实验结果表明，边界流体层厚度是水动力学条件的函数。
The experimental results show that the thickness is the function of hydrodynamic conditions.
基于以上实验手段，进一步对短管内弹状泡上升流动的水动力学与传递进行了实验研究与理论分析。
Applying the same experimental method, the hydrodynamics and the transfer of the plug-rising flow regime is investigated and discussed in detail.
实验均发现在跨越水临界点时矿物(或岩石)与水反应的动力学涨落。
Those experiments found the fluctuation of reaction rates of minerals in water in the case of crossing the critical state of water.
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