Far-field approximation and the Kirchhoff method

is the propagation constant in free space and k sv ´ ´ m 22 Ž . zg g is the propagation constant in the ground. The scaling factors, A q and A y , are determined by Ž . evaluating Eq. 15 at the interface z s0. vm q y A sA s 23 Ž . k qk Ž . z zg Ž . Using this solution of Eq. 15 , the conjugate of Ž . the Green’s function, shown in Eq. 14 , takes the form k X x X U G , z ;v ž 2 vm s 1r2 1r2 X X 2 2 2 2 v k v k x 2 y q y ž ž ž ž Õ 2 c 2 = 1r2 X 2 2 ° ¶ v k 2 ~ • exp j y 2 z 24 Ž . ž ž ¢ ß Õ 2 while the image is expressed as S k X , k X Ž . x z Õ 2 mk X z s 1r2 2 2 Õ Õ X X 2 X 2 X 2 4 k q k q k yk z z x x ž ž ½ 5 c c = Õ 1r2 X X 2 X 2 U k ;vs k qk . 25 Ž . x z x ž 2

6. Far-field approximation and the Kirchhoff method

The general form for the matched-filter defi- nition of the image is expressed in the fre- quency domain as X X U T S r , v s U r ;v a G r , r , v O Ž . Ž . Ž . ˆ HH r r X X Y r G r , r , v a d rd v . 26 Ž . Ž . Ž . ˆ i t Fig. 3. Far-field approximation to monostatic scattering and collection. The configuration includes an x-directed X antenna, and a scatterer at a distance r yr from the antenna with only the u component of the scattering x matrix. In the monostatic radar configuration, both the transmitting and receiving antennas have the same location and like polarization. r sr Y 27 Ž . a sa sx 28 Ž . ˆ ˆ ˆ t r Furthermore, using a far-field approximation, the induced currents within the scattering object can be limited only to the u direction relative x to the transmitting antenna as shown by Fig. 3. This is expressed mathematically in the object scattering matrix. X X O r sO r 29 Ž . Ž . Ž . uu When the monostatic configuration and far-field Ž . approximation are applied to Eq. 26 , the im- age can be expressed with scalar values as S r X ;v s U U r;v G 2r X ,2r;v d r , 30 Ž . Ž . Ž . Ž . H u x where G is the u -directed field due to an u x x x-directed source and all dimensions have been increased by a factor of two due to the explod- ing reflector model. An expression for G is obtained from the u x Ž free-space dyadic Green’s function Chew, . 1990 , X 2 = = = = G yk Gsyjvmd ryr , 31 Ž . Ž . where 1 X 4 G r,r syjvm exp yjkR sin u , Ž . Ž . u x x 4p R 32 Ž . X R s r yr 33 Ž . and u is the angle between the x-axis and the x vector r X yr. An expression for the image is Ž . Ž . realized by substituting Eq. 32 into Eq. 30 . sin u Ž . x X S r ;v s jvm Ž . HH 8p R = 4 U exp yjk2 R U r,v d rd v 34 Ž . Ž . The integral over v can be divided into three operations on the measured response, U. The exponential represents sampling at y2 RrÕ while the complex conjugate translates into a time reversal. The combination of these two operations is equivalent to sampling the response at 2 RrÕ, which corresponds to the two-way travel time. Finally, the jv term is interpreted as a derivative operation in the time-domain. m sin u E 2 R Ž . x X S r s u r ;t s d r . 35 Ž . Ž . H ž 8p R Et Õ Ž . The form of Eq. 35 is similar to Kirchhoff migration, cos u E 2 R Ž . z X S r s u r ;t s d r . 36 Ž . Ž . H ž 2p RÕ Et Õ Ž . Ž . In Eq. 35 , the sin u term is a result of the Fig. 4. Two-dimensional configuration of four 4-in. diame- ter air-filled PVC pipes buried in dry sand. Fig. 5. Raw data with a linear gain applied. radiation pattern of a infinitesimal dipole, while Ž . Ž . in Eq. 36 the cos u is a result of the solution to Kirchhoff integral.

7. FDTD reverse-time migration