{"title":"钻爆三维应力路径下深部硬岩瞬态卸荷断裂机理的数值研究","authors":"Weiqi Wang, Yawei Zhang, Rui Kong, Qihu Wang, Yulong Zhang","doi":"10.1007/s10064-025-04539-x","DOIUrl":null,"url":null,"abstract":"<div><p>Transient unloading and rapid stress adjustment of surrounding rock during deep drilling and blasting excavation can easily induce hard rock fracture. Aiming at the dynamic adjustment of the magnitude and direction of the three principal stresses in transient unloading, the proposed spherical discrete element model was used to reveal the influence mechanism of principal stress magnitude, stress rotation and strain rate on transient unloading fracture for the first time. The results show that the transient unloading fracture rate of hard rock is significantly correlated with the magnitude and change trend of principal stress and has obvious inertia. The fracture rate is positively correlated with the maximum differential stress (<i>σ</i><sub>1</sub>-<i>σ</i><sub>3</sub>) and strongly negatively correlated with the minimum principal stress (<i>σ</i><sub>3</sub>). Both transient unloading and stress rotation will induce tensile strain rates with certain inertia and directionality. The stress rotation causes the transient unloading fracture rate significantly related to the strain rate component along the <i>σ</i><sub>3</sub> axis (effective strain rate) rather than the principal strain rate. The maximum differential stress, minimum principal stress and effective strain rate constitute the stress-strain rate conditions for rapid fracture of rock under transient unloading. Increasing <i>σ</i><sub>3</sub> will suppress the rate effect of transient unloading fracture, and there is a threshold (8.4 MPa in this study). The mutual influence between the tensile deformation and fracture of rock under transient unloading is weak and is related to the initial maximum unloading direction and the minimum principal stress direction, respectively, which is obviously different from the static mechanical response.</p></div>","PeriodicalId":500,"journal":{"name":"Bulletin of Engineering Geology and the Environment","volume":"84 11","pages":""},"PeriodicalIF":4.2000,"publicationDate":"2025-10-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Numerical study on transient unloading fracture mechanism of deep hard rock under 3D stress path induced by drilling and blasting\",\"authors\":\"Weiqi Wang, Yawei Zhang, Rui Kong, Qihu Wang, Yulong Zhang\",\"doi\":\"10.1007/s10064-025-04539-x\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Transient unloading and rapid stress adjustment of surrounding rock during deep drilling and blasting excavation can easily induce hard rock fracture. Aiming at the dynamic adjustment of the magnitude and direction of the three principal stresses in transient unloading, the proposed spherical discrete element model was used to reveal the influence mechanism of principal stress magnitude, stress rotation and strain rate on transient unloading fracture for the first time. The results show that the transient unloading fracture rate of hard rock is significantly correlated with the magnitude and change trend of principal stress and has obvious inertia. The fracture rate is positively correlated with the maximum differential stress (<i>σ</i><sub>1</sub>-<i>σ</i><sub>3</sub>) and strongly negatively correlated with the minimum principal stress (<i>σ</i><sub>3</sub>). Both transient unloading and stress rotation will induce tensile strain rates with certain inertia and directionality. The stress rotation causes the transient unloading fracture rate significantly related to the strain rate component along the <i>σ</i><sub>3</sub> axis (effective strain rate) rather than the principal strain rate. The maximum differential stress, minimum principal stress and effective strain rate constitute the stress-strain rate conditions for rapid fracture of rock under transient unloading. Increasing <i>σ</i><sub>3</sub> will suppress the rate effect of transient unloading fracture, and there is a threshold (8.4 MPa in this study). The mutual influence between the tensile deformation and fracture of rock under transient unloading is weak and is related to the initial maximum unloading direction and the minimum principal stress direction, respectively, which is obviously different from the static mechanical response.</p></div>\",\"PeriodicalId\":500,\"journal\":{\"name\":\"Bulletin of Engineering Geology and the Environment\",\"volume\":\"84 11\",\"pages\":\"\"},\"PeriodicalIF\":4.2000,\"publicationDate\":\"2025-10-18\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Bulletin of Engineering Geology and the Environment\",\"FirstCategoryId\":\"5\",\"ListUrlMain\":\"https://link.springer.com/article/10.1007/s10064-025-04539-x\",\"RegionNum\":2,\"RegionCategory\":\"工程技术\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"ENGINEERING, ENVIRONMENTAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Bulletin of Engineering Geology and the Environment","FirstCategoryId":"5","ListUrlMain":"https://link.springer.com/article/10.1007/s10064-025-04539-x","RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENGINEERING, ENVIRONMENTAL","Score":null,"Total":0}
Numerical study on transient unloading fracture mechanism of deep hard rock under 3D stress path induced by drilling and blasting
Transient unloading and rapid stress adjustment of surrounding rock during deep drilling and blasting excavation can easily induce hard rock fracture. Aiming at the dynamic adjustment of the magnitude and direction of the three principal stresses in transient unloading, the proposed spherical discrete element model was used to reveal the influence mechanism of principal stress magnitude, stress rotation and strain rate on transient unloading fracture for the first time. The results show that the transient unloading fracture rate of hard rock is significantly correlated with the magnitude and change trend of principal stress and has obvious inertia. The fracture rate is positively correlated with the maximum differential stress (σ1-σ3) and strongly negatively correlated with the minimum principal stress (σ3). Both transient unloading and stress rotation will induce tensile strain rates with certain inertia and directionality. The stress rotation causes the transient unloading fracture rate significantly related to the strain rate component along the σ3 axis (effective strain rate) rather than the principal strain rate. The maximum differential stress, minimum principal stress and effective strain rate constitute the stress-strain rate conditions for rapid fracture of rock under transient unloading. Increasing σ3 will suppress the rate effect of transient unloading fracture, and there is a threshold (8.4 MPa in this study). The mutual influence between the tensile deformation and fracture of rock under transient unloading is weak and is related to the initial maximum unloading direction and the minimum principal stress direction, respectively, which is obviously different from the static mechanical response.
期刊介绍:
Engineering geology is defined in the statutes of the IAEG as the science devoted to the investigation, study and solution of engineering and environmental problems which may arise as the result of the interaction between geology and the works or activities of man, as well as of the prediction of and development of measures for the prevention or remediation of geological hazards. Engineering geology embraces:
• the applications/implications of the geomorphology, structural geology, and hydrogeological conditions of geological formations;
• the characterisation of the mineralogical, physico-geomechanical, chemical and hydraulic properties of all earth materials involved in construction, resource recovery and environmental change;
• the assessment of the mechanical and hydrological behaviour of soil and rock masses;
• the prediction of changes to the above properties with time;
• the determination of the parameters to be considered in the stability analysis of engineering works and earth masses.