암반대수층 내 순간충격시험 시 관찰된 요동반응의 해석

Analysis of oscillatory responses of slug tests in a crystalline rock aquifer

  • 류일호 (한국원자력연구원 방사성폐기물기술개발부) ;
  • 지성훈 (한국원자력연구원 방사성폐기물기술개발부) ;
  • 고용권 (한국원자력연구원 방사성폐기물기술개발부)
  • 발행 : 2009.08.31

초록

순간충격시험은 대수층의 수리특성을 빠르고 효과적으로 측정할 수 있는 가장 일반적인 방법이다. 한국원 자력연구원(KAERI) 부지 내 YS-4 시추공에서 부지의 수리특성을 알아보기 위하여 순간충격시험을 수행하였고, 그 결과 일반적인 수리반응과 다른 요동수리반응을 관찰하였다. 이 반응결과를 일반적인 해석방법과 시추공내 유체의 관성 영향을 고려한 해석방법으로 해석하여 각각 비교하였다. 그 결과 일반적인 해석 방법으로는 수리전도도가 $3.10{\times}10^{-6}{\sim}3.63{\times}10^{-5}$ m/sec로 예측되어 해석결과의 차이가 크게 나타났지만, 유체의 관성효과를 고려하였을 때는 $4.85{\times}10^{-6}{\sim}5.44{\times}10^{-6}$ m/sec로 그 해석결과가 거의 비슷하였다. 이는 순간충격시험 시 요동수리 반응은 반드시 공내 유체의 관성 효과를 고려하여 해석하여야 함을 보여준다.

Slug test is a common characterization method that estimates aquifer hydraulic conductivity rapidly and economically. To characterize the hydraulic property near the borehole YS-4 in the Korea Atomic Energy Research Institute (KAERI) site, slug tests were performed, and oscillatory hydraulic responses were observed. We analyzed the observations with the modified Hvorslev and Bouwer&Rice methods considering the casing inertia, and then the results were compared with those from the general Hvorslev and Bouwer&Rice methods. The estimated hydraulic conductivities from the modified methods are ranged from $4.85{\times}10^{-6}$ to $5.44{\times}10^{-6}$ m/sec, but those from the general ones are ranged from $3.10{\times}10^{-6}$ to $3.63{\times}10^{-5}$ m/s, which shows that the oscillatory responses should be analyzed with consideration of the flowing water inertia effect.

키워드

참고문헌

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