Deformability of intact rock

Author(s):  
G.I. Ofoegbu ◽  
J.H. Curran
Keyword(s):  
2016 ◽  
Vol 16 (2) ◽  
pp. 04015059 ◽  
Author(s):  
Hossein Masoumi ◽  
Serkan Saydam ◽  
Paul C. Hagan
Keyword(s):  

2019 ◽  
Vol 9 (1) ◽  
Author(s):  
Hengxing Lan ◽  
Junhui Chen ◽  
Renato Macciotta
Keyword(s):  

Energies ◽  
2020 ◽  
Vol 13 (1) ◽  
pp. 286
Author(s):  
Ying Zhu ◽  
Han Zhang ◽  
Dongbin Pan ◽  
Lianghao Zhai ◽  
Shuai Gao ◽  
...  

A horizontal well with hydraulic fractures is key to forming a fracture network in oil shale for the generated hydrocarbon flows. By considering the influence of anisotropic strength, a prediction model is proposed for fracture initiation by studying different fracture initiation modes (FIMs) in oil shale: failure of the intact rock matrix and of the bedding planes. Through a case study on Nong’an oil shale, the influences of wellbore trajectory and bedding planes on the fracture initiation pressure (FIP), location (FIL), and FIM were analyzed and the induced changes in wellbore trajectory design were concluded. The preferred angle between the wellbore axis and the minimum horizontal principal stress was the same of 90° or 270°, when the lowest required FIP corresponded to the failure of the intact rock matrix. However, when the angle corresponded to the failure of the bedding planes, the preferred direction of the wellbore axis was away from the fixed direction and not corresponding to the lowest required FIP due to the fracture morphology. The error between the theoretical and experimental results ranges from 7% to 9%. This research provides a framework for the design of horizontal wellbore trajectories in oil shale, for easier fracture initiation and more complex fracture networks.


Author(s):  
Benedek A. Lógó ◽  
Balázs Vásárhelyi

Although Poisson’s ratio is one of the basic rock mechanical parameters, it is less investigated than the other parameters. It can be assumed, that this material constant depends on the rigidity of the rock, among the others. The goal of this research is to find a theoretical relationship between the rigidity of the intact rock and Poisson’s ratio. It was assumed that there is a connection between the internal friction angle (or cohesion) and rigidity of the isotropic, linear elastic material, using the Mohr-Coulomb theory. Based on these equations from different published limit equilibrium, six different equations were compared. It is published that the rigidity value is equal (within the experimental error) to the Hoek-Brown material constant (mi) which value is well-known for many different rock types. Plotting the published Poisson’s ratio in the function of the rigidity of the intact rock the optimal connection was chosen.


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