{"title":"Contributions of rock structure and terrain to rockslide/rockfall-induced air blast: insights from 3D CFD-DEM analyses","authors":"Zhiyuan Zhu, Yihan Wu, Yuzhang Bi, Lu Zheng","doi":"10.1007/s10064-025-04301-3","DOIUrl":null,"url":null,"abstract":"<div><p>Evidence of rockslide-induced air blasts has been documented in numerous investigation records, showing similar terrain features. Terrains and rock structures combine to influence rock runout, yet their effects on the generation and propagation of air blasts remain poorly understood. We proposed a generalized model to account for the influence of rock structure and terrain. The generation and propagation of air blasts under different conditions are quantitatively analyzed using the discrete element method (DEM) and computational fluid dynamics (CFD). The results show that (1) The precondition for inducing air blasts is that rockslides maintain high runout speed with large front-cross sections, impacting mountains and causing significant fragmentations. (2) Representing the source rock mass as unbonded particles underestimates the influence range of air blasts; Structural planes parallel to the sliding surface enhance rockslide spreading and facilitate the further propagation of air blasts. (3) Steep slopes and scarps significantly increase the energy released during rock impact, leading to a peak air blast pressure increase of 603.3% and 79.8%, respectively, compared to gentle slopes. Winding and narrow valley terrain restricts the escape of air, making it easier for high-speed air blasts to form.</p></div>","PeriodicalId":500,"journal":{"name":"Bulletin of Engineering Geology and the Environment","volume":"84 6","pages":""},"PeriodicalIF":4.2000,"publicationDate":"2025-05-17","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/s10064-025-04301-3","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}
引用次数: 0
Abstract
Evidence of rockslide-induced air blasts has been documented in numerous investigation records, showing similar terrain features. Terrains and rock structures combine to influence rock runout, yet their effects on the generation and propagation of air blasts remain poorly understood. We proposed a generalized model to account for the influence of rock structure and terrain. The generation and propagation of air blasts under different conditions are quantitatively analyzed using the discrete element method (DEM) and computational fluid dynamics (CFD). The results show that (1) The precondition for inducing air blasts is that rockslides maintain high runout speed with large front-cross sections, impacting mountains and causing significant fragmentations. (2) Representing the source rock mass as unbonded particles underestimates the influence range of air blasts; Structural planes parallel to the sliding surface enhance rockslide spreading and facilitate the further propagation of air blasts. (3) Steep slopes and scarps significantly increase the energy released during rock impact, leading to a peak air blast pressure increase of 603.3% and 79.8%, respectively, compared to gentle slopes. Winding and narrow valley terrain restricts the escape of air, making it easier for high-speed air blasts to form.
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.