QUANTITATIVE ESTIMATION OF VOLUMETRIC ICE CONTENT IN FROZEN GROUND BY DIPOLE ELECTROMAGNETIC PROFILING METHOD

Volumetric estimation of the ice content in frozen soils is known as one of the main problems in the engineering geocryology and the permafrost geophysics. A new way to use the known method of dipole electromagnetic profiling for the quantitative estimation of the volumetric ice content in frozen so...

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Published in:Ice and Snow
Main Author: L. G. Neradovskiy
Format: Article in Journal/Newspaper
Language:Russian
Published: Nauka 2018
Subjects:
Q
Ice
Online Access:https://doi.org/10.15356/2076-6734-2018-1-94-104
https://doaj.org/article/1dc06597124a4894b87a1eea8df29231
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spelling ftdoajarticles:oai:doaj.org/article:1dc06597124a4894b87a1eea8df29231 2023-05-15T16:36:55+02:00 QUANTITATIVE ESTIMATION OF VOLUMETRIC ICE CONTENT IN FROZEN GROUND BY DIPOLE ELECTROMAGNETIC PROFILING METHOD L. G. Neradovskiy 2018-04-01T00:00:00Z https://doi.org/10.15356/2076-6734-2018-1-94-104 https://doaj.org/article/1dc06597124a4894b87a1eea8df29231 RU rus Nauka https://ice-snow.igras.ru/jour/article/view/438 https://doaj.org/toc/2076-6734 https://doaj.org/toc/2412-3765 2076-6734 2412-3765 doi:10.15356/2076-6734-2018-1-94-104 https://doaj.org/article/1dc06597124a4894b87a1eea8df29231 Лëд и снег, Vol 58, Iss 1, Pp 94-104 (2018) метод дэмп мёрзлые грунты объёмная льдистость параметр амплитудного ослабления поля ввмд разнос слой годовых теплооборотов Science Q article 2018 ftdoajarticles https://doi.org/10.15356/2076-6734-2018-1-94-104 2023-03-19T01:40:13Z Volumetric estimation of the ice content in frozen soils is known as one of the main problems in the engineering geocryology and the permafrost geophysics. A new way to use the known method of dipole electromagnetic profiling for the quantitative estimation of the volumetric ice content in frozen soils is discussed. Investigations of foundation of the railroad in Yakutia (i.e. in the permafrost zone) were used as an example for this new approach. Unlike the conventional way, in which the permafrost is investigated by its resistivity and constructing of geo-electrical cross-sections, the new approach is aimed at the study of the dynamics of the process of attenuation in the layer of annual heat cycle in the field of high-frequency vertical magnetic dipole. This task is simplified if not all the characteristics of the polarization ellipse are measured but the only one which is the vertical component of the dipole field and can be the most easily measured. Collected data of the measurements were used to analyze the computational errors of the average values of the volumetric ice content from the amplitude attenuation of the vertical component of the dipole field. Note that the volumetric ice content is very important for construction. It is shown that usually the relative error of computation of this characteristic of a frozen soil does not exceed 20% if the works are performed by the above procedure using the key-site methodology. This level of accuracy meets requirements of the design-and-survey works for quick, inexpensive, and environmentally friendly zoning of built-up remote and sparsely populated territories of the Russian permafrost zone according to a category of a degree of the ice content in frozen foundations of engineering constructions. Article in Journal/Newspaper Ice permafrost Yakutia Directory of Open Access Journals: DOAJ Articles Ice and Snow 58 1 94 104
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language Russian
topic метод дэмп
мёрзлые грунты
объёмная льдистость
параметр амплитудного ослабления поля ввмд
разнос
слой годовых теплооборотов
Science
Q
spellingShingle метод дэмп
мёрзлые грунты
объёмная льдистость
параметр амплитудного ослабления поля ввмд
разнос
слой годовых теплооборотов
Science
Q
L. G. Neradovskiy
QUANTITATIVE ESTIMATION OF VOLUMETRIC ICE CONTENT IN FROZEN GROUND BY DIPOLE ELECTROMAGNETIC PROFILING METHOD
topic_facet метод дэмп
мёрзлые грунты
объёмная льдистость
параметр амплитудного ослабления поля ввмд
разнос
слой годовых теплооборотов
Science
Q
description Volumetric estimation of the ice content in frozen soils is known as one of the main problems in the engineering geocryology and the permafrost geophysics. A new way to use the known method of dipole electromagnetic profiling for the quantitative estimation of the volumetric ice content in frozen soils is discussed. Investigations of foundation of the railroad in Yakutia (i.e. in the permafrost zone) were used as an example for this new approach. Unlike the conventional way, in which the permafrost is investigated by its resistivity and constructing of geo-electrical cross-sections, the new approach is aimed at the study of the dynamics of the process of attenuation in the layer of annual heat cycle in the field of high-frequency vertical magnetic dipole. This task is simplified if not all the characteristics of the polarization ellipse are measured but the only one which is the vertical component of the dipole field and can be the most easily measured. Collected data of the measurements were used to analyze the computational errors of the average values of the volumetric ice content from the amplitude attenuation of the vertical component of the dipole field. Note that the volumetric ice content is very important for construction. It is shown that usually the relative error of computation of this characteristic of a frozen soil does not exceed 20% if the works are performed by the above procedure using the key-site methodology. This level of accuracy meets requirements of the design-and-survey works for quick, inexpensive, and environmentally friendly zoning of built-up remote and sparsely populated territories of the Russian permafrost zone according to a category of a degree of the ice content in frozen foundations of engineering constructions.
format Article in Journal/Newspaper
author L. G. Neradovskiy
author_facet L. G. Neradovskiy
author_sort L. G. Neradovskiy
title QUANTITATIVE ESTIMATION OF VOLUMETRIC ICE CONTENT IN FROZEN GROUND BY DIPOLE ELECTROMAGNETIC PROFILING METHOD
title_short QUANTITATIVE ESTIMATION OF VOLUMETRIC ICE CONTENT IN FROZEN GROUND BY DIPOLE ELECTROMAGNETIC PROFILING METHOD
title_full QUANTITATIVE ESTIMATION OF VOLUMETRIC ICE CONTENT IN FROZEN GROUND BY DIPOLE ELECTROMAGNETIC PROFILING METHOD
title_fullStr QUANTITATIVE ESTIMATION OF VOLUMETRIC ICE CONTENT IN FROZEN GROUND BY DIPOLE ELECTROMAGNETIC PROFILING METHOD
title_full_unstemmed QUANTITATIVE ESTIMATION OF VOLUMETRIC ICE CONTENT IN FROZEN GROUND BY DIPOLE ELECTROMAGNETIC PROFILING METHOD
title_sort quantitative estimation of volumetric ice content in frozen ground by dipole electromagnetic profiling method
publisher Nauka
publishDate 2018
url https://doi.org/10.15356/2076-6734-2018-1-94-104
https://doaj.org/article/1dc06597124a4894b87a1eea8df29231
genre Ice
permafrost
Yakutia
genre_facet Ice
permafrost
Yakutia
op_source Лëд и снег, Vol 58, Iss 1, Pp 94-104 (2018)
op_relation https://ice-snow.igras.ru/jour/article/view/438
https://doaj.org/toc/2076-6734
https://doaj.org/toc/2412-3765
2076-6734
2412-3765
doi:10.15356/2076-6734-2018-1-94-104
https://doaj.org/article/1dc06597124a4894b87a1eea8df29231
op_doi https://doi.org/10.15356/2076-6734-2018-1-94-104
container_title Ice and Snow
container_volume 58
container_issue 1
container_start_page 94
op_container_end_page 104
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