Efectos de sitio por resonancia geométrica
Abstract
Las características de los movimientos sísmicos se modifican cuando las ondas cambian de medio depropagación, el contacto entre el suelo y el aire es uno de estos casos, al igual que el contacto entre la corteza y los depósitos de suelo superficiales, a estas modificaciones del movimiento se les denomina efectos locales, y se deben no sólo al contraste entre las propiedades mecánicas de los dos medios en contacto, sino a la geometría del contacto. En este artículo se caracterizan algunos efectos locales debidos a la geometría del contacto entre el medio de propagación y la superficie. Para resolver el problema se utiliza, en los casos más complejos, el método de elementos de frontera, porque permite modelar de
manera exacta la condición de radiación, y para casos
más simples, pero muy ilustrativos, se utiliza la teoría
de rayos.
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