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水平应力的英文

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"水平应力"怎么读用"水平应力"造句

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  • horizontal stress

例句与用法

  • Test method for time - to - failure of plastics using plane strain tensile specimens
    使用水平应力拉伸样品测定塑料失效时间的试验方法
  • However , the interparticle friction did not appear to have a significant effect on the magnitude of the lateral stress developed during the uniaxial compression
    然而,颗粒间的摩擦对轴向加载时系统产生的水平应力没有很强的影响。
  • The inversion confirms that plate boundary actions are main factors controlling the regional stress field , and spreading forces of mountains and seashores are another important factor
    同时显示了板块在垂直载荷下的弯曲对局部水平应力场造成相当的影响。
  • The stress distribution is far from uniform in this stratified rock , the horizontal stress magnitude in hard rock layers is significantly higher the that in soft layers
    在软硬相间的层状岩体中地应力分布很不均匀,应力大小与岩层硬度具有正相关性,硬岩中的水平应力大于软岩的水平应力。
  • When the effect of intermediate principal stress was considered in different degrees , the dimensions and shapes of surrounding rock mass is rather different , and this phenomenon will be more obvious with the increase of the difference of horizontal stress and vertical stress
    当不同程度地考虑中间主应力的影响时,围岩塑性区形状和大小有较大不同,且随水平应力与垂直应力差异性的增大,这种影响趋于明显。
  • Through contrasting the characteristics of stress field inside the slope before and after the excavation , the results show that the horizontal stress upside the slope and the shear stress pointing to the outside slope near the foot change clearly
    通过对比开挖前后边坡内部的应力场特征,发现:在影响边坡稳定的指标性应力中,边坡上部的水平应力受开挖影响较大;在成坡坡脚附近,指向坡体外的剪应力显著增加。
  • Depending on how the ground surface is denuded , the feature of the current crustal stress field and rock stress environment can be calculated analyzing the result in this paper : by analyzing the recovering feature of the elastic deformation of the rockmass in unload - stage under various pressures , it has been found there is close relationship between the recovering degree of the elastic deformation of the rockmass and the unloading degree of the pressure the direction of the major principal stress in the crustal stress field is not consistent with the direction of the crushing stress regional tectonics borne during the last tectonic movement . the evolving degree of the regional geomorphology evidently affects the current crustal stress field , which changes from the self - weight stress field to the horizontal stress field , with the changing of the eroding degree of the regional geomorphology ranging from valley area to hilly country to flat country . in valley area , where there is two stress belts , the bankslope s tress belt and the self - weight stress belt within the mountain . the direction of the major principal stress is nearly parallel to the ground surface and inclines towards the valley in the bankslope stress belt . it is nearly vertical in the self - weight stress belt
    通过本文的研究成果,根据区域性地貌的演化特征,我们可以大致地对现今地应力场进行判断:在分级卸荷条件下,岩体中弹性变形的恢复具有明显的规律性,这种规律对于研究地应力场的演变是有帮助的;地应力场中最大主应力方向与区域构造形迹在最近的构造运动中所受区域性挤压应力的方向无明显的对应性;区域性地貌形态的演化程度对现今地应力场的特征具明显的影响,随着区域性地貌侵蚀程度由峡谷区、丘陵区、平原区的变化,现今地应力场特征由自重应力场、水平应力场为主含少量自重应力场特征向水平应力场的规律变化;在峡谷区,山体中具有两个应力带:自重应力带和卸荷应力带,最大主应力方向在卸荷应力带中近平行于坡面并倾向于河谷、在自重应力带中近于直立;根据原始地面遭剥蚀的程度,可以大致地估算最大主应力和中间主应力的量值和方向;在丘陵区和平原区,最大主应力的方向近于水平,并与附近区域性侵蚀盆地和河流的展布方向基本平行,根据原始地面遭剥蚀的程度,可以大致估算其最大主应力的量值;根据区域性地貌形态的特征来分析工程区的现今地应力场特征,并进而大致了解岩石的应力环境,这种分析方法得出的结论与许多实际的地应力测试成果基本一致,对于大型水电工程地下厂房和压力隧洞的设计是有所帮助的。
  • The evolving degree of the regional geomorphology evidently affects on the features of the current crustal stress field . so the crustal stress fields change from the self - weight stress field to the horizontal stress field with the changing of the eroding degree of the regional geomorphology from valley area to hilly country to flat country
    然而,区域性地貌的演化特征对现今地应力场具明显的控制性,当区域性地貌特征从高山峡谷区向低山丘陵区和平原残丘区转变时,现今地应力场的特征也从自重应力场向水平应力场转变。
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