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Examiantion of Variation Seismic P-Velocity with the Joint Density in Rocks

Year 2010, Volume: 9 Issue: 2, 10 - 18, 13.07.2016

Cengiz Kurtuluş Kenan Yazan Maral Üçkardeş O. Kaptan Turan

Abstract

The seismic velocities are greatly affected by rock type, density, grain size and shape, porosity, temperature and water content etc. In addition to these parameters, it is known the effect of joint system and density on ultrasonic pulse velocity (UPV) was measured on the artificial joints created in different distances in two different rock types and the relationship between joint rock density and UPV was investigated statistically and the results were assessed with the results found in literature

References

  • ALTINDAG, R., GÜNEY A., 2005. Evaluation of the relationships between P-wave velocity (VP) and joint density. The 19th International Mining Congress and Fair of Turkey, IMCET 2005 Izmit Turkey, June 09.12.2005
  • ALTINLI, İ.E., 1968. Geological studies of İzmit- Hereke- Kurucadağ section M.T.A. Bulletin 71 1-26 (in Turkish) Ankara.
  • BAMFORD, D. and NUNN, K.R. 1979. In situ seismic measurement of crack anisotropy in the carboniferous limestone of North-West England. Geophys. Prospec, 27 (1), 322–338.
  • CRAMPIN, S., 1978. Seismic-wave propagation through a cracked solid: Polarization as a possible dilatancy diagnostic, Geophys. J. R. Astron. Soc., 53, 467-496.
  • ÇAKIR, Ş., 2000. Geology of Demirciler-Sadıklar- Gündoğdu- Tütünçiftlik (Kocaeli) Area (Unpublished Ph.D. Thesis) Kocaeli University Natural Sciences Institute 173 İzmit.
  • GUEGUEN, Y. and SCHUBNEL, A., 2003. Elastic wave velocities and permeability of cracked rocks, Tectonophysics, 370, 163–176.
  • GUPTA, N. I., 1973. Seismic velocities in rock subjected to axial loading up to shear fracture, J. Geophys, Res., 78, 6936-6942.
  • IDZIAK, A.,1988. Seismic wave velocities in fracturedsedimentary carbonate rocks, Acta GeophysicaPolonica, vol.XXXVI, no.2, 101–114.
  • IDZIAK, A., 1992. Seismic wave velocity anisotropy and itsrelation to crack orientation of rock masses. Katowice: Silesian Univ. Publishing, (in Polish with English abstract).
  • IDZIAK, A. and STAN-KLECZEK, I.: 2006a. Geomechanical properties of fractured carbonate rock mass detrmined by geophysical methods, in: A.V. Cotthem et al (eds), Multiphysics Coupling and Long Term Behaviour in Rock Mechanics, Taylor &Francis, London.
  • IIDA, K., SUGINO T, FURUHASHI H. and KUMAZAWA M., 1967. Elastic dilatational wave velocity in crystalline schists from Sanbagava metamorphic terrain, Shikoku, Japan, J. Earth Sci., Nagoya Univ., 15, 112-147.
  • KAHRAMAN S., 2001. A correlation between P-wave velocity, number of joints and schmidt hammer rebound number, bit J rock Mech of Min Sei, 38, 729-773
  • KETİN, İ. ve Gümüş, A., 1963. Sinop-Ayancık arasında III. Bölgeye dahil sahaların jeolojisi. Türkiye Petrolleri Anonim Ortaklığı, Arşiv No. 288, Ankara (yayımlanmamış).
  • KING, M., CHAUDHRY, N. & SHAKEEL, A., 1995. Experimental ultrasonic velocities and permeability for sandstones with aligned cracks, Int. J. Rock Mech. Mining Sci., 32, 155–163.
  • LOCKNER, D., WALSH J.B., and BYERLEE, J. D., 1977. Changes in seismic velocity and attenuation during deformation of granite, J. Geophys. Res., 82, 5374-5378.
  • NUR, A. and SIMMONS, G., 1969. Stress-induced velocity anisotropy in rock: an experimental study, J. geophys. Res., 74, 6667–6674.
  • ODA, M., 1993. Elastic stress and strain in jointed rock masses by means of crack tensor analysis, Rock Mech. Rock Engng., 26, 2, 89-112.
  • SAYERS, C., 2002. Stress-dependent elastic anisotropy of sandstones, Geophys. Prospect., 50, 85– 95.
  • SAYERS, C. and KACHANOV, M., 1995. Microcrack-induced elastic wave anisotropy of brittle rocks, J. geophys. Res., 100, 4149–4156.
  • SOGA, N., MIZUTANI, H. and SPETZLER, H. and MARTIN, R. J., 1978. The effect of dilatancy on velocity anisotropy in Westerly granite, J. Geophys. Res., 83, 4451-4458.
  • WANG, C., LIN, W. and WENK, H.R., 1975. The effects of water and pressure on velocities of elastic waves in a foliated rock, J. Geophys. Res., 80, 1065-1069.

