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鄂尔多斯盆地东南部致密砂岩孔隙结构对可动流体及气水渗流的影响

Effect of pore-throat structure on movable fluid and gas-water seepage in tight sandstone from the southeastern Ordos Basin, China.

作者信息

Chang Bin, Tong Qiang, Cao Cheng, Zhang Yunde

机构信息

State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an, 710069, Shaanxi, China.

Shaanxi Polytech Inst, Civil Engineering, Xianyang, 712000, Shaanxi, China.

出版信息

Sci Rep. 2025 Mar 5;15(1):7714. doi: 10.1038/s41598-025-92584-7.

Abstract

This study investigates the micro-pore-throat structure of Upper Paleozoic tight sandstone gas reservoirs in the southeastern Ordos Basin, China, with a focus on the Yan'an gas field. The aim is to analyze the micro-pore-throat characteristics and their influence on fluid seepage to optimize gas-water two-phase flow, reservoir evaluation, and development strategies. The research integrates core analysis, thin section petrography, FE-SEM, MICP, NMR, and gas-water relative permeability tests. By combining NMR and HPMI, it offers a comprehensive characterization of pore-throat structures across various size ranges, and applies fractal dimensions to assess heterogeneity at multiple scales. Results indicate that the reservoir's pore space is primarily composed of dissolved pores and micropores with limited connectivity and low permeability, influenced by clay content and pore-throat morphology. The pore-throat structure exhibits fractal characteristics with distinct large and small pore-throats. Larger pore-throats (> 0.1 μm) are more heterogeneous, while smaller pore-throats exhibit less variation. Permeability is largely controlled by larger pore-throats, which enhance reservoir properties. Well-developed pore-throat structures promote the occurrence of movable fluids and improve the seepage capacity of both gas and water. Larger pore-throats (> 1 μm) significantly increase relative permeability and gas displacement efficiency. A new reservoir quality parameter (H) is introduced, classifying reservoirs into four types, with Type I being most favorable for development. This parameter can be directly applied to improve reservoir management and to maximize gas recovery and optimize fluid flow. This study enhances understanding of fluid flow in tight sandstone gas reservoirs and provides a novel framework for efficient reservoir evaluation, management, and optimization in reservoir development.

摘要

本研究调查了中国鄂尔多斯盆地东南部上古生界致密砂岩气藏的微观孔喉结构,重点研究了延安气田。目的是分析微观孔喉特征及其对流体渗流的影响,以优化气水两相流、储层评价和开发策略。该研究综合了岩心分析、薄片岩石学、场发射扫描电子显微镜、压汞法、核磁共振以及气水相对渗透率测试。通过结合核磁共振和高精度压力微渗透率仪,全面表征了不同尺寸范围的孔喉结构,并应用分形维数评估多尺度非均质性。结果表明,储层孔隙空间主要由溶蚀孔和微孔组成,连通性有限且渗透率低,受黏土含量和孔喉形态影响。孔喉结构呈现分形特征,大小孔喉明显不同。较大孔喉(>0.1μm)的非均质性更强,而较小孔喉的变化较小。渗透率在很大程度上受较大孔喉控制,较大孔喉增强了储层性能。发育良好的孔喉结构促进了可动流体的出现,提高了气水的渗流能力。较大孔喉(>1μm)显著提高了相对渗透率和气驱效率。引入了一个新的储层质量参数(H),将储层分为四类,其中I类最有利于开发。该参数可直接用于改善储层管理,最大限度地提高天然气采收率并优化流体流动。本研究加深了对致密砂岩气藏流体流动的理解,并为储层开发中的高效储层评价、管理和优化提供了一个新的框架。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7c75/11882982/e4721d4d627e/41598_2025_92584_Fig1_HTML.jpg

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