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首页> 外文期刊>Scientific reports. >Creep and permeability evolution behavior of red sandstone containing a single fissure under a confining pressure of 30?MPa
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Creep and permeability evolution behavior of red sandstone containing a single fissure under a confining pressure of 30?MPa

机译:在30℃的限制压力下含有单个裂缝的红砂岩的蠕变和渗透性进化行为

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The long-term deformation and permeability evolution with time are key issues for geo-engineering applications such as radioactive waste disposal. Rock permeability concurrent with deformation is significantly influenced by cracking. This study investigated the creep-permeability evolution behavior of red sandstone specimens containing a single fissure under a confining pressure of 30?MPa. First, the effects of stress ratio (SR) and fissure dip angle on the creep behavior of rock were investigated. The more loading/unloading cyclic numbers, the larger the irrecoverable axial deformation. The instant elastic strains and visco-elastic strains linearly increased with SR for both the intact and fissured specimens, whereas the instant plastic strains showed different results. The visco-plastic strains nonlinearly increased. For fissured and intact specimens, the creep strains and the steady-state creep rates nonlinearly increased as SR increased. The instantaneous strains, instant elastic strains, and visco-elastic strains slightly varied when the fissure dip angle was less than 45° but notably decreased with increasing fissure dip angle beyond 45°. However, the fissure dip angle had no obvious effects on the plastic and creep strains. Damage (D) was defined using the ratio of non-elastic strains to the total strain. D increased approximately linearly with SR, but the fissure dip angle had no obvious influences. Subsequently, the long-term strength (LTS) of the red sandstone was determined using two different methods. The LTS first decreased when the fissure dip angle increased from 0 to 45° but increased with increasing dip angle. The triaxial and creep failure modes were mainly shear along anti-wing cracks for the fissured specimens but shear failure occurred for the intact specimen. Moreover, the permeability of the fissured red sandstone was governed by SR and deformation or time. During the multi-step loading/unloading creep process, the permeability first decreased and then had a sudden rise when tertiary creep occurred.
机译:随着时间的推移,随着时间的推理,长期变形和渗透性进化是放射性废物处理等地球工程应用的关键问题。岩石渗透性随变形的同时受到破裂的显着影响。本研究调查了在30μm≤MPa的限制压力下含有单个裂缝的红色砂岩样本的蠕变渗透性进化行为。首先,研究了应力比(SR)和裂缝倾角对岩石蠕变行为的影响。循环数字越多,无法恢复的轴向变形越大。瞬间弹性菌株和粘弹性菌株用Sr线性增加,适用于完整和裂缝的样本,而瞬发塑性菌株显示出不同的结果。粘型塑料菌株非线性增加。对于裂纹和完整的样品,随着SR增加,蠕变菌株和稳态蠕变率非线性增加。当裂隙倾角小于45°时,瞬时菌株,瞬时弹性菌株和粘弹性菌株略有变化,但随着裂隙倾角超过45°的裂缝倾角而显着降低。然而,裂缝倾角对塑料和蠕变菌株没有明显的影响。使用非弹性菌株与总菌株的比率定义损伤(D)。 D与SR大致线性增加,但裂缝倾角不会影响明显的影响。随后,使用两种不同的方法测定红色砂岩的长期强度(LTS)。当裂隙倾角从0增加到45°时,LTS首先降低,但随着倾角的增加而增加。三轴和蠕变失效模式主要是沿着裂缝样品的防翼裂缝剪切,但完整标本发生剪切失效。此外,裂隙红色砂岩的渗透率受到Sr的控制和变形或时间。在多步装载/卸载蠕变过程中,渗透率首先降低,然后在第三次蠕变发生时突然上升。

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