Kayalar İçinde Sismik P-Dalgasının Kırık Yoğunluğu İle Değişiminin İncelenmesi

Year 2010, Volume: 9 Issue: 2, 10 - 18, 13.07.2016

Cengiz Kurtuluş Kenan Yazan Maral Üçkardeş O. Kaptan Turan

Abstract

Sismik hızlar büyük ölçüde kayaç türü, yoğunluk, dane büyüklük ve şekli, porozite, sıcaklık, su içeriği vs. gibi parametrelerden etkilenir. Bunların dışında kayaçlar içinde bulunan kırık sistem ve yoğunluğunun da sismik hızlar üzerindeki etkileri bilinmektedir. Bu çalışmada iki farklı tipteki prizmatik kaya örnekleri içinde farklı mesafelerde oluşturulan yapay eklem dizilerinde ultrasonik puls hızı (UPH) ölçülmüş ve eklem sayıları ile (UPH) hızları arasındaki ilişkiler istatistiksel olarak incelenmiş ve sonuçlar literatürdeki değerlerle karşılaştırılmıştır

References

  • ALTINDAG, R., GÜNEY A., 2005. Evaluation of the relationships between P-wave velocity (VP) and joint density. The 19th International Mining Congress and Fair of Turkey, IMCET 2005 Izmit Turkey, June 09.12.2005
  • ALTINLI, İ.E., 1968. Geological studies of İzmit- Hereke- Kurucadağ section M.T.A. Bulletin 71 1-26 (in Turkish) Ankara.
  • BAMFORD, D. and NUNN, K.R. 1979. In situ seismic measurement of crack anisotropy in the carboniferous limestone of North-West England. Geophys. Prospec, 27 (1), 322–338.
  • CRAMPIN, S., 1978. Seismic-wave propagation through a cracked solid: Polarization as a possible dilatancy diagnostic, Geophys. J. R. Astron. Soc., 53, 467-496.
  • ÇAKIR, Ş., 2000. Geology of Demirciler-Sadıklar- Gündoğdu- Tütünçiftlik (Kocaeli) Area (Unpublished Ph.D. Thesis) Kocaeli University Natural Sciences Institute 173 İzmit.
  • GUEGUEN, Y. and SCHUBNEL, A., 2003. Elastic wave velocities and permeability of cracked rocks, Tectonophysics, 370, 163–176.
  • GUPTA, N. I., 1973. Seismic velocities in rock subjected to axial loading up to shear fracture, J. Geophys, Res., 78, 6936-6942.
  • IDZIAK, A.,1988. Seismic wave velocities in fracturedsedimentary carbonate rocks, Acta GeophysicaPolonica, vol.XXXVI, no.2, 101–114.
  • IDZIAK, A., 1992. Seismic wave velocity anisotropy and itsrelation to crack orientation of rock masses. Katowice: Silesian Univ. Publishing, (in Polish with English abstract).
  • IDZIAK, A. and STAN-KLECZEK, I.: 2006a. Geomechanical properties of fractured carbonate rock mass detrmined by geophysical methods, in: A.V. Cotthem et al (eds), Multiphysics Coupling and Long Term Behaviour in Rock Mechanics, Taylor &Francis, London.
  • IIDA, K., SUGINO T, FURUHASHI H. and KUMAZAWA M., 1967. Elastic dilatational wave velocity in crystalline schists from Sanbagava metamorphic terrain, Shikoku, Japan, J. Earth Sci., Nagoya Univ., 15, 112-147.
  • KAHRAMAN S., 2001. A correlation between P-wave velocity, number of joints and schmidt hammer rebound number, bit J rock Mech of Min Sei, 38, 729-773
  • KETİN, İ. ve Gümüş, A., 1963. Sinop-Ayancık arasında III. Bölgeye dahil sahaların jeolojisi. Türkiye Petrolleri Anonim Ortaklığı, Arşiv No. 288, Ankara (yayımlanmamış).
  • KING, M., CHAUDHRY, N. & SHAKEEL, A., 1995. Experimental ultrasonic velocities and permeability for sandstones with aligned cracks, Int. J. Rock Mech. Mining Sci., 32, 155–163.
  • LOCKNER, D., WALSH J.B., and BYERLEE, J. D., 1977. Changes in seismic velocity and attenuation during deformation of granite, J. Geophys. Res., 82, 5374-5378.
  • NUR, A. and SIMMONS, G., 1969. Stress-induced velocity anisotropy in rock: an experimental study, J. geophys. Res., 74, 6667–6674.
  • ODA, M., 1993. Elastic stress and strain in jointed rock masses by means of crack tensor analysis, Rock Mech. Rock Engng., 26, 2, 89-112.
  • SAYERS, C., 2002. Stress-dependent elastic anisotropy of sandstones, Geophys. Prospect., 50, 85– 95.
  • SAYERS, C. and KACHANOV, M., 1995. Microcrack-induced elastic wave anisotropy of brittle rocks, J. geophys. Res., 100, 4149–4156.
  • SOGA, N., MIZUTANI, H. and SPETZLER, H. and MARTIN, R. J., 1978. The effect of dilatancy on velocity anisotropy in Westerly granite, J. Geophys. Res., 83, 4451-4458.
  • WANG, C., LIN, W. and WENK, H.R., 1975. The effects of water and pressure on velocities of elastic waves in a foliated rock, J. Geophys. Res., 80, 1065-1069.
There are 21 citations in total.

