Recent Progress in Japanese Studies on Storm Runoff Processes

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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.

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詳細情報 詳細情報について

  • CRID
    1390282679304322304
  • NII論文ID
    10002504590
  • NII書誌ID
    AA10518430
  • DOI
    10.4157/grj1984b.69.144
  • ISSN
    21851700
    02896001
  • 本文言語コード
    en
  • データソース種別
    • JaLC
    • Crossref
    • CiNii Articles
  • 抄録ライセンスフラグ
    使用不可

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