ZHANG Ke, GUAN Shi-hao, QI Fei-fei, et al. Macromechanical properties and microstructure of sandstone
under scouring effect[J]. 2024, 45(7): 1929-1938.
DOI:
ZHANG Ke, GUAN Shi-hao, QI Fei-fei, et al. Macromechanical properties and microstructure of sandstone
under scouring effect[J]. 2024, 45(7): 1929-1938.DOI: 10.16285/j.rsm.2023.1271.
Macromechanical properties and microstructure of sandstone
under scouring effect
The deterioration of rocks on reservoir bank slopes under flowing water conditions can seriously compromise slope stability. Meticulously exploring the macro-mechanical properties and microstructures of rocks under dynamic water scouring conditions is of great significance for disaster prevention and control in reservoir areas. To simulate the water flow environment of reservoir bank slopes
a rock scour resistance test device was designed. Taking sandstone as the research object
three conditions namely
natural drying
hydrostatic immersion
and hydrodynamic scouring
were considered. Combining with laboratory test results
digital image correlation techniques
scanning electron microscopy
and fractal theory
the influences of different water environments on the mechanical properties of rocks were systematically explored in terms of macro-mechanical parameters
distribution characteristics of strain fields
and microstructure. The results indicate that the softening coefficients of compressive strength and elastic modulus of hydrodynamically scoured specimens decrease by 0.07 and 0.06 units
respectively
compared to those of water-saturated specimens. The inflection point of the strain field differentiation rate-axial strain curve appears before the peak stress
associated with the localization of the fracture process zone
serving as a precursor signal for rock fracture. Compared to the effect of hydrostatic immersion
the precursor point of hydrodynamically scoured specimens appears earlier
as hydrodynamic scouring aggravates the development of internal defects
thereby facilitating the earlier appearance of the precursor point. Furthermore
the loss of mineral particles and cementing materials within the sandstone increases significantly after hydrodynamically scouring
leading to a more pronounced degradation of its microstructure than that of water-saturated specimens. This change is confirmed by the fractal dimension calculations of scanning electron microscope images
indicating that the hydrodynamically scoured specimens exhibit the largest fractal dimension.