The Study of Seepage on the Incline of Multilayer Soils
碩士 === 國立臺灣大學 === 農業工程學系 === 82 === The objective of this study is to discuss the behavior of on the incline of multilayer soils. Since it is difficult to the seepage point, the problem is analyzed theoretically appropriate boundary condition an...
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1994
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ndltd-TW-082NTU004040042016-07-18T04:09:33Z http://ndltd.ncl.edu.tw/handle/78303447556363438822 The Study of Seepage on the Incline of Multilayer Soils 坡地多層土壤滲流之研究 Lai,Shih-Pao 賴世寶 碩士 國立臺灣大學 農業工程學系 82 The objective of this study is to discuss the behavior of on the incline of multilayer soils. Since it is difficult to the seepage point, the problem is analyzed theoretically appropriate boundary condition and then the free surface estimated using Boussinesq equation. By simplifying the conditions in soil layers, the amount of seepage is calculated one- dimensional assumption. Theoretical and labortary study performed to analyze this problem. A sandbox experiment has conducted. The variation of head is measured at 48 measurement using manometer. Dye tracer is introduced to observe the and seepage point. Then the seepage flow equations are sectionally by one-dimensional assumption. Results show that possible to calculate the amount of seepage using assumption for the case of one or two layer aquifer system will have significant errors for three-layers soils. The of vertical flow has been observed in the laboratory experiment. Tan,Yih-Chi 譚義績 1994 學位論文 ; thesis 82 zh-TW |
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碩士 === 國立臺灣大學 === 農業工程學系 === 82 === The objective of this study is to discuss the behavior of on
the incline of multilayer soils. Since it is difficult to the
seepage point, the problem is analyzed theoretically
appropriate boundary condition and then the free surface
estimated using Boussinesq equation. By simplifying the
conditions in soil layers, the amount of seepage is calculated
one- dimensional assumption. Theoretical and labortary
study performed to analyze this problem. A sandbox
experiment has conducted. The variation of head is measured at
48 measurement using manometer. Dye tracer is introduced to
observe the and seepage point. Then the seepage flow
equations are sectionally by one-dimensional assumption.
Results show that possible to calculate the amount of
seepage using assumption for the case of one or two layer
aquifer system will have significant errors for three-layers
soils. The of vertical flow has been observed in the
laboratory experiment.
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author2 |
Tan,Yih-Chi |
author_facet |
Tan,Yih-Chi Lai,Shih-Pao 賴世寶 |
author |
Lai,Shih-Pao 賴世寶 |
spellingShingle |
Lai,Shih-Pao 賴世寶 The Study of Seepage on the Incline of Multilayer Soils |
author_sort |
Lai,Shih-Pao |
title |
The Study of Seepage on the Incline of Multilayer Soils |
title_short |
The Study of Seepage on the Incline of Multilayer Soils |
title_full |
The Study of Seepage on the Incline of Multilayer Soils |
title_fullStr |
The Study of Seepage on the Incline of Multilayer Soils |
title_full_unstemmed |
The Study of Seepage on the Incline of Multilayer Soils |
title_sort |
study of seepage on the incline of multilayer soils |
publishDate |
1994 |
url |
http://ndltd.ncl.edu.tw/handle/78303447556363438822 |
work_keys_str_mv |
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