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Asymmetric continuum mechanics: deviations from elasticity and symmetry

Autorzy
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The Kröner approach to continua with a distribution of self-field sources is applied to a wide class of deviations from the classical ideal elasticity; the same approach is applied to the theory of continua with asymmetric fields. The corresponding equations of motion are derived. Such an approach replaces other methods based on the constitutive relations specific for each type of the medium; here, the reference constitutive relation remains the same, but deviations from the classical ideal elasticity are attributed to different sources and defects introduced into continuum theory. Both methods lead to the expressions for the related currents. The nuclei responsible for the deviations from classical elasticity can be related to the defect distribution (dislocation and disclination densities), thermal excitation, some features of internal structure and different types of nuclei (e.g. electric nuclei, rotation nuclei); other deviations lead to an elastoplastic behavior. Our considerations extend also on deviations from the stress symmetry and related incompatibilities; we consider the resulting equations of motion.
Rocznik
Strony
115--126
Opis fizyczny
Bibliogr. 24 poz.
Twórcy
autor
  • Institute of Geophysics, Polish Academy of Sciences, Księcia Janusza 64, 01-452 Warszawa, Poland
Bibliografia
  • Ager, D.V., 1980, The Geology of Europe, McGraw-Hill Book Co., London, 554 pp.
  • Ernst, T., 1981, A comparison of two methods of the transfer function calculation using the least square criterion in time and frequency domain. Pubis. Inst. Geophys. Pol. Acad. Sci. G-2(143), 13-24.
  • Ernst, T., R. Teisseyre, A. Meloni, P. Palangio and M. Marchetti, 1994, Magneto-telluric studies in the Central Appenines, 1992-1993, Acta Geophys. Pol. 42, 3, 209-228.
  • Ernst, T., E.Yu. Sokolova, I.M. Varentsov and N.G. Golubiev, 2001, Comparison of two techniques for magnetotelluric data processing using synthetic data sets. Acta Geophys. Pol. 49, 213-243.
  • Groom, R.W., and R.C. Bailey, 1989, Decomposition of magnetotelluric impedance tensor in the presence of local three-dimensional galvanic distortion, J. Geophys. Res. 94, 1913-1925.
  • Jankowski, J., J. Marianiuk, A. Ruta, C. Sucksdorff and H. Kivinen, 1984, Long-term stability of the torque-balance variometer with photoelectric converters in observatory practice. Geophysical Surveys 6, 367-380.
  • Jozwiak, W., K. Meyer and T. Ernst, 1992, Numerical modeling of 2D electric conductivity variation in earthquake preparatory areas, Geophysica 28, 1-2, 15-28.
  • Nowozynski, K., 2004, Estimation of magnetotelluric transfer functions in the time domain over a wide frequency band, Geophys. J. Int. 158, 32-41.
  • Nowozynski, K., and P.Yu. Pushkarev, 2001, The efficiency analysis of programs for 2D inversion of magnetotelluric data, Izvestiya, Physics of the Solid Earth 37, 6, 72-85.
  • Reihnger, R.E., S.C. McClusky, M.B. Oral, R.W. King, M.N. Toksoz, A.A. Barka, I. Kinik, O. Lenk and I. Sanli, 1997, Global Positioning System measurements of present-day crustal movements in the Arabia-Africa-Eurasia plate collision zone, J. Geophys. Research 102, B5, 9983-9999.
  • Sarlis, N, M. Lazaridou, P. Kapiris and P. Varotsos, 1999, Numerical model of the selectivity effect and the AV/L criterion, Geophys. Res. Lett. 26, 21, 3245-3248.
  • Varotsos, P., 2005, The Physics of Seismic Electric Signals, Terra Publ., Tokyo.
  • Varotsos, P., and K. Alexopouios, 1984, Physical properties of the variations of the electric field of the Earth preceding earthquakes. II - Determination of epicenter and magnitude, Tectonophysics 110, 99-125.
  • Wielądek, R., and T. Ernst, 1977, Application of the method of least squares to determining impulse responses, and transfer functions. Pubis. Inst. Geophys. Pol. Acad. Sci. G-1 (110), 3-12.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0009-0010
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