首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Molecular dynamics investigation of viscosity, chemical diffusivities and partial molar volumes of liquids along the MgO-SiO2 join as functions of pressure
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Molecular dynamics investigation of viscosity, chemical diffusivities and partial molar volumes of liquids along the MgO-SiO2 join as functions of pressure

机译:沿着MgO-SiO2连接的液体的黏度,化学扩散性和部分摩尔体积的分子动力学研究,它是压力的函数

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Molecular dynamics simulations are carried out to systematically address the effects of composition and pressure on melts, along the MgO-SiO2 join and elucidate the role of structural modifier content on silicate melt properties. The MgO-SiO2 System shows non-ideal mixing with a negative excess volume of mixing at low pressures, but the mixing becomes closer to ideal at higher pressures. At atmospheric pressure, the viscosities and diffusivities vary by more than 3 orders of magnitude as the composition is varied along this join, with the low SiO2 melts characterized by lower viscosities and higher diffusivities these results are in quantitative agreement with experimental results for the dependence of viscosity and diffusivity on structural modifier content in a wide range of silicate systems. The transport properties of melts in this system converge at higher pressures; at pressures greater than similar to 15 GPa the viscosity and diffusivities vary by less than an order of magnitude across the entire range of compositions. The relevance of equations that relate the viscosity and diffusivity is also addressed. (c) 2006 Elsevier Inc. All rights reserved.
机译:进行了分子动力学模拟,系统地研究了成分和压力对熔体的影响,沿着MgO-SiO2的连接,并阐明了结构改性剂含量对硅酸盐熔体性能的作用。 MgO-SiO2系统显示出非理想的混合,在低压下混合量为负过量,但在高压下混合变得更接近理想状态。在大气压下,随着组成的变化,粘度和扩散率变化超过3个数量级,低SiO2熔体的特征在于较低的粘度和较高的扩散率,这些结果与实验结果在定量上吻合,因为各种硅酸盐体系中结构改性剂含量的粘度和扩散率。熔体在该系统中的传输特性在更高的压力下会聚。在大于类似于15 GPa的压力下,粘度和扩散率在整个组合物范围内变化的幅度小于一个数量级。还解决了与粘度和扩散率有关的方程式的相关性。 (c)2006 Elsevier Inc.保留所有权利。

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