The mechanical behaviour of synthetic sandstone with varying brittle cement content

被引:63
作者
David, C [1 ]
Menendez, B [1 ]
Bernabe, Y [1 ]
机构
[1] Universite Louis Pasteur, CNRS UMR 7516, Ecole & Observ Sci Terre, F-67084 Strasbourg, France
来源
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES | 1998年 / 35卷 / 06期
关键词
D O I
10.1016/S0148-9062(98)00003-5
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The purpose of this work was to investigate the influence of cement on the mechanical behaviour of granular rocks. Following the technique described in den BI ok et al. [den Brok, S. W. J., David, C. and Bernabe, Y., Preparation of synthetic sandstones with variable cementation for studying the physical properties of granular rocks. C. R. Acad. Sci., 1997, 325, 487-492], two blocks of synthetic sandstones with different cement content were prepared for mechanical testing under hydrostatic and triaxial conditions. The results of the mechanical tests show that the behaviour of the synthetic locks compares well with that of natural sandstones. Increasing the amount of cement from 3 to 5% in volume had important consequences on the mechanical properties: the critical pressure, strength and elastic moduli were significantly increased and the brittle-to-ductile transition was shifted towards higher pressures. We compared our results to the models of Zhang et al. [Zhang, J., Wong, T. -F. and Davis, D. M., Micromechanics of pressure-induced grain crushing in porous' rocks. J. Geophys. Res., 1990, 95, 341-352] and Wong et al. [Wong, T. -F., David, C. and Zhu, W, The transition from brittle faulting to cataclastic flow in porous sandstones: Mechanical deformation. J. Geophys. Res., 1997, 102, 3009-3025]. We conclude that Zhang et al.%s microstructural parameter phi D (i.e. the product of porosity phi by grain size D) appeal ed to be a scaling parameter for both the failure envelopes and the critical pressure as defined in these models. Intuitively, the contact length L is expected to play a crucial role in the mechanical propel ties of granular materials. Accordingly, we made a statistical analysis of this microstructural parameter in our synthetic materials and in a suite of natural sandstones. A positive correlation with Young's modulus and a negative correlation with porosity were found. This last result gives a physical background for the use of parameter (phi D) in theoretical models. We want to emphasize that working on synthetic sandstones allows for a better control of the structural parameters (grain size, sorting, cement content, etc.) which appear to be so important for the mechanical properties of granular rocks. (C) 1998 Elsevier Science Ltd.
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页码:759 / 770
页数:12
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