A Study of a Three Phases Structure and the Mechanical Properties of Partly Saturated Soil
A Study of a Three Phases Structure and the Mechanical Properties of Partly Saturated Soil
批准号:
60550347
负责人:
UNO Takao
金额:
$1.22万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for General Scientific Research (C)
财政年份:
1985
资助国家:
日本
项目状态:
已结题
起止时间:
1985 至 1987
中文摘要
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英文摘要
A study of a three phases structure of partly saturated soil is necessary to make clear its mechanical properties. First experimental study is conducted in triaxial compression test using silt specimen, and second the behavior of pore air/water pressure generated by external load or fluid pressure is investigated analytically as well as experimentally. Main results obtained from the present study are as follows.(1) Examination of state variables measurement of partly saturated soil in triaxial apparatus is important to describe its mechanical properties.(2) Negative pore water pressure measured by suction plate method is adequate for all range of degree of saturation.(3) The observed relationship among volume strain, pore air pressure and all round external pressure in triaxial test on silt can be explained by the two phases mixture ( air and soil skelton ) theory if soil sample is below the thirty percent of degree of saturation.(4) Two dimensional particulate model is formulated in the assembly of rod particle with equal diameter and examined to describe the structure and its properties( void ratio, number of contact point, mean diameter of pore space and so on ) in the experiment of uniform sand.(5) Darcy's law can be applied to air flow through partly saturated soil underlow pressure. The coefficient of air flow through soil varies with degree of saturation, and it vanishes to zero about over sixty percent.(6) Pore air/water pressure generated in partly saturated soil is investigatedunder the sample of sand column with different degree of saturation in some conditions of dewatering and/or air intrusion. As a result, it is shown in both analysis and experiment that soil water moves, being caused by air pressure fluctuation.
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宇野尚雄: 第21回土質工学研究発表会講演集. 2の1. 187-188 (1986)
Nao Uno:第 21 届土壤工程研究会议论文集,187-188(1986)。
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作者:
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通讯作者:
宇野尚雄: Natural Disaster Science. Vol.8No.1. (1987)
宇野奈央:自然灾害科学。第 8 卷第 1 期(1987 年)。
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宇野尚雄: 土質工学会「不飽和土の工学的性質研究の現状シンポジウム」発表論文集. 229-236 (1987)
Nao Uno:日本土壤工程学会会议记录,“非饱和土工程特性研究现状研讨会”,229-236 (1987)
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作者:
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通讯作者:
Uno Takao: "An Experimental Study on Air Flow Through Sandy Soils," Proc. of Symposium on the Research for Engineering Properties of Unsaturated Soils, Japanese Society of SMFE.,. 229-236 (1987)
Uno Takao:“通过沙土的气流的实验研究”,Proc。
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Uno Takao: "Soil-Water Retention Characteristics of Several Sandy Soils," Proc. of Symposium on the Research for Engineering Properties of Unsaturated Soils, Japanese Society of SMFE.,. 187-192 (1987)
Uno Takao:“几种沙质土壤的水土保持特性”,Proc。
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共 16 条
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