Studies of anisotropy of dielectric permeability of soil rocks under pressure

This paper presents the results of experimental measurements of anisotropy of dielectric permeability of wet sand samples appearing as a result of applied external pressure in the frequency range 90—150 MHz. The measurements were made on special measuring stand with use of two developed sensors, one...

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Дата:2014
Автори: Sugak, V.G., Bormotov, V.N., Parkhomenko, V.A.
Формат: Стаття
Мова:Російська
Опубліковано: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/111572
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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author Sugak, V.G.
Bormotov, V.N.
Parkhomenko, V.A.
author_facet Sugak, V.G.
Bormotov, V.N.
Parkhomenko, V.A.
author_sort Sugak, V.G.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:55:34Z
description This paper presents the results of experimental measurements of anisotropy of dielectric permeability of wet sand samples appearing as a result of applied external pressure in the frequency range 90—150 MHz. The measurements were made on special measuring stand with use of two developed sensors, one of which measures dielectric permeability along the vector of pressure and another one — in perpendicular direction. As a result, the anisotropy coefficient of dielectric permeability of the wet sand samples reached the value of 1,6.
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spelling journalsuranua-geofizicheskiy-article-1115722020-10-07T11:55:34Z Studies of anisotropy of dielectric permeability of soil rocks under pressure Sugak, V.G. Bormotov, V.N. Parkhomenko, V.A. This paper presents the results of experimental measurements of anisotropy of dielectric permeability of wet sand samples appearing as a result of applied external pressure in the frequency range 90—150 MHz. The measurements were made on special measuring stand with use of two developed sensors, one of which measures dielectric permeability along the vector of pressure and another one — in perpendicular direction. As a result, the anisotropy coefficient of dielectric permeability of the wet sand samples reached the value of 1,6. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-10-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111572 10.24028/gzh.0203-3100.v36i5.2014.111572 Geofizicheskiy Zhurnal; Vol. 36 No. 5 (2014); 118-127 Геофизический журнал; Том 36 № 5 (2014); 118-127 Геофізичний журнал; Том 36 № 5 (2014); 118-127 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/111572/106562 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Sugak, V.G.
Bormotov, V.N.
Parkhomenko, V.A.
Studies of anisotropy of dielectric permeability of soil rocks under pressure
title Studies of anisotropy of dielectric permeability of soil rocks under pressure
title_full Studies of anisotropy of dielectric permeability of soil rocks under pressure
title_fullStr Studies of anisotropy of dielectric permeability of soil rocks under pressure
title_full_unstemmed Studies of anisotropy of dielectric permeability of soil rocks under pressure
title_short Studies of anisotropy of dielectric permeability of soil rocks under pressure
title_sort studies of anisotropy of dielectric permeability of soil rocks under pressure
url https://journals.uran.ua/geofizicheskiy/article/view/111572
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