Structural-functional concept of thermophysical condition of the soils of Altai Region

The goal of this study was to reveal the quantitative interrelations between the thermophysical indices (thermal conductivity and thermal diffusivity) and physical soil properties such as; moisture content, density and detachability. According to the research targets, the soil samples including diff...

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Main Authors: Sergey Makarychev, Andrey Bolotov
Format: Article
Language:English
Published: Federation of Eurasian Soil Science Societies 2016-10-01
Series:Eurasian Journal of Soil Science
Subjects:
Online Access:http://ejss.fesss.org/10.18393/ejss.2016.4.279-284
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spelling doaj-d666b0d7633a46d784da492030be03622020-11-25T01:12:57ZengFederation of Eurasian Soil Science SocietiesEurasian Journal of Soil Science 2147-42492147-42492016-10-015427928410.18393/ejss.2016.4.279-284Structural-functional concept of thermophysical condition of the soils of Altai RegionSergey Makarychev0Andrey Bolotov1Altai State Agricultural University, Barnaul, Russia Altai State Agricultural University, Barnaul, Russia The goal of this study was to reveal the quantitative interrelations between the thermophysical indices (thermal conductivity and thermal diffusivity) and physical soil properties such as; moisture content, density and detachability. According to the research targets, the soil samples including different genesis and soil particle size distribution were taken in different soil and climatic zones of the Altai Region. These were the sod-podzolic sandy loam soils of the dry steppes, chernozems and chestnut soils of light and medium loamy particle size distribution of temperately arid zone, and the heavy loamy gray forest soils and clayey chernozems of the Altai foothills and low mountains. The samples of undisturbed structures in different soil horizons were studied. To measure the thermophysical properties in laboratory setting, a pulse method of a two-dimensional heat source was used. The method takes into account the patterns of temperature field equalization in an unbounded medium after the heat source termination. A feature of this process is the occurrence of peak temperature at the investigated point of the medium at a given instant. The knowledge of this temperature and time enables to determine the soil thermal capacity, thermal conductivity and thermal diffusivity.http://ejss.fesss.org/10.18393/ejss.2016.4.279-284Soilsoil-physical factorsthermal capacitythermal conductivitythermal diffusivity
collection DOAJ
language English
format Article
sources DOAJ
author Sergey Makarychev
Andrey Bolotov
spellingShingle Sergey Makarychev
Andrey Bolotov
Structural-functional concept of thermophysical condition of the soils of Altai Region
Eurasian Journal of Soil Science
Soil
soil-physical factors
thermal capacity
thermal conductivity
thermal diffusivity
author_facet Sergey Makarychev
Andrey Bolotov
author_sort Sergey Makarychev
title Structural-functional concept of thermophysical condition of the soils of Altai Region
title_short Structural-functional concept of thermophysical condition of the soils of Altai Region
title_full Structural-functional concept of thermophysical condition of the soils of Altai Region
title_fullStr Structural-functional concept of thermophysical condition of the soils of Altai Region
title_full_unstemmed Structural-functional concept of thermophysical condition of the soils of Altai Region
title_sort structural-functional concept of thermophysical condition of the soils of altai region
publisher Federation of Eurasian Soil Science Societies
series Eurasian Journal of Soil Science
issn 2147-4249
2147-4249
publishDate 2016-10-01
description The goal of this study was to reveal the quantitative interrelations between the thermophysical indices (thermal conductivity and thermal diffusivity) and physical soil properties such as; moisture content, density and detachability. According to the research targets, the soil samples including different genesis and soil particle size distribution were taken in different soil and climatic zones of the Altai Region. These were the sod-podzolic sandy loam soils of the dry steppes, chernozems and chestnut soils of light and medium loamy particle size distribution of temperately arid zone, and the heavy loamy gray forest soils and clayey chernozems of the Altai foothills and low mountains. The samples of undisturbed structures in different soil horizons were studied. To measure the thermophysical properties in laboratory setting, a pulse method of a two-dimensional heat source was used. The method takes into account the patterns of temperature field equalization in an unbounded medium after the heat source termination. A feature of this process is the occurrence of peak temperature at the investigated point of the medium at a given instant. The knowledge of this temperature and time enables to determine the soil thermal capacity, thermal conductivity and thermal diffusivity.
topic Soil
soil-physical factors
thermal capacity
thermal conductivity
thermal diffusivity
url http://ejss.fesss.org/10.18393/ejss.2016.4.279-284
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AT andreybolotov structuralfunctionalconceptofthermophysicalconditionofthesoilsofaltairegion
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