泥岩超压释放深度和次数及其主要影响因素

在泥岩超压形成机制和条件研究的基础上,通过泥岩超压形成与演化规律的研究,建立了一套泥岩超压释放深度和次数的研究方法,利用此方法通过理论计算对泥岩超压释放深度和次数的主要影响因素进行了研究,得到泥岩超压是其压实过程中的阶段产物,只有当压实成岩达到一定程度后方可形成,当超过泥岩破裂极限后便发生破裂超压释放,超压降低以致消失。泥岩超压释放主要受压实速率和欠压实程度的影响,随着压实速率和欠压实程度增大,泥岩超压释放深度逐渐减小,压实速率对泥岩释放深度的影响较欠压实程度对泥岩超压释放深度的影响大,尤其是当压实速率小于0.0005时,这种影响程度更大。泥岩超压释放次数也主要受压实速率和欠压实程度的影响,随压实速率和欠压实程度增大,泥岩超压释放次数增多,在压实速率小于或等于0.001和欠压实程度(声波时差)小于500μm/s时,泥岩超压释放次数增大幅度相对较小,在压实速率大于或等于0.001和欠压实程度(声波时差)大于500μm/s时,泥岩超压释放次数增大幅度相对较大。

Hot compression deformation characteristics of Mg-Mn alloys

The hot deformation behaviors of solution treated Mg-1.8Mn-0.4Er-0.2Al alloys were investigated by means of compression tests on Gleeble-1500 in strain rate range of 0.01-10s-1,deformation temperature range of 250-450℃ and a true strain of 0.6.The constitutive relationships among flow stress,strain rate and deformation temperature were described by Arrhenius-type equations,based on the fact that the material constants could be calculated under a wide range of strains.The results show that the flow stress of the experimental alloy decreases with temperature increasing and strain rate decreasing.Under the experimental conditions,the products of constant α and n in the constitutive equation are stable within certain strains,and the deformation activation energy ranges from 160 to 220 kJ/mol.It is proved that the values of calculated flow stress are close to the experimental results with average error of 2.01%.

泥岩相似材料力学性能影响因素的试验研究

为了分析成型压力、压实速率、重复搅拌次数对泥岩相似材料力学性能的影响,选取相似模型试验中常用的石膏作为胶结材料,黄沙、石英砂及重晶石粉作为骨料制成相似材料试件,进行单轴压缩试验、巴西劈裂试验,得到试件的单轴抗压强度、抗拉强度及弹性模量。结果表明:成型压力由2.0MPa增加至4.0MPa,材料的单轴抗压强度、抗拉强度及弹性模量分别增加49.9%、54.4%、88.6%;压实速率由0.5mm/min增加至4.0mm/min,材料的单轴抗压强度、抗拉强度及弹性模量分别增加22.9%、89.6%、32.5%;重复搅拌次数由1次增加至9次,材料的单轴抗压强度、抗拉强度及弹性模量分别减小31.6%、22.2%、43.2%。这些研究成果对提高模型试验精度、指导模型试验的操作具有一定意义。