Ground ice and hydrothermal ground motions on aufeis plots of river valleys
Localized groundwater outflow and layered freezing of them in forms of large ice clusters on the surface creates specific conditions for energy and mass exchange in the «atmosphere–soil–lithosphere» system. In winter, the soil temperature profile is essentially deformed due to heat emission by the a...
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ftdoajarticles:oai:doaj.org/article:2be7a90e94d84e0caf52abe559022fd6 2023-05-15T16:37:39+02:00 Ground ice and hydrothermal ground motions on aufeis plots of river valleys V. R. Alekseev 2015-03-01T00:00:00Z https://doi.org/10.15356/2076-6734-2015-1-69-88 https://doaj.org/article/2be7a90e94d84e0caf52abe559022fd6 RU rus Nauka https://ice-snow.igras.ru/jour/article/view/13 https://doaj.org/toc/2076-6734 https://doaj.org/toc/2412-3765 2076-6734 2412-3765 doi:10.15356/2076-6734-2015-1-69-88 https://doaj.org/article/2be7a90e94d84e0caf52abe559022fd6 Лëд и снег, Vol 55, Iss 1, Pp 69-88 (2015) бугры пучения криогенное движение грунтов криогенные явления наледи наледные процессы подземный лёд термокарст Science Q article 2015 ftdoajarticles https://doi.org/10.15356/2076-6734-2015-1-69-88 2023-03-19T01:40:13Z Localized groundwater outflow and layered freezing of them in forms of large ice clusters on the surface creates specific conditions for energy and mass exchange in the «atmosphere–soil–lithosphere» system. In winter, the soil temperature profile is essentially deformed due to heat emission by the aufeis layer of water at its freezing that forms a specific thermocline layer. Deformation of the temperature profile, gradually decreasing, moves down the cross-section and disappearing at the interface between frozen and thawed rocks. Magnitude and number of the temperature deviations from a «normal» state depends on the heat storage of the aufeis-forming waters and on the number of outflows at a given point. The thermocline formation changes conditions of freezing for underlying ground layers together with mechanism of ice saturation of them, and that results in formation of two-layer ice-ground complexes (IGC) which differ drastically from cryogenic features in adjacent parts of the valley. Analysis of genetic characteristics and relation of components of the surface and subsurface layers allowed identification of seven types of the aufeis IGC: massive-segregation, cement-basal, layered-segregation, basal-segregation, vacuum-filtration, pressureinjection, and fissure-vein. Yearly formation and destruction of aufeises and subsurface ices is accompanied by a sequence of particularly hazardous geodynamical phenomena, among which the most important are winter flooding of territories, layered freezing of water, ground heaving, thermokarst, and thermoerosion. Combination of these processes may cause a rapid (often unexpected) reconfiguration of channels of both surface and subsurface runoff, abrupt uplifts and subsidences of the surface, and decompaction and «shaking-up» of seasonally thawing and seasonally freezing rocks, which may create exceptionally unfavorable conditions for construction and operation of engineering structures. Aufeis plots of river valleys are the most «hot» points of the permafrost zone. A ... Article in Journal/Newspaper Ice permafrost Thermokarst термокарст* Directory of Open Access Journals: DOAJ Articles Ice and Snow 55 1 69 88 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
Russian |
topic |
бугры пучения криогенное движение грунтов криогенные явления наледи наледные процессы подземный лёд термокарст Science Q |
spellingShingle |
бугры пучения криогенное движение грунтов криогенные явления наледи наледные процессы подземный лёд термокарст Science Q V. R. Alekseev Ground ice and hydrothermal ground motions on aufeis plots of river valleys |
topic_facet |
бугры пучения криогенное движение грунтов криогенные явления наледи наледные процессы подземный лёд термокарст Science Q |
description |
Localized groundwater outflow and layered freezing of them in forms of large ice clusters on the surface creates specific conditions for energy and mass exchange in the «atmosphere–soil–lithosphere» system. In winter, the soil temperature profile is essentially deformed due to heat emission by the aufeis layer of water at its freezing that forms a specific thermocline layer. Deformation of the temperature profile, gradually decreasing, moves down the cross-section and disappearing at the interface between frozen and thawed rocks. Magnitude and number of the temperature deviations from a «normal» state depends on the heat storage of the aufeis-forming waters and on the number of outflows at a given point. The thermocline formation changes conditions of freezing for underlying ground layers together with mechanism of ice saturation of them, and that results in formation of two-layer ice-ground complexes (IGC) which differ drastically from cryogenic features in adjacent parts of the valley. Analysis of genetic characteristics and relation of components of the surface and subsurface layers allowed identification of seven types of the aufeis IGC: massive-segregation, cement-basal, layered-segregation, basal-segregation, vacuum-filtration, pressureinjection, and fissure-vein. Yearly formation and destruction of aufeises and subsurface ices is accompanied by a sequence of particularly hazardous geodynamical phenomena, among which the most important are winter flooding of territories, layered freezing of water, ground heaving, thermokarst, and thermoerosion. Combination of these processes may cause a rapid (often unexpected) reconfiguration of channels of both surface and subsurface runoff, abrupt uplifts and subsidences of the surface, and decompaction and «shaking-up» of seasonally thawing and seasonally freezing rocks, which may create exceptionally unfavorable conditions for construction and operation of engineering structures. Aufeis plots of river valleys are the most «hot» points of the permafrost zone. A ... |
format |
Article in Journal/Newspaper |
author |
V. R. Alekseev |
author_facet |
V. R. Alekseev |
author_sort |
V. R. Alekseev |
title |
Ground ice and hydrothermal ground motions on aufeis plots of river valleys |
title_short |
Ground ice and hydrothermal ground motions on aufeis plots of river valleys |
title_full |
Ground ice and hydrothermal ground motions on aufeis plots of river valleys |
title_fullStr |
Ground ice and hydrothermal ground motions on aufeis plots of river valleys |
title_full_unstemmed |
Ground ice and hydrothermal ground motions on aufeis plots of river valleys |
title_sort |
ground ice and hydrothermal ground motions on aufeis plots of river valleys |
publisher |
Nauka |
publishDate |
2015 |
url |
https://doi.org/10.15356/2076-6734-2015-1-69-88 https://doaj.org/article/2be7a90e94d84e0caf52abe559022fd6 |
genre |
Ice permafrost Thermokarst термокарст* |
genre_facet |
Ice permafrost Thermokarst термокарст* |
op_source |
Лëд и снег, Vol 55, Iss 1, Pp 69-88 (2015) |
op_relation |
https://ice-snow.igras.ru/jour/article/view/13 https://doaj.org/toc/2076-6734 https://doaj.org/toc/2412-3765 2076-6734 2412-3765 doi:10.15356/2076-6734-2015-1-69-88 https://doaj.org/article/2be7a90e94d84e0caf52abe559022fd6 |
op_doi |
https://doi.org/10.15356/2076-6734-2015-1-69-88 |
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Ice and Snow |
container_volume |
55 |
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69 |
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1766027947448205312 |