The theoreitical improvement and development of circulation flow test.

碩士 === 國立中央大學 === 應用地質研究所 === 92 === Single-well tests are less expensive than multiple well tests in hydrogeologic investigation. Single-well tests also withdraw limited amount of water and hence are suitable for contamination sites. The dipole flow test (DFT) is a single-well circulation flow test...

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Main Authors: Kung-Lin Lee, 李岡林
Other Authors: Chia-Shyun Chen
Format: Others
Language:zh-TW
Published: 2004
Online Access:http://ndltd.ncl.edu.tw/handle/75093472864410315246
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spelling ndltd-TW-092NCU055030102015-10-13T13:04:44Z http://ndltd.ncl.edu.tw/handle/75093472864410315246 The theoreitical improvement and development of circulation flow test. 單井循環流水力實驗之理論改進與發展 Kung-Lin Lee 李岡林 碩士 國立中央大學 應用地質研究所 92 Single-well tests are less expensive than multiple well tests in hydrogeologic investigation. Single-well tests also withdraw limited amount of water and hence are suitable for contamination sites. The dipole flow test (DFT) is a single-well circulation flow test (CFT), which generates a circulation flow field in the aquifer by pumping water in the upper well screen section using a constant flow rate +Q and discharging the pumped water through the lower well screen section in -Q. In theory, DFT is able to estimate the horizontal hydraulic conductivity (Kr), the vertical hydraulic conductivity (Kz), and the storage coefficient (S).However, field experiments of DFT under different hydorgeological conditions showed that DFTs reached steady state rapidly, unfavorable for the estimation of Kz and S. This study improves the design of DFT, and develops the constant head circulation flow test (CHCFT), which generates a circulation flow field in the aquifer by pumping water in the upper well screen section using a positive constant head and discharging water through the lower well screen section using a constant negative head (drawdown). This constant-head condition renders CHCFT to reach steady state after a long period time, during which Kr, Kz, and S can be determined without difficulty. However, current constant drawdown pumping techniques can not discharge water continuously with a constant water level between 8 to 45 meters below ground surface, and makes the application of CHCFT limited. Hence we replace the constant drawdown pumping in CHCFT with a constant rate pumping which has less limitation on the drawdown level and develop another CFT model: constant rate – constant head circulation flow test (QHCFT). Due to two different pumping techniques are applied in two different screen sections, QHSCT reaches steady state after a long period as CHCFT, and Kr, Kz, and S can be determined without difficulty. When developing CHCFT and QHSCT, both confined and unconfined condition with skin effect are considered, and the type curve analysis is tested with hypothetical data for the determination of skin factor (Sk), Kr, Kz, and S. It is found if skin exists but its effect is neglected will result in a false determination of Kz and S. Chia-Shyun Chen 陳家洵 2004 學位論文 ; thesis 107 zh-TW
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description 碩士 === 國立中央大學 === 應用地質研究所 === 92 === Single-well tests are less expensive than multiple well tests in hydrogeologic investigation. Single-well tests also withdraw limited amount of water and hence are suitable for contamination sites. The dipole flow test (DFT) is a single-well circulation flow test (CFT), which generates a circulation flow field in the aquifer by pumping water in the upper well screen section using a constant flow rate +Q and discharging the pumped water through the lower well screen section in -Q. In theory, DFT is able to estimate the horizontal hydraulic conductivity (Kr), the vertical hydraulic conductivity (Kz), and the storage coefficient (S).However, field experiments of DFT under different hydorgeological conditions showed that DFTs reached steady state rapidly, unfavorable for the estimation of Kz and S. This study improves the design of DFT, and develops the constant head circulation flow test (CHCFT), which generates a circulation flow field in the aquifer by pumping water in the upper well screen section using a positive constant head and discharging water through the lower well screen section using a constant negative head (drawdown). This constant-head condition renders CHCFT to reach steady state after a long period time, during which Kr, Kz, and S can be determined without difficulty. However, current constant drawdown pumping techniques can not discharge water continuously with a constant water level between 8 to 45 meters below ground surface, and makes the application of CHCFT limited. Hence we replace the constant drawdown pumping in CHCFT with a constant rate pumping which has less limitation on the drawdown level and develop another CFT model: constant rate – constant head circulation flow test (QHCFT). Due to two different pumping techniques are applied in two different screen sections, QHSCT reaches steady state after a long period as CHCFT, and Kr, Kz, and S can be determined without difficulty. When developing CHCFT and QHSCT, both confined and unconfined condition with skin effect are considered, and the type curve analysis is tested with hypothetical data for the determination of skin factor (Sk), Kr, Kz, and S. It is found if skin exists but its effect is neglected will result in a false determination of Kz and S.
author2 Chia-Shyun Chen
author_facet Chia-Shyun Chen
Kung-Lin Lee
李岡林
author Kung-Lin Lee
李岡林
spellingShingle Kung-Lin Lee
李岡林
The theoreitical improvement and development of circulation flow test.
author_sort Kung-Lin Lee
title The theoreitical improvement and development of circulation flow test.
title_short The theoreitical improvement and development of circulation flow test.
title_full The theoreitical improvement and development of circulation flow test.
title_fullStr The theoreitical improvement and development of circulation flow test.
title_full_unstemmed The theoreitical improvement and development of circulation flow test.
title_sort theoreitical improvement and development of circulation flow test.
publishDate 2004
url http://ndltd.ncl.edu.tw/handle/75093472864410315246
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