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Physical and Mechanical Characteristics of the Antarctic Rocks Exposed to the Extreme Environment

극한환경에 노출된 남극 암석의 물리적·역학적 특성

  • Received : 2012.07.06
  • Accepted : 2012.09.03
  • Published : 2012.11.15

Abstract

The Antarctic continent exposed to strong wind, very low temperature, and extremely dry condition. The freezing-thawing cycles under this extreme environment change the mechanical characteristics of rocks near the ground surface. To investigate the effect of freezing-thawing cycles under the extreme environment understand on geotechnical properties of rocks, rocks from the Antarctica were collected from two places: (1) West Antarctic Cape Burks and (2) East Antarctic Terra Nova Bay areas. The rock characteristics of these two areas were described and compared. For Terra Nova Bay area, rock characteristics of rocks near the surface and depths exceeding 2.9 m were examined. The 'near-the-surface rocks' averages of absorption rate, P-wave velocity, and unconfined compressive strength were 0.56%, 3,717 m/s, and 109MPa, respectively; while, those values of 'deep-sited rocks' were 0.24%, 4,670 m/s, and 88MPa. From the measurements, it was found that the effects of weathering were not significant on mechanical characteristics (strength) but were pronounced on physical characteristics(absorption and P-wave velocity).

남극대륙은 바람이 강하며 지구상에서 가장 기온이 낮고 건조한 극한환경 조건으로서 지표면의 암석은 동결-융해에 의해 암석의 역학적 특성이 변해왔다. 극지 암석의 지반공학적 특성을 이해하기 위하여 남극에서 직접 암석을 채취하여 암석의 물리적 역학적 특성을 분석하였다. 서남극 케이프 벅스 및 동남극 테라노바 만의 암석은 국내 편마암이 보이는 대표적인 물성 값의 범위내에 존재하고 있었으며, 케이프 벅스의 노출된 암석이 테라노바 만에 비하여 암반 강도가 큰 것으로 나타났다. 테라노바 만의 지표에 노출된 암석의 평균 흡수율은 0.56%, 평균 P파 속도는 3,717m/s, 일축압축 강도는 109MPa로 측정되었으며, 시추조사로부터 채취한 심도 2.9m 이상의 암석 평균 흡수율은 0.24%, 평균 P파 속도는 4,670m/s, 일축압축 강도는 88MPa로 측정되었다. 테라노바 만의 지표면에 노출된 암석과 심부에서 채취한 암석을 비교한 결과, 노출된 암석은 동결-융해의 영향으로 판단되는 역학적 특성 변화는 나타나지 않았으나 흡수율-P파 속도 변화의 물리적 특성 변화는 잘 나타났다.

