Multiple Fracture Initiation in Openhole Without Mechanical Isolation: First Step to Fulfill an Ambition

Author(s):  
Frank F. Chang ◽  
Kirk Bartko ◽  
Steve Dyer ◽  
Gallyam Aidagulov ◽  
Roberto Suarez-Rivera ◽  
...  
2018 ◽  
Vol 52 (3) ◽  
pp. 827-840 ◽  
Author(s):  
Zai-Le Zhou ◽  
Guang-Qing Zhang ◽  
Yue-Kun Xing ◽  
Zong-Yang Fan ◽  
Xi Zhang ◽  
...  

2020 ◽  
Author(s):  
Frank Fakuen Chang ◽  
Danish Ahmed ◽  
Mohammad Arifin ◽  
Devesh Pathak ◽  
Adzlan Ayob

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.


2009 ◽  
Author(s):  
Chris E. Shuchart ◽  
Shalawn Jackson ◽  
Janette Mendez-Santiago ◽  
Nancy Hyangsil Choi ◽  
John K. Montgomery ◽  
...  

Author(s):  
Manfred Staat

AbstractExtension fractures are typical for the deformation under low or no confining pressure. They can be explained by a phenomenological extension strain failure criterion. In the past, a simple empirical criterion for fracture initiation in brittle rock has been developed. In this article, it is shown that the simple extension strain criterion makes unrealistic strength predictions in biaxial compression and tension. To overcome this major limitation, a new extension strain criterion is proposed by adding a weighted principal shear component to the simple criterion. The shear weight is chosen, such that the enriched extension strain criterion represents the same failure surface as the Mohr–Coulomb (MC) criterion. Thus, the MC criterion has been derived as an extension strain criterion predicting extension failure modes, which are unexpected in the classical understanding of the failure of cohesive-frictional materials. In progressive damage of rock, the most likely fracture direction is orthogonal to the maximum extension strain leading to dilatancy. The enriched extension strain criterion is proposed as a threshold surface for crack initiation CI and crack damage CD and as a failure surface at peak stress CP. Different from compressive loading, tensile loading requires only a limited number of critical cracks to cause failure. Therefore, for tensile stresses, the failure criteria must be modified somehow, possibly by a cut-off corresponding to the CI stress. Examples show that the enriched extension strain criterion predicts much lower volumes of damaged rock mass compared to the simple extension strain criterion.


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