Frost sorting on slopes by needle ice: A laboratory simulation on the effect of slope gradient |
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| Authors: | Anyuan Li Norikazu Matsuoka Fujun Niu |
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| Institution: | 1. State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, Gansu, China;2. College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China;3. Graduate School of Life and Environmental Sciences, University of Tsukuba, Tsukuba, Japan;4. Faculty of Life and Environmental Sciences, University of Tsukuba, Tsukuba, Japan |
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| Abstract: | Following a previous attempt to reproduce miniature sorted patterns on a level surface, we report the results of a full‐scale laboratory simulation on frost sorting produced by needle ice activity on inclined surfaces. Four models, with different slope gradients (5°, 7°, 9°, 11°), were designed. Stones 6 mm in diameter placed in a grid covered 20% of the surface of frost‐susceptible water‐saturated soil. These models were subjected to 20–40 freeze–thaw cycles between 10°C and ?5°C in 12 hours. The evolution of surface patterns was visually traced by photogrammetry. Needle ice growth and collapse induced downslope movement and concentrations of stones. A model produced incipient sorted circles on a 5° slope, whereas it resulted in three distinct sorted stripes on a 7° slope. The average diameter or spacing of these forms is 9.7–19.4 cm, comparable to those in the field dominated by diurnal freeze–thaw cycles. Surface parallel displacements of stone markers were traced with motion analysis software. The observed downslope stone displacements agree with those expected assuming that surface soil and stones move by repeated heaving perpendicular to the surface and vertical settlement due to gravity, although the growth of curved needle adds complexity to the overall displacements. Copyright © 2017 John Wiley & Sons, Ltd. |
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| Keywords: | sorted stripes freeze– thaw needle ice laboratory simulation frost creep patterned ground periglacial process |
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