Interpretacja statystyczna w zastosowaniu do badań geochemicznych

Abstract

STATISTICAL INTERPRETATION IN GEOCHEMICAL RESEARCH

Summary

The paper presents a statistical method in the interpretation of the results of geochemical research, with allows us to draw objective conclusiuons as to the interpretation between trace elements in any geochemical environment. Of particular importance are here data concerning both geochemical affinity of chemical elements and their migration ability obtained due to the introduction of the formulae (5), (7), (9–11), and (12). It has been ascertained that NI, Co, Cr as well as Zn and Pb make and association of chemical elements, characterized by the strong connections of the simple linear correlation in various types of rocks from the zone of hypergenesis, as well as in plants growing in the areas considered.
In the research particular attention paid was to the distribution types of trace elements within the zone of hypergenesis of basic und ultrabasic rocks. It appears that most chemical elements of Fe group, as well as Cu, Zn·and Pb, are characterized by normal type of distribution in soils, in weathered rock material, and in plans. This phenomena should be related to the complex physical and chemical processes that take place in the zone hypergenesis, to the multiphase genesis of the formations of this zone, and to the occurrence of these chemical elements in numerous mineral and chemical compounds, dissolved in water of the given geochemical environment. The statistical methods presented in this paper may satisfactory be introduced into different domains of geological sciences.