• The Journal of Engineering Geology
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• v.11 no.1
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• pp.63-79
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• 2001

This study is aimed for estimating hydraulic parameters using the Cooper-Bredehoeft-Papadopulos, the Hvorslev, and the Bouwer & Rice methods at nineteen test holes in Me. Geumjeong area composed of Bulguksa granites, and for characterizing hydraulic properties at the test holes with relatioll to drill core data. The relation among hydraulic Dammeters obtained by the three methods is also considered. The study area is divided into four sub-areas to consider the hydraulic characteristics. The difference of hydraulic conductivity estimates between the injection and the withdrawal slug test may be due to penncable fracture distlibutions around the test hole and/or the disturbance of fine mateIials in the fractures induced by the pressure variation due to different mechanisms of test initiation. The hydraulic conductivity estimates detennined by the Cooper-Bredehoeft-Papadopulos, the Hvorslev and the Bouwer & Rice methods ranges from 10$^{-8}$ to lO$^{-5}$m/sec, and the ranges of average values are from 10$^{-7}$ to 10$^{-6}$m/sec. Also, the transmissivity ranges from 10$^{-7}$ to 10$^{-5}$$m^2$/sec. Comparing average hydraulic conductivity by the Cooper-Bredehoeft-Papadopulos, the Hvorslev and the Bouwer & Rice methods, by the Hvorslev method has the highest values, then the Bouwer & Rice method, and the Cooper-Bredehoeft-Papadopulos method has the lowest.

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 2002.09a
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• pp.378-381
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• 2002

금정산지역의 수리적인 특성을 파악하기 위하여 27개 지하수 공을 대상으로 순간충격시험(주입, 인양시험)을 실시하였다. 순간충격시험자료는 C-B-P법, Hvorslev법, Bouwer & Rice법을 이용하여 분석하였으며, 분석을 위해서는 AQTESOLV(Version 3.01) 소프트웨어를 이용하였다. 또한, 자료의 해석을 위해서 시추자료와 연관하여 해석하였으며, 이때 시추시 용출심도와 수리전도도와의 관련성 분석으로 dummy의 충격과 심도의 관련성을 고찰해 보았다. 순간충격시험 분석결과 얻어진 수리전도도는 7.69E-8 ~ 2.30E-5m/sec를 보인다.