“…Coal measure strata are usually composed of numerous bedded sedimentary formations of varying thickness, strength and stiffness. Therefore, apart from the topographical condition, the strata sequences, the Lithology-controlled performance and the presence of weak interfaces between alternating soft and stiff layers (Ghazvinian et al., 2010; Liang et al., 2017b; Liang et al., 2014; Lu et al., 2016; Majdi et al., 2012; Palchik, 2003; Whittles et al., 2006; Xu et al., 2011b), which have not aroused adequate attention, also significantly affect the deformation and movement of the overburden and the resulting failure and performance of SMCBs, which traverse the overlying strata (Karacan, 2009; Liang et al., 2017b; Liu et al., 2017b; Xu et al., 2011a; Zhai et al., 2015).…”
The shear failure of surface methane capture boreholes (SMCBs) is the main reason for the life cycle shortening of surface methane capture boreholes but lacks a comprehensive lithological analysis. To improve the surface methane capture borehole stability and drainage period efficiency, it is of great importance to investigate the influence of lithology on the shear failure of surface methane capture boreholes. The results of direct shear tests and geological investigations show that the shear displacement increases as the grain size decreases. A jump in mechanical properties occurs at the lithological boundaries and is mainly controlled by the composition of the rock specimens. The change in cohesion is the main possible reason for the step change of the shear strength. High quartz and low clay contents may effectively improve the shear strength and failure resistance of rock. Boreholes may potentially experience preferential casing failure in the section of the weaker mudstone and siltstone due to larger shear displacements and lower shear strengths of those rock types. Protective measures at these sections may improve the stability of the borehole casing. The detection results at the close of the borehole verify the prediction.
“…Coal measure strata are usually composed of numerous bedded sedimentary formations of varying thickness, strength and stiffness. Therefore, apart from the topographical condition, the strata sequences, the Lithology-controlled performance and the presence of weak interfaces between alternating soft and stiff layers (Ghazvinian et al., 2010; Liang et al., 2017b; Liang et al., 2014; Lu et al., 2016; Majdi et al., 2012; Palchik, 2003; Whittles et al., 2006; Xu et al., 2011b), which have not aroused adequate attention, also significantly affect the deformation and movement of the overburden and the resulting failure and performance of SMCBs, which traverse the overlying strata (Karacan, 2009; Liang et al., 2017b; Liu et al., 2017b; Xu et al., 2011a; Zhai et al., 2015).…”
The shear failure of surface methane capture boreholes (SMCBs) is the main reason for the life cycle shortening of surface methane capture boreholes but lacks a comprehensive lithological analysis. To improve the surface methane capture borehole stability and drainage period efficiency, it is of great importance to investigate the influence of lithology on the shear failure of surface methane capture boreholes. The results of direct shear tests and geological investigations show that the shear displacement increases as the grain size decreases. A jump in mechanical properties occurs at the lithological boundaries and is mainly controlled by the composition of the rock specimens. The change in cohesion is the main possible reason for the step change of the shear strength. High quartz and low clay contents may effectively improve the shear strength and failure resistance of rock. Boreholes may potentially experience preferential casing failure in the section of the weaker mudstone and siltstone due to larger shear displacements and lower shear strengths of those rock types. Protective measures at these sections may improve the stability of the borehole casing. The detection results at the close of the borehole verify the prediction.
“…Pressure vs. distance at approximately t=27.8 hours for: a) σx=5 MPa and σz=7 MPa, b) σx=5 MPa and σz=9 MPa, c) σx=7 MPa and σz=5 MPa, and d) σx=9 MPa and σz=5 MPa .............. 111 Figure 6.1. Stress distribution in front of the mining face (modified after Zhai et al, 2015) ......... 114 Figure 6.2. Roadway and the coal around the boreholes (Zhai et al, 2015) ................................... 115 Figure 6.3.…”
Section: Declaration By Authormentioning
confidence: 99%
“…In-situ stress zone (initial stress zone). (Zhai et al, 2015) As aforementioned, in some researches, it is assumed that the original stress is equal in all directions and hence hydrostatic (Li, Li and Yifeng, 2015;; and the time-dependent deformation does not occur around drainage boreholes for the sake of model simplicity (Zhai et al, 2015). The corresponding failure and deformation zones to the redistributed stresses around drainage boreholes under hydrostatic and deviatoric in-situ stresses are shown in Figure 6.3.…”
Section: Stress Deformation and Permeability Evolution Around Drainamentioning
confidence: 99%
“…Their study does not reveal the impact of post-peak and time-dependent deformation on permeability during continuous pore pressure depletion and the effects of matrix shrinkage on permeability evolution are neglected. Xue et al, 2017) In some studies, the stress profile and permeability evolution around drainage boreholes has been considered analogous to that around roadways in a smaller scale (Zhai et al, 2015), where the drainage borehole wall is analogous to the mining face in underground coal mine. Like the mining face, the zones around the borehole wall present a similar stress profile and permeability distribution (Wang, Elsworth and Liu, 2013).…”
Section: Stress Deformation and Permeability Evolution Around Drainamentioning
confidence: 99%
“…However, after borehole drilling and disturbance to coal reservoir, the deformation process may accelerate due to the increase of effective stress during the extraction of fluids in the reservoir (Schatz and Carroll, 1981). Instability of gas drainage boreholes due to repeated disturbances exerted by external stress, such as mining activities (Zhai et al, 2015) and roadway and branch borehole excavations (Hu et al, 2015) has been widely studied. In such a case, the collapse of borehole walls is likely to occur, which results in blockage of gas-flow channels and therefore a hindrance to CSG drainage.…”
Coal as a soft rock experiences a time-dependent deformation induced by continuous change in effective stress in reservoir during Coal Seam Gas (CSG) production and during well shut-in at static reservoir pressure. This deformation results in compaction of coal microstructure and loss of porosity and permeability over the course of gas production. Limited studies have considered the impact of time-dependent deformation (i.e. consolidation and creep) on coal permeability that may play a key role in determining the efficiency of CSG production. Negligence of the impact of consolidation and creep on coal permeability may result in overestimation of level of drained gas. This research aims to characterize time-dependent deformation in the coal injected with gas and investigate its impact on permeability and gas drainage efficiency. This has been achieved via implementation of two triaxial tests and development of governing equations (i.e. permeability models and mass balance equation) required for simulation of gas transport in coal. In the first test, V
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