The Use of the Value of Heat Cycle to Assess the Energy Stability of Permafrost Soils at the Change of Conditions on the Surface
The basis for assessing the stability of geosystems to changes in external heat cycle conditions is the calculation method. It is shown that permafrost soils are characterized by increased values of annual heat cycle QY ≥ 300 MJ/m2, i.e., half-sum of heat arrival and flow rate per year. This...
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MDPI AG
2019-03-01
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| Series: | Geosciences |
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| Online Access: | http://www.mdpi.com/2076-3263/9/3/112 |
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| author | Anatoly Kulikov Nimazhap Badmaev Darima Sympilova Ayur Gyninova |
| author_facet | Anatoly Kulikov Nimazhap Badmaev Darima Sympilova Ayur Gyninova |
| author_sort | Anatoly Kulikov |
| collection | DOAJ |
| description | The basis for assessing the stability of geosystems to changes in external heat cycle conditions is the calculation method. It is shown that permafrost soils are characterized by increased values of annual heat cycle QY ≥ 300 MJ/m2, i.e., half-sum of heat arrival and flow rate per year. This is due to the high heat consumption for melting soils (QPh = 0.7–0.8 QY) and warming them in the negative temperature range (QF). The heat cycle in frozen soil (QF) always has more heat cycle than in the thawed soil (QH). The condition QF > QH means the dominance of processes occurring at negative temperature, and the difference QF − QH is a quantitative assessment of the energy stability of soils to changes in heat exchange conditions on the surface. |
| first_indexed | 2024-12-23T03:20:44Z |
| format | Article |
| id | doaj.art-294d58de5c204a1581f81957aa448db9 |
| institution | Directory Open Access Journal |
| issn | 2076-3263 |
| language | English |
| last_indexed | 2024-12-23T03:20:44Z |
| publishDate | 2019-03-01 |
| publisher | MDPI AG |
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| series | Geosciences |
| spelling | doaj.art-294d58de5c204a1581f81957aa448db92022-12-21T18:02:00ZengMDPI AGGeosciences2076-32632019-03-019311210.3390/geosciences9030112geosciences9030112The Use of the Value of Heat Cycle to Assess the Energy Stability of Permafrost Soils at the Change of Conditions on the SurfaceAnatoly Kulikov0Nimazhap Badmaev1Darima Sympilova2Ayur Gyninova3Institute of General and Experimental Biology, Siberian Branch, Russian Academy of Sciences, Sakhyanovoi str.6, 670000 Ulan-Ude, RussiaInstitute of General and Experimental Biology, Siberian Branch, Russian Academy of Sciences, Sakhyanovoi str.6, 670000 Ulan-Ude, RussiaInstitute of General and Experimental Biology, Siberian Branch, Russian Academy of Sciences, Sakhyanovoi str.6, 670000 Ulan-Ude, RussiaInstitute of General and Experimental Biology, Siberian Branch, Russian Academy of Sciences, Sakhyanovoi str.6, 670000 Ulan-Ude, RussiaThe basis for assessing the stability of geosystems to changes in external heat cycle conditions is the calculation method. It is shown that permafrost soils are characterized by increased values of annual heat cycle QY ≥ 300 MJ/m2, i.e., half-sum of heat arrival and flow rate per year. This is due to the high heat consumption for melting soils (QPh = 0.7–0.8 QY) and warming them in the negative temperature range (QF). The heat cycle in frozen soil (QF) always has more heat cycle than in the thawed soil (QH). The condition QF > QH means the dominance of processes occurring at negative temperature, and the difference QF − QH is a quantitative assessment of the energy stability of soils to changes in heat exchange conditions on the surface.http://www.mdpi.com/2076-3263/9/3/112permafrost soilsheat cyclethermal and energy stabilitiesCryosols |
| spellingShingle | Anatoly Kulikov Nimazhap Badmaev Darima Sympilova Ayur Gyninova The Use of the Value of Heat Cycle to Assess the Energy Stability of Permafrost Soils at the Change of Conditions on the Surface Geosciences permafrost soils heat cycle thermal and energy stabilities Cryosols |
| title | The Use of the Value of Heat Cycle to Assess the Energy Stability of Permafrost Soils at the Change of Conditions on the Surface |
| title_full | The Use of the Value of Heat Cycle to Assess the Energy Stability of Permafrost Soils at the Change of Conditions on the Surface |
| title_fullStr | The Use of the Value of Heat Cycle to Assess the Energy Stability of Permafrost Soils at the Change of Conditions on the Surface |
| title_full_unstemmed | The Use of the Value of Heat Cycle to Assess the Energy Stability of Permafrost Soils at the Change of Conditions on the Surface |
| title_short | The Use of the Value of Heat Cycle to Assess the Energy Stability of Permafrost Soils at the Change of Conditions on the Surface |
| title_sort | use of the value of heat cycle to assess the energy stability of permafrost soils at the change of conditions on the surface |
| topic | permafrost soils heat cycle thermal and energy stabilities Cryosols |
| url | http://www.mdpi.com/2076-3263/9/3/112 |
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