PERIODICITY IN VARIATION OF THERMODYNAMIC, PHYSICAL, AND BIOGEOCHEMICAL PROPERTIES OF ELEMENTS

dc.contributor.author	Marakushev A.A.
dc.contributor.author	Gavrilov N.M.
dc.contributor.author	Marakushev S.A.
dc.date.accessioned	2022-01-13T08:02:18Z
dc.date.available	2022-01-13T08:02:18Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13429324
dc.identifier.citation	Doklady Earth Sciences, 2003, 393, 8, 1185-1191
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34246
dc.description.abstract	The heat capacity and entropy of elementary substances are considered in this work as a thermodynamic basis of geochemical systematics of the respective elements. According to the Oddo–Harkins rule, they are divided into even and odd groupings based on their abundance. In order to justify this division, the mean composition of carbonaceous chondrites (C) that makes up only 2–5% of the total chondrite dips [2] has been used in [1]. The predominant ordinary chondrites are divided into approximately equal low-Fe (L) and high-Fe (H) varieties. This subdivision reﬂects a bimodality of the dominating group of meteorites [3].
dc.title	PERIODICITY IN VARIATION OF THERMODYNAMIC, PHYSICAL, AND BIOGEOCHEMICAL PROPERTIES OF ELEMENTS
dc.type	Статья

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