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Introduction to Geophysics Ali Oncel [email_address] Department of Earth Sciences KFUPM Seismic Reflection 4: Acquisiton, Processing, and Waveform Analysis Introduction to Geophysics-KFUPM
Example: Disk Formula  Seismic Waveform: Input Seismic Signal  Homogenous Medium  Strong Interface   Amplitude  Minimum Phase Pulse  Zero Phase Pulse   Acoustic Impedance  Coefficients of Reflection and Transmission  Example: Air-water reflection  Example: Water-Air Reflection   Reflection from Single Interface  Reflections from Several Interfaces   Previous Lecture Introduction to Geophysics-KFUPM
Convolution Earth as   a Filter of Seismic Energy G(t)   *   F(t)   =  H(t)  Source  Earth  =  Seismogram  Wavelet  Ref. Coeff.  Introduction to Geophysics-KFUPM
Source and Earth Response Mathematical Description of Filter Convolution Introduction to Geophysics-KFUPM See pp. 353 of Reynolds, 2002
Convolutional Model for the Earth SOURCE *  Reflection Coefficient = DATA (input)  (earth)  (output) where * stands for convolution Reflections in the earth  are viewed as equivalent to a convolution  process between  the earth  and  the input seismic wavelet. Introduction to Geophysics-KFUPM
Introduction to Geophysics-KFUPM (MORE REALISTIC) Convolutional Model for the Earth
Introduction to Geophysics-KFUPM
Example 1: Convolution Introduction to Geophysics-KFUPM 1) Folding 2) Shifting 3) Multiplication 4) Summation The process of convolution consists of 4 simple mathematical operations   Seismic Wavelet (1, -1/2, 1/2) Reflectivity Sequence (1, 1/2, 1/2)
Solution Reflectivity  Output Sequence  Response 1  1/2  1/2 1/2 -1/2  1  1x1=   1 1/2 -1/2  1  -1/2x1+1/2x1=   0 1/2 -1/2  1  1/2x1+1/2x-1/2+1/2x1=   3/4  1/2 -1/2  1  …………………=   0 1/2 -1/2  1  …………=   1/4   1/2 -1/2  1  …………=   0 Introduction to Geophysics-KFUPM
Convolution Output Response Plot amplitudes as a  seismogram using  travel times 1 , 0 , 3/4 , 1/4, 0 Introduction to Geophysics-KFUPM
Introduction to Geophysics-KFUPM For example,  a double spike function ,  2, 0, 1  convolved with  an impulse response function   4, 3, 2, 1  . Example 2: Convolution From Kearey, Brooks, and Hill, 2002
Recall: Elastic waves Amplitude:  the  peak to trough height divided by two. Wavelength:  the  distance over which the wave goes through one complete cycle. Period:  the  time over which the wave is observed to complete a single cycle. V =   Velocity = wavelength x frequency Introduction to Geophysics-KFUPM
Seismic Resolution Vertical –   /4  to   /2  wavelength V  =    V  = 2000 m/sec    = 25 Hz    = V /   =  80 meters Resolution 20 to 40 m Introduction to Geophysics-KFUPM
What is their period? 12 sec What is the amplitude of these waves? 1mm What is their frequency? 1/12 Hz = 0.083 Hz Example 1 Introduction to Geophysics-KFUPM V  =   
What is the amplitude of these waves?  1.2 mm What is their wavelength? 1.75 m If the frequency of these waves is 5 Hz,  what is their speed? v = 1.75 m • 5Hz= 8.75 m/sec = 0.00875 km/sec Example 2 Introduction to Geophysics-KFUPM V  =   
Homework, Due to April 26 What is the amplitude of these waves? What is their period? These waves were recorded in rock with a seismic velocity of 5km/sec. What is their wavelength? Introduction to Geophysics-KFUPM V  =   
Homework, Due to April 26 What is the amplitude of these waves? What is their period? What is their frequency? Introduction to Geophysics-KFUPM V  =   
Homework, Due to April 26 In one typed page, discuss applications of  a) the seismic reflection method b)  the seismic refraction method 2.  Calculating by hand  Convolve the spike function: 2 0 0 3 3 1 3 -1 1 -2 -1 with the impulse response function: 1 2 1 -0.5 0 0.5 0 Show your working for the hand calculated version.  Introduction to Geophysics-KFUPM