Keywords

References

  1. 류성훈, 송재준(2010) 극지 암석의 역학적 특성 분석에 관한 연구 동향, 터널과 지하공간, 한국암반공학회지, 한국암반공학회, Vol. 20, No. 4, pp. 241-251.
  2. 백환조, 곽진철(2000) 풍화에 의한 국내 편마암체의 지질공학적 물성의 변화, 한국자원공학회지, 한국자원공학회, 제37권, pp. 262-271.
  3. 윤지선(1991) 암석.암반의 조사와 시험, 구미서관, p. 671.
  4. 이방용(1991) 남극의 자연환경 고찰, Ocean Research, Vol. 13, No. 1, pp. 51-69.
  5. 장현식, 장보안, 이준성(2004) 강원도 횡성군 풍암분지 백악기 셰일의 동결-융해에 따른 지질공학적 특성 변화, The Journal of Engineering Geology, Vol. 14, No. 4, pp. 401-416.
  6. 한국건설기술연구원(2010) 남극 제2기지의 건설후부지 적합성 평가 및 친환경 건설기본 계획 구축, p. 326.
  7. 한원준(2004) 한국 화성암 및 변성암의 물리적, 역학적 특성에 관한 연구, 강원대학교 학위논문(석사), p. 122.
  8. ANARE (1988) A low temperature record, ANARE News 14, Antarctic Division, Dept. of the Arts, Sport, the Environment, Tourism and Territories, Tasmania, Australia.
  9. Barton, N. and Choubey, V. (1977) The shear strength of rock joints in theory and practice, Rock Mechanics, Vol. 10, pp. 1-54. https://doi.org/10.1007/BF01261801
  10. Bockheim, J. G., Campbell, I. B., and McLeod, M. (2007) Permafrost Distribution and Active-Layer Depths in the McMurdo Dry Valleys, Antarctica, Permafrost and Periglac. Process, Vol. 18, pp. 217-227.
  11. Bonner, W. N. and Walton, D. W. H. (1985) Key environments Antarctica, Pergamon Press, Cambridge, England.
  12. Bortz, S., Stecih, J., Wonneberger, B. and Chin, I., (1993) Accelerated weathering in building stone, International Journal of Rock Mechanics and Mining Sciences, Vol. 30, pp. 1559-1562. https://doi.org/10.1016/0148-9062(93)90156-8
  13. Deere, D.U. and Miller, R.P. (1966) Engineering classification and index properties for intact rocks. Techinial Report No. AFLTR-65-116, Air Force Weapon's Laboratory, New Mexico, p. 308.
  14. Doran, P.T., McKay, C.P., Clow, G.C., Dana, G.L., Fountain, A.G., Nylen, T., and Lyons, W.B. (2002) Valley floor climate observations from the McMurdo dry valleys, Antarctica, 1986-2000. Journal of Geophysical Research, Vol. 107 D24, 4772. DOI:10.1029/2001JD002045.
  15. Elliot, D.H. (1975) Tectoincs of Antarctica: A review. Am. J. Sci., Vol. 275A, pp. 45-106.
  16. Hale, P. and Shakoor, A. (1998) A laboratory in vestigation of the effects of climatic changes on unconfined compressive strength of selected sandstones, Proc. of 8th Congress of the International Association for Engineering geology and the Environment, Vol. 4, pp. 2859-2867.
  17. Hall, K. (1997) Rock Temperatures and Implications for Cold Region Weathering. I: New Data from Viking Valley, Alexander Inland, Antarctica, Permafrost and Periglacial Processes, Vol. 8, pp. 69-90. https://doi.org/10.1002/(SICI)1099-1530(199701)8:1<69::AID-PPP236>3.0.CO;2-Q
  18. ISRM (1978) Suggest Methods for Determining Tensile Strength of Rock Materials, Int. J. of Rock Mech. Min. Sci. &Geomech. Abstr, Vol. 15, pp. 99-103. https://doi.org/10.1016/0148-9062(78)90003-7
  19. ISRM (1979) Suggested methods for determining water content, porosity, density absorption and related properties and swelling and slakedurability index properties, Int. J. of Rock Mech. Min. Sci. &Geomech. Abstr, Vol. 16, pp. 141-156.
  20. ISRM (1979) Suggest Methods for Determining the Uniaxial Compressive Strength and Deformability of Rock Materials, Int. J. of Rock Mech. Min. Sci. &Geomech. Abstr, Vol. 16, pp. 135-140.
  21. ISRM (1985) Suggest Methods for Determining the Strength of Rock Materials in Triaxial Compression : Revised version, Int. J. of Rock Mech. Min. Sci. &Geomech. Abstr, Vol. 22, No. 2, pp. 51-60. https://doi.org/10.1016/0148-9062(85)92327-7
  22. John, M. (1988) The Greenpeace book of Antartica. Macdonald, New Zealand.
  23. Matsuoka, N. (1995) Rock weathering processes and landform development in the Sor Rondane Mountains, Antarctica, Geomorphology, Vol. 12, pp. 323-339. https://doi.org/10.1016/0169-555X(95)00013-U
  24. Oxman, B. H. (1978) Thermohaline circulation below the Ross Ice Shelf: A consequence of tidally induced vertical mixing and basal melting. J. Geophys. Res., Vol. 89, No. C1, pp. 597-606.
  25. Salvini, F. and Storti, F. (1999) Cenozoic tectonic lineaments of the Terra Nova Bay region, Ross Embayment, Antarctica, Global and Planetary Change, Vol. 23, pp. 129-144. https://doi.org/10.1016/S0921-8181(99)00054-5

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