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Subject: PE-309



Muhammad Fawwad Obaida



Roll No: PE-14041



Question-1 Name and describe three types of seismic waves described in this chapter. Solution



Seismic waves are the waves of energy caused by the sudden breaking of rock within the earth or an explosion. They are the energy that travels through the earth and is recorded on seismographs.



Types of Seismic Waves There are several different kinds of seismic waves, and they all move in different ways. The two main types of waves are body waves and surface waves. Body waves can travel through the earth's inner layers, but surface waves can only move along the surface of the planet like ripples on water. Earthquakes radiate seismic energy as both body and surface waves.



BODY WAVES Traveling through the interior of the earth, body waves arrive before the surface waves emitted by an earthquake. These waves are of a higher frequency than surface waves.



P-WAVES The first kind of body wave is the p-wave or primary wave. This is the fastest kind of seismic wave, and, consequently, the first to 'arrive' at a seismic station. The p-wave can move through solid rock and fluids, like water or the liquid layers of the earth. It pushes and pulls the rock it moves through just like sound waves push and pull the air. P-waves are also known as compressional waves, because of the pushing and pulling they do. Subjected to a p-wave, particles move in the same direction that the wave is moving in, which is the direction that the energy is traveling in , and is sometimes called the 'direction of wave propagation'.



S-WAVES



Subject: PE-309



Muhammad Fawwad Obaida



Roll No: PE-14041



The second type of body wave is the S-wave or secondary wave, which is the second wave you feel in an earthquake. An S-wave is slower than a P-wave and can only move through solid rock, not through any liquid medium. It is this property of S-waves that led seismologists to conclude that the Earth's outer core is a liquid. S-waves move rock particles up and down, or side-to-side—perpendicular to the direction that the wave is traveling in (the direction of wave propagation).



SURFACE WAVES Travelling only through the crust, surface waves are of a lower frequency than body waves, and are easily distinguished on a Seismogram as a result. Though they arrive after body waves, it is surface waves that are almost entirely responsible for the damage and destruction associated with earthquakes. This damage and the strength of the surface waves are reduced in deeper earthquakes.



LOVE-WAVES The first kind of surface wave is called a Love wave, named after A.E.H.Love, a British mathematician who worked out the mathematical model for this kind of wave in 1911. It's the fastest surface wave and moves the ground from side-to-side. Confined to the surface of the crust, Love waves produce entirely horizontal motion.



Subject: PE-309



Muhammad Fawwad Obaida



Roll No: PE-14041



RAYLEIGH WAVE The other kind of surface wave is the Rayleigh wave, named for John William Strutt, Lord Rayleigh, who mathematically predicted the existence of this kind of wave in 1885 .A Rayleigh wave rolls along the ground just like a wave rolls across a lake or an ocean. Because it rolls, it moves the ground up and down, and side-to-side in the same direction that the wave is moving. Most of the shaking felt from an earthquake is due to the Rayleigh wave, which can be much larger than the other waves.



Question-2 Define the following terms: 1.Acoustic Impedance 2.Snell’s Law of refraction 3.Critical angle Solution



Acoustic Impedance Acoustic Impedance is the measure of the opposition that a system presents to the acoustic flow resulting of an acoustic pressure applied to the system. It is represented by “Z “ and its SI unit Pa.s/m2.



Snell’s Law of refraction Snell's law states that the ratio of the sines of the angles of incidence and refraction is equivalent to the ratio of phase velocities in the two media, or equivalent to the reciprocal of the ratio of the indices of refraction:



Critical Angle Critical Angle is the angle of incidence that provides an angle of refraction of 90 degrees.



Subject: PE-309



Muhammad Fawwad Obaida



Roll No: PE-14041



Question-3



Table 3.3 lists densities and velocities of three layers. What can you infer about the magnitudes and polarities of reflection coefficient 1 (for the interface between layers1 and 2) and reflection coefficient 2 (for the interface between layers 2 and 3)?



Solution We know that, Acoustic Impedance=Z=ρv Hence, Z1=2.2*1000*15000 =3300000Pa.s/m3 Z2=2.9*1000*3000 =8700000Pa.s/m3 Z3=2.6*1000*2500 =6500000Pa.s/m3 For interface between layer 1 and 2 R1=(Z2-Z1)/(Z2+Z1) =(8700000-330000)/(8700000+3300000) =0.45 Comment, Since Z2>Z1, so the reflection coefficient is positive and it is not reversed For interface between layer 2 and 3 R2=(Z3-Z2)/(Z3+Z2) =(6500000-8700000)/(6500000+8700000) =-0.1447 Comment, Since Z2>Z3, so the reflection coefficient is negative and the polarity is reversed.



Question-4



Consider two reflectors, or interfaces between two layers. In the first case, the velocity of the upper layer is 2.5km/s and the velocity of the lower layer is 5.0km/s. In the second case, the velocity of the upper layer is 3.25km/s and the velocity of the lower layer is 4.75km/s if a ray travels downward



Subject: PE-309



Muhammad Fawwad Obaida



Roll No: PE-14041



through the top layer at an angle of incidence of 20 in each case, which will result in a larger angle of refraction. Solution For case-1 Using Snell’s law, (sinΦ/sinθ)=(Vl/Vu) sinΦ=(5/2.5)*sin(20) sinΦ=0.68404 Φ=sin^-1(0.68404) Φ=43.16degress For case-2 Using Snell’s law, (sinΦ/sinθ)=(Vl/Vu) sinΦ=(4.75/3.25)*sin(20) sinΦ=0.5 Φ=sin^-1(0.5) Φ=30 degrees Comment, Hence case-1 results in larger angle of refraction. Question-5 Below a flat, horizontal surface is a layer of 1500m thickness that has a constant velocity of 2500m/s. Twelve detectors are placed at 100m intervals from the source. Table 3.4 lists total path length to each detector. Determine T0 and NMO( T) for traces corresponding to each detector. List answers in ms. (1ms=1000s.)



Solution



Detector



Offset (m)



Reflection Path length (m)



Tj (sec)



ΔTj (sec)



ΔT (msec)



Subject: PE-309



1



Muhammad Fawwad Obaida



100



Roll No: PE-14041



3001.7



1.2006 8



0.0006 8



0.68



1.2026 8



0.0026 8



2.68



1.206



0.006



2



200



3006.7



3



300



3015



4



400



3026.5



1.2106



0.0106



10.6



0.0165 6



16.56



6



5



500



3041.4



1.2165 6



6



600



3059.4



1.2237 6



0.0237 6



23.76



7



700



3080.6



1.2322 4



0.0322 4



32.24



0.0419 2



41.92



8



800



3104.8



1.2419 2



9



900



3132.1



1.2528 4



0.0528 4



52.84



10



1000



3162.3



1.2649 2



0.0649 2



64.92



0.0781 2



78.12



0.0944 4



94.44



11



1100



3195.3



1.2781 2



12



1200



3236.1



1.2944 4



We know that, To=2Z/V Where ‘z’ is the thickness of the layer and ‘V’ is the velocity Hence, To=2(1500)/2500 =1.2sec Also, ΔTj =To+ΔTj j=1,2,3,4,……. ΔTj=Tj-ΔTo