Irwandi, Ibnu Rusydy, Umar Muksin, Ariska Rudyanto, Daryono
Wave vibration confined in the boundary will produce stationary wave solution in discrete states called modes. There are many physics applications related to modal solutions such as air column resonance, string vibration, and emission spectrum of the atomic Hydrogen. Naturally, energy is distributed in several modes so that the complete calculation is obtained from the sum of the whole modes called modal summation. The modal summation technique was applied to simulate the surface wave propagation above crustal structure of the earth. The method is computational because it uses 1D structural model which is not necessary to calculate the overall wave propagation. The simulation results of the magnitude 6.5 Pidie Jaya earthquake show the response spectral of the Summation Technique has a good correlation to the observed seismometer and accelerometer waveform data, especially at the KCSI (Kotacane) station. On the other hand, at the LASI (Langsa) station shows the modal simulation result of response is relatively lower than observation. The lower value of the reaction spectral estimation is obtained because the station is located in the thick sedimentary basin causing the amplification effect. This is the limitation of modal summation technique, and therefore it should be combined with different finite simulation on the 2D local structural model of the basin. © Published under licence by IOP Publishing Ltd.
Physics Department, Syiah Kuala University, Banda Aceh, Indonesia; Geology Department, Syiah Kuala University, Banda Aceh, Indonesia; Tsunami and Disaster Mitigation Research Center, Syiah Kuala University, Banda Aceh, Indonesia; Indonesian Agency for Meteorology, Climatology and Geophysics, Indonesia
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