DEFORMABLE POROUS-MEDIA WITH DOUBLE POROSITY - QUASI-STATICS .2. MEMORY EFFECTS

被引:72
作者
AURIAULT, JL [1 ]
BOUTIN, C [1 ]
机构
[1] ECOLE NATL TRAVAUX PUBL ETAT,GEOMAT LAB,F-69518 VAULX EN VELIN,FRANCE
关键词
DEFORMABLE POROUS MEDIA; DOUBLE POROSITY; CONSOLIDATION; MEMORY EFFECT;
D O I
10.1007/BF00617006
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
As in our previous paper, we investigate the macroscopic quasi-static description of a porous medium with a double porosity constituted by pores and fractures. For this purpose, we use a homogenization technique. As expected, the macroscopic description is sensitive to the ratios between the different scales, l/l' and l'/l'' where l, l', l'' are characteristic lengths of the pores, the fractures, and the macroscopic medium, respectively. In the first paper, we investigated the case l'/l'' = O(l2/l'2) much less than 1 (case 1) which exhibits a coupling between the flows through the pores and the fractures. In the present paper, we deal with the other homogenizable cases. The case 3 where l/l'= O(l'2/l''2) much less than 1 gives a macroscopic description similar to that of a single porosity medium. The main result, however, is the case 2, where l/l' = O(l'/l'') much less than 1, which exhibits memory effects. These are due to the seepage through the micropores.
引用
收藏
页码:153 / 169
页数:17
相关论文
共 7 条
[1]  
Auriault Jean-Louis, 1990, GEOMATERIALS CONSTIT, P311
[2]   HETEROGENEOUS MEDIUM - IS AN EQUIVALENT MACROSCOPIC DESCRIPTION POSSIBLE [J].
AURIAULT, JL .
INTERNATIONAL JOURNAL OF ENGINEERING SCIENCE, 1991, 29 (07) :785-795
[3]   DEFORMABLE POROUS-MEDIA WITH DOUBLE POROSITY - QUASI-STATICS .1. COUPLING EFFECTS [J].
AURIAULT, JL ;
BOUTIN, C .
TRANSPORT IN POROUS MEDIA, 1992, 7 (01) :63-82
[4]   ATTENUATION OF SEISMIC-WAVES IN DRY AND SATURATED ROCKS .2. MECHANISMS [J].
JOHNSTON, DH ;
TOKSOZ, MN ;
TIMUR, A .
GEOPHYSICS, 1979, 44 (04) :691-711
[5]   VISCOELASTIC PROPERTIES OF FLUID-SATURATED CRACKED SOLIDS [J].
OCONNELL, RJ ;
BUDIANSKY, B .
JOURNAL OF GEOPHYSICAL RESEARCH, 1977, 82 (36) :5719-5735
[6]   ATTENUATION OF SEISMIC-WAVES IN DRY AND SATURATED ROCKS .1. LABORATORY MEASUREMENTS [J].
TOKSOZ, MN ;
JOHNSTON, DH ;
TIMUR, A .
GEOPHYSICS, 1979, 44 (04) :681-690
[7]  
van Golf-Racht T.D., 1982, FUNDAMENTALS FRACTUR