大气溶胶粒子的热泳动理论

B.V Derjaguin, Yu Yalamov
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引用次数: 92

摘要

昂萨格的动力学系数对称原理被用来建立在温度梯度存在下气溶胶粒子和气体运动的统一理论。只考虑了大部分气体的输送热;克努森层的输运热被认为不重要而忽略。这一理论的基础是Derjaguin和Bakanov对克努森层中气体分子速度分布的计算,当表面被气体流流线化时。在相对于分子路径长度的宽度较大的毛细管中,所得的热-分子压差公式与现有的实验数据吻合较好,与麦克斯韦基于热滑移表达式所得的公式相反。考虑到颗粒表面的温度跳跃,还得到了大颗粒和中等大小气溶胶颗粒热游速度的公式,该公式是对Derjaguin-Bakanov公式的改进。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Theory of thermophoresis of large aerosol particles

Onsager's principle of kinetic coefficient symmetry is used to build a uniform theory of motion of aerosol particles and gases in the presence of temperature gradients. Only the transport heat in the bulk of the gas is taken into account; the heat of transport in the Knudsen layer is neglected as insignificant. The basis for this is Derjaguin and Bakanov's calculations of the velocity distribution of the gas molecules in the Knudsen layer when a surface is streamlined by a flow of gas. The formulas obtained for the thermomolecular pressure difference in capillaries whose width is large relative to the path length of the molecules are in good agreement with available experimental data, in contrast to Maxwell's formula based on the expression he obtained for the thermal slip. A formula has also been obtained for the velocity of thermophoresis of large and moderately large aerosol particles, with allowance for the temperature jump at the particle surfaces, this formula being a refinement of the Derjaguin-Bakanov formula.

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