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Wave velocity variation with temperature: influential properties of temperature coefficient (\(\partial {\varvec{V}}/\partial {\varvec{T}}\)) of selected rocks

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Abstract

The intrinsic compressional and shear wave’s velocities of rocks decrease with increasing temperature. An important parameter that quantifies the temperature effect on rocks’ wave velocities is the temperature coefficient (\(\partial V/\partial T\)), which is the gradient of the linear relationship between the wave velocity and temperature. This study investigated properties affecting the temperature coefficient of selected lithology in Ogun State Southwestern Nigeria. The samples were heated and the compressional velocities were measured at a constant pressure of 0.01 GPa and 50 °C intervals from 50 to 300 °C. The result showed that both elastic modulus and density varied directly with the absolute compressional temperature coefficient, \(\partial {V}_{P}/\partial T\) while porosity had an inverse variation. The elastic modulus, density, and porosity exhibited a notable effect on the temperature coefficient with their respective correlation coefficient as 0.98495, 0.97594 and − 0.93787. Clay content, which also exhibited an inverse variation with the temperature coefficient had a correlation coefficient of − 0.44668. For both the same and different rock types, elastic modulus is the most important property that controls the temperature coefficient.

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Abbreviations

\(V\) :

Wave velocity

\({V}_{P}\) :

P-wave velocity

\(v\) :

Poisson’s ratio

\(t\) :

Pulse time

\(d\) :

Sample width

\(M\) :

Compressional wave modulus

\(G\) :

Shear modulus

\(E\) :

Elastic modulus

ρ :

Density

\({\rho }_{d}\) :

Dry bulk density

\({W}_{dry}\) :

Dry weight

\({W}_{sat}\) :

Saturated weight

\({W}_{Total}\) :

Total weight

References

  • Abatan OA, Akinyemi OD, Olowofela JA, Salako FK (2016) Experimental investigation of factors affecting compressional and shear wave velocities in shale and limestone of Ewekoro formation of Southern Nigeria sedimentary basin. Environ Earth Sci 75(22):1442

    Article  Google Scholar 

  • Al-Dousari M, Garrouch AA, Al-Omair O (2016) Investigating the dependence of shear wave velocity on petrophysical parameters. J Pet Sci Eng 146:286–296

    Article  Google Scholar 

  • Badmus BS, Olatinsu OB (2009) Geophysical evaluation and chemical analysis of kaolin clay deposit of Lakiri village, southwestern Nigeria. Int J Phys Sci 4(10):592–606

    Google Scholar 

  • Bayuk EI, Tedeev RV (1974) The effect of temperature on velocity of longitudinal waves in rocks at high pressures. foreign technology division wright-patterson air force base, Ohio

  • Chauhan A, Chauhan P (2014) Powder XRD technique and its applications in science and technology. J Analyt Bioanalyt Tech 5(5):212. https://doi.org/10.4172/2155-9872.1000212

    Article  Google Scholar 

  • Chen WZ, Ma YS, Yu HD, Li FF, Li XL, Sillen X (2017) Effects of temperature and thermally-induced microstructure change on hydraulic conductivity of Boom Clay. J Rock Mech Geotech Eng 9(3):383–395

    Article  Google Scholar 

  • Christensen NI (1979) Compressional wave velocities in rocks at high temperatures and pressures, critical thermal gradients, and crustal low-velocity zones. J Geophys Res: Solid Earth 84(B12):6849–6857

    Article  Google Scholar 

  • Dutrow BL and Clark CM (2016) X-ray powder diffraction (XRD). Geochemical instrumentation and analysis, slideshare.net. https://www.slideshare.net/SumitTiwari69/xraypowder-diffraction-xrd

  • Erickson SN, Jarrard RD (1998) Velocity-porosity relationships for water-saturated siliciclastic sediments. J Geophys Res: Solid Earth 103(B12):30385–30406. https://doi.org/10.1029/98jb02128

    Article  Google Scholar 

  • Fakolujo OS, Olokode OS, Aiyedun PO, Oyeleke YT, Anyanwu BU (2012) Studies on the five (5) selected clays in Abeokuta, Nigeria. Pacific J Sci Technol 13(1):83–90

    Google Scholar 

  • Gassmann F (1951) Elastic waves through a packing of sheres. Geophysics 16:673–685

    Article  Google Scholar 

  • Hills JF, Pettifer GS (1985) The clay mineral content of various rock types compared with the methylene blue value. J Chem Technol Biotechnol 35A:168–180. https://doi.org/10.1002/jctb.5040350404

    Article  Google Scholar 

  • Kern H (1978) The effect of high temperature and high confining pressure on compressional wave velocities in quartz-free igneous and metamorphic rocks. Tectonophysics 44:185–203

    Article  Google Scholar 

  • Kern H, Tubia JM (1993) Pressure and temperature dependence of P- and S-wave velocities, seismic anisotropy and density of sheared rocks from the Sierra Alpujata massif (Ronda peridotites, Southern Spain). Earth Planet Sci Lett 119(1993):191–205

    Article  Google Scholar 

  • Lawal AO (1998) Pasture distribution in the derived savanna area Of Ogun State. Niger J Anim Prod 25(1):173–175

    Google Scholar 

  • Matsushima S (1981) Compressional and shear wave velocities of igneous rocks and volcanic glasses to 900°C and 20 kbar. Tectonophysics 75(3):257–271

    Article  Google Scholar 

  • Mokhfi T, William P (2008) Temperature effects on physical properties and mechanical behavior of granite: experimental investigation of material damage. J ASTM Int 5(3):100464

    Article  Google Scholar 

  • Nadeau PH, Wilson MJ, McHardy WJ, Tait JM (1984) Interparticle diffraction: a new concept for Interstratified Clays. Clay Miner 19:757–769

    Article  Google Scholar 

  • Nigeria Geologic Survey Agency (2006) Published by the authority of the Federal Republic of Nigeria

  • Pandian MS (2014) X-ray diffraction analysis: principle, instrument and applications. researchgate samples by X-ray diffraction: discussion. Am Miner 72:438–440

    Google Scholar 

  • Proceq (2011) Operating Instructions Pundit Lab / Pundit Lab+ Ultrasonic Instrument

  • Raymer LL, Hunt ER, Gardner JS (1980) An improved sonic transit time-to-porosity transform. Society of Petrophysicists and Well-Log Analysts. SPWLA 21st Annual Logging Symposium, 8–11 July, Lafayette, Louisiana

  • Salami BM, Olorunfemi MO (2014) Hydrogeophysical evaluation of the groundwater potential of the central part of Ogun State. Nigeria Ife J Sci 16(2):291–299

    Google Scholar 

  • Sayed NA, El Abuseda H, Kassab MA (2015) Acoustic wave velocity behavior for some Jurassic carbonate samples. J Afr Earth Sci 111:14–25

    Article  Google Scholar 

  • Spencer JW, Nur AM (1976) The effects of pressure, temperature, and pore water on velocities in westerly granite. J Geophys Res 81(5):899–904

    Article  Google Scholar 

  • Wyllie MRJ, Gregory AR, Gardner GHF (1958) An experimental investigation of factors affecting elastic wave velocities in porous media. Geophysics 23:459–493

    Article  Google Scholar 

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Correspondence to H. I. Kuforiji.

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Kuforiji, H.I., Olurin, O.T., Akinyemi, O.D. et al. Wave velocity variation with temperature: influential properties of temperature coefficient (\(\partial {\varvec{V}}/\partial {\varvec{T}}\)) of selected rocks. Environ Earth Sci 80, 638 (2021). https://doi.org/10.1007/s12665-021-09937-4

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