Volume Contraction and Reduction in Hydraulic Conductivity during Particle Crushing

被引:1
作者
Rodriguez-Hernandez, Carlos D. [1 ]
Park, Junghee [2 ]
Echezuria, Heriberto [3 ]
Santamarina, J. Carlos [4 ]
机构
[1] King Abdullah Univ Sci & Technol, Energy Resources & Petr Engn, Bldg 5, Thuwal 239556900, Saudi Arabia
[2] Incheon Natl Univ, Dept Civil & Environm Engn, 119 Acad ro, Incheon 22012, South Korea
[3] Univ Catolica Andres Bello, Sch Civil Engn, Caracas 1020, Venezuela
[4] Georgia Inst Technol, Sch Civil & Environm Engn, Atlanta, GA 30332 USA
关键词
Grain size distribution; Specific surface; Particle crushing; Hydraulic conductivity; Yield stress; ONE-DIMENSIONAL COMPRESSION; BREAKAGE MECHANICS; SAND; PROPPANTS; BEHAVIOR; PERFORMANCE; SHEARING; INSIGHTS; STRESS; SOILS;
D O I
10.1061/JGGEFK.GTENG-12234
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Particle crushing takes place in a wide range of engineering applications and affects fluid flow through granular materials. This study examines volumetric changes and the evolution of hydraulic conductivity during particle crushing using a combination of high-stress experiments, data compilation from published studies and particle-scale numerical simulations. An asymptotically correct hyperbolic model fits void ratio versus stress data and provides reliable estimates of the yield stress. Alternatively, hydraulic conductivity follows a power law with void ratio and the trend extends into the grain crushing regime. Hydraulic conductivity diminishes rapidly as sand grains start crushing; the reduction in hydraulic conductivity can reach 1-to-4 orders of magnitude depending on mineral composition, particle shape and initial packing density. Crushing involves the progressive detachment of small fragments; these small particles move into the larger pores, increase the drag resistance, clog pore constrictions, and effectively hinder fluid flow after the yield stress.
引用
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页数:9
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