Study on the Flow Behavior of Gas and Water in Fractured Tight Gas Reservoirs Considering Matrix Imbibition Using the Digital Core Method

Processes Pub Date : 2024-03-30 DOI:10.3390/pr12040709
Feifei Chen, Yong-gang Duan, Kun Wang
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Abstract

Tight gas reservoirs possess unique pore structures and fluid flow mechanisms. Delving into the flow and imbibition mechanisms of water in fractured tight gas reservoirs is crucial for understanding and enhancing the development efficiency of such reservoirs. The flow of water in fractured tight gas reservoirs encompasses the flow within fractures and the imbibition flow within the matrix. However, conventional methods typically separate these two types of flow for study, failing to accurately reflect the true flow characteristics of water. In this study, micro-CT imaging techniques were utilized to evaluate the impact of matrix absorption and to examine water movement in fractured tight gas deposits. Water flooding experiments were conducted on tight sandstone cores with different fracture morphologies. Micro-CT scanning was performed on the cores after water injection and subsequent static conditions, simulating the process of water displacement gas in fractures and the displacement of gas in matrix pores by water through imbibition under reservoir conditions. Changes in gas–water distribution within fractures were observed, and the impact of fracture morphology on water displacement recovery was analyzed. Additionally, the recovery rates of fractures and matrix imbibition at different displacement stages were studied, along with the depth of water infiltration into the matrix along fracture walls. The insights gained from this investigation enhance our comprehension of the dynamics of fluid movement within tight gas deposits, laying a scientific foundation for crafting targeted development plans and boosting operational efficiency in such environments.
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使用数字岩心法研究考虑基质共生的裂缝致密气藏中气和水的流动行为
致密气藏具有独特的孔隙结构和流体流动机制。深入研究水在裂缝致密气藏中的流动和浸润机制,对于理解和提高这类气藏的开发效率至关重要。水在裂缝致密气藏中的流动包括裂缝内的流动和基质中的浸润流动。然而,传统方法通常将这两种流动分开研究,无法准确反映水的真实流动特征。在本研究中,利用微CT成像技术评估了基质吸水的影响,并研究了裂缝致密气矿床中水的流动情况。在具有不同断裂形态的致密砂岩岩心上进行了水浸实验。在注水和随后的静态条件下,对岩心进行了显微 CT 扫描,模拟了在储层条件下水在裂缝中置换气体以及水通过浸润作用在基质孔隙中置换气体的过程。观察了裂缝内气水分布的变化,分析了裂缝形态对水置换采收率的影响。此外,还研究了不同位移阶段裂缝和基质浸润的回收率,以及水沿裂缝壁渗入基质的深度。通过这项研究,我们加深了对致密气藏内部流体运动动力学的理解,为制定有针对性的开发计划和提高此类环境下的运营效率奠定了科学基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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