Soil temperature regimes in Finland

Soil temperature regime substantially influences soil classification in Soil Taxonomy particularly in temperate areas. To facilitate correct classification of soils of Finland, the temperature regimes in soils of the country were determined. The mean annual soil temperature, measured at 50 cm below...

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Main Authors: M. YLI-HALLA, D. MOKMA
Format: Article
Language:English
Published: Scientific Agricultural Society of Finland 2008-12-01
Series:Agricultural and Food Science
Online Access:https://journal.fi/afs/article/view/5606
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author M. YLI-HALLA
D. MOKMA
author_facet M. YLI-HALLA
D. MOKMA
author_sort M. YLI-HALLA
collection DOAJ
description Soil temperature regime substantially influences soil classification in Soil Taxonomy particularly in temperate areas. To facilitate correct classification of soils of Finland, the temperature regimes in soils of the country were determined. The mean annual soil temperature, measured at 50 cm below soil surface, ranged from 6.4°C at the warmest site (Anjala) to 1.9°C at the coldest one (Utsjoki, Kevo), and the mean summer soil temperature from 13.7°C to 6.2°C at the same stations, all being in the range of the cryic temperature regime. The mean annual soil temperature was 2 to 5°C higher than the mean annual air temperature, the difference (Y, °C) depending on the duration of snow coverage (X, days) according to the following equation: Y = 0.0305 X - 2.16, R2 = 0.91, n = 9. Even soils of the warmest areas in southern Finland and the mineral soils of the coldest areas in the north, at least for the most part, have cryic soil temperature regimes. Therefore, most soils of Finland, classified according to Soil Taxonomy, have names where the cryic temperature regime appears on the suborder or great group level.;
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spelling doaj.art-f85796075b534e8181fe05f38fb2ef022022-12-21T21:20:00ZengScientific Agricultural Society of FinlandAgricultural and Food Science1459-60671795-18952008-12-0174Soil temperature regimes in FinlandM. YLI-HALLAD. MOKMASoil temperature regime substantially influences soil classification in Soil Taxonomy particularly in temperate areas. To facilitate correct classification of soils of Finland, the temperature regimes in soils of the country were determined. The mean annual soil temperature, measured at 50 cm below soil surface, ranged from 6.4°C at the warmest site (Anjala) to 1.9°C at the coldest one (Utsjoki, Kevo), and the mean summer soil temperature from 13.7°C to 6.2°C at the same stations, all being in the range of the cryic temperature regime. The mean annual soil temperature was 2 to 5°C higher than the mean annual air temperature, the difference (Y, °C) depending on the duration of snow coverage (X, days) according to the following equation: Y = 0.0305 X - 2.16, R2 = 0.91, n = 9. Even soils of the warmest areas in southern Finland and the mineral soils of the coldest areas in the north, at least for the most part, have cryic soil temperature regimes. Therefore, most soils of Finland, classified according to Soil Taxonomy, have names where the cryic temperature regime appears on the suborder or great group level.;https://journal.fi/afs/article/view/5606
spellingShingle M. YLI-HALLA
D. MOKMA
Soil temperature regimes in Finland
Agricultural and Food Science
title Soil temperature regimes in Finland
title_full Soil temperature regimes in Finland
title_fullStr Soil temperature regimes in Finland
title_full_unstemmed Soil temperature regimes in Finland
title_short Soil temperature regimes in Finland
title_sort soil temperature regimes in finland
url https://journal.fi/afs/article/view/5606
work_keys_str_mv AT mylihalla soiltemperatureregimesinfinland
AT dmokma soiltemperatureregimesinfinland