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Integrated modeling and validation for phase change with natural convection

机译:自然相变的集成建模和验证   对流

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摘要

Water-ice systems undergoing melting develop complex spatio-temporalinterface dynamics and a non-trivial temperature field. In this contribution,we present computational aspects of a recently conducted validation study thataims at investigating the role of natural convection for cryo-interfacedynamics of water-ice. We will present a fixed grid model known as the enthalpyporosity method. It is based on introducing a phase field and employs mixturetheory. The resulting PDEs are solved using a finite volume discretization. Thesecond part is devoted to experiments that have been conducted for modelvalidation. The evolving water-ice interface is tracked based on optical imagesthat shows both the water and the ice phase. To segment the phases, we use abinary Mumford Shah method, which yields a piece-wise constant approximation ofthe imaging data. Its jump set is the reconstruction of the measured phaseinterface. Our combined simulation and segmentation effort finally enables usto compare the modeled and measured phase interfaces continuously. We concludewith a discussion of our findings.
机译:经历融化的水冰系统会产生复杂的时空界面动力学和非平凡的温度场。在此贡献中,我们介绍了最近进行的验证研究的计算方面,该研究旨在调查自然对流对水冰的低温界面动力学的作用。我们将介绍一种称为焓孔法的固定网格模型。它基于引入相场并采用混合理论。使用有限体积离散化可解决生成的PDE。第二部分专门介绍了为进行模型验证而进行的实验。基于显示水和冰相的光学图像跟踪不断演变的水冰界面。为了分割相位,我们使用二进制Mumford Shah方法,该方法产生成像数据的分段恒定近似值。它的跳变集是所测相位界面的重建。最终,我们结合了仿真和分段工作,可以连续比较建模和测量的相界面。最后,我们讨论了我们的发现。

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