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关注:1 2013-05-23 12:21

求翻译:For example, the following sequence of observations of soil behavior have lead to improved models: Effects of virgin(primary) loading and unloading-reloading, confining pressure, stress path (stress history), intermediate principal stress, instability (leading to shear banding in dense sand and overconsolidated soils and to liquefaction in loose silty sands), anisotropy, and stress rotation (note: this list of phenomena is not exhaustive). While all of these (and many more) effects have been known to exist for some time, some of them are still to be researched and understood in detail before they may be modeled correctly. Thus, the simple models can only handle the first mentioned phenomena, while the more advanced models may handle additional phenomena. It is difficult to say that any one of these phenomena has definitively been researched, understood, and included in any given model. The latter two topics (effects of anisotropy and effects of stress rotation) are in the forefront of current research, and practically applicable models that correctly capture these effects are still to be developed.是什么意思?

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For example, the following sequence of observations of soil behavior have lead to improved models: Effects of virgin(primary) loading and unloading-reloading, confining pressure, stress path (stress history), intermediate principal stress, instability (leading to shear banding in dense sand and overconsolidated soils and to liquefaction in loose silty sands), anisotropy, and stress rotation (note: this list of phenomena is not exhaustive). While all of these (and many more) effects have been known to exist for some time, some of them are still to be researched and understood in detail before they may be modeled correctly. Thus, the simple models can only handle the first mentioned phenomena, while the more advanced models may handle additional phenomena. It is difficult to say that any one of these phenomena has definitively been researched, understood, and included in any given model. The latter two topics (effects of anisotropy and effects of stress rotation) are in the forefront of current research, and practically applicable models that correctly capture these effects are still to be developed.
问题补充:

  • 匿名
2013-05-23 12:26:38
例如,下面的土行为的观测序列产生一种改进的模型: 影响的 virgin(primary) 加载和卸载重装,围压应力路径 (应力历史),中间主应力,不稳定 (通往剪显密砂和 overconsolidated 土壤和松粉细砂液化),各向异性,强调旋转 (注: 此列表的现象并不详尽)。虽然所有这些 (以及更多) 的影响,向来存在一段时间,其中有些仍以研究和了解详细之前他们可能正确建模。因此,简单的模型只能处理第一次提到的现象,而更高级的模型可以处理附加的现象。很难说这些现象中的任何一个明确研究、 理解,并包含在任何给定的模型中。后者的两个主题 (各向异性的影响) 和应力旋转的影响是在当前研究的前沿和正确地捕获这些影响的几乎适用机型仍要发展。
 
 
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