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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    International journal of fracture 106 (2000), S. 81-93 
    ISSN: 1573-2673
    Keywords: Body force method ; elasticity ; elliptical inclusion ; interaction effect ; longitudinal shear ; numerical analysis ; singular integral equation stress concentration.
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Abstract This paper deals with an interaction problem of arbitrarily distributed elliptical inclusions under longitudinal shear loading. The problem is formulated as a system of singular integral equations with Cauchy-type or logarithmic-type singularities, where unknown functions are the densities of body forces distributed in the longitudinal directions of infinite bodies having the same elastic constants as those of the matrix and inclusions. In order to satisfy the boundary conditions along the elliptical inclusions, four kinds of fundamental density functions are introduced in a similar way of previous papers treating plane stress problems. Then the body force densities are approximated by a linear combination of those fundamental density functions and polynomials. In the analysis, elastic constants of matrix and inclusion are varied systematically; then the magnitude and position of the maximum stress are shown in tables and the stress distributions along the boundary are shown in figures. For any fixed shape, size and elastic constant of inclusions, the relationships between number of inclusions and maximum stress are investigated for several arrangements.
    Type of Medium: Electronic Resource
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  • 2
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    In:  Geophys. Res. Lett., Colorado Springs, US Air Force Academy, vol. 27, no. 10, pp. 1535-1538, pp. L12S08, (ISSN: 1340-4202)
    Publication Date: 2000
    Description: Nagao et al. monitor the geoelectric potential difference between pairs of electrodes (or dipoles) buried at about 2 m depth at several stations in Japan for the purpose of observing co-seismic signals. Studying several recent earthquakes, they report that the signals commence not with the origin time of the earthquakes but with the arrival time of seismic waves. They find two types of co-seismic changes: offset/decay type, which last long after the seismic vibrations cease, and oscillatory type, which decay with the seismic vibrations. They also find that the amplitude of the co-seismic signals does not scale with the dipole length. Also in this issue, Hayakawa et al. [1531] investigate ultra low frequency (ULF) electromagnetic emissions associated with a large earthquake that occurred at Biak Island, Indonesia, in February 1996. Examining data from Biak and Darwin, they find that the ULF emissions observed about 1.5 months before the quake serve as a precursory signature of the earthquake.
    Keywords: Earthquake ; Electromagnetic methods/phenomena ; 0699 ; Electromagnetics ; General ; or ; miscellaneous ; 7223 ; Seismology ; Seismic ; hazard ; assessment ; and ; prediction ; 9320 ; Information ; related ; to ; geographic ; region ; Asia ; 9810 ; General ; or ; miscellaneous ; New ; fields ; (not ; classifiable ; under ; other ; headings) ; GRL
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