Pore structure evolution of anthracite modified by CO2 foam fracturing fluid under different temperature and pressure conditions

IF 6.7 1区 工程技术 Q2 ENERGY & FUELS
Fuel Pub Date : 2025-06-07 DOI:10.1016/j.fuel.2025.135929
Yangfeng Zheng , Cheng Zhai , Shuxun Sang , Aikun Chen , Jizhao Xu , Yong Sun , Hexiang Xu , Hongyang Xu , Yongshuai Lai
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引用次数: 0

Abstract

CO2 foam fracturing technology has significant potential for enhancing coalbed methane (CBM) recovery. Intrusion of the CO2 foam fracturing fluid into coal seams alters coal pore and fracture structures, thereby influencing CBM recovery. However, coal pore structural evolution modified by CO2 foam fracturing fluid under varying reservoir temperatures and injection pressures remains unclear. To address this, a self-constructed high-temperature and high-pressure reactor was used to modify anthracite under different temperature (30–60℃) and pressure (3–6 MPa) conditions for 15 h. The pore structure and mineral composition of the modified anthracite were subsequently analyzed using low-temperature nitrogen adsorption, low-field nuclear magnetic resonance, environmental scanning electron microscopy, and X-ray diffraction. The results showed that temperature and CO2 pressure significantly affected the modified coal-pore structure. Specifically, as the temperature decreased or the CO2 pressure increased, the average pore diameter, total and effective porosities, NMR permeability, proportion of free fluid, and adsorption pore fractal dimension D2 showed increasing trends, whereas the Brunauer–Emmett–Teller (BET)-specific surface area, and fractal dimensions D1, and DS decreased. Moreover, the combined effects of carbonic acid and sodium dodecyl sulfate in the CO2 foam promoted the dissolution of clay and carbonate minerals, resulting in an increase in the number of surface fractures, pore enlargement, and the transformation of isolated pores into interconnected fractures. Pore structure evolution is primarily driven by mineral, and organic matter dissolution and fracturing, and CO2 adsorption-induced matrix swelling. After performing CO2 foam fracturing in deep high-temperature coal seams, implementing higher shut-in pressures can further enhance CBM recovery. These findings provide a fundamental theoretical basis for engineering applications of CO2 foam fracturing technology to enhance CBM recovery.
不同温度和压力条件下CO2泡沫压裂液改性无烟煤孔隙结构演化
CO2泡沫压裂技术具有提高煤层气采收率的巨大潜力。CO2泡沫压裂液侵入煤层,改变煤层孔隙和裂缝结构,影响煤层气采收率。然而,在不同储层温度和注入压力下,CO2泡沫压裂液对煤孔隙结构演化的影响尚不清楚。为此,利用自建的高温高压反应器,在不同温度(30-60℃)和压力(3-6 MPa)条件下对无烟煤进行了15 h的改性。随后,利用低温氮吸附、低场核磁共振、环境扫描电镜和x射线衍射分析了改性后无烟煤的孔隙结构和矿物组成。结果表明,温度和CO2压力对煤的孔隙结构有显著影响。其中,随着温度的降低或CO2压力的升高,平均孔径、总孔隙度和有效孔隙度、核磁共振渗透率、自由流体比例、吸附孔分形维数D2呈增大趋势,而比表面积、分形维数D1、分形维数DS呈减小趋势。此外,CO2泡沫中碳酸和十二烷基硫酸钠的共同作用促进了粘土和碳酸盐矿物的溶解,导致表面裂缝数量增加,孔隙扩大,孤立孔隙转变为相互连接的裂缝。孔隙结构演化主要受矿物、有机质溶解和破裂以及CO2吸附引起的基质膨胀驱动。在深部高温煤层进行CO2泡沫压裂后,提高关井压力可以进一步提高煤层气采收率。研究结果为CO2泡沫压裂技术提高煤层气采收率的工程应用提供了基础理论依据。
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来源期刊
Fuel
Fuel 工程技术-工程:化工
CiteScore
12.80
自引率
20.30%
发文量
3506
审稿时长
64 days
期刊介绍: The exploration of energy sources remains a critical matter of study. For the past nine decades, fuel has consistently held the forefront in primary research efforts within the field of energy science. This area of investigation encompasses a wide range of subjects, with a particular emphasis on emerging concerns like environmental factors and pollution.
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