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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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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zh-TW |
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Others
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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 |
work_keys_str_mv |
AT liujianhung studyonthefencediagramofaquiferbyusingtransmissivity AT liújiànhóng studyonthefencediagramofaquiferbyusingtransmissivity AT liujianhung yóuliútōngxìshùtàntǎohánshuǐcéngzhīshānzhuàngtú AT liújiànhóng yóuliútōngxìshùtàntǎohánshuǐcéngzhīshānzhuàngtú |
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1718352420181901312 |