Chinese translation for "挤压应力"
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- extrusion stress
racking stress
Related Translations:
连续挤压: continuous extrusionstraight through extrusion 复合挤压: coextrusioncombined extrusion 挤压挠曲: compaction flexture
- Example Sentences:
| 1. | Numerical analysis of creep pressing stress of casing in deep salt rock stratum
深井石油套管盐膏岩层蠕变挤压应力计算研究 | | 2. | The compressional stress mainly comes from sw , and the ne direction acts as a resistance
挤压应力主要来自南西方向、北东方向起阻挡作用。 | | 3. | Study on squeezing effect against soil and pore pressure by pile pushing in saturated soft clay foundation
饱和软粘土地基沉桩过程中桩土挤压应力及超孔压计算 | | 4. | The rock foundation bent under the horizontal compressive stress . it is called fold . the regional or local stress direction can be analyzed according to the fold structure
岩层受到水平挤压应力，发生弯曲称作褶皱。通常依据褶皱构造可分析区域或局部应力方向。 | | 5. | The conclusion is that the extrusion presses between primary and secondary linings , elasticity of the waterproof layer and unblocked drainage layer are the vital factors influencing the waterproof layer of spraying - on acrylate membrane in tunnel composite linings
试验结果表明，衬砌间的挤压应力、防水层的弹性恢复能力、通畅的排水层对丙烯酸盐喷膜防水层在隧道复合式衬砌中的防水效能发挥重要作用。 | | 6. | 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。 | | 7. | Abstract : the excess pore water pressure of saturated soft clay foundation caused by pile pushing is obvious . the method for calculating squeezing stress and excess pore pressure by elastic - plastic theory is deduced in this paper , and furthermore , the reasonable pile spacing by regarding the influence of both squeezing stress and excess water pressure is given
文摘:饱和软粘土地基沉桩过程中桩土挤压所引起的桩周土体超孔隙水压力效应是非常显的.本文从弹塑性理论出发推导出沉桩过程中桩周土体挤压应力及超孔隙水压力的计算公式，给出了考虑挤压应力和超孔隙水压力影响因素的合理打桩间距的确定方法 | | 8. | The meso - cenozoic evolution of bachu fault - uplift is closely related to its south and north subsiding foredeep . under the background of indian plate subducting under asia - europe plate , bachu forebulge was greatly affected by the development of southwest depression and awati depression . almost all of its structure reversed , and as a result of it , both of its south and north boundary migrated . according to its evolution history and its feature , the authors tentatively use both - side migration model to interpret the evolution of compound forebulge . since triassic , almost all the spheres above lithosphere synchronously became flexure . because transpressional stress field became increasingly strong , bachu forebulge continued uplifting and big faults formed . then , bachu uplift , as a whole , slipped upward along those big faults and showed migrating toward thrust zone in plane . in tectonic tranquility , the lithosphere bounded back and in consequence of it , bachu uplift slipped down and showed migration toward craton , at that moment negative inversion structures developed . while the forebulge migrated toward its south and north foredeep , it was very possible that locally extensional stress appeared in the forebulge
在印度板块向欧亚板块俯冲的大背景下，巴楚前缘断隆受西南坳陷和阿瓦提凹陷的影响，新生代时构造体制发生反转，边界向南北迁移。根据其发育过程特征，作者用复合前缘隆起两端迁移模式对复合前缘隆起独特的构造发育史进行了解释：即三叠纪以来岩石圈各圈层同步挠曲变形。随着挤压应力场的增大，巴楚隆起在挠曲基础上不断抬升，形成几条大型断裂带。 | | 9. | Measurements demonstrate that the regional tectonic setting apparently does not control the features of the current crustal stress field , the direction of the major principal stress in the current crustal stress field is not consistent with the direction of the crushing stress regional tectonics borne during the last tectonic movement
许多地应力场的实测资料表明：区域性地质构造特征对现今地应力场并无明显的控制性，现今地应力场中最大主应力的方向与挽近期区域性挤压应力方向并非具一一对应的关系。 | | 10. | Research results show that different conformation mode of tectonite roof result in the difference of preservation condition of gas , intense pressing process of structural stress in the front of gliding structure result in mine gas outburst , and control on no . 2 gas source in tectonite roof is the best means by which the gas problem can be perfectly solved in gliding structure area
研究结果表明：由于滑动构造区煤层顶板不同的结构类型，导致矿井瓦斯保存条件的差异；滑动构造前缘挤压带内强烈的挤压应力作用是本区瓦斯突出的根本原因；控制采空区顶板的二次瓦斯源是治理滑动构造区瓦斯地质灾害的根本之策。 |
- Similar Words：
- "挤压样" Chinese translation, "挤压液" Chinese translation, "挤压翼" Chinese translation, "挤压因数" Chinese translation, "挤压应变" Chinese translation, "挤压用畔" Chinese translation, "挤压用润滑剂" Chinese translation, "挤压油膜" Chinese translation, "挤压油膜轴承" Chinese translation, "挤压诱发逆断裂活动" Chinese translation
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