The Study for the Effect of Hydrogeological Simulation by Using Geostatistical Methods

碩士 === 國立成功大學 === 資源工程學系碩博士班 === 97 === This study investigated the effects of the geostatistical simulator on the hydrogeology fields, two simulated techniques are applied: the indicator cross variogram function and transition probability function. The resulted connectivity of the flow field are e...

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Main Authors: Yuan Liu, 劉原
Other Authors: Kuo-Chin Hsu
Format: Others
Language:zh-TW
Published: 2009
Online Access:http://ndltd.ncl.edu.tw/handle/87092770724496917672
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spelling ndltd-TW-097NCKU53970652016-05-04T04:26:29Z http://ndltd.ncl.edu.tw/handle/87092770724496917672 The Study for the Effect of Hydrogeological Simulation by Using Geostatistical Methods 地質統計方法對水文地質場模擬影響之研究 Yuan Liu 劉原 碩士 國立成功大學 資源工程學系碩博士班 97 This study investigated the effects of the geostatistical simulator on the hydrogeology fields, two simulated techniques are applied: the indicator cross variogram function and transition probability function. The resulted connectivity of the flow field are explored. The study area is a contaminated site in Tainan. The major integral range in horizontal direction is about 272m and the minor integral range is 50m, the vertical integral range is 5m. Using the transition probability, the high hydraulic conductivity soil continued in horizontal direction is found to be 300m and the mean length is about 700m, while the low hydraulic conductivity soil continued in horizontal direction is 100m and the mean length is 120m, and the high hydraulic conductivity soil continued in vertical direction is 5m and the mean length is 3.7m, the low hydraulic conductivity soil continued in vertical direction is 3m and the mean length is 1.2m. The simulation resulting using the transition probability are found to be with a higher connectivity which may result in a faster transport path of contamination. Kuo-Chin Hsu 徐國錦 2009 學位論文 ; thesis 77 zh-TW
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description 碩士 === 國立成功大學 === 資源工程學系碩博士班 === 97 === This study investigated the effects of the geostatistical simulator on the hydrogeology fields, two simulated techniques are applied: the indicator cross variogram function and transition probability function. The resulted connectivity of the flow field are explored. The study area is a contaminated site in Tainan. The major integral range in horizontal direction is about 272m and the minor integral range is 50m, the vertical integral range is 5m. Using the transition probability, the high hydraulic conductivity soil continued in horizontal direction is found to be 300m and the mean length is about 700m, while the low hydraulic conductivity soil continued in horizontal direction is 100m and the mean length is 120m, and the high hydraulic conductivity soil continued in vertical direction is 5m and the mean length is 3.7m, the low hydraulic conductivity soil continued in vertical direction is 3m and the mean length is 1.2m. The simulation resulting using the transition probability are found to be with a higher connectivity which may result in a faster transport path of contamination.
author2 Kuo-Chin Hsu
author_facet Kuo-Chin Hsu
Yuan Liu
劉原
author Yuan Liu
劉原
spellingShingle Yuan Liu
劉原
The Study for the Effect of Hydrogeological Simulation by Using Geostatistical Methods
author_sort Yuan Liu
title The Study for the Effect of Hydrogeological Simulation by Using Geostatistical Methods
title_short The Study for the Effect of Hydrogeological Simulation by Using Geostatistical Methods
title_full The Study for the Effect of Hydrogeological Simulation by Using Geostatistical Methods
title_fullStr The Study for the Effect of Hydrogeological Simulation by Using Geostatistical Methods
title_full_unstemmed The Study for the Effect of Hydrogeological Simulation by Using Geostatistical Methods
title_sort study for the effect of hydrogeological simulation by using geostatistical methods
publishDate 2009
url http://ndltd.ncl.edu.tw/handle/87092770724496917672
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