| Project/Area Number |
61560260
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| Research Category |
Grant-in-Aid for General Scientific Research (C)
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| Allocation Type | Single-year Grants |
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| Research Field |
農業土木
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| Research Institution | Gifu University |
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Principal Investigator |
NISHIDE Tsutomu (1987-1988) Gifu University prof, 農学部, 教授 (80021690)
足立 忠司 (1986) 岐大, 農学部, 助教授 (20012007)
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| Co-Investigator(Kenkyū-buntansha) |
HARA Tetsuo Gifu University assistant prof, 農学部, 助教授 (50021720)
SENGE Masateru Gifu University lecturer, 農学部, 講師 (00144006)
ADACHI Tadashi Okayama University prof, 農学部, 教授 (20012007)
西出 勤 岐阜大学, 農学部, 教授 (80021690)
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| Project Period (FY) |
1986 – 1988
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| Project Status |
Completed (Fiscal Year 1988)
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| Budget Amount *help |
¥2,300,000 (Direct Cost: ¥2,300,000)
Fiscal Year 1988: ¥500,000 (Direct Cost: ¥500,000)
Fiscal Year 1987: ¥500,000 (Direct Cost: ¥500,000)
Fiscal Year 1986: ¥1,300,000 (Direct Cost: ¥1,300,000)
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| Keywords | surface irrigation / avaliable rainfall / irrigation efficiency / surface runoff / rotational paddy field / simulation / 排水量 / 地表灌漑 / 灌漑効率 / 田畑輪換 / 流出モデル / 単位排水量 / ピーク流出係数 / 降雨強度 / 雑草調節機能 |
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| Research Abstract |
The study is made up of two sections which are undermentioned.
(1) On the problems of the water requirment of rotational paddy fields. At first on the problem of water requirment of rotational paddy fields, effective soil layer of rotational paddy field, soil moisture extraction pattern, amount of each irrigation and soil moisture content when plant had to be irrigated were examined. Consequently, for the existence of plowsole effective soil layer of rotational paddy field is shallow and soil moisture extraction pattern becomes shallow layer extraction pattern. For the reason it became clear that value of total readily available moisture became small, and interval of irrigation became short and the number of times of irrigation became large. And when plants are cultiwated in the rotational paddy field, it is necessary that soil moisture is wet when plants are irrigated.
(2) On the problems of the drainage of rotational paddy fields. In oder to predict the surface drainage discharge of a rotational paddy field, we proposed the runoff simulation model, which was composed of the eqeations of water balance and motion in ridge soil and furrow space. And by applying it to the observed runoff data of test fields, the value of the model parameters was able to be identifiedand the relation between the value of the parameters and soil permeability of test fields was examined. Furthermore, as a result of simulation by this model, the runoff coefficients of a design rainfall was able to be obtained.
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