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2<br />

(a) Transform the isotropic ray tracing system<br />

dp<br />

dσ<br />

= S(x) ∇S (1)<br />

dx<br />

dσ = p (2)<br />

dT<br />

dσ = S2 (x) (3)<br />

into an equivalent system that uses ξ instead of σ, where ξ is constrained<br />

by equation (4):<br />

dp<br />

dξ<br />

dx<br />

dξ<br />

dT<br />

dξ<br />

What are the physical units of ξ?<br />

= ∇S<br />

S 2 (x)<br />

(4)<br />

= (5)<br />

= (6)<br />

(b) Suppose you are given T (x) – the traveltime from the source to all points<br />

x in the domain of interest. Your task is to find ξ(x) for all x. Derive a<br />

first-order partial differential equation that connects ∇ξ and ∇T .<br />

2. The so-called “parabolic” or 15 ◦ eikonal equation (Tappert, 1977; Claerbout,<br />

1985; Bamberger et al., 1988) has the form<br />

∂T<br />

+ 1<br />

∂x 1 2 S(x)<br />

( ∂T<br />

∂x 2<br />

) 2<br />

= S(x) (7)<br />

where x = {x 1 , x 2 } is a point in space, T (x) is the traveltime, and S(x) is<br />

slowness.<br />

(a) Derive the ray tracing system for equation (7)<br />

dx 2<br />

dx 1<br />

= (8)<br />

dp 1<br />

dx 1<br />

= (9)<br />

dp 2<br />

dx 1<br />

= (10)<br />

dT<br />

dx 1<br />

= (11)<br />

where p 1 represents ∂T/∂x 1 and p 2 represents ∂T/∂x 2 .<br />

(b) Assuming constant slowness S(x) ≡ S 0 , solve the ray tracing system for a<br />

point source at the origin {x 1 , x 2 } = {0, 0}.

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