Application of an Integrated and Self-contained Electromagnetic Acoustic Recorder for Monitoring the Rock Mass Structure and Development of Geodynamic Processes in Ore Mines / A. A. Bespalko (Bespal'ko) [et al.]

Уровень набора: (RuTPU)RU\TPU\network\4526, MATEC Web of ConferencesАльтернативный автор-лицо: Bespalko (Bespal'ko), A. A., physicist, Leading researcher of Tomsk Polytechnic University, Candidate of physical and mathematical sciences, 1948-, Anatoly Alekseevich;Yavorovich, L. V., specialist in the field of electrophysics, senior researcher of Tomsk Polytechnic University, 1957-, Ludmila Vasilievna;Fedotov, P. I., specialist in the field of electrical engineering, researcher of Tomsk Polytechnic University, 1982-, Pavel Ivanovich;Pomishin, E. K., physicist, technician of Tomsk Polytechnic University, 1993-, Evgeny Karlovich;Vedyashkin, M. V., Specialist in the field of non-destructive testing, Senior Lecturer of Tomsk Polytechnic University, Candidate of technical sciences, 1978-, Maxim ViktorovichКоллективный автор (вторичный): Национальный исследовательский Томский политехнический университет (ТПУ), Институт неразрушающего контроля (ИНК), Проблемная научно-исследовательская лаборатория электроники, диэлектриков и полупроводников (ПНИЛ ЭДиП)Язык: английский.Резюме или реферат: The paper presents a block diagram of the recorder of electromagnetic and acoustic signals. The recorder provides monitoring of electromagnetic and acoustic signals under changing stress-strain state of heterogeneous materials and rocks. The analog amplifier input sensitivity of electromagnetic signals in 4 channels is 10 [mu]V, that of the electromagnetic signal intensity is 10 [mu] and that of acoustic signals is 50 [mu]V. The operating frequency range of recording is (1±100) kHz. The averaging of electromagnetic and acoustic signal amplitudes is performed within 1 or 5 seconds. The data on electromagnetic and acoustic emission materials is recorded in digital format in the internal memory of the recorder. The recorder operates off-line within 7 days. Repeated testing of the recorder in natural conditions of the Tashtagol mine showed that the changes in the amplitude and frequency parameters of electromagnetic signals (EMC) indicate the structural damage in mines made of rocks which differ in their electrical properties. Measurements of the intensity of electromagnetic signals enable monitoring the changes in the stress-strain state of rocks during and after blasting and other geodynamic phenomena..Примечания о наличии в документе библиографии/указателя: [References: 26 tit.].Тематика: электронный ресурс | труды учёных ТПУ | рекордеры | мониторинг | горные массы | геодинамические процессы | рудники | сигналы | напряженно-деформированные состояния | электромагнитные сигналы | акустические сигналы | горные породы Ресурсы он-лайн:Щелкните здесь для доступа в онлайн | Щелкните здесь для доступа в онлайн
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[References: 26 tit.]

The paper presents a block diagram of the recorder of electromagnetic and acoustic signals. The recorder provides monitoring of electromagnetic and acoustic signals under changing stress-strain state of heterogeneous materials and rocks. The analog amplifier input sensitivity of electromagnetic signals in 4 channels is 10 [mu]V, that of the electromagnetic signal intensity is 10 [mu] and that of acoustic signals is 50 [mu]V. The operating frequency range of recording is (1±100) kHz. The averaging of electromagnetic and acoustic signal amplitudes is performed within 1 or 5 seconds. The data on electromagnetic and acoustic emission materials is recorded in digital format in the internal memory of the recorder. The recorder operates off-line within 7 days. Repeated testing of the recorder in natural conditions of the Tashtagol mine showed that the changes in the amplitude and frequency parameters of electromagnetic signals (EMC) indicate the structural damage in mines made of rocks which differ in their electrical properties. Measurements of the intensity of electromagnetic signals enable monitoring the changes in the stress-strain state of rocks during and after blasting and other geodynamic phenomena.

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