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Fig. 3.7 Cryogenic processes evidenced from thin sections and micromorphology (Fox 1985 )
The preferred time for sampling cryosols is at the end of the summer, because the
active layer is deepest at that time. Sampling earlier requires power tools to get to
the base of the soil profi le and a correction to be made for the end-of-season thick-
ness of the active layer. Three kinds of samples normally are collected from cryo-
sols: bulk samples for routine analysis, minimally disturbed volumetric samples for
bulk density and water retention, and thin-section samples for micromorphological
analysis. Physical, chemical, mineralogical, and micromorphological analyses are
normally performed for cryosols as with all soils.
References
Bockheim JG, Tarnocai C (1998) Recognition of cryoturbation for classifying permafrost-affected
soils. Geoderma 81:281-293
Bullock P, Fedoroff N, Jongerius A, Stoops G, Tursina TE, Babel U (1985) Handbook for thin sec-
tion description. WAINE Research Publication, Albrighton
Burt R (ed) (2004) Soil survey laboratory methods manual. Soil survey investigation report, no. 42,
Ver. 4. U.S. Department of Agriculture, Natural Resource Conservation Service, Washington,
DC
Fox CA (1985) Micromorphology of an Orthic Turbic cryosol-a permafrost soil. In: Bullock P,
Murphy CP (eds) Soil micromorphology, vol 2, Soil genesis. Academic, Berkhamsted,
pp 699-705
Gerasimova MI, Lebedeva II, Khitrov NB (2013) Soil horizon designation: state of the art, problems,
and proposals. Eurasian Soil Sci 46:599-609
Hugelius G, Tarnocai C, Bockheim JG, Camill P, Elberling B, Grosse G, Harden JW, Johnson K,
Jorgensen T, Koven CD, Kuhry P, Michaelson G, Mishra U, Palmtag J, Ping C-L, O'Donnell J,
Schirrmeister L, Schuur EAG, Sheng Y, Smith LC, Strauss J, Yu Z (2013) Short communica-
tion: a new dataset for estimating organic carbon storage to 3 m depth soils of the northern
circumpolar permafrost region. Earth Syst Sci Data Discuss 6:93-93
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