Study of interrelation between electromagnetic radiation and rock strength; IOP Conference Series: Materials Science and Engineering; Vol. 110 : Radiation-Thermal Effects and Processes in Inorganic Materials (RTEP2015)

Bibliografische gegevens
Parent link:IOP Conference Series: Materials Science and Engineering
Vol. 110 : Radiation-Thermal Effects and Processes in Inorganic Materials (RTEP2015).— 2016.— [012085, 6 p.]
Coauteur: Национальный исследовательский Томский политехнический университет (ТПУ) Институт неразрушающего контроля (ИНК) Проблемная научно-исследовательская лаборатория электроники, диэлектриков и полупроводников (ПНИЛ ЭДиП)
Andere auteurs: Yavorovich L. V. Ludmila Vasilievna, Bespalko (Bespal'ko) A. A. Anatoly Alekseevich, Fedotov P. I. Pavel Ivanovich, Pomishin E. K. Evgeny Karlovich
Samenvatting:Title screen
The paper presents the study of the electromagnetic radiation of real rock samples under acoustic impact. The test samples are made of kerns from the iron ore mine with different petrophysical features and strength. The study has shown that the electromagnetic radiation parameters are related to the sample strength. However, this dependence is not observed for samples with magnetite that can be due to individual structural-textural features and quartz inclusions.
Режим доступа: по договору с организацией-держателем ресурса
Taal:Engels
Gepubliceerd in: 2016
Onderwerpen:
Online toegang:http://dx.doi.org/10.1088/1757-899X/110/1/012085
http://earchive.tpu.ru/handle/11683/18093
Formaat: Elektronisch Hoofdstuk
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=647054
Omschrijving
Samenvatting:Title screen
The paper presents the study of the electromagnetic radiation of real rock samples under acoustic impact. The test samples are made of kerns from the iron ore mine with different petrophysical features and strength. The study has shown that the electromagnetic radiation parameters are related to the sample strength. However, this dependence is not observed for samples with magnetite that can be due to individual structural-textural features and quartz inclusions.
Режим доступа: по договору с организацией-держателем ресурса
DOI:10.1088/1757-899X/110/1/012085