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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Federation of Eurasian Soil Science Societies
2016-10-01
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Online Access: | http://ejss.fesss.org/10.18393/ejss.2016.4.279-284 |
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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 |
work_keys_str_mv |
AT sergeymakarychev structuralfunctionalconceptofthermophysicalconditionofthesoilsofaltairegion AT andreybolotov structuralfunctionalconceptofthermophysicalconditionofthesoilsofaltairegion |
_version_ |
1725164086589652992 |