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Simulations of solid-liquid friction at ice-I_h/water interfaces

机译:冰-I_h /水界面的固液摩擦模拟

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We have investigated the structural and dynamic properties of the basal and prismatic facets of the ice I_h/water interface when the solid phase is drawn through the liquid (i.e., sheared relative to the fluid phase). To impose the shear, we utilized a velocity-shearing and scaling approach to reverse non-equilibrium molecular dynamics. This method can create simultaneous temperature and velocity gradients and allow the measurement of transport properties at interfaces. The interfacial width was found to be independent of the relative velocity of the ice and liquid layers over a wide range of shear rates. Decays of molecular orientational time correlation functions gave similar estimates for the width of the interfaces, although the short- and longer-time decay components behave differently closer to the interface. Although both facets of ice are in "stick" boundary conditions in liquid water, the solid-liquid friction coefficients were found to be significantly different for the basal and prismatic facets of ice.
机译:我们已经研究了当固相通过液体(即相对于液相剪切)时,I_h /水界面的基面和棱柱面的结构和动力学特性。为了施加剪切力,我们使用了速度剪切和缩放方法来逆转非平衡分子动力学。这种方法可以同时创建温度和速度梯度,并可以测量界面处的传输特性。发现在宽的剪切速率范围内,界面宽度与冰层和液体层的相对速度无关。分子取向时间相关函数的衰减对界面的宽度给出了相似的估计,尽管较短和较长时间的衰减分量在靠近界面时表现不同。尽管冰的两个面在液态水中都处于“粘滞”边界条件下,但发现冰的基面和棱柱面的固-液摩擦系数显着不同。

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