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(see also http://www.mines.edu/fs_home/tboyd/GP311/MODULES/SEIS/main.html)n Seismic Methods: Refraction
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Seismic Waves Body Surface P S Love Rayleigh
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Seismic Wave Speeds MaterialP wave Velocity (m/s)S wave Velocity (m/s) Air332 Water1400-1500 Petroleum1300-1400 Steel61003500 Concrete36002000 Granite5500-59002800-3000 Basalt64003200 Sandstone1400-4300700-2800 Limestone5900-61002800-3000 Sand (Unsaturated)200-100080-400 Sand (Saturated)800-2200320-880 Clay1000-2500400-1000 Glacial Till (Saturated)1500-2500600-1000
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Reflection and Refraction sin 1 = sin 3 = Vp 1 Vs 1 sin 2 = sin 4 = Vs 2 Vp 2 p (ray parameter)
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Critical Refraction
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Seismic Refraction Waves passing from slow to fast medium
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Reflection & Refraction 0 200 400 T, msec Direct Reflected Refracted
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Refraction Analysis (flat): Velocity estimation
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Depth from TT curve
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Structure from TT curve
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Refraction: One layer case
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Refraction: 3 layer case
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Engineering Quad 1/27/00 12 gauge source 1m geophone spacing, 1 m minimum offset
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Data from Treman (11/2/05)
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Engineering Quad 1/27/00 12 gauge source 1m geophone spacing, 1 m minimum offset SHOT *
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Seismic Raytracing (forward modeling) http://www.scielo.cl/scielo.php?pid=S0716-02082003000100006&script=sci_arttext&tlng=en
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