Please use this identifier to cite or link to this item: http://earchive.tpu.ru/handle/11683/47001
Title: Experimental research of the influence of the strength of ore samples on the parameters of an electromagnetic signal during acoustic excitation in the process of uniaxial compression
Authors: Yavorovich, Ludmila Vasilievna
Bespalko (Bespal'ko), Anatoly Alekseevich
Fedotov, Pavel Ivanovich
Keywords: экспериментальные исследования; прочность; руды; электромагнитные сигналы; акустическое возбуждение; одноосное сжатие; горные породы; напряженно-деформированные состояния; электромагнитные излучения
Issue Date: 2018
Publisher: IOP Publishing
Citation: Yavorovich L. V. Experimental research of the influence of the strength of ore samples on the parameters of an electromagnetic signal during acoustic excitation in the process of uniaxial compression / L. V. Yavorovich, A. A. Bespalko (Bespal'ko), P. I. Fedotov // IOP Conference Series: Materials Science and Engineering. — 2018. — Vol. 289 : Modern Technologies for Non-Destructive Testing : 6th International Conference, 9–14 October 2017, Tomsk, Russian Federation : [proceedings]. — [012025, 10 p.].
Abstract: Parameters of electromagnetic responses (EMRe) generated during uniaxial compression of rock samples under excitation by deterministic acoustic pulses are presented and discussed. Such physical modeling in the laboratory allows to reveal the main regularities of electromagnetic signals (EMS) generation in rock massive. The influence of the samples mechanical properties on the parameters of the EMRe excited by an acoustic signal in the process of uniaxial compression is considered. It has been established that sulfides and quartz in the rocks of the Tashtagol iron ore deposit (Western Siberia, Russia) contribute to the conversion of mechanical energy into the energy of the electromagnetic field, which is expressed in an increase in the EMS amplitude. The decrease in the EMS amplitude when the stress-strain state of the sample changes during the uniaxial compression is observed when the amount of conductive magnetite contained in the rock is increased. The obtained results are important for the physical substantiation of testing methods and monitoring of changes in the stress-strain state of the rock massive by the parameters of electromagnetic signals and the characteristics of electromagnetic emission.
URI: http://earchive.tpu.ru/handle/11683/47001
Appears in Collections:Материалы конференций

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