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柯尔任斯基根据野外和室内的地质研究,提出了活动组份概念。应用热力学原理及过滤和扩散效应的理论,推导出相应的热力学方程式及渗滤和扩散交代作用方程式。从而得出了一系列有关交代作用的结论。他的这些研究成果,对地质学的研究方法及对地质学某些方面的理论和实践的进展,无疑具有一定的意义。关于活动组份概念及化学热力学方面,F·J·台尔纳(1948)、B·A·尼格拉也夫(1956)、D.F.Weill和W.S.Fyfe(1964)、(1964)等提出了自已的看法。关于渗滤和扩散交代作用理论,虽然在地质结论方面,有人提出疑义,但未涉及渗滤和扩散交代作用方程式的推导和有关基本理论,本文试图对此提出初步看法,仅供参考。
Korrzinski proposed the concept of an active ingredient based on field and indoor geological studies. Based on the theory of thermodynamics and the theory of filtration and diffusion, the corresponding equations of thermodynamics and the equation of infiltration and diffusion are deduced. This leads to a series of conclusions about the role of accountability. His research achievements undoubtedly have certain significance for the research methods of geology and the progress of the theory and practice of certain aspects of geology. In terms of the concepts of active components and chemical thermodynamics, J. Deliner (1948), B. Nigellaf (1956), DFWeill and WSFyfe (1964) and (1964) proposed their own view. Although the theory of percolation and diffusion is explained by some people in the geological conclusion, it has not been involved in the derivation of the equation of percolation and diffusion and the basic theory. This article attempts to provide a preliminary view for reference only.