Research results indicate that the pore geometry of the rock and soil shows the fractal behavior over the range from atom scale to grain size.
大量的研究表明，岩土介质的孔隙几何从原子尺度到晶粒尺寸范围内均表现出分形特征。
The characteristics of the second phases, pore formation and grain growth were illustrated.
显微相片阐明了第二相(玻璃相)、气孔的形成以及晶粒生长特性。
The simulation results reflect the microscopic process such as grain contact, sintering neck growth and pore spheroidization.
模拟结果反映了颗粒间接触，烧结颈生长和气孔球化的微观过程。
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