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Properties of Permafrost Soils on the Northern Seward Peninsula, Northwest Alaska
Author(s) -
Höfle Claudia,
Ping ChienLu,
Kimble John M.
Publication year - 1998
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1998.03615995006200060021x
Subject(s) - permafrost , soil water , tundra , geology , frost weathering , active layer , frost heaving , frost (temperature) , soil horizon , physical geography , arctic , soil science , earth science , hydrology (agriculture) , geomorphology , geotechnical engineering , oceanography , layer (electronics) , geography , chemistry , organic chemistry , thin film transistor
Soil processes in permafrost regions differ markedly from those of the mid and low latitudes. Permafrost soils are cold during the short growing season and frozen the rest of the year. This study was conducted to describe permafrost soils on the tundra coastal plain of northern Seward Peninsula with emphasis on soil characteristics below the active layer and cryogenic structures, both aspects which were widely neglected in previous studies of permafrost soils. We used cryogenic structures to determine active layer depths. In describing these soils, we applied the previous soil taxonomy and tested the utility of the new Gelisol order. Seven pedons were excavated and described in different topographic positions. Most pedons are influenced by frost action, as evidenced by irregular and broken horizons and weakly developed soils. Mineral horizons have predominantly reduced colors. Organic horizons of 7‐ to 50‐cm thickness occur in the study area. All soils contain segregated ice and ice wedges. Segregated ice includes ice lenses, ice nets, and ataxitic ice concentrations at the base of the active layer. With the identification of these cryogenic features, it was possible to determine active layer depths independently of thaw season. For describing the properties of permafrost soils, the new Gelisol order is shown to be a significant improvement on the previous soil taxonomy.