Details

Other ID JA25PB47KG
Journal Section Articles
Authors

Cengiz Kurtuluş This is me

Kenan Yazan This is me

Maral Üçkardeş This is me

O. Kaptan Turan This is me

Publication Date July 13, 2016
Published in Issue Year 2010 Volume: 9 Issue: 2

Cite

APA Kurtuluş, C., Yazan, K., Üçkardeş, M., Turan, O. K. (2016). Kayalar İçinde Sismik P-Dalgasının Kırık Yoğunluğu İle Değişiminin İncelenmesi. Uygulamalı Yerbilimleri Dergisi, 9(2), 10-18.
AMA Kurtuluş C, Yazan K, Üçkardeş M, Turan OK. Kayalar İçinde Sismik P-Dalgasının Kırık Yoğunluğu İle Değişiminin İncelenmesi. uybd. July 2016;9(2):10-18.
Chicago Kurtuluş, Cengiz, Kenan Yazan, Maral Üçkardeş, and O. Kaptan Turan. “Kayalar İçinde Sismik P-Dalgasının Kırık Yoğunluğu İle Değişiminin İncelenmesi”. Uygulamalı Yerbilimleri Dergisi 9, no. 2 (July 2016): 10-18.
EndNote Kurtuluş C, Yazan K, Üçkardeş M, Turan OK (July 1, 2016) Kayalar İçinde Sismik P-Dalgasının Kırık Yoğunluğu İle Değişiminin İncelenmesi. Uygulamalı Yerbilimleri Dergisi 9 2 10–18.
IEEE C. Kurtuluş, K. Yazan, M. Üçkardeş, and O. K. Turan, “Kayalar İçinde Sismik P-Dalgasının Kırık Yoğunluğu İle Değişiminin İncelenmesi”, uybd, vol. 9, no. 2, pp. 10–18, 2016.
ISNAD Kurtuluş, Cengiz et al. “Kayalar İçinde Sismik P-Dalgasının Kırık Yoğunluğu İle Değişiminin İncelenmesi”. Uygulamalı Yerbilimleri Dergisi 9/2 (July 2016), 10-18.
JAMA Kurtuluş C, Yazan K, Üçkardeş M, Turan OK. Kayalar İçinde Sismik P-Dalgasının Kırık Yoğunluğu İle Değişiminin İncelenmesi. uybd. 2016;9:10–18.
MLA Kurtuluş, Cengiz et al. “Kayalar İçinde Sismik P-Dalgasının Kırık Yoğunluğu İle Değişiminin İncelenmesi”. Uygulamalı Yerbilimleri Dergisi, vol. 9, no. 2, 2016, pp. 10-18.
Vancouver Kurtuluş C, Yazan K, Üçkardeş M, Turan OK. Kayalar İçinde Sismik P-Dalgasının Kırık Yoğunluğu İle Değişiminin İncelenmesi. uybd. 2016;9(2):10-8.