Determining free surface from potential and streamline plane

碩士 === 國立臺灣大學 === 土木工程學研究所 === 89 === This paper studies the problem of seepage through an earth dam and is intended to determine the location of free surface. The free surface is defined at where the pore water pressure equals to zero. Effects of the capillary fringe may be obtained by using field...

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Main Authors: Ruei Cheng Kuo, 郭瑞成
Other Authors: T.K. Tsay
Format: Others
Language:zh-TW
Published: 2001
Online Access:http://ndltd.ncl.edu.tw/handle/16667639534094993061
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spelling ndltd-TW-089NTU000151232016-07-04T04:17:53Z http://ndltd.ncl.edu.tw/handle/16667639534094993061 Determining free surface from potential and streamline plane 由勢線與流線平面反向推求土石壩之穩態自由水面 Ruei Cheng Kuo 郭瑞成 碩士 國立臺灣大學 土木工程學研究所 89 This paper studies the problem of seepage through an earth dam and is intended to determine the location of free surface. The free surface is defined at where the pore water pressure equals to zero. Effects of the capillary fringe may be obtained by using field formula depending on properties of soil. In this paper, numerical procedures are established to calculate the free surface distribution by applying the relation between physical plane and potential and streamline plane. This model has an advantage of avoiding tedious iterations in quasi-steady scheme, and therefore is more efficient. From numerical solutions, the seepage face due to capillary effects may be easily identified. After defining the free surface distribution, this model could further determine velocity field and flow rate within an earth dam. Present model is employed to simulate an anisotropic dam and an earth dam with a drained layer to demonstrate its flexible application capabilities. T.K. Tsay 蔡丁貴 2001 學位論文 ; thesis 62 zh-TW
collection NDLTD
language zh-TW
format Others
sources NDLTD
description 碩士 === 國立臺灣大學 === 土木工程學研究所 === 89 === This paper studies the problem of seepage through an earth dam and is intended to determine the location of free surface. The free surface is defined at where the pore water pressure equals to zero. Effects of the capillary fringe may be obtained by using field formula depending on properties of soil. In this paper, numerical procedures are established to calculate the free surface distribution by applying the relation between physical plane and potential and streamline plane. This model has an advantage of avoiding tedious iterations in quasi-steady scheme, and therefore is more efficient. From numerical solutions, the seepage face due to capillary effects may be easily identified. After defining the free surface distribution, this model could further determine velocity field and flow rate within an earth dam. Present model is employed to simulate an anisotropic dam and an earth dam with a drained layer to demonstrate its flexible application capabilities.
author2 T.K. Tsay
author_facet T.K. Tsay
Ruei Cheng Kuo
郭瑞成
author Ruei Cheng Kuo
郭瑞成
spellingShingle Ruei Cheng Kuo
郭瑞成
Determining free surface from potential and streamline plane
author_sort Ruei Cheng Kuo
title Determining free surface from potential and streamline plane
title_short Determining free surface from potential and streamline plane
title_full Determining free surface from potential and streamline plane
title_fullStr Determining free surface from potential and streamline plane
title_full_unstemmed Determining free surface from potential and streamline plane
title_sort determining free surface from potential and streamline plane
publishDate 2001
url http://ndltd.ncl.edu.tw/handle/16667639534094993061
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AT guōruìchéng yóushìxiànyǔliúxiànpíngmiànfǎnxiàngtuīqiútǔshíbàzhīwěntàizìyóushuǐmiàn
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