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ÖNCEL AKADEMİ: INTRODUCTION TO GEOPHYSICS

  • 1. Introduction to Geophysics Ali Oncel [email_address] Department of Earth Sciences KFUPM Seismic Reflection 4: Acquisiton, Processing, and Waveform Analysis Introduction to Geophysics-KFUPM
  • 2. Example: Disk Formula Seismic Waveform: Input Seismic Signal Homogenous Medium Strong Interface Amplitude Minimum Phase Pulse Zero Phase Pulse Acoustic Impedance Coefficients of Reflection and Transmission Example: Air-water reflection Example: Water-Air Reflection Reflection from Single Interface Reflections from Several Interfaces Previous Lecture Introduction to Geophysics-KFUPM
  • 3. Convolution Earth as a Filter of Seismic Energy G(t) * F(t) = H(t) Source Earth = Seismogram Wavelet Ref. Coeff. Introduction to Geophysics-KFUPM
  • 4. Source and Earth Response Mathematical Description of Filter Convolution Introduction to Geophysics-KFUPM See pp. 353 of Reynolds, 2002
  • 5. Convolutional Model for the Earth SOURCE * Reflection Coefficient = DATA (input) (earth) (output) where * stands for convolution Reflections in the earth are viewed as equivalent to a convolution process between the earth and the input seismic wavelet. Introduction to Geophysics-KFUPM
  • 6. Introduction to Geophysics-KFUPM (MORE REALISTIC) Convolutional Model for the Earth
  • 8. Example 1: Convolution Introduction to Geophysics-KFUPM 1) Folding 2) Shifting 3) Multiplication 4) Summation The process of convolution consists of 4 simple mathematical operations Seismic Wavelet (1, -1/2, 1/2) Reflectivity Sequence (1, 1/2, 1/2)
  • 9. Solution Reflectivity Output Sequence Response 1 1/2 1/2 1/2 -1/2 1 1x1= 1 1/2 -1/2 1 -1/2x1+1/2x1= 0 1/2 -1/2 1 1/2x1+1/2x-1/2+1/2x1= 3/4 1/2 -1/2 1 …………………= 0 1/2 -1/2 1 …………= 1/4 1/2 -1/2 1 …………= 0 Introduction to Geophysics-KFUPM
  • 10. Convolution Output Response Plot amplitudes as a seismogram using travel times 1 , 0 , 3/4 , 1/4, 0 Introduction to Geophysics-KFUPM
  • 11. Introduction to Geophysics-KFUPM For example, a double spike function , 2, 0, 1 convolved with an impulse response function 4, 3, 2, 1 . Example 2: Convolution From Kearey, Brooks, and Hill, 2002
  • 12. Recall: Elastic waves Amplitude: the peak to trough height divided by two. Wavelength: the distance over which the wave goes through one complete cycle. Period: the time over which the wave is observed to complete a single cycle. V =  Velocity = wavelength x frequency Introduction to Geophysics-KFUPM
  • 13. Seismic Resolution Vertical –  /4 to  /2 wavelength V =   V = 2000 m/sec  = 25 Hz  = V /  = 80 meters Resolution 20 to 40 m Introduction to Geophysics-KFUPM
  • 14. What is their period? 12 sec What is the amplitude of these waves? 1mm What is their frequency? 1/12 Hz = 0.083 Hz Example 1 Introduction to Geophysics-KFUPM V =  
  • 15. What is the amplitude of these waves? 1.2 mm What is their wavelength? 1.75 m If the frequency of these waves is 5 Hz, what is their speed? v = 1.75 m • 5Hz= 8.75 m/sec = 0.00875 km/sec Example 2 Introduction to Geophysics-KFUPM V =  
  • 16. Homework, Due to April 26 What is the amplitude of these waves? What is their period? These waves were recorded in rock with a seismic velocity of 5km/sec. What is their wavelength? Introduction to Geophysics-KFUPM V =  
  • 17. Homework, Due to April 26 What is the amplitude of these waves? What is their period? What is their frequency? Introduction to Geophysics-KFUPM V =  
  • 18. Homework, Due to April 26 In one typed page, discuss applications of a) the seismic reflection method b) the seismic refraction method 2. Calculating by hand Convolve the spike function: 2 0 0 3 3 1 3 -1 1 -2 -1 with the impulse response function: 1 2 1 -0.5 0 0.5 0 Show your working for the hand calculated version. Introduction to Geophysics-KFUPM

Editor's Notes

  • #2: qqq
  • #4: Convolution means replacing each reflection coefficient with the input seismic signal, scaled to the amplitude and polarity of the reflection coefficient.