砂防学会誌
Online ISSN : 2187-4654
Print ISSN : 0286-8385
ISSN-L : 0286-8385
揖斐川上流の地質の異なる流域における流出の遅れ時間の違い
加藤 祐子恩田 裕一水山 高久小杉 賢一朗吉川 愛辻村 真貴秦 耕二岡本 正男
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2000 年 53 巻 4 号 p. 38-43

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Rainfall and runoff were monitored in 10 th small catchments underlain by Granitic rock basins and Mesozoic sedimentary rock basins upstream of Ibi River in Gifu Prefecture. Following findings were obtained (1) Runoff peak response time (it's time lag) is longer in Mesozoic sedimentary rock basins than in Granitic rock basins. (2) Large changed runoff duration curve were obtained only in P 1 and P 2 catchments of Mesozoic sedimentary rock basins. Runoff characteristics of Granitic rock basins are one pattern, but these of Mesozoic sedimentary rock basins are two patterns. This suggests that Granitic rock basins are enough to obtain one basin, but Mesozoic sedimentary rock basins are not enough to do it.

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