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      암석의 종류와 방향에 따른 물리적 특성과 상호관계 = Char acter istics of Physical Pr oper ties of Rocks and Their Mutual Relations

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      https://www.riss.kr/link?id=A76139210

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      다국어 초록 (Multilingual Abstract)

      The main objectives of this study are to investigate the anisotropic characteristics of rocks and to evaluate the the relationships between physical properties. A series of experiments were performed in three mutually perpendicular directions for thre...

      The main objectives of this study are to investigate the anisotropic characteristics of rocks and to evaluate the the relationships between physical properties. A series of experiments were performed in three mutually perpendicular directions for three rock types, which are granite, granitic gneiss and limestone. The relationships of measured physical properties were evaluated. The results of ultrasonic wave velocity measurement show that granite of three rock types gives the largest directional difference, and that the wave velocity in a plane parallel to a transversely isotropic one is dominantly faster than that in a subvertical or vertical plane. It implies that ultrasonic wave velocity for rock could be used as a useful tool for estimating the degree of anisotropy. The ratio of uniaxial compressive strength to Brazilian tensile strength ranges approximately from 13 to 16 for granite, from 8 to 9 for granite gneiss, and from 9 to 18 for limestone. The directional differences for granite and granitic gneiss are very small, and on the other hand, is relatively large for limestone. It is suggested that strength of rock makes quite difference depending on the rock types and loading directions, especially for the anisotropic rocks such as transversely isotropic or orthotropic rocks. The ratio of uniaxial compressive strength to point load strength index ranges from 18 to 20 for granite, from 17 to 19 for granitic gneiss, and from 21 to 24 for limestone. These results show that point load strength index makes also a difference depending on rock types and directions. Therefore, it should be noted that the ratio of uniaxial compressive strength to point load strength index could be applied to all rock types. Uniaxial compressive strength shows relatively good relationship with point load strength index, Schmidt hammer rebound value, and tensile strength. In particulat, point load strength index is shown to be the best comparative relationship. It is indicated that point load test is the most useful tool to estimate an uniaxial compressive strength indirectly.

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      목차 (Table of Contents)

      • Abstract
      • 1. 서론
      • 2. 시료
      • 3. 실내 시험 방법
      • 4. 결과 및 해석
      • Abstract
      • 1. 서론
      • 2. 시료
      • 3. 실내 시험 방법
      • 4. 결과 및 해석
      • 5. 고찰
      • 6. 결론
      • 참고문헌
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      참고문헌 (Reference)

      1 송무영, "한반도 중부권 지각물질의 구조와 물성연구 퇴적암류 코아시료의 탄성파 속도와 점재하 강도 비교" 3 : 21-37, 1993

      2 김영환, "이방성 재료에서의 탄성파 전파 과정에 대한 시뮬레이션" 17 : 227-236, 1997

      3 박형동, "암석의 공학적 이방성 측정을 위한 실험실내 P파 속도 측정기법에 대한 연구" 5 : 237-247, 1995

      4 Osborne, "grain and hardway in some Rre-Cambrian granites" 540-551, 1965

      5 Postma, "Wave propagation in a stratified medium" 20 : 780-806, 1955

      6 Birch, "The velocity of compressional waves in rocks to 10 kilobars Journal of Geophysical Res." 66 : 2199-2224, 1961

      7 McWilliams, "The role of microstructure in the physical properties of rock Testing techniques for rock mechanics" 175-402 189, 1966

      8 Soga, "The effect of dilatancy on velocity anisotropy in Westerly granite" 4451-4458, 1978

      9 "Suggested methods for determining point load strength Int. J. of Rock Mech. and Min. Sci & Geomechanics Abstracts" 22 : 51-60, 1985

      10 "Suggested methods for determining hardness of rocks Int. Jour. of Rock Mech. and Min. Sci. & Geomech. Abstr." 15 : 89-97, 1987

      1 송무영, "한반도 중부권 지각물질의 구조와 물성연구 퇴적암류 코아시료의 탄성파 속도와 점재하 강도 비교" 3 : 21-37, 1993

      2 김영환, "이방성 재료에서의 탄성파 전파 과정에 대한 시뮬레이션" 17 : 227-236, 1997

      3 박형동, "암석의 공학적 이방성 측정을 위한 실험실내 P파 속도 측정기법에 대한 연구" 5 : 237-247, 1995

      4 Osborne, "grain and hardway in some Rre-Cambrian granites" 540-551, 1965

      5 Postma, "Wave propagation in a stratified medium" 20 : 780-806, 1955

      6 Birch, "The velocity of compressional waves in rocks to 10 kilobars Journal of Geophysical Res." 66 : 2199-2224, 1961

      7 McWilliams, "The role of microstructure in the physical properties of rock Testing techniques for rock mechanics" 175-402 189, 1966

      8 Soga, "The effect of dilatancy on velocity anisotropy in Westerly granite" 4451-4458, 1978

      9 "Suggested methods for determining point load strength Int. J. of Rock Mech. and Min. Sci & Geomechanics Abstracts" 22 : 51-60, 1985

      10 "Suggested methods for determining hardness of rocks Int. Jour. of Rock Mech. and Min. Sci. & Geomech. Abstr." 15 : 89-97, 1987

      11 "Suggested method for rock characterization testing and monitoring" Pergamon Press. 1981

      12 Peng, "Stress analysis of cylindrical rock discs subjected th axial double point-load" 97-101, 1976

      13 Brace, "Relation of elastic properties of rocks th fabric" 70 : 5657-5667, 1965

      14 McCabe, "High Pressure shear strength of anisotropic micaschist rock" 219-228, 1975

      15 King, M.S.,, "Experimental ultrasonic velocities and permeability for sandstones with aligned cracks" 32.2 : 155- 163, 1995

      16 Kahraman, S.,, "Evaluation of simple methods for assessing the uniaxial compressive strength of rock" 38. : 981--994., 2001

      17 R. Mcgonigle, "Estimating crack prameters from observations of P-wave velocity anisotropy" 45 : 345-360, 1980

      18 Anderson, "Estimating crack parameter from observations of P-wave velocity anisotropy" 45 : 345-360, 1980

      19 Deere, "Engineering classification and index properties for intact rock" 300-, 1966

      20 T, "Engineering behaviour of phyllites" 33 : 209-225, 1993

      21 Judd, "Correlation of rock properties by statistical method" 1961

      22 Douglass, "Anisotropy of granites A reflection of microscopic fabric" 376-389, 1969

      23 E.Z, "Anisotropic of a schistose gneiss" 1. 465-470. : 1966

      24 Teufel, "Acoustic Emissions during Anelastic Strain Recovery of Cores Form Deep Boreholes 30th U.S. Symp. on Rock Mech." 269-276, 1989

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      2026 평가예정 재인증평가 신청대상 (재인증)
      2020-01-01 평가 등재학술지 유지 (재인증) KCI등재
      2019-08-21 학회명변경 영문명 : Korean Society for Rock Mechanics -> Korean Society for Rock Mechanics and Rock Engineering KCI등재
      2017-01-01 평가 등재학술지 유지 (계속평가) KCI등재
      2013-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2010-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2008-05-07 학회명변경 영문명 : Korean Society For Rock Mechanics -> Korean Society for Rock Mechanics KCI등재
      2008-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2006-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2003-01-01 평가 등재학술지 선정 (등재후보2차) KCI등재
      2002-01-01 평가 등재후보 1차 PASS (등재후보1차) KCI등재후보
      2000-07-01 평가 등재후보학술지 선정 (신규평가) KCI등재후보
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      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.47 0.47 0.41
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.37 0.36 0.547 0.3
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