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contributor authorJingyu Xie
contributor authorRen Wang
contributor authorMeng Zhao
contributor authorXuegang Li
contributor authorYifu Long
contributor authorJianlong Wang
contributor authorZhengyu Kan
contributor authorJiwei Song
date accessioned2025-08-17T22:51:46Z
date available2025-08-17T22:51:46Z
date copyright6/1/2025 12:00:00 AM
date issued2025
identifier otherJLEED9.EYENG-5655.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4307564
description abstractAcoustic 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.
publisherAmerican Society of Civil Engineers
titleAE Response Characteristics of Intersections between Hydraulic Fractures and Embedded-Discontinuous Rock in Granitic HDR
typeJournal Article
journal volume151
journal issue3
journal titleJournal of Energy Engineering
identifier doi10.1061/JLEED9.EYENG-5655
journal fristpage04025014-1
journal lastpage04025014-15
page15
treeJournal of Energy Engineering:;2025:;Volume ( 151 ):;issue: 003
contenttypeFulltext


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