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Numerical Simulation of Phase Change at High Hydrostatic Pressure under Variable-Gravity Environment

机译:重力环境下高静水压力下相变的数值模拟

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We present a numerical investigation of phase change of water at high hydrostatic pressure conditions occurring under a gravitational environment and a low-gravity environment. A computational model consists of conservation equations of mass, momentum, and energy. Phase-transition phenomena are modeled with an enthalpy-porosity approach. Numerical solutions are obtained for process stages dominated by free convection as well as by forced convection. A high pressure-assisted freezing / thawing is carried out in the pressure range from the ambient pressure up to 150 MPa. Differences in the thermofluid dynamics observed in the high-pressure chamber operated under gravity and low-gravity conditions are discussed. The results reveal significant influence of gravity on the distribution of temperature and velocity and consequently on the different ice growth characteristics.
机译:我们提出了在重力和低重力环境下高静水压条件下水的相变的数值研究。一个计算模型由质量,动量和能量的守恒方程组成。相变现象是用焓-孔隙率方法建模的。对于以自由对流和强制对流为主的工艺阶段,可获得数值解。在从环境压力到150 MPa的压力范围内进行高压辅助的冻融。讨论了在重力和低重力条件下运行的高压室中观察到的热流体动力学差异。结果表明,重力对温度和速度的分布有很大影响,因此对不同的冰生长特性也有很大的影响。

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