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单词 Poroelasticity
释义

Poroelasticity

中文百科

渗流力学 Poromechanics

(重定向自Poroelasticity)

渗流力学是流体力学的一个分支,主要研究流体在多孔介质中的运动方式。由于多孔介质之间的空隙尺寸微小,因此渗流力学具有毛细作用突出、分子力作用显著和流动阻力较大等特性,因此流动速度往往比较慢,另外惯性力也可忽略不计。

英语百科

Poromechanics 渗流力学

(重定向自Poroelasticity)

Poromechanics is a branch of physics and specifically continuum mechanics and acoustics that studies the behaviour of fluid-saturated porous media. A porous medium or a porous material is a solid (often called matrix) permeated by an interconnected network of pores (voids) filled with a fluid (liquid or gas). Usually both solid matrix and the pore network (also known as the pore space) are assumed to be continuous, so as to form two interpenetrating continua such as in a sponge. Many natural substances such as rocks, soils, biological tissues, and man made materials such as foams and ceramics can be considered as porous media. Porous media whose solid matrix is elastic and the fluid is viscous are called poroelastic. A poroelastic medium is characterised by its porosity, permeability as well as the properties of its constituents (solid matrix and fluid).

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更新时间:2025/6/22 12:00:45