AE Response Characteristics of Intersections between Hydraulic Fractures and Embedded-Discontinuous Rock in Granitic HDRSource: Journal of Energy Engineering:;2025:;Volume ( 151 ):;issue: 003::page 04025014-1Author:Jingyu Xie
,
Ren Wang
,
Meng Zhao
,
Xuegang Li
,
Yifu Long
,
Jianlong Wang
,
Zhengyu Kan
,
Jiwei Song
DOI: 10.1061/JLEED9.EYENG-5655Publisher: American Society of Civil Engineers
Abstract: Acoustic emission (AE) is one of the most common means used to evaluate the geometries of hydraulic fractures (HFs). The preexisting discontinuities can significantly affect the propagation behaviors of HFs, which is the key to thermal reservoir construction. Hot dry rock (HDR) is high-temperature rock with no fluid and refers to high-temperature crystalline rock masses, such as granite, that exhibit low porosity and low permeability. Based on the geological survey and well-core analysis, not only natural fractures but also quartz veins and lithologic interfaces develop in granite, and the latter two are essentially different from conventional discontinuities. AE can effectively assess the development of HFs in HDRs; however, the AE response characteristics of intersections between HFs and embedded-discontinuous rock in granite have not been well understood. This study aims to address this. Physical simulation experiments of hydraulic fracturing and AE tests were conducted on granite with different preexisting discontinuities, especially the embedded-discontinuous rocks. Our results show that HF propagation in the granite matrix or through several discontinuities could cause stronger AE responses. For example, the AE events are in greater numbers and have higher energy. Intersections of HFs with natural fractures and lithologic interfaces induced stronger responses than did quartz veins. The AE response characteristics were tightly associated with the cementing strength, physical property differences, and interfacial roughness. Microobservation experiments show the defects at the interface between the embedded-discontinuous rocks provide conditions for the initiation and propagation of HFs. The AE response and injection pressure–time curve could reflect the properties of the fracturing process, and there was a positive correlation between the fluctuations of curves and AE energy. The analysis of the AE response can assist in obtaining the distribution information of preexisting discontinuities.
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contributor author | Jingyu Xie | |
contributor author | Ren Wang | |
contributor author | Meng Zhao | |
contributor author | Xuegang Li | |
contributor author | Yifu Long | |
contributor author | Jianlong Wang | |
contributor author | Zhengyu Kan | |
contributor author | Jiwei Song | |
date accessioned | 2025-08-17T22:51:46Z | |
date available | 2025-08-17T22:51:46Z | |
date copyright | 6/1/2025 12:00:00 AM | |
date issued | 2025 | |
identifier other | JLEED9.EYENG-5655.pdf | |
identifier uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4307564 | |
description abstract | Acoustic emission (AE) is one of the most common means used to evaluate the geometries of hydraulic fractures (HFs). The preexisting discontinuities can significantly affect the propagation behaviors of HFs, which is the key to thermal reservoir construction. Hot dry rock (HDR) is high-temperature rock with no fluid and refers to high-temperature crystalline rock masses, such as granite, that exhibit low porosity and low permeability. Based on the geological survey and well-core analysis, not only natural fractures but also quartz veins and lithologic interfaces develop in granite, and the latter two are essentially different from conventional discontinuities. AE can effectively assess the development of HFs in HDRs; however, the AE response characteristics of intersections between HFs and embedded-discontinuous rock in granite have not been well understood. This study aims to address this. Physical simulation experiments of hydraulic fracturing and AE tests were conducted on granite with different preexisting discontinuities, especially the embedded-discontinuous rocks. Our results show that HF propagation in the granite matrix or through several discontinuities could cause stronger AE responses. For example, the AE events are in greater numbers and have higher energy. Intersections of HFs with natural fractures and lithologic interfaces induced stronger responses than did quartz veins. The AE response characteristics were tightly associated with the cementing strength, physical property differences, and interfacial roughness. Microobservation experiments show the defects at the interface between the embedded-discontinuous rocks provide conditions for the initiation and propagation of HFs. The AE response and injection pressure–time curve could reflect the properties of the fracturing process, and there was a positive correlation between the fluctuations of curves and AE energy. The analysis of the AE response can assist in obtaining the distribution information of preexisting discontinuities. | |
publisher | American Society of Civil Engineers | |
title | AE Response Characteristics of Intersections between Hydraulic Fractures and Embedded-Discontinuous Rock in Granitic HDR | |
type | Journal Article | |
journal volume | 151 | |
journal issue | 3 | |
journal title | Journal of Energy Engineering | |
identifier doi | 10.1061/JLEED9.EYENG-5655 | |
journal fristpage | 04025014-1 | |
journal lastpage | 04025014-15 | |
page | 15 | |
tree | Journal of Energy Engineering:;2025:;Volume ( 151 ):;issue: 003 | |
contenttype | Fulltext |