Rock and Soil Mechanics ›› 2024, Vol. 45 ›› Issue (7): 1967-1975.doi: 10.16285/j.rsm.2023.1297

• Fundamental Theory and Experimental Research • Previous Articles     Next Articles

Breaking rate of coral sand and gravel based on volume change

WANG Bu-xue-yan1, 2, MENG Qing-shan2, 3, QIAN Jian-gu1   

  1. 1. Department of Geotechnical Engineering, Tongji University, Shanghai, China; 2. State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, Hubei 430071, China; 3.College of Civil Engineering and Architecture, Guilin University of Technology, Guilin, Guangxi 541004, China
  • Received:2023-08-30 Accepted:2024-01-02 Online:2024-07-10 Published:2024-07-19
  • Supported by:
    This work was supported by the Special Fund for Basic Scientific Research Business Expenses of Central Universities (2023-2-ZD-08) and the National Natural Science Foundation of China (41877267).

Abstract: The breakage behavior of granular materials is prevalent across various fields and significantly impacts the mechanical properties of granular materials. A substantial amount of research on particle breakage behavior relies on reasonable calculation methods for breakage rate. This article proposes a calculation method for particle breakage rate based on particle volume as the fundamental parameter, addressing the current limitation of existing methods in accurately evaluating the breakage rate of irregular particles, exemplified by coral gravel. It improves upon the existing Hardin breakage rate calculation formula, which is based on particle size, to better assess the breakage rate of irregular particles. Breakage tests of coral gravel with different shapes were designed and conducted to conduct reliability validation of the aforementioned theoretical formulas, and the causes of errors generated by traditional methods were analyzed. Through experiments, the breakage rate values of particles with different shapes under different pressures and algorithms were obtained. Meanwhile, combining stress, deformation, and image observations from the experimental process, the fragmentation thresholds of coral gravel in three shapes—sheet, block, and rod—were determined, revealing the evolution characteristics of fragmentation modes exhibited by particles with different morphologies during the pressure change process.

Key words: particle breakage, breakage rate, coral sand

CLC Number: 

  • TU 411
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