(see also n Seismic Methods: Refraction.

(see also http://www.mines.edu/fs_home/tboyd/GP311/MODULES/SEIS/main.html)n

Seismic Methods: Refraction

Seismic Waves

Body

Surface

P

S

Love

Rayleigh

Seismic Wave Speeds

Material P wave Velocity (m/s) S wave Velocity (m/s)

Air 332

Water 1400-1500

Petroleum 1300-1400

Steel 6100 3500

Concrete 3600 2000

Granite 5500-5900 2800-3000

Basalt 6400 3200

Sandstone 1400-4300 700-2800

Limestone 5900-6100 2800-3000

Sand (Unsaturated) 200-1000 80-400

Sand (Saturated) 800-2200 320-880

Clay 1000-2500 400-1000

Glacial Till (Saturated) 1500-2500 600-1000

Reflection and Refraction

sin 1 = sin 3 = Vp1 Vs1

sin 2 = sin 4 = Vs2 Vp2

p (ray parameter)

Critical Refraction

Seismic Refraction

Waves passing from slow to fast medium

Reflection & Refraction

0

200

400T

, mse

c

Direct

Reflected Refracted

Refraction Analysis (flat):

Velocity estimation

Depth from TT curve

Structure from TT curve

Refraction: One layer case

Refraction: 3 layer case

Engineering Quad 1/27/00 12 gauge source

1m geophone spacing, 1 m minimum offset

Data from Treman (11/2/05)

Seismic Raytracing(forward modeling)

http://www.scielo.cl/scielo.php?pid=S0716-02082003000100006&script=sci_arttext&tlng=en