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砂防学会誌,Vol.55,No.3,p.3-11,2002
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沖縄島の圃場地表面に形成される過飽和層での赤土砂侵食機構
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Red soil erosion at the over‐saturated layer formed at the Pineapple field surface in Okinawa
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論文
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南 哲 行* 仲 野 公 章** 山 田 孝***
Noriyuki MINAMI, Masaaki NAKANO, Takashi YAMADA
下 村 幸 男**** 小 野 寺 勝*****
Sachio SHIMOMURA, Masaru ONODERA
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Abstract
In Okinawa, red soil erosion and its sedimentation in reef areas have caused serious environmental problems. The major sources of red sediment are pineapple fields which consist mainly of cohesive soil. When the surface of a pineapple field is saturated by rainfall, the soil surface swells and forms an over‐saturated layer. The authors carried out soil tests and hydrological experiments to evaluate the over‐saturated layer strength using a two‐dimensional flume and the ground‐erosion resistance tester developed by the Public Works Research Institute, Ministry of Construction in1992.
The following conclusions were drawn from this study.
1) According to artificial rainfall and submersion testing with field red soil obtained on the site, an over‐saturated layer with apparent degree of saturation over100% forms at a depth of about5mm from the surface of the specimen within30minutes.
2) The shear strength of the over‐saturated layer falls in inverse proportion to the rise in the moisture content. The shear strength of the over‐saturated layer and that of the non over‐saturated layer (apparent degree of saturation of100% or less) are1kPa (10gf/cm2) and0.51kPa (5gf/cm2) respectively.
3) A ground‐erosion resistance test showed that when the rotation rate exceeds10to20rpm, the erosion rate of the saturated layer increases proportionally to the rotation rate, and if the viscosity falls, the erosion rate tends to rise.
4) The critical tractive force of the over‐saturated layer was calculated as approximately0.65Pa. This value corresponds to the critical tractive force of the thin sheet flow produced by the critical rainfall intensity of10mm/h, and is close to the red soil runoff critical rainfall that has been measured by field observations.
Key words:red soil erosion, over‐saturated layer, thin sheet flow, critical tractive force
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砂防学会誌 Vol.55 No.3(242)September 2002
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