Fluid distribution effect on sonic attenuation in partially saturated limestones

被引:117
作者
Cadoret, T
Mavko, G
Zinszner, B
机构
[1] Elf Explorat Prod, Dept Sism, CSTJF, F-64018 Pau, France
[2] Stanford Univ, Dept Geophys, Rock Phys Lab, Stanford, CA 94305 USA
[3] Inst Francais Petr, Lab Phys Roches, F-92506 Rueil Malmaison, France
关键词
D O I
10.1190/1.1444308
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Extensional and torsional wave-attenuation measurements are obtained at a sonic frequency around 1 kHz on partially saturated limestones using large resonant bars, 1 m long. To study the influence of the fluid distribution, we use two different saturation methods: drying and depressurization, When water saturation (S-w) is higher than 70%, the extensional wave attenuation is found to depend on whether the resonant bar is jacketed. This tan be interpreted as the Biot-Gardner-White effect. The experimental results obtained on jacketed samples show that, during a drying experiment, extensional wave attenuation is influenced strongly by the fluid content when S-w is between approximately 60% and 100%. This sensitivity to fluid saturation vanishes when saturation is obtained through depressurization. Using a computer-assisted tomographic (CT) scan, we found that, during depressurization, the fluid distribution is homogeneous at the millimetric scale at all saturations, In contrast. during drying, heterogeneous saturation was observed at high water-saturation levels, Thus, we interpret the dependence of the. extensional wave attenuation upon the saturation method as principally caused by a fluid distribution effect, Torsional attenuation shows no sensitivity to fluid saturation for S-w between 5% and 100%.
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页码:154 / 160
页数:7
相关论文
共 34 条
[1]  
[Anonymous], 1979, THESIS STANFORD U
[3]  
BIRCH F, 1938, B SEISMOL SOC AM, V38, P243
[5]  
BLAND D., 1960, The Theory of Linear Viscoelasticity
[6]  
Bourbie T., 1987, Acoustic of porous media
[7]   INFLUENCE OF FREQUENCY AND FLUID DISTRIBUTION ON ELASTIC-WAVE VELOCITIES IN PARTIALLY SATURATED LIMESTONES [J].
CADORET, T ;
MARION, D ;
ZINSZNER, B .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1995, 100 (B6) :9789-9803
[8]  
Cadoret T., 1993, Effet de la saturation eau-gaz sur les proprietes acoustiques des roches: Etude aux frequences sonores et ultrasonores
[9]   EFFECT OF BRINE-GAS MIXTURE ON VELOCITY IN AN UNCONSOLIDATED SAND RESERVOIR [J].
DOMENICO, SN .
GEOPHYSICS, 1976, 41 (05) :882-894
[10]  
Dullien F, 1979, POROUS MEDIA FLUID T, DOI DOI 10.1016/0300-9467(81)80049-4