和孔隙结构关系密切,从Ⅰ类至Ⅲ类气驱水由均匀驱替过渡为网状驱替再到指状驱替,两相共渗区域由宽变窄,等渗点由高变低,且束缚水饱和度逐渐增高,渗流能力由强变弱。基于储层渗流规律,预测研究区有利开发区域,为研究区勘探开发提供依据。

       

      Abstract: The reservoir pore structure of He 8 member in Lian 102 well block in the south area of Sulige gas field is complex and the law of gas-water seepage is unclear.Therefore, this paper analyzes the reservoir pore structure in the study area by using cast thin section, image pore, scanning electron microscope and high-pressure mercury injection, and studies the characteristics of gas-water seepage in the process of reservoir formation by using gas-water phase permeability and visual seepage experiments.The results show that the pores of He 8 reservoir in the study area are mainly rock debris dissolved pores, followed by intergranular pores, intergranular pores and intergranular dissolved pores less developed, and the throat types are mainly flaky throat and curved flaky throat, with an average throat radius of 0.3 μm.According to porosity, permeability, displacement pressure and maximum mercury saturation, the pore structure of He 8 reservoir in the study area is divided into three types.From class I to class III, the pore combination types are intergranular pore dissolved pore, intergranular pore dissolved pore and dissolved pore intergranular pore respectively.The distribution of pore throat radius changes from single peak type or left high right low bimodal type to left low right high bimodal type, and the radius of mainstream throat gradually decreases.The physical property of the reservoir changes from good to bad, and the pore connectivity also gradually becomes worse.The types of gas drive water in the target layer in the study area are divided into three types: uniform displacement, mesh displacement and finger displacement.For reservoirs with different types of gas drive water, there are great differences in gas-water two-phase seepage, irreducible water saturation and two-phase seepage area width.The characteristics of gas water seepage are closely related to physical properties and pore structure.From class I to class III gas drive water, it changes from uniform displacement to mesh displacement, and then to finger displacement.The two-phase permeability area changes from wide to narrow, and the isopermeability point changes from high to low, the irreducible water saturation gradually increases, and the seepage capacity changes from strong to weak.Based on the reservoir seepage law, the favorable development area in the study area is predicted to provide a basis for exploration and development in the study area.

       

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