Chapter 6: Cryosolic Order
A diagrammatic representation of profiles of some subgroups of the Cryosolic order is shown in Figures 30 and 31. Individual subgroups may include soils that have horizon sequences different from those shown. In the description of each subgroup, presented later in this chapter, a common horizon sequence is given; diagnostic horizons are underlined and some other commonly occurring horizons are listed.
Soils of the Cryosolic order occupy much of the northern third of Canada where permafrost exists close to the surface of both mineral and organic deposits. Cryosolic soils predominate north of the tree line, are common in the subarctic forest area in fine-textured soils, and extend into the boreal forest in some organic materials and into some alpine areas of mountainous regions. Cryoturbation of these soils is common and may be indicated by patterned ground features such as sorted and nonsorted nets, circles, polygons, stripes, and earth hummocks.
Cryosolic soils are formed in either mineral or organic materials that have permafrost either within 1 m of the surface or within 2 m if the pedon has been strongly cryoturbated laterally within the active layer, as indicated by disrupted, mixed, or broken horizons. They have a mean annual temperature ≤0°C. Differentiation of Cryosolic soils from soils of other orders involves either determining or estimating the depth to permafrost.
The Cryosolic order is divided into three great groups: Turbic Cryosol, Static Cryosol, and Organic Cryosol based on the degree of cryoturbation and the nature of soil material, mineral or organic, as indicated in the Cryosolic order chart.
Turbic Cryosol | Static Cryosol | Organic Cryosol | |
---|---|---|---|
Diagnostic horizons are underlined | |||
Soil | mineral | mineral | organic |
Cryoturbation | marked, usually patterned ground | none | none |
Permafrost | within 2m of surface | within 1m of surface | within 1m of surface |
Great Group | Subgroup |
---|---|
Turbic Cryosol | Orthic Eutric Turbic Cryosol OE.TC |
Orthic Dystric Turbic Cryosol OD.TC | |
Brunisolic Eutric Turbic Cryosol BRE.TC | |
Brunisolic Dystric Turbic Cryosol BRD.TC | |
Gleysolic Turbic Cryosol GL.TC | |
Regosolic Turbic Cryosol R.TC | |
Histic Eutric Turbic Cryosol HE.TC | |
Histic Dystric Turbic Cryosol HD.TC | |
Histic Regosolic Turbic Cryosol HR.TC | |
Static Cryosol | Orthic Eutric Static Cryosol OE.SC |
Orthic Dystric Static Cryosol OD.SC | |
Brunisolic Eutric Static Cryosol BRE.SC | |
Brunisolic Dystric Static Cryosol BRD.SC | |
Luvisolic Static Cryosol L.SC | |
Gleysolic Static Cryosol GL.SC | |
Regosolic Static Cryosol R.SC | |
Histic Eutric Static Cryosol HE.SC | |
Histic Dystric Static Cryosol HD.SC | |
Histic Regosolic Static Cryosol HR.SC | |
Organic Cryosol | Fibric Organic Cryosol FI.OC |
Mesic Organic Cryosol ME.OC | |
Humic Organic Cryosol HU.OC | |
Terric Fibric Organic Cryosol TFI.OC | |
Terric Mesic Organic Cryosol TME.OC | |
Terric Humic Organic Cryosol THU.OC | |
Glacic Organic Cryosol GC.OC |
Source: The Canadian System of Soil Classification (Third Edition)