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arXiv 1908.00402cond-mat.mtrl-sci
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分子动力学方法研究多孔镁铝石的热导率

Thermal conductivity of porous jennite by molecular dynamics method

Song-Nam Hong, Chol-Jun Yua, Un-Song Hwang, Chung-Hyok Kim, Byong-Hyok Ri

摘要:

采用分子动力学方法,在ClayFF力场的作用下,模拟了水泥浆体中主要组分-多孔镁铝榴石的导热系数及其孔隙率和温度的相关性。通过去除块状jennite模型中球体内的原子,得到了具有不同孔隙率的多孔jennite模型。在300 K时,用平衡Green-Kubo方法和非平衡Müller-Plathe(MP)方法计算的块体jennite的导热系数基本一致。在300 K时,多孔镁铝榴石的体积热导率随着孔隙率从0%增加到72.22%而从1.141 W/m $\cdot$ K减小到0.144 W/m $\cdot$ K,并符合经验相干势模型。随着温度的升高,孔隙率为0、15.99和32.79%的多孔珍妮岩的热导率从240 K增加到560 K,然后逐渐减小,直到1100 K。

英文摘要:

The thermal conductivity of porous jennite, as the major component of cement paste, and its porosity and temperature dependences are simulated by molecular dynamics methods using ClayFF force field. The porous jennite models with different porosities are created by removing atoms within the sphere from bulk jennite model. The thermal conductivity elements of bulk jennite calculated by equilibrium Green-Kubo method are almost identical to those by non-equilibrium Müller-Plathe (MP) method at 300 K. The volumetric thermal conductivity of porous jennite is found to decrease from 1.141 W/m$\cdot$K to 0.144 W/m$\cdot$K as increasing the porosity from 0\% to 72.22\% at 300 K, following the empirical coherent potential model when the pore is assumed to be filled with air. As increasing temperature, the thermal conductivity is observed to increase from 240 K to 560 K and gradually decrease until 1100 K for porous jennites with the porosities of 0\%, 15.99\% and 32.79\%.

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