These four models' parameters can be determined conveniently by tests with simple stress path.

所建立的模型可以通过简单应力路径下的试验测定模型参数。

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The real dike pattern can be approximately duplicated theoretically by the superposition of two very simple stress fields.

实际岩脉式从理论上可以通过两个最简单的应力场的叠加复现。

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Using experimental stress-strain curves in various simple stress states, generalized effective stress-strain formulae may be derived correspondingly in various forms.

用不同的简单应力状态下的应力-应变试验曲线，可以得到不同的广义等效应力-应变关系。

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Using experimental stress-strain curves in various simple stress states, generalized effective stress-strain formulae may be derived correspondingly in various forms.

用不同的简单应力状态下的应力-应变试验曲线，可以得到不同的广义等效应力-应变关系。

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