Arid
DOI10.1016/j.catena.2003.10.002
Volcanic soils of Iceland
Arnalds, O
通讯作者Arnalds, O
来源期刊CATENA
ISSN0341-8162
EISSN1872-6887
出版年2004
卷号56期号:1-3页码:3-20
英文摘要

The parent materials of all Icelandic soils are volcanic in origin, and most of the soils are classified as Andosols. Iceland has the largest area of Andosols in Europe, and may have >5% of all Andosols in the world. A new classification scheme based on the World Reference Base (World Reference Base for Soil Resources. World Soil Resources Reports 84, FAO, Rome) is used to provide an overview of Icelandic volcanic soils. The data were acquired as part of a recently initiated effort to build a database for Icelandic soils, but are also partly based on data from the EU COST-622 action, a literature review and unpublished Icelandic research. The main soil types in Iceland are Histosols, Histic Andosols, Gleyic Andosols, Brown Andosols, Vitrisols and Leptosols. In the Icelandic language, a single term is used to refer to each soil type. This system reflects the dominant influence of eolian deposition and drainage conditions on the formation of Histosols and Andosols. The parent materials of Icelandic soils are mixtures of tephra layers and eolian sediments consisting mostly of volcanic glass. The steady flux of eolian sediments from unstable sandy deserts constantly recharges the surface with basaltic tephra materials. The Histosols (>20% C) have appreciable amounts of andic materials because of the eolian deposition. The Andosols (Histic, Gleyic and Brown Andosols) show characteristic properties of soils dominated by andic materials with allophane contents of up to 30%. Ferrihydrite commonly accounts for 5-15% of the soil. The contents of both allophane and ferrihydrite generally decrease with increasing organic C content of soil horizons, as organic matter inhibits allophane formation and iron tends to become reduced and lost in poorly drained locations. The Vitrisols are soils of desert surfaces with low organic content, but they usually meet criteria for andic materials with >30% glass and (Al+1/2Fe)(o)>0.4%. Cryoturbation is intense in Iceland, resulting in a range of geomorphic surface features. The cryoturbation is related to both climatic factors and the andic soil properties including high water retention and rapid hydraulic conductivity. (C) 2003 Elsevier B.V. All rights reserved.


英文关键词andosols Iceland classification allophane ferrihydrite vitrisols
类型Article
语种英语
国家Iceland
收录类别SCI-E
WOS记录号WOS:000220487700002
WOS关键词BASALTIC SOILS ; CLAY-MINERALS ; 4 ANDEPTS ; CLASSIFICATION ; ALLOPHANE ; TEPHRA ; GEOCHEMISTRY ; DISSOLUTION ; ANDISOLS ; HOLOCENE
WOS类目Geosciences, Multidisciplinary ; Soil Science ; Water Resources
WOS研究方向Geology ; Agriculture ; Water Resources
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/146445
作者单位(1)Agr Res Inst, Reykjavik, Iceland
推荐引用方式
GB/T 7714
Arnalds, O. Volcanic soils of Iceland[J],2004,56(1-3):3-20.
APA Arnalds, O.(2004).Volcanic soils of Iceland.CATENA,56(1-3),3-20.
MLA Arnalds, O."Volcanic soils of Iceland".CATENA 56.1-3(2004):3-20.
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