Experimental study of the time-dependent behaviour of fracture propagation in salt rock

This paper presents an experimental study investigating the time-dependent behaviour of fracture propagation in salt rock. The research is aimed at enhancing the understanding of the fracture mechanics of salt rock, which is crucial for applications such as underground storage of hazardous waste and...

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Detalles Bibliográficos
Autores: Escanellas Tur, Andreu|||0009-0009-1359-1122, Camara Zapata, Eduardo, Liaudat, Joaquín, Carol, Ignacio|||0000-0002-1821-7203
Tipo de recurso: artículo
Fecha de publicación:2025
País:España
Institución:Universitat Politècnica de Catalunya (UPC)
Repositorio:UPCommons. Portal del coneixement obert de la UPC
Idioma:inglés
OAI Identifier:oai:upcommons.upc.edu:2117/439519
Acceso en línea:https://hdl.handle.net/2117/439519
https://dx.doi.org/10.1016/j.gete.2025.100687
Access Level:acceso abierto
Palabra clave:Salt rock
Fracture mechanics
Wedge splitting test
Creep
Creep-Fracture interaction
Àrees temàtiques de la UPC::Enginyeria civil::Geotècnia::Mecànica de roques
Descripción
Sumario:This paper presents an experimental study investigating the time-dependent behaviour of fracture propagation in salt rock. The research is aimed at enhancing the understanding of the fracture mechanics of salt rock, which is crucial for applications such as underground storage of hazardous waste and energy storage. Thirteen Wedge Splitting Tests (WST) were performed on salt rock specimens at four different loading rates, complemented by nine uniaxial creep tests on the same material at three stress levels. The WST results revealed major effects of the loading rate on the fracturing process, with decreasing rates leading to increased mechanical work required for splitting and reduced peak splitting force. The produced experimental dataset offers an excellent benchmark for the validation of numerical models including creep and fracture of salt rock. Additionally, the paper includes preliminary finite element simulations incorporating an inviscid discrete fracture representation and linear viscoelastic creep modelling in the bulk material that provide first insights into the origin of the observed loading rate effects. The numerical study concludes that these effects are mainly due to phenomena developed in the fracture process zone. The findings emphasise the need to consider time-dependency in Cohesive Zone Models used for salt rock fracture representation.