Концентрационная конвекция в замкнутой области пористой среды при заданном вертикальном перепаде концентрации и учете иммобилизации примеси

Борис Сергеевич Марышев
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Abstract

This work is devoted to the study of stability of horizontal filtration flow of a mixture through a closed porous domain taking into account impurity immobilization. The instability arises due to the vertical concentration difference of heavy impurities, which creates unstable density stratification. A general mathematical model describing the transport of an impurity through a porous medium is presented. The equations are simplified for the case of low impurity concentration. Simplification made it possible to analytically obtain the solution corresponding to homogeneous horizontal filtration and to study its stability. It is known that, in the narrow regions of porous medium and at weak intensities of the external flow, convection is excited in a monotonous manner. On the contrary, in the case of an infinite horizontal layer, oscillatory instability is observed. A study of the transition between the instability modes is presented. It is shown that the oscillatory regime is observed in long regions or at significant intensity of the external horizontal flow. At low flow intensities, convective cells do not move relative to the region and, hence, there is no reason for oscillations. It has been established that the range of flow intensity values, in which oscillations are observed, grows with increasing length of the domain. Impurity immobilization leads to the stabilization of horizontal filtration with respect to convective perturbations. Critical curves and stability maps are obtained in a wide range of problem parameters and then analyzed. For limiting cases, a comparison is made with the known results obtained for an infinite layer.
在给定垂直浓度差并考虑到杂质固定的情况下,多孔介质封闭区域内的浓度对流
这项工作致力于研究通过封闭多孔域的混合物水平过滤流的稳定性,同时考虑到杂质固定问题。不稳定性的产生是由于重杂质的垂直浓度差造成了不稳定的密度分层。本文提出了一个描述杂质通过多孔介质的一般数学模型。在杂质浓度较低的情况下,对方程进行了简化。简化后,可以通过分析获得与均匀水平过滤相对应的解,并研究其稳定性。众所周知,在多孔介质的狭窄区域和外部流动强度较弱的情况下,对流以单调的方式被激发。相反,在无限水平层的情况下,会出现振荡不稳定性。本文对不稳定模式之间的过渡进行了研究。结果表明,在长区域或外部水平流动强度较大时,会出现振荡机制。在低气流强度下,对流单元不会相对于区域移动,因此不会产生振荡。可以确定的是,出现振荡的流动强度值范围随着区域长度的增加而增大。杂质固定化导致水平过滤在对流扰动方面趋于稳定。在广泛的问题参数范围内获得临界曲线和稳定图,然后进行分析。在极限情况下,与无限层的已知结果进行了比较。
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