Journal of Jilin University(Earth Science Edition) ›› 2025, Vol. 55 ›› Issue (1): 298-311.doi: 10.13278/j.cnki.jjuese.20230190

Previous Articles     Next Articles

Pore Structure Evaluation of Low-Permeability Sandstones Based on LDA Assisted SSOM Algorithm

Wang Ya, Liu Zongbin, Ma Kuiqian, Lu Yan, Liu Chao   

  1. Tianjin Branch, CNOOC China Limited, Tianjin 300452, China
  • Received:2024-01-07 Online:2025-01-26 Published:2025-02-07
  • Supported by:
    the National Science and Technology Major Project  of China (2016ZX05058001)

Abstract: The pore structure determines the storage and seepage capacity of the reservoir, and controls the initial production capacity of the oilfield and even the distribution of the remaining oil in the middle and late stages of development. However, at present, the characterization of the pore structure mostly stays in the core scale. To up-scale characterization of pore structure, pore structure types of cores are divided based on pore and throat size, fluid mobility and physical property parameters obtained from high-pressure mercury intrusion, nuclear magnetic resonance, and conventional physical property analysis experiments, and are used as learning supervised samples. LDA (linear discriminant analysis) algorithm is used to excavate log curves sensitive to pore structure features, and a nonlinear log prediction model is established in collaboration with SSOM (supervised self-organizing map) algorithm to evaluate pore structure of  low-permeability sandstones  in the fourth member of J oilfield in Bohai Bay basin. The results show that there are six types of pore structures developed, among which, microfractures are developed in the type Ⅰ pore structure, which is characterized by low porosity and relative high permeability. The type Ⅱ pore structure is mainly developed in fine sandstone and consists of residual intergranular pores and secondary dissolved pores. The type Ⅲ pore structure is mainly composed of secondary dissolution pores and a few residual intergranular pores, which are common in siltstone. The type Ⅳ pore structure is mainly composed of secondary dissolved pores, and pore-filled carbonate cements are commonly observed. The type Ⅴ pore structure is characterized by extensive carbonate cementation, and the pore system is dominated by micropore throats. The volume fraction of argillaceous matrix in type Ⅵ pore structure is high, and the phenomenon of relatively high porosity and low permeability often occurs. The overall accuracy rate of the LDA-SSOM prediction model attains 86.20%. In terms of the accuracy rate in blind tests, which stands at 82.67%, it outperforms prediction models like LDA-BP (back propagation) (77.00%), LDA (65.67%), and SSOM (73.33%). Moreover, it is capable of fulfilling the objective of escalating the research scale regarding pore structure.

Key words: low-permeability sandstones, pore structure evaluation, linear discriminants analysis, supervised self-organizing map

CLC Number: 

  • TE122
[1] Lu Yan, Liu Zongbin, Liao Xinwu, Li Chao, Wang Ya. Fluid Flow Characteristics in Low-Permeability Sandstone Reservoirs [J]. Journal of Jilin University(Earth Science Edition), 2025, 55(4): 1077-1090.
[2] Liu Zongbin, Li Chao, Lu Yan, Wang Ya, Huang Jianting. Fluid Occurrence State and Permeability Evaluation of Low-Permeability Sandstone Based on Pore Structure Characterization [J]. Journal of Jilin University(Earth Science Edition), 2024, 54(4): 1124-1136.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] CHU Feng-you, SUN Guo-sheng,LI Xiao-min,MA Wei-lin, ZHAO Hong-qiao. The Growth Habit and Controlling Factors of the CobaltRich Crusts in Seamount of the Central Pacific[J]. J4, 2005, 35(03): 320 -0325 .
[2] ZHOU Li-ping, SHEN Xiang-dong, LI Xue-bin, BAI Zhong-qiang. Experiment Study of Mechanical Properties of Natual Pumice Powder Cement-Soil[J]. J4, 2009, 39(3): 492 -497 .
[3] HUANG Yu-long, WANG Pu-jun, SHAO Rui. Porosity and Permeability of Pyroclastic Rocks of the Yingcheng Formation in Songliao Basin[J]. J4, 2010, 40(2): 227 -236 .
[4] PAN Dian-qi,ZHANG Zu-pei,PAN Dian-cai,CHEN Yi-min,XU Rui. A Test Research on Longitudinal Wave Velocity of Artificial Frozen Clay Under Different Temperature and Moisture Conditions[J]. J4, 2006, 36(04): 588 -591 .
[5] FU Zhe,ZHOU Yun-xuan, LIU Dian-wei, LIU Wan-song. Design of the FeatureBased ObjectOriented Data Model and Implementation of Prototype System for a Virtual GIS[J]. J4, 2006, 36(04): 647 -652 .
[6] TENG Ji-wen, LIU Cai, HAN Li-guo, RUAN Xiao-min, YAN Ya-fen, ZHANG Yong-qian. The Dynamical Mechanism for Medium Rapture and Motion of Deep Matler on Wenchuan-Yingxiu MS8.0 Earthquarce,2008[J]. J4, 2009, 39(4): 559 -583 .
[7] LU Jin-cai, LI Yu-hong, WEI Xian-yang, WEI Jian-she. Research on the Depositional Environment and Resources Potential of the Oil Shale in the Chang7 Member,Triassic Yanchang Formation in the Ordos Basin[J]. J4, 2006, 36(6): 928 -0932 .
[8] HUANG Ji-guo,HUANG Guo-xin,NIE Guang-zheng,WEI Hai-juan,LV Ai-min,WANG Xue-song. Experimental Study on the Treatment of Landfill Leachate in a TwoPhase(UBF-UASB) Anaerobic System at Mid-Temperature[J]. J4, 2007, 37(1): 144 -0147 .
[9] SUN Cai-zhi, LIU Yu-lan, YANG Jun. Research on the Ecological and Sustainable Groundwater Table Regulation in the Lower Liaohe River Plain[J]. J4, 2007, 37(2): 249 -254 .
[10] SHU Ping, QU Yan-ming, WANG Guo-jun, DING Ri-xin, AI Xing-bo,JI Xue-yan, TANG Hua-feng, BIAN Wei-hua, WANG Pu-jun. Geological features of the volcanic reservoirs of the Songliao Basin and their geophysical detection[J]. J4, 2007, 37(4): 726 -0733 .