1) ideal fluid layer
理想流体层
1.
In order to reveal the dynamic properties of the Stoneley wave in elastic half-space-ideal fluid layer and further to provide a surveying method for exploring oceanic resources,a characteristic equation expressing the Stoneley wave in half-infinite solid-ideal fluid layer is derived based on the dynamic equations of elastic solid and ideal fluid.
为了解弹性半空-理想流体层中Stoneley波的动力特性,并为进一步开发利用海洋资源提供调查方法,根据弹性固体与理想流体动力学方程,推导了弹性半空间-理想流体层中Stoneley波的特征方程。
2) ideal fluid
理想流体
1.
Effect of sediment model on dynamic pressure in overlying ideal fluid due to P wave incidence;
淤砂层模拟方法对上层理想流体动力反应的影响——平面P波入射
2.
Analytical solutions to convective heat transfer of ideal fluid;
理想流体对流传热问题的理论解
3.
Effect of sediment model on dynamic pressures of overlying ideal fluid due to SV wave incidence;
淤砂层模型对上层理想流体动力反应的影响——平面SV波入射
3) perfect fluid
理想流体
1.
It have been geven that collape process is equal entropy in perfect fluid systems and collape process is reduction entropy in thermal radiation ope systems.
在共动坐标系下，对引力塌缩系统的熵变进行了研究，证明了理想流体系统的塌缩是等熵过程，有辐射热流的开放系统的塌缩是减熵过程。
4) nonidea fluid
非理想流体
1.
In this paper the Bernoulli s equation for nonidea fluid is deduced, and its use in meteorology is discussed.
本文推导出非理想流体的伯努利方程。
5) ideal rheological body
理想流变体
6) ideal magnetohydrodynamic
理想磁流体
补充资料：理想流体
见粘性流体。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条