Sains Malaysiana 41(12)(2012): 1621–1627
Beamforming Technique for
Investigation of Lateral Variability at Geotechnical Sites
(Teknik Alur Bentuk untuk Mengkaji Kebolehubahan Sisi di Tapak Geoteknik)
Norfarah Nadia Ismail*, Sung-Ho Joh & Raja Hassanul Musa Raja Ahmad
Department of Civil and Environmental
Engineering, Chung-Ang University
221 HeulSeok-Dong, DongJak-Gu, Seoul,
156-756 Republic of Korea
Diserahkan: 7 Mei 2012 / Diterima: 6 Ogos 2012
ABSTRACT
A beamformer in seismology is a signal
receptor with a series of geophones, in which a beam of elastic waves is formed
like a light beam by adjusting signal delays at individual geophones. Recently, beamforming has extended its applications to
surface-wave measurement. In surface-wave measurement, beamforming provides unique advantages over other surface-wave methods, such as full
automation in data analysis as well as directional signal reception to minimize
scattered noise and multiple reflections in signals. However, certain defects
depreciate the value of beamforming in terms of its
practicality and feasibility. These include the requirement of having many
receivers and the loss of small wavelength data due to spatial aliasing. It
leads to insensitivity in identification of lateral variability, which creates
the problem of having to smooth out geologic features and complexities like
folding, faults and fractures. In this paper, advances in the refinement of beamforming were described on two counts: improvement of
sensitivity in identification of lateral variability and recovery of aliased
wave numbers, which enables evaluation of shallow material. On the passage to
refinement, synthetic waveforms for typical layering systems were generated to
figure out characteristics of beamformer velocities
in comparison with SASW velocities and theoretical normal-mode
velocities.
Keywords: Beamforming theory; phase
velocities; refined beamformer; spatial aliasing
ABSTRAK
Alur bentuk dalam konteks seismologi ialah pengesan isyarat yang menggunakan sebilangan geofon, dengan alur gelombang kenyal seperti jalur cahaya yang dibentuk dengan mengubah lengah isyarat pada setiap geofon. Kebelakangan ini, aplikasi alur bentuk telah dikembangkan dalam kaedah pengukuran gelombang permukaan. Dalam kaedah pengukuran gelombang permukaan, alur bentuk mempunyai kelebihan yang unik berbanding kaedah gelombang permukaan yang lain, seperti automasi penuh dalam menganalisis data serta penerimaan isyarat terarah untuk meminimumkan taburan hingar dan pantulan berganda dalam isyarat. Walau bagaimanapun, terdapat beberapa kekangan yang boleh menurunkan nilai alur bentuk daripada segi praktikal dan pelaksanaan. Ia termasuklah keperluan untuk menggunakan banyak penerima dan kehilangan data pada panjang gelombang yang pendek akibat herotan ruang. Ini membuatkan tahap pengenalpastian terhadap kebolehubahan sisi menjadi kurang sensitif dan boleh menimbulkan masalah kerana terpaksa melicinkan fitur geologi serta struktur rencamnya seperti lipatan, sesaran dan retakan. Dalam kertas ini, kemajuan dalam tapisan alur bentuk diterangkan berdasarkan dua penekanan: penambahbaikan kepekaan dalam pengenalpastian kebolehubahan sisi dan pemulihan nombor gelombang yang terherot, bagi membolehkan penilaian dilakukan ke atas bahan cetek. Dalam proses penapisan ini, sejumlah gelombang sintetik untuk sistem berlapais yang tipikal telah dihasilkan bagi mencari dan menentukan ciri-ciri halaju beamformer, berdasarkan perbandingan dengan halaju SASW dan halaju teori mod-normal.
Kata kunci: Alur bentuk tertapis; halaju fasa; herotan ruang; teori alur bentuk
RUJUKAN
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*Pengarang untuk surat-menyurat, email: norfarahnadia@gmail.com