Viscoelasticity expression and extension of seismic dispersion and attenuation in porous media with multiple fracture sets

2020 ◽  
Vol 68 (6) ◽  
pp. 1679-1688
Author(s):  
Jinwei Zhang ◽  
Renwei Ding ◽  
Lihong Zhao ◽  
Deying Wang
2018 ◽  
Vol 214 (1) ◽  
pp. 583-595 ◽  
Author(s):  
Jinwei Zhang ◽  
Handong Huang ◽  
Chunhua Wu ◽  
Sheng Zhang ◽  
Gang Wu ◽  
...  

2021 ◽  
Vol 9 ◽  
Author(s):  
Fansheng Xiong ◽  
Jiawei Liu ◽  
Zhenwei Guo ◽  
Jianxin Liu

Simulating and predicting wave propagation in porous media saturated with two fluids is an important issue in geophysical exploration studies. In this work, wave propagation in porous media with specified structures saturated with two immiscible fluids was studied, and the main objective was to establish a wave equation system with a relatively simple structure. The wave equations derived by Tuncay and Corapcioglu were analyzed first. It was found that the coefficient matrix of the equations tends to be singular due to the inclusion of a small parameter that characterizes the effect of capillary stiffening. Therefore, the previously established model consisting of three governing equations may be unstable under natural conditions. An improved model based on Tuncay and Corapcioglu’s work was proposed to ensure the nonsingularity of the coefficient matrix. By introducing an assumption in which one fluid was completely wrapped by the other, the governing equation of the wrapped fluid was degenerated. In this way, the coefficient matrix of wave equations became nonsingular. The dispersion and attenuation prediction resulting from the new model was compared with that of the original model. Numerical examples show that although the improved model consists of only two governing equations, it can obtain a result similar to that of the original model for the case of a porous medium containing gas and water, which simplifies the complexity of the calculations. However, in a porous medium with oil and water, the predictions of dispersion and attenuation produced by the original model obviously deviate from the normal trend. In contrast, the results of the improved model exhibit the correct trend with a smooth curve. This phenomenon shows the stability of the improved model and it could be used to describe wave propagation dispersions and attenuations of porous media containing two immiscible fluids in practical cases.


2008 ◽  
Vol 123 (5) ◽  
pp. 3036-3036
Author(s):  
Bernard R. Castagnede ◽  
Denis Lafarge ◽  
Claude Depollier ◽  
Naima Sebaa ◽  
Michel Henry

Author(s):  
M.V. Parthasarathy ◽  
C. Daugherty

The versatility of Low Temperature Field Emission SEM (LTFESEM) for viewing frozen-hydrated biological specimens, and the high resolutions that can be obtained with such instruments have been well documented. Studies done with LTFESEM have been usually limited to the viewing of small organisms, organs, cells, and organelles, or viewing such specimens after fracturing them.We use a Hitachi 4500 FESEM equipped with a recently developed BAL-TEC SCE 020 cryopreparation/transfer device for our LTFESEM studies. The SCE 020 is similar in design to the older SCU 020 except that instead of having a dedicated stage, the SCE 020 has a detachable cold stage that mounts on to the FESEM stage when needed. Since the SCE 020 has a precisely controlled lock manipulator for transferring the specimen table from the cryopreparation chamber to the cold stage in the FESEM, and also has a motor driven microtome for precise control of specimen fracture, we have explored the feasibility of using the LTFESEM for multiple-fracture studies of the same sample.


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