Polymodality of the Geochemical Process Intensity Distribution: A Marker of the Implementation of Various Geochemical Reactions; Theoretical Foundations of Chemical Engineering; Vol. 59, iss. 4

Bibliographic Details
Parent link:	Theoretical Foundations of Chemical Engineering=Теоретические основы химической технологии.— .— New York: Pleiades Publishing, Ltd. Vol. 59, iss. 4.— 2025.— P. 937-948
Main Author:	Melnik I. A. Igor Anatolevich
Summary:	Conducted studies of the statistical distribution of secondary mineral contents in sandy rocks reveal the following pattern: the distribution forms of these contents are polymodal. The purpose of the presented work is to prove the following hypothesis: when unifying the polymodal statistical distribution of the intensity of an established geochemical process, each sample of intensity value within a separate mode will be characterized by a predictable implementation principle interpreted by a specific chemical reaction. The intensity of the geochemical reactions caused by superimposed epigenesis is determined using the method of statistical correlation interpretation of geophysical research materials of a well. The statistical intensities of the secondary processes of kaolinitization, carbonatization, and pelitization of sand deposits are calculated based on the patterns of geochemical dominance of covariance effects on the recorded parameters of geophysical well surveys. As a result, the dependence of the intensity of the rock transformation process on the product of the statistical correlation parameters of the geophysical data is obtained, specifically, the correlation coefficient and the interval parameter. Using the universal equation of modes of unified polymodal probability density distributions for transformation processes of any open systems, the unification of the intensity modes of secondary processes is conducted and the principles of the transformation process states within each calculated mode are determined. The secondary transformations of the sand deposits of the Tambey oil and gas fields are studied. The correlations between the samples of the process intensities under consideration within each manifested mode are investigated. Conclusions.It is confirmed that each intensity mode of the geochemical process under consideration is due to the manifestation of a specific geochemical reaction. The conducted comparisons of the descriptions of the process state principles with the studied states of geochemical transformations prove the equality of their dynamic transformation modes. Knowing the intensity of the secondary process as an attribute of the calculated mode, it is possible to determine the geochemical state mode of the open reservoir system Текстовый файл AM_Agreement
Language:	English
Published:	2025
Subjects:	polymodal distributions intensity of secondary processes synergetics, geochemistry geophysical studies of wells statistical correlation электронный ресурс труды учёных ТПУ
Online Access:	https://doi.org/10.1134/S0040579525602651
Format:	Electronic Book Chapter
KOHA link:	https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=685655