지질공학 (The Journal of Engineering Geology)

  • 제12권4호
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  • Pages.405-419
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  • 2002
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  • 1226-5268(pISSN)
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  • 2287-7169(eISSN)
대한지질공학회 (The Korean Society of Engineering Geology)
권호 표지

콘포컬 레이저 현미경을 이용한 불연속면의 거칠기 측정 연구

A Study of Roughness Measurement of Rock Discontinuities Using a Confocal Laser Scanning Microscope

  • 발행 : 2002.12.01
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초록

새롭게 개발된 레이저 콘포컬 현미경을 이용해 암석 불연속면의 거칠기를 측정하였다. 레이저의 파장은 488 nm이며, 현미경은 두 개의 galvano-meter scanner mirror를 이용한 광 편광법에 의해 제어된다. 레이저 반사를 통한 자동 초점기능은 관찰대상을 빠르고 정확하게 측정할 수 있다. 이 현미경은 기존의 다른 콘포컬 현미경에 비해 광축방향의 해상도를 크게 개선하였고, 특수 제작한 현미경 스테이지를 이용해 최대 $10{\;}{\times}{\;}10{\;}cm$ 까지 크기의 시료를 측정할 수 있다. 측정간격은 x와 y 방향으로 $2.5{\;}\mu\textrm{m}$씩이며, z방향의 최대 측정해상도는 $10{\;}\mu\textrm{m}$로서, 다른 방범에 비해 훨씬 정확하다. 조립질과 세립질의 입도가 다른 화강암을 대상으로 인장시험(Brazilian test)를 통해 인공절리를 생성시켰고, 생성된 좌우의 절리면에 각각 3개씩의 측선을 설정하였다. 각 측선을 따라 측정한 높이는 1차원은 물론 거칠기의 세밀한 양상을 보여주는 2차원과 3차원의 디지털 이미지로 표현된다. 조립질 화강암의 1차원 단면은 세립질보다 불연속면의 기복이 더 심함을 잘 보여준다. 거칠기를 정량적으로 특성화하고 거칠기를 구성하는 성분 중 가장 큰 영향을 미치는 성분을 파악하기 위해 고속퓨리에 변환 (FFT)를 이용한 스펙트럼 분석을 실시하였다. 스펙트럼 분석결과 저주파 성분이 큰 시효의 경우 거칠기의 기복변화가 심하고 긴 파장을 나타내는 경향이 있음을 구명하였다.

Fracture roughness of rock specimens is observed by a new confocal laser scanning microscope (CLSM; Olympus OLS1100). The wave length of laser is 488 nm, and the laser scanning is managed by a light polarization method using two galvano-meter scanner mirrors. The function of laser reflection auto-focusing enables us to measure line data fast and precisely. The system improves resolution in the light axis (namely z) direction because of the confocal optics. Using the CLSM, it is Possible to measure a specimen of the size up to $10{\;}{\times}{\;}10{\;}cm$ which is fixed on a specially designed stage. A sampling is managed in a spacing $2.5{\;}\mu\textrm{m}$ along x and y directions. The highest measurement resolution of z direction is $10{\;}\mu\textrm{m}$, which is more accurate than other methods. Core specimens of coarse and fine grained granite are provided. Fractures are artificially maneuvered by a Brazilian test method. Measurements are performed along three scan lines on each fracture surface. The measured data are represented as 2-D and 3-D digital images showing detailed features of roughness. Line profiles of the coarse granites represent more frequent change of undulation than those of the fine granite. Spectral analyses by the fast Fourier transform (FFT) are performed to characterize the roughness data quantitatively and to identify influential frequency of roughness. The FFT results suggest that a specimen loaded by large and low frequency energy tends to have high values of undulation change and large wave length of fracture roughness.

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