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隧道及地下工程岩体突水损害与声发射特征。

Tunnel and underground engineering rock mass water inrush damage and acoustic emission characteristics.

机构信息

College of Civil and Construction Engineering, Hunan Institute of Technology, Hengyang, China.

School of Resource Environment and Safety Engineering, University of South China, Hengyang, China.

出版信息

PLoS One. 2024 Sep 20;19(9):e0307700. doi: 10.1371/journal.pone.0307700. eCollection 2024.

Abstract

To achieve the actual situation of water pressure stabilization during underground and tunnel water inrush disasters, the team independently developed a stable water pressure test system and conducted fracture and failure tests on fissured rock masses under the coupling effect of 1MPa stable water pressure and stress and without water pressure. Combined with data collected by acoustic emission instruments, the mechanical characteristics of fracture and failure, crack propagation mechanism, and acoustic emission response mechanism of fissured rock masses under the coupling effect of stable hydraulic pressure and stress were studied. The results showed that throughout the entire experimental process, the hydraulic pressure remained continuously stable, with a decrease of only 0.14%; The variation pattern of peak strength of fissured rock mass with increasing crack inclination angle under stable hydraulic pressure changes from a decrease and then an increase in the absence of hydraulic pressure to an increasing trend; The crack propagation length of low angle fissured rock mass is generally higher than that of high angle fissured specimens. The longer propagation path increases the range and effect of hydraulic pressure, and the initial crack propagation length of fissured rock mass under hydraulic pressure is also significantly longer than that of specimens without hydraulic pressure; During the loading process, both the acoustic emission ringing count and damage variable can be divided into four stages. From the cumulative total number of acoustic emission ringing counts, it can be seen that during the loading process, the total number of acoustic emission ringing in fissured rock masses subjected to hydraulic pressure is significantly lower than that of specimens without hydraulic pressure, and the trend is also relatively stable.

摘要

为了实现地下和隧道突水灾害过程中水压稳定的实际情况,团队自主研发了稳定水压测试系统,并对在 1MPa 稳定水压和应力耦合作用下以及无水压作用下的裂隙岩体进行了断裂破坏试验。结合声发射仪器采集的数据,研究了裂隙岩体在稳定水压和应力耦合作用下的断裂破坏力学特性、裂纹扩展机制和声发射响应机制。结果表明,在整个实验过程中,水压保持持续稳定,仅下降 0.14%;在有稳定水压作用下,裂隙岩体峰值强度随裂隙倾角增大的变化模式由先减小后增大变为单调递增,而在无水压作用下则单调减小;低角度裂隙岩体的裂纹扩展长度一般高于高角度裂隙试件。较长的扩展路径增加了水压的范围和效果,并且有压条件下裂隙岩体的初始裂纹扩展长度也明显长于无压条件下的试件;在加载过程中,声发射振铃计数和损伤变量都可以分为四个阶段。从声发射振铃计数的累积总数可以看出,在加载过程中,受水压作用的裂隙岩体的声发射振铃总数明显低于无水压作用的试件,且趋势也相对稳定。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2bc4/11414891/85053c26fda4/pone.0307700.g001.jpg

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