Organic soils of Canada: Part 1. Wetland Organic soils

被引:0
|
作者
Kroetsch, David J. [1 ]
Geng, Xiaoyuan [1 ]
Chang, Scott X. [2 ]
Saurette, Daniel D. [3 ]
机构
[1] Agr & Agri Food Canada, Eastern Cereal & Oilseed Res Ctr, Ottawa, ON K1A 0C6, Canada
[2] Univ Alberta, Dept Renewable Resources, Edmonton, AB T6G 2E3, Canada
[3] Agr & Agri Food Canada, Guelph, ON N1G 4S9, Canada
关键词
Organic soils; wetland; peatlands; paludification; terrestrialization; Histosol; Canadian System of Soil Classification; soil taxonomy; CONTINENTAL WESTERN CANADA; GREENHOUSE-GAS EMISSIONS; CARBON ACCUMULATION; PEAT ACCUMULATION; METHANE EMISSIONS; MINERAL SUBSOIL; RICH FENS; BOREAL; PEATLANDS; PALUDIFICATION;
D O I
10.4141/CJSS10043
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Kroetsch, D. J., Geng, X., Chang, S. X. and Saurette, D. D. 2011. Organic soils of Canada: Part 1. Wetland Organic soils. Can. J. Soil Sci. 91: 807-822. In the Canadian System of Soil Classification, the Organic order represents those soils that have developed from materials that are comprised primarily of plant tissue remains and includes both wetland Organic soils and upland Organic soils. This review focuses on the first group; the latter group is discussed in Fox and Tarnocai (2011). Wetland Organic soils can be subdivided into three great groups: Fibrisol, Mesisol, and Humisol, reflecting the degree of decomposition of organic material and the vertical arrangement of different organic horizons and other horizons. Wetland Organic soils are present in all regions of Canada and are commonly referred to as (unfrozen) peatland soils. Unfrozen peatlands with Organic soils cover approximately 75 5568 km(2) (8.4%) of the land area of Canada. The two primary processes of formation of wetland Organic soils are paludification and terrestrialization. The major taxonomic issues identified for the wetland Organic soils concerns the lack of taxonomic protocols for limnic materials within the soil control section. This is an issue for those soil profiles in which the middle tier is dominated by, if not entirely composed of, deposited limnic materials. Further work is required to determine if these issues should be expressed at the great group or subgroup level of classification. Our understanding of the effects of management practices such as cultivation, tree removal, drainage, and peat extraction on soil properties needs to be translated into models of soil development.
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页码:807 / 822
页数:16
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