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Non-linear thermodynamic laws application to soil processes

机译:非线性热力学定律在土壤过程中的应用

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An attempt has been made to analyze the possibility to use nonequilibrium thermodynamics for the soil dynamic ope n systems treatment. Entropy change of such a system and the entropy coming from or going into the outer sphere. In the steady state, dynamic soil - formation processes occur within an organized structure and are characterized by stable parameters close to e quilibrium. Accordingly, when examining soil, one can proceed from the conventional thermodynamic equilibrium. However, the matter of Onzager - Prigozhin general phenomenological theory applicability to soil processes is more complicated. To study soil stabi lity it is necessary to go beyond the limits of linear thermodynamics.
机译:尝试分析使用非平衡热力学进行土壤动力系统处理的可能性。这种系统的熵变化以及来自或进入外球体的熵。在稳定状态下,动态土壤形成过程发生在有组织的结构内,其特征在于接近于平衡的稳定参数。因此,当检查土壤时,可以从常规的热力学平衡出发。但是,Onzager-Prigozhin一般现象学理论在土壤过程中的适用性更为复杂。为了研究土壤的稳定性,有必要超越线性热力学的极限。

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