Георадарный метод обнаружения водонасыщенных слоев грунта с оценкой их объемной влажности
Geo-radar method of revealing ground water local zones in upper ground layers (up to 20—30 m) with evaluation of their three-dimensional humidity concerning the sounding signal with stepwise alteration of its carrier frequency has been considered. The method is based on phase structure of reflected...
Збережено в:
| Дата: | 2014 |
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| Автори: | , , , |
| Формат: | Стаття |
| Мова: | Russian |
| Опубліковано: |
Інститут геофізики ім. С.I. Субботіна НАН України
2014
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| Назва видання: | Геофизический журнал |
| Онлайн доступ: | http://dspace.nbuv.gov.ua/handle/123456789/100401 |
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| Назва журналу: | Digital Library of Periodicals of National Academy of Sciences of Ukraine |
| Цитувати: | Георадарный метод обнаружения водонасыщенных слоев грунта с оценкой их объемной влажности / В.Г. Сугак, О.А. Овчинкин, Ю.С. Силаев, А.В. Сугак // Геофизический журнал. — 2014. — Т. 36, № 2. — С. 127-137. — Бібліогр.: 17 назв. — рос. |
Репозитарії
Digital Library of Periodicals of National Academy of Sciences of Ukraine| Резюме: | Geo-radar method of revealing ground water local zones in upper ground layers (up to 20—30 m) with evaluation of their three-dimensional humidity concerning the sounding signal with stepwise alteration of its carrier frequency has been considered. The method is based on phase structure of reflected signals which characteristics are determined to essential degree by three-dimensional humidity of ground rocks. Effectiveness of the method was evaluated by practical example of revealing water-saturated ground layers at the depths up to 20 m and was confirmed by the data of drilling and laboratory tests. |
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