Volume 28, Issue 2 p. 433-445
Research Article

Soil Physical and Environmental Conditions Controlling Patterned‐Ground Variability at a Continuous Permafrost Site, Svalbard

Tatsuya Watanabe

Corresponding Author

Department of Civil and Environmental Engineering, Faculty of Engineering, Kitami Institute of Technology, Kitami, Hokkaido, Japan

Department of Geology, The University Centre in Svalbard (UNIS), Longyearbyen, Norway

Correspondence to: T. Watanabe, Department of Civil and Environmental Engineering, Faculty of Engineering, Kitami Institute of Technology, Kitami, Hokkaido, Japan. E‐mail: twata@mail.kitami‐it.ac.jp

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Norikazu Matsuoka

Faculty of Life and Environmental Sciences, University of Tsukuba, Tsukuba, Ibaraki, Japan

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Hanne H. Christiansen

Department of Geology, The University Centre in Svalbard (UNIS), Longyearbyen, Norway

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Stefanie Cable

Department of Geology, The University Centre in Svalbard (UNIS), Longyearbyen, Norway

Center for Permafrost (CENPERM), Department of Geosciences and Natural Resource Management, University of Copenhagen, Copenhagen, Denmark

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First published: 05 November 2016
Citations: 8

Abstract

This study examines soil physical and environmental conditions controlling patterned‐ground variability on an alluvial fan in a continuous permafrost landscape, at Adventdalen, Svalbard. On‐site monitoring of ground temperature, soil moisture and snow depth, laboratory analyses of soil physical properties and principal component analysis indicate that the distribution of patterned ground depends primarily on soil texture, soil moisture and the winter ground thermal regime associated with snow cover. Mudboils and composite patterns (mudboils surrounded by small polygons) occupy well‐drained areas composed of clay‐rich aeolian sediments. Compared to mudboils, composite patterns show a sharper contrast in soil texture between barren centres and vegetated rims. Hummocks filled with organic materials develop on poorly drained lowlands associated with a shallow water table. Ice‐wedge polygons are dominant on sandy loess‐covered areas where the local wind regime minimises snow cover, enhancing ground cooling that promotes thermal contraction cracking. Copyright © 2016 John Wiley & Sons, Ltd.

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