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- TANAKA Tadashi
- Institute of Geoscience, University of Tsukuba
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Recent Japanese studies on storm runoff processes in forested drainage basins showed the important role of subsurface water, especially groundwater flow during storm events. It was recognized that several mechanisms such as rapid flow through soil pipes, capillary water effect, air pressure effect and capillary barrier effect operate inducing a rapid response of groundwater to storm events depending on differences in local hydrologic conditions. All of these mechanisms were chiefly attributed to inhomogeneities and hydraulic property differences of the soil deposits. Interactions between storm runoff processes and geomorphic processes were also investigated.
収録刊行物
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- Geographical review of Japan, Series B
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Geographical review of Japan, Series B 69 (2), 144-159, 1996
公益社団法人 日本地理学会
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詳細情報 詳細情報について
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- CRID
- 1390282679304322304
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- NII論文ID
- 10002504590
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- NII書誌ID
- AA10518430
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- ISSN
- 21851700
- 02896001
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- 本文言語コード
- en
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- データソース種別
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- JaLC
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- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可