Fluid Mobility Evaluation of Tight Sandstones in Chang 7 Member of Yanchang Formation, Ordos Basin

被引:13
|
作者
Wu, Songtao [1 ,2 ,3 ]
Li, Shixiang [4 ]
Yuan, Xuanjun [1 ,2 ,3 ]
Yang, Zhi [1 ]
Li, Aifen [3 ,5 ]
Cui, Jingwei [1 ,2 ]
Pan, Songqi [1 ]
Mao, Zhiguo [1 ,2 ,3 ]
Su, Ling [1 ,2 ,3 ]
Zhou, You [1 ,2 ,3 ,6 ]
机构
[1] Res Inst Petr Explorat & Dev, CNPC, Beijing 100083, Peoples R China
[2] Key Lab Oil & Gas Reservoirs, CNPC, Beijing 100083, Peoples R China
[3] Natl Energy Tight Oil & Gas R&D Ctr, Beijing 100083, Peoples R China
[4] Changqing Oilfield Co, PetroChina, Xian 710000, Peoples R China
[5] China Univ Petr, Qingdao 266510, Peoples R China
[6] Hebei Univ Engn, Sch Civil Engn, Handan 056000, Peoples R China
基金
中国国家自然科学基金;
关键词
tight oil; shale oil; unconventional petroleum accumulation; nano-pores; movable oil; PORE-THROAT; OIL; SHALE; GAS; POROSIMETRY; RESERVOIR; WOODFORD; BARNETT; FLOW;
D O I
10.1007/s12583-020-1050-2
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Fluid mobility has been important topic for unconventional reservoir evaluation. The tight sandstones in Chang 7 Member of the Ordos Basin has been selected to investigate the fluid mobility based on the application of core flooding-NMR combined method and core centrifugation-NMR combined method, and the porous structure is studied using optical microscope, field emission scanning electron microscope (FE-SEM), CT and mercury injection. Our results include: (i) Feldsparrock fragments dissolution pores, calcite dissolution pores, clay mineral dissolution pores, intergranular dissolution expansion pores, inter-granular pores, intra-kaolinite pores, and intra-illite/smectite mixed layer pores are developed in Chang 7 tight sandstones; 3D CT pore structure shows that the pore connectivity is positively related to physical properties, and the overall storage space is connected by the throat with diameter between 0.2 and 0.3 mu m. The percentage of storage space connected by throats with diameter less than 100 nm can reach more than 35%. (ii) Movable fluid saturation of Chang 7 tight sandstones is between 10% and 70%, and movable oil saturation is between 10% and 50%. Movable fluid saturation may cause misunderstanding when used to evaluate fluid mobility, so it is recommended to use movable fluid porosity in the evaluation of fluid mobility. The porosity ranging from 5% to 8% is the inflection point of the fluidity and pore structure. For samples with porosity less than 8%, the movable fluid porosity is generally less than 5%. Moreover, the movable fluid is mainly concentrated in the storage space with a throat diameter of 0.1 to 1 mu m. For samples with porosity greater than 8%, the porosity of the movable fluid is more than 5%, and the movable fluid is mainly concentrated in the storage space with a throat diameter of 0.2 to 2 mu m. (iii) The movable fluid saturation measured by core flooding-NMR combined method is generally higher than that measured by core centrifugation-NMR combined method. The former can evaluate the mobility of the oil-water two-phase fluid in samples, while the latter can better reflect the pore structure and directly evaluate the movable fluid in the pore system controlled by different throat diameters. All these results will provide valuable reference for fluid mobility evaluation in tight reservoirs.
引用
收藏
页码:850 / 862
页数:13
相关论文
共 50 条
  • [41] Gas Desorption Characteristics of the Chang 7 Member Shale in the Triassic Yanchang Formation, Yan'an Area, Ordos Basin
    Fan, Bojiang
    Dai, Xinyang
    Wang, Chi
    [J]. MINERALS, 2023, 13 (05)
  • [42] PROVENANCE ANALYSIS OF THE CHANG 7 MEMBER OF THE UPPER TRIASSIC YANCHANG FORMATION IN ZHENYUAN AREA, ORDOS BASIN, CHINA
    He, Weiling
    Lyu, Qiqi
    Li, Yudong
    Xi, Mingli
    Duan, Changjiang
    [J]. FRESENIUS ENVIRONMENTAL BULLETIN, 2020, 29 (02): : 1190 - 1199
  • [44] Lithology and oil-bearing properties of tight sandstone reservoirs: Chang 7 member of Upper Triassic Yanchang Formation, southwestern Ordos Basin, China
    Feng, Congjun
    Yang, Hua
    Pu, Renhai
    Wang, Yaning
    Wang, Daxing
    Liang, Xiaowei
    Zhang, Mengbo
    Huang, Yougen
    Fei, Shixiang
    [J]. GEOSCIENCES JOURNAL, 2017, 21 (02) : 201 - 211
  • [45] Lithology and oil-bearing properties of tight sandstone reservoirs: Chang 7 member of Upper Triassic Yanchang Formation, southwestern Ordos Basin, China
    Congjun Feng
    Hua Yang
    Renhai Pu
    Yaning Wang
    Daxing Wang
    Xiaowei Liang
    Mengbo Zhang
    Yougen Huang
    Shixiang Fei
    [J]. Geosciences Journal, 2017, 21 : 201 - 211
  • [46] Analysis of tight oil accumulation mechanism of Chang 7 member in the Ordos basin
    Qu, Tong
    Gao, Gang
    Liang, Xiaowei
    Sun, Mingliang
    You, Yuan
    Dang, Wenlong
    Dan, Weidong
    [J]. Dizhi Xuebao/Acta Geologica Sinica, 2022, 96 (02): : 616 - 629
  • [47] STUDY ON THE VARIATION RULE OF ROCK ELECTRICAL PARAMETERS FOR TIGHT SANDSTONE RESERVOIRS IN CHANG 7 MEMBER OF YANCHANG FORMATION IN LONGDONG AREA OF ORDOS BASIN, CHINA
    Zhong, Gaorun
    Zhang, Xiaoli
    Li, Yajun
    [J]. FRESENIUS ENVIRONMENTAL BULLETIN, 2020, 29 (01): : 385 - 392
  • [48] Features of Tight Sandstone Reservoir and Origin of Tightness:An Example from Chang-7 Member,Triassic Yanchang Formation in Chenghao Area,Ordos Basin
    ER Chuang
    ZHAO Jingzhou
    BAI Yubin
    WU Weitao
    ZHANG Jie
    WEI Zhikun
    [J]. Acta Geologica Sinica(English Edition), 2015, 89(S1) (English Edition) - 26
  • [49] Features of Tight Sandstone Reservoir and Origin of Tightness:An Example from Chang-7 Member,Triassic Yanchang Formation in Chenghao Area,Ordos Basin
    ER Chuang
    ZHAO Jingzhou
    BAI Yubin
    WU Weitao
    ZHANG Jie
    WEI Zhikun
    [J]. Acta Geologica Sinica(English Edition), 2015, (S1) : 25 - 26
  • [50] Characteristics and controlling factors of lacustrine tight oil reservoirs of the Triassic Yanchang Formation Chang 7 in the Ordos Basin, China
    Xu, Zhengjian
    Liu, Luofu
    Wang, Tieguan
    Wu, Kangjun
    Dou, Wenchao
    Song, Xingpei
    Feng, Chenyang
    Li, Xiaozhong
    Ji, Haitao
    Yang, Yueshu
    Liu, Xiaoxiang
    [J]. MARINE AND PETROLEUM GEOLOGY, 2017, 82 : 265 - 296