Cryosol

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Soil profile of a Turbic Cryosol

Cryosol is a reference soil assembly from the World Reference Base for Soil Resources (WRB). Cryosols are characterized by permafrost , which means that the subsoil is permanently frozen and only the topsoil thaws every summer. Cryosols are defined by the diagnostic cryic horizon . This is characterized by a massive layer of ice or clearly visible ice crystals. If the water content is lower, it is defined by a temperature <0 ° C for at least two years. Seasonal thawing and freezing often result in cryoturbation, i.e. a strong mixing of the near-surface horizons. Equally typical are the incorporation of organic matter into the soil as wellFrost elevation with subsequent grain size sorting . This leads, among other things, to stone rings or, on inclined surfaces, to stone strips and solifluction . As a result of global warming, more and more permafrost is permanently thawing . As a result, the organic material in the cryosol is mineralized and carbon dioxide and methane are released into the atmosphere . This leads to an intensification of the greenhouse effect .

distribution

Cryosols occur only in regions with permafrost conditions . They are the dominant soil type in the polar and subpolar zones and are common as a companion soil type in the boreal zone (mostly under coniferous forests) and in the high mountains. In total, they currently cover around 18 million km² and thus around 13% of the earth's surface.

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