Study on the Fence Diagram of Aquifer by using Transmissivity

碩士 === 國立臺灣大學 === 農業工程學系 === 82 === The information of groundwater is often limited of economic, technique , and the object on the surface in groundwater study . It's only obtained in the specific location . To the complex stratum stru...

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Main Authors: Liu,Jian-Hung, 劉建宏
Other Authors: Lin,Chun-Nan
Format: Others
Language:zh-TW
Published: 1994
Online Access:http://ndltd.ncl.edu.tw/handle/54060890065641349314
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spelling ndltd-TW-082NTU004040242016-07-18T04:09:33Z http://ndltd.ncl.edu.tw/handle/54060890065641349314 Study on the Fence Diagram of Aquifer by using Transmissivity 由流通係數探討含水層之柵狀圖 Liu,Jian-Hung 劉建宏 碩士 國立臺灣大學 農業工程學系 82 The information of groundwater is often limited of economic, technique , and the object on the surface in groundwater study . It's only obtained in the specific location . To the complex stratum structure , it can be obtained by the comparison of lag diagram and the information of geophysical method . There is a good relation between hydrogeologic parameters and the forming of stratum structure . It is expected that the fence diagram of aquifer can offer efficient information of stratum in this study. And it can be available to groundweater resource in planning , using , management and protecting . The results appear that : (1) There are two different geologic areas in two side of the Cho-Shui River. (2) There exists a good collection of stratum profile in Yun - Lin area. (3) There are four different geologic areas between Szhu-Malu and the coast. (4) There exist a borderline between Dilu-Tuku and Linnei at Hulai. (5) Because the information is deficiency in Chang - Hwa area, it's a hard to form a good stratum.But it shows different geologic forms in this area. Lin,Chun-Nan 林俊男 1994 學位論文 ; thesis 83 zh-TW
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language zh-TW
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sources NDLTD
description 碩士 === 國立臺灣大學 === 農業工程學系 === 82 === The information of groundwater is often limited of economic, technique , and the object on the surface in groundwater study . It's only obtained in the specific location . To the complex stratum structure , it can be obtained by the comparison of lag diagram and the information of geophysical method . There is a good relation between hydrogeologic parameters and the forming of stratum structure . It is expected that the fence diagram of aquifer can offer efficient information of stratum in this study. And it can be available to groundweater resource in planning , using , management and protecting . The results appear that : (1) There are two different geologic areas in two side of the Cho-Shui River. (2) There exists a good collection of stratum profile in Yun - Lin area. (3) There are four different geologic areas between Szhu-Malu and the coast. (4) There exist a borderline between Dilu-Tuku and Linnei at Hulai. (5) Because the information is deficiency in Chang - Hwa area, it's a hard to form a good stratum.But it shows different geologic forms in this area.
author2 Lin,Chun-Nan
author_facet Lin,Chun-Nan
Liu,Jian-Hung
劉建宏
author Liu,Jian-Hung
劉建宏
spellingShingle Liu,Jian-Hung
劉建宏
Study on the Fence Diagram of Aquifer by using Transmissivity
author_sort Liu,Jian-Hung
title Study on the Fence Diagram of Aquifer by using Transmissivity
title_short Study on the Fence Diagram of Aquifer by using Transmissivity
title_full Study on the Fence Diagram of Aquifer by using Transmissivity
title_fullStr Study on the Fence Diagram of Aquifer by using Transmissivity
title_full_unstemmed Study on the Fence Diagram of Aquifer by using Transmissivity
title_sort study on the fence diagram of aquifer by using transmissivity
publishDate 1994
url http://ndltd.ncl.edu.tw/handle/54060890065641349314
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