Yangfeng Zheng , Cheng Zhai , Shuxun Sang , Aikun Chen , Jizhao Xu , Yong Sun , Hexiang Xu , Hongyang Xu , Yongshuai Lai
{"title":"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","authors":"Yangfeng Zheng , Cheng Zhai , Shuxun Sang , Aikun Chen , Jizhao Xu , Yong Sun , Hexiang Xu , Hongyang Xu , Yongshuai Lai","doi":"10.1016/j.fuel.2025.135929","DOIUrl":null,"url":null,"abstract":"<div><div>CO<sub>2</sub> foam fracturing technology has significant potential for enhancing coalbed methane (CBM) recovery. Intrusion of the CO<sub>2</sub> foam fracturing fluid into coal seams alters coal pore and fracture structures, thereby influencing CBM recovery. However, coal pore structural evolution modified by CO<sub>2</sub> 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 CO<sub>2</sub> pressure significantly affected the modified coal-pore structure. Specifically, as the temperature decreased or the CO<sub>2</sub> pressure increased, the average pore diameter, total and effective porosities, NMR permeability, proportion of free fluid, and adsorption pore fractal dimension <em>D</em><sub>2</sub> showed increasing trends, whereas the Brunauer–Emmett–Teller (BET)-specific surface area, and fractal dimensions <em>D</em><sub>1</sub>, and <em>D</em><sub>S</sub> decreased. Moreover, the combined effects of carbonic acid and sodium dodecyl sulfate in the CO<sub>2</sub> 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 CO<sub>2</sub> adsorption-induced matrix swelling. After performing CO<sub>2</sub> 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 CO<sub>2</sub> foam fracturing technology to enhance CBM recovery.</div></div>","PeriodicalId":325,"journal":{"name":"Fuel","volume":"401 ","pages":"Article 135929"},"PeriodicalIF":6.7000,"publicationDate":"2025-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Pore structure evolution of anthracite modified by CO2 foam fracturing fluid under different temperature and pressure conditions\",\"authors\":\"Yangfeng Zheng , Cheng Zhai , Shuxun Sang , Aikun Chen , Jizhao Xu , Yong Sun , Hexiang Xu , Hongyang Xu , Yongshuai Lai\",\"doi\":\"10.1016/j.fuel.2025.135929\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>CO<sub>2</sub> foam fracturing technology has significant potential for enhancing coalbed methane (CBM) recovery. Intrusion of the CO<sub>2</sub> foam fracturing fluid into coal seams alters coal pore and fracture structures, thereby influencing CBM recovery. However, coal pore structural evolution modified by CO<sub>2</sub> 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 CO<sub>2</sub> pressure significantly affected the modified coal-pore structure. Specifically, as the temperature decreased or the CO<sub>2</sub> pressure increased, the average pore diameter, total and effective porosities, NMR permeability, proportion of free fluid, and adsorption pore fractal dimension <em>D</em><sub>2</sub> showed increasing trends, whereas the Brunauer–Emmett–Teller (BET)-specific surface area, and fractal dimensions <em>D</em><sub>1</sub>, and <em>D</em><sub>S</sub> decreased. Moreover, the combined effects of carbonic acid and sodium dodecyl sulfate in the CO<sub>2</sub> 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 CO<sub>2</sub> adsorption-induced matrix swelling. After performing CO<sub>2</sub> 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 CO<sub>2</sub> foam fracturing technology to enhance CBM recovery.</div></div>\",\"PeriodicalId\":325,\"journal\":{\"name\":\"Fuel\",\"volume\":\"401 \",\"pages\":\"Article 135929\"},\"PeriodicalIF\":6.7000,\"publicationDate\":\"2025-06-07\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Fuel\",\"FirstCategoryId\":\"5\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0016236125016540\",\"RegionNum\":1,\"RegionCategory\":\"工程技术\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"ENERGY & FUELS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Fuel","FirstCategoryId":"5","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0016236125016540","RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENERGY & FUELS","Score":null,"Total":0}
Pore structure evolution of anthracite modified by CO2 foam fracturing fluid under different temperature and pressure conditions
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.
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.