The effect of temperature on the mechanical behavior of Berea sandstone under confining pressure: experiments

IF 2.6 Q2 ENGINEERING, GEOLOGICAL International Journal of Geo-Engineering Pub Date : 2023-11-02 DOI:10.1186/s40703-023-00191-0
Ch Mohammad Abbas Iftikhar, Akhtar S. Khan, Venkata Nambori
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Abstract

Abstract For the first time, axial and circumferential (diametral) strains are measured directly on Berea sandstone cylindrical samples at different high temperatures as a function of confining pressure. The maximum compressive principal stress was in the direction perpendicular to the bedding plane. Tri-axial compression tests have been conducted under confining pressures ranging from atmospheric pressure to 12,000 psi “82.73 MPa” (gage), and the temperature was varied from room temperature (RT) to 250°F (121.11 °C). In all the experiments, specimens are dry, and no pore pressure is applied. Uniaxial axial force (100 lbs/min or 444.82 N/min) and strains in the three directions ( $$\varepsilon$$ ε 1 , $$\varepsilon$$ ε 2 , $$\varepsilon$$ ε 3 ) is directly measured from the strain gages mounted on the specimen; hence the study reflects the behavior of the Berea sandstone up to the initiation of the failure only. The experimental observations involving yield, failure, transition from brittle to ductile behavior, and their dependence on temperature and confining pressure are presented. Parameters like ductility and dilatancy (reflecting volumetric behavior before failure) and their variation with temperature and confining pressure are given. The initial yield and failure of Berea sandstone are presented in terms of the generalized von-Mises criteria, i.e., variation of octahedral shear stress ("Image missing") with the mean stress. The loads at yield and failure are found to decrease with increasing temperature and augment with increasing confining pressure. The ductility and dilatancy reduction are computed using measured strains with increasing temperature. With an increase in temperature, the volume decreases first, partly due to the initial closure of micro cracks and voids, then increases due to generation of additional microcracks and voids (damage). There is less volume decrease in the uniaxial test response at higher temperature as compared to the corresponding ambient temperature response. A monotonic increase in the octahedral shear stress at yield and failure is observed with increasing confining pressure.

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围压作用下温度对伯里亚砂岩力学行为影响的实验研究
首次直接测量了不同高温条件下Berea砂岩柱状试样的轴向和周向(直径)应变随围压的变化规律。最大主压应力方向垂直于顺层面方向。三轴压缩试验的围压范围从大气压力到12,000 psi " 82.73 MPa "(计压),温度范围从室温(RT)到250°F(121.11℃)。在所有的实验中,试样都是干燥的,没有施加孔隙压力。单轴轴向力(100磅/分钟或444.82 N/分钟)和三个方向($$\varepsilon$$ ε 1, $$\varepsilon$$ ε 2, $$\varepsilon$$ ε 3)的应变直接从安装在试样上的应变片测量;因此,该研究仅反映了伯里亚砂岩在破坏开始前的行为。给出了屈服、破坏、脆性向延性转变及其对温度和围压的依赖关系。给出了塑性和剪胀等参数(反映破坏前的体积行为)及其随温度和围压的变化规律。Berea砂岩的初始屈服和破坏是用广义的von-Mises准则来表示的,即八面体剪切应力(“图像缺失”)随平均应力的变化。屈服载荷和破坏载荷随温度升高而减小,随围压升高而增大。利用随温度升高的实测应变计算塑性和剪胀减量。随着温度的升高,体积首先减小,部分原因是微裂纹和孔洞的初始闭合,然后由于产生额外的微裂纹和孔洞(损伤)而增大。与相应的环境温度响应相比,较高温度下单轴试验响应的体积减小较小。随着围压的增加,屈服和破坏时的八面体剪应力单调增加。
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来源期刊
International Journal of Geo-Engineering
International Journal of Geo-Engineering ENGINEERING, GEOLOGICAL-
CiteScore
3.70
自引率
0.00%
发文量
10
审稿时长
13 weeks
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