Dynamic tests using a Split Hopkinson Pressure Bar show increased tensile strength in gypsum, indicating strong rate dependency in soft rocks.
Understanding the deformation behaviour of rocks under dynamic loads is crucial in rock mechanics. This study investigates the rate-dependent tensile strength and fracture response of gypsum, a model material for soft rocks, across two different sample porosities. Quasi-static Brazilian disc tests were conducted using a servo-controlled universal testing machine, revealing that tensile strength decreases with increasing porosity. However, in the quasi-static regime, strength remains relatively constant across different strain rates. Dynamic tests were performed using a Split Hopkinson Pressure Bar (SHPB) setup, showing that dynamic tensile strength is consistently higher than quasi-static strength, regardless of porosity. Furthermore, as the dynamic strain rate increases, strength values further rise, indicating a strong rate dependency. Also, due to gypsum’s brittle nature and low tensile strength, fracture resulted in significant powder formation. To capture real-time fracture evolution, high-speed imaging was employed. Full-field strain distribution and fracture evolution has been studied using Digital Image Correlation (DIC). The findings demonstrate a strong correlation between porosity, tensile strength, and fracture behaviour, offering valuable insights into the dynamic response of soft rocks.
No takes yet. Share an insight, caveat, or question.
Imtiyaz et al. (2025) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: