書誌事項
- タイトル別名
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- The Delayed Runoff Hydrograph: a Possibility for Bedrock Groundwater Outflow
- ハイドログラフ ノ ヒカク ニ ヨル オクレタ リュウシュツ ピーク ト サンタイ チカスイ ノ カンレン
この論文をさがす
説明
<p>The relationship between bedrock subsurface flow and delayed runoff response was studied by several published papers. Two types of basin topography were found among the watersheds showing delayed runoff responses: 1) underlain by thick colluvium at the “source area” of the basins, having mostly gentle relief, and 2) steep sedimentary rock or fractured rock basins, where bedrock fracture flow may be dominant. The other type-2 response is the watershed underlain by limestone or similar rock types where bedrock flow should be dominant. These two types can be conventionally classified by the basin relief, but bedrock spring could exist in the colluvium in most watersheds. This reviewing work suggests that the mechanism for quick or mostly identical time runoff response to rain storm, which can be revealed by analyzing delayed type runoff response.</p>
収録刊行物
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- 日本水文科学会誌
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日本水文科学会誌 31 (2), 2_49-2_58, 2001
日本水文科学会
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詳細情報 詳細情報について
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- CRID
- 1390564238060814976
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- NII論文ID
- 130007543099
- 10006388636
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- NII書誌ID
- AA11123427
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- ISSN
- 18837166
- 13429612
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- NDL書誌ID
- 5857440
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可
