Journal of the Agricultural Engineering Society, Japan
Online ISSN : 1884-7218
ISSN-L : 1884-7218
Volume 32, Issue 5
Displaying 1-6 of 6 articles from this issue
  • [in Japanese], [in Japanese]
    1965 Volume 32 Issue 5 Pages 247-257_2
    Published: January 20, 1965
    Released on J-STAGE: March 09, 2011
    JOURNAL FREE ACCESS
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  • [in Japanese]
    1965 Volume 32 Issue 5 Pages 257-263
    Published: January 20, 1965
    Released on J-STAGE: March 09, 2011
    JOURNAL FREE ACCESS
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  • Comparison with Hydraulic Calculation at the Site of Project II in the Southern Part of the Hachirogata Lagoon, Tohoku District.
    Ryo KANBKO, Shoichiro NAKAGAWA, Toshisuke MARUYAMA
    1965 Volume 32 Issue 5 Pages 265-269
    Published: January 20, 1965
    Released on J-STAGE: March 09, 2011
    JOURNAL FREE ACCESS
    The amount of seepage water under the levee was obtained by means of water balance and hydraulic calculation methods, and the two results were compared. As an example, investigation was carried out at the site of Project II, newly reclaimed area located in the southern part of the Hachirogata Lagoon, Tohoku District, Japan. It is 187 ha in area and consists of sandy soil. The reclaimed land is usually surrounded by outside water level which is higher than inside water level.
    Water balance in such case of swampy lowland is generally expressed by the following equation :
    P= (D2-D1) +E-G1S
    Where, P : precipitation, D1; inflow of surface water, D2 : amount of water pumped out, E : evapotranspiration, G1 : amount of seepage water under the levee, ΔS : amount of change in water valume.
    During the non-irrigation period, the inflow of surface water (D1) equals zero. P, E and D2 can be obtained by measurement and pump operation records. ΔS can be obtained from the change of ground-water level. The amount of seepage water under the levee (G1), therefore, can be obtained indirectly by using the above equation. During the irrigation period, G1 is presumed by taking in account the difference between the inside and outside water levels of the levee, basing on G1 in non-irrigation period. G1 in this period can be checked from the above equation by substituting D1 obtained by measuring the water duty per unit area.
    On the other hand, G1 is obtained by hydraulic calculation. The value of G1 in this method was confirmed to accord with that in the water balance method. In the case of hydraulic calculation, however, the permeability coefficient is obtained by using G1 in the water balance method.
    The estimation of the amount of seepage water under the levee is very difficult. In the planning of drainage for swampy lowlands and reclaimed lands, however, it is required to estimate the amount of seepage water under the levee. From the above result, it is proved that the method in which the water balance and hydraulic calculation methods are combined can be usefully employed in that case.
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  • [in Japanese]
    1965 Volume 32 Issue 5 Pages 270
    Published: January 20, 1965
    Released on J-STAGE: March 09, 2011
    JOURNAL FREE ACCESS
    Download PDF (254K)
  • [in Japanese]
    1965 Volume 32 Issue 5 Pages 273
    Published: January 20, 1965
    Released on J-STAGE: March 09, 2011
    JOURNAL FREE ACCESS
    Download PDF (258K)
  • 1965 Volume 32 Issue 5 Pages 301
    Published: 1965
    Released on J-STAGE: March 09, 2011
    JOURNAL FREE ACCESS
    Download PDF (108K)
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