Active high-frequency acoustic thermometry of frozen water-saturated media

The article discusses promising method of active high-frequency acoustic thermometry, which measures the duration of the backscattering signal of ultrasonic pulses Delta t in the upper layer of water-saturated rocks or seabed sediments. An acoustic model is proposed to explain the strong temperature...

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Published in:Acoustical Physics
Main Authors: Yusupov, Vladimir I., Semiletov, Igor P., Chernykh, Denis V., Salomatin, Aleksandr S.
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.1134/S1063771022050128
https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:001015414
id fttomskstateuniv:koha:001015414
record_format openpolar
spelling fttomskstateuniv:koha:001015414 2024-01-07T09:41:23+01:00 Active high-frequency acoustic thermometry of frozen water-saturated media Yusupov, Vladimir I. Semiletov, Igor P. Chernykh, Denis V. Salomatin, Aleksandr S. 2022 https://doi.org/10.1134/S1063771022050128 https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:001015414 eng eng koha:001015414 doi:10.1134/S1063771022050128 https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:001015414 Acoustical physics. 2022. Vol. 68, № 5. P. 459-466 обратное рассеяние акустические сигналы вечная мерзлота арктический шельф акустическая термометрия статьи в журналах info:eu-repo/semantics/article 2022 fttomskstateuniv https://doi.org/10.1134/S1063771022050128 2023-12-12T17:42:13Z The article discusses promising method of active high-frequency acoustic thermometry, which measures the duration of the backscattering signal of ultrasonic pulses Delta t in the upper layer of water-saturated rocks or seabed sediments. An acoustic model is proposed to explain the strong temperature dependence of the duration of this signal in the region of zero and negative temperatures. It is shown that Delta t increases with decreasing temperature due to an increase in the reflection coefficient of ultrasonic waves from a layered structure and to a decrease in the absorption coefficient in a water-saturated medium. Field studies carried out on a vast area of the Arctic shelf confirmed the existence of such a dependence. The proposed approach can be effective for remote monitoring of temperature changes in frozen water-saturated rocks on land and in the upper layer of seabed sediments on the shallow Arctic shelf, which is necessary to estimate various environmental risks associated with global warming. Article in Journal/Newspaper Arctic Global warming вечная мерзлота Tomsk State University Research Library Arctic Acoustical Physics 68 5 459 466
institution Open Polar
collection Tomsk State University Research Library
op_collection_id fttomskstateuniv
language English
topic обратное рассеяние
акустические сигналы
вечная мерзлота
арктический шельф
акустическая термометрия
spellingShingle обратное рассеяние
акустические сигналы
вечная мерзлота
арктический шельф
акустическая термометрия
Yusupov, Vladimir I.
Semiletov, Igor P.
Chernykh, Denis V.
Salomatin, Aleksandr S.
Active high-frequency acoustic thermometry of frozen water-saturated media
topic_facet обратное рассеяние
акустические сигналы
вечная мерзлота
арктический шельф
акустическая термометрия
description The article discusses promising method of active high-frequency acoustic thermometry, which measures the duration of the backscattering signal of ultrasonic pulses Delta t in the upper layer of water-saturated rocks or seabed sediments. An acoustic model is proposed to explain the strong temperature dependence of the duration of this signal in the region of zero and negative temperatures. It is shown that Delta t increases with decreasing temperature due to an increase in the reflection coefficient of ultrasonic waves from a layered structure and to a decrease in the absorption coefficient in a water-saturated medium. Field studies carried out on a vast area of the Arctic shelf confirmed the existence of such a dependence. The proposed approach can be effective for remote monitoring of temperature changes in frozen water-saturated rocks on land and in the upper layer of seabed sediments on the shallow Arctic shelf, which is necessary to estimate various environmental risks associated with global warming.
format Article in Journal/Newspaper
author Yusupov, Vladimir I.
Semiletov, Igor P.
Chernykh, Denis V.
Salomatin, Aleksandr S.
author_facet Yusupov, Vladimir I.
Semiletov, Igor P.
Chernykh, Denis V.
Salomatin, Aleksandr S.
author_sort Yusupov, Vladimir I.
title Active high-frequency acoustic thermometry of frozen water-saturated media
title_short Active high-frequency acoustic thermometry of frozen water-saturated media
title_full Active high-frequency acoustic thermometry of frozen water-saturated media
title_fullStr Active high-frequency acoustic thermometry of frozen water-saturated media
title_full_unstemmed Active high-frequency acoustic thermometry of frozen water-saturated media
title_sort active high-frequency acoustic thermometry of frozen water-saturated media
publishDate 2022
url https://doi.org/10.1134/S1063771022050128
https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:001015414
geographic Arctic
geographic_facet Arctic
genre Arctic
Global warming
вечная мерзлота
genre_facet Arctic
Global warming
вечная мерзлота
op_source Acoustical physics. 2022. Vol. 68, № 5. P. 459-466
op_relation koha:001015414
doi:10.1134/S1063771022050128
https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:001015414
op_doi https://doi.org/10.1134/S1063771022050128
container_title Acoustical Physics
container_volume 68
container_issue 5
container_start_page 459
op_container_end_page 466
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