Fracture and fragmentation of dolomite rock using the JH-2 constitutive model: Parameter determination, experiments and simulations

•A procedure for determination of JH-2 model parameters for dolomite is presented in detail.•Fracture and damage parameters were obtained based on the proposed drop-weight laboratory stand and FEA.•The JH-2 model was used for simulating the shock induced fracture and damage of the dolomite.•Small di...

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Published inInternational journal of impact engineering Vol. 140; p. 103543
Main Authors Baranowski, Paweł, Kucewicz, Michał, Gieleta, Roman, Stankiewicz, Michał, Konarzewski, Marcin, Bogusz, Paweł, Pytlik, Mateusz, Małachowski, Jerzy
Format Journal Article
LanguageEnglish
Published Oxford Elsevier Ltd 01.06.2020
Elsevier BV
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Summary:•A procedure for determination of JH-2 model parameters for dolomite is presented in detail.•Fracture and damage parameters were obtained based on the proposed drop-weight laboratory stand and FEA.•The JH-2 model was used for simulating the shock induced fracture and damage of the dolomite.•Small discrepancies between experimental and numerical results were obtained. The paper presents a procedure for determining Johnson-Holmquist II (JH-2) model parameters for dolomite rock. The constants were determined based on experiments supplemented with literature data. The parameters responsible for damage and fracture were iteratively obtained based on a proposed drop-weight impact laboratory stand method and numerical simulations. The results demonstrated that some material parameters are dependent on the element dimensions and should be adjusted depending on the problem scale and geometry. In the next step, a numerical blast loading simulation was conducted to analyze the influence of mesh properties. Finally, the JH-2 model for the dolomite rock was verified, and the corresponding parameters were implemented to simulate rock fragmentation. Comparisons with actual tests proved that the model is efficient and accurate for simulating blasting followed by fracture and fragmentation of dolomite rock.
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ISSN:0734-743X
1879-3509
DOI:10.1016/j.ijimpeng.2020.103543