4.7 Article

Single-particle crushing behaviour of carbonate sands studied by X-ray microtomography and a combined finite-discrete element method

Journal

ACTA GEOTECHNICA
Volume 17, Issue 8, Pages 3195-3209

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s11440-022-01469-w

Keywords

Carbonate soils; FDEM modelling; Intra-particle pore structure; Particle crushing; Particle morphology; X-ray mu CT

Funding

  1. National Natural Science Foundation of China [41877233, 42072298, 41931286]

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This paper investigates the particle breakage behaviour of carbonate sand using single-particle compression experiments and simulation methods. The results show that the strength of sand particles is influenced by the presence of intra-particle pores, with those filled having higher strength.
This paper investigates the particle breakage behaviour of a carbonate sand based on single-particle compression experiments with in situ X-ray microtomography scanning (mu CT) and a combined finite-discrete element method (FDEM). Specifically, X-ray mu CT is applied to extract the information on grain morphology and intra-particle pores of carbonate sand particles to establish an FDEM model. The model is first calibrated by comparing the simulation results of two carbonate sand grains with the corresponding single-particle compression experiment results and then applied to model the stress evolution, cracking propagation and failure of other carbonate sand particles under single-particle compression. To study the influence of intra-particle pores, FDEM modelling of carbonate sands with completely filled intra-particle pores is also performed. The particle strength of carbonate sands both with and without pore filling is found to follow a Weibull distribution, with that of the sand with pore filling being considerably higher. This behaviour is associated with lower stress concentration, resulting in later crack development in the pore-filled sand than in the sand without pore filling. The cracks are found to usually pass through the intra-particle pores. Consequently, a larger proportion of particles fail in the fragmentation mode in the sand without pore filling.

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