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Isofrigid soils could also have a cryic temperature regime. A few with organic materials in the upper part are exceptions. The concepts of the soil temperature regimes described below are used in defining classes of soils in the low categories. —A soil with a frigid temperature regime is warmer in summer than a soil with a cryic regime, but its mean annual temperature is lower than 8 oC and the difference between mean summer (June, July, and August) and mean winter (December, January, and February) soil temperatures is more than 6 oC either at a depth of 50 cm from the soil surface or at a densic, lithic, or paralithic contact, whichever is shallower.
Other Aqualfs that have a natric horizon. Natraqualfs, p. 49 JAE. Other Aqualfs that have a fragipan with an upper boundary within 100 cm of the mineral soil surface. Fragiaqualfs, p. 47 JAF. Other Aqualfs that have a kandic horizon. Kandiaqualfs, p. 48 JAG. Other Aqualfs that have one or more layers, at least 25 cm thick (cumulative) within 100 cm of the mineral soil surface, that have 50 percent or more (by volume) recognizable bioturbation, such as filled animal burrows, wormholes, or casts.
It may only mean that the level of free iron in the soil is below the sensitivity limit of the test or that the soil is in an oxidized phase at the time of testing. Use of alpha,alphadipyridyl in a 10 percent acetic-acid solution is not recommended because the acid is likely to change soil conditions, for example, by dissolving CaCO3. The duration of reduction required for creating aquic conditions is not specified. 3. Redoximorphic features associated with wetness result from alternating periods of reduction and oxidation of iron and manganese compounds in the soil.