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  1. 防災科研関係論文

Experimental analysis of preferential flow in dry snowpack

https://nied-repo.bosai.go.jp/records/4246
https://nied-repo.bosai.go.jp/records/4246
b3e02525-5794-4c01-a7c3-1c9cef91c1cc
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Experimental analysis of preferential flow in dry snowpack
言語
言語 eng
著者 Takafumi Katsushima

× Takafumi Katsushima

en Takafumi Katsushima

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Satoru Yamaguchi

× Satoru Yamaguchi

en Satoru Yamaguchi

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Toshiro Kumakura

× Toshiro Kumakura

en Toshiro Kumakura

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Atsushi Sato

× Atsushi Sato

en Atsushi Sato

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抄録
内容記述タイプ Other
内容記述 Preferential flow in snowpack is an important phenomenon and influences snowpack modeling, avalanche forecasting and runoff forecasting for snow-covered basins. However, the theoretical foundation is not sufficient to develop a snowpack model that includes a water movement process including preferential flow. The water ponding process, which is caused by the water-entry value of capillary pressure, is a key process for capillary pressure overshoot, water saturation overshoot and the formation of preferential flow in other porous media like homogeneous dry sand. We attempted to apply theories of preferential flow in homogeneous dry soil to initially dry snow. Infiltration experiments into homogeneous dry snow and theoretical analysis were carried out to reveal the developing process of preferential flow during infiltration into a homogeneous dry snowpack and to obtain critical conditions for that process. The capillary pressure was measured just above the interface between the dry/wet snow layer by the tensiometer. Concurrently we conducted experiments with a dye-tracer in order to observe the flow patterns. The capillary pressure overshoot and the water-entry value were observed in experiments for samples of a large grain diameter (&gt
0.25. mm). The capillary pressure overshoot was directly linked to the formation of preferential flow. The velocity criterion and the pressure head criterion which are used to predict preferential flow for dry sand were able to predict the preferential flow for three out of our four different samples. The velocity criterion failed, however, to predict the stable case (no occurrence of preferential flow) for the experiment with the smallest grain diameter and pore size. Good agreement experimental results and both criterions were obtained from the analysis. These results showed some similarities between the developing process of preferential flow in dry sand and in dry snowpack. © 2012 Elsevier B.V.
言語 en
書誌情報 en : COLD REGIONS SCIENCE AND TECHNOLOGY

巻 85, p. 206-216
出版者
言語 en
出版者 ELSEVIER
ISSN
収録物識別子タイプ EISSN
収録物識別子 1872-7441
DOI
関連識別子 10.1016/j.coldregions.2012.09.012
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