IMAGE, RADON, AND FOURIER SPACE F1D R f ( , t )(t ) F2 D f ( x, y)(x t cos , y t sin ) FILTERED BACK-PROJECTION FOR PLANAR PARALLEL PROJECTIONS f ( x, y) 2 0 R f ( , t ) g (t )( , t x cos y sin ) d P convolution back-projection ramp filter 1 j t t g (t ) F t e dt t 2π P 1 1D FILTERED BACK-PROJECTION FOR FAN BEAM PLANAR DETECTOR CASE y a Fan beam projection on linear detector: pF(,a) arct an P(x,y) a , R P’ a t R sin R sin arct an R S x R U 1) Weighing by cos and ramp filtering F R p (, a ) p (, a ) R2 a2 F g P (a ) p F (, a ) cos g P (a ) 2) Back-projection R2 F f FBPF (x, y) p (, a (x, y, ))d 2 U(x, y, ) 2 0 x sin y cos a ( x, y, ) R , U( x, y, ) R x cos y sin R x cos y sin CONE BEAM PROJECTIONS ON FLAT PANEL DETECTORS Flat Panel Detector RX CONE z, b RX SOURCE y a R t an a b R 2 a 2 t an arct an a R arct an b R2 a2 VIRTUAL DETECTO R x FELDKAMP, DAVIS, KRESS (FDK) ALGORITHM (1984) Approximated Filtered Back-Projection for cone-beam and circular trajectory Satisfactory approximation even with quite high copolar angles (e.g., 20°) It reconstructs the volume crossed by rays at any source position on the circles; hence a cilinder plus two cones. z, b detector inclined fan z S Sorgente Fan a FDK ALGORITHM z, b 1) Weighing by coscos : R R 2 a 2 b2 p F (, a, b) cos cos p F (, a, b) y P(x,y) a P’ 2) Row by row filtering with the ramp filter p F (, a, b) cos cosp F (, a, b) g P (a) S virtual planar detector 3) Back-projection f FDK ( x, y, z ) 2 0 R2 U ( x, y, ) 2 p F ( , a( x, y, ), b( x, y, z, ))d x sin y cos R , b( x, y, z, ) z R x cos y sin R x cos y sin U( x, y, ) R x cos y sin a ( x, y, ) R x FDK PROPERTIES FDK algorithm is an approximate extension to the 3D cone beam case on planar detector of the 2D 1) Exact on the central plane, z=0, where it coincides with the Fan Beam solution 2) Exact for objects homogeneous along z, f(x,y,z) = f(x,y). 3) Integrals along z, f(x,y,z)dz, is preserved 4) Integrals on moderately tilted lines preserved as well Main artifact: blurring along z at high copolar angles FDK artifact Satisfactory reconstructions were demonstrated even at fairly high copolar angles (40°-50°). Usually much lower copolar angles are exlored (10°) in the field of view, with higher precision. Theory of 3D reconstruction from projections RADON TRANSFORM IN 3D The full Radon transform implies integration of volume over planes which are projected on a point located at the intercept of the normal line through the origin integration plane Eˆ ,t : r ˆ t , z x ( x, y , z ) T integration plane 0 versor normal to the integration plane ˆ( , ) (sin cos , sin sin , cos )T Radon value t ˆ Rf (, , t) f (x )(x ˆ t) dx R f ( , , t ) p 2 D ( , ) (t ) x x y CENTRAL SECTION THEOREM IN 3D – FULL RADON TRANSFORM Full Radon transform, 2D projection of parallel planes on the orthogonal axis R f ( , , t ) p 2 D ( , ) (t ) F3 D f ( x, y, z )(0,0, t ) f ( x, y, z )e ( r r s s tt ) dr ds dt |r 0 s 0 2tt f ( x, y, z )drds e dt F1D p2 D (t )(t ) Result: The 1D Fourier transform of the projection axis t gives the 3D Fourier values on the corresponding axis t THE FULL RADON TRANSFORM IS A SUFFICIENT DATA SET FOR 3D IMAGE RECONSTRUCTION Rf(,,t) z f(x,y,z) z F3Df(x, y, z) z F1D t t y y y x x x . F3D A complete set of data is defined if all integration planes through the object are present. The subset of parallel planes defined by the normal direction (,) fill the radial axis with the same direction in F3Df(x,y,z). So we need 2 directions times parallel shifts; i.e., 3 planar integrations. These can be provided by 2 planar projections. CENTRAL SECTION THEOREM IN 3D – PARTIAL RADON TRANSFORM Partial Radon transform, p1D, r (s,t) = projection of lines parallel to a ray axis r on the orthogonal projection plane at coordinates (s,t) The 2D Fourier transform of projected values on the projection plane (s,t) gives the 3D Fourier values on the corresponding plane frequency domain plane (s , t) F3 D f ( x, y, z )(0, s , t ) f ( x, y, z )e 2 ( rr ss tt ) dr ds dt |r 0 2 ( ss tt ) f ( x , y , z ) dr ds dt F2 D p1D ,r ( s, t )(s , t ) e Deriving Full Radon (integrals on planes) Transform from Partial Radon Transform (line integrals) projection plane integration plane E rˆ,0 (s, t ) z z E ˆt ,t (r, s) 0 s s r F3D r t t t0 y x p 1D , r y x ( s, t t0 )ds p2 D ,( , ) (t t0 ) t t 0 Points on a projection plane represent 1D line integrals parallel to r. A further integration on a line t=t0 correspond to a 2D integration on a plane orthogonal to t and a distance t0 from the origin. Hence the Full Radon Transform sample in position (r=0, s=0, t=t0) . Note that 1D projections are much more informative than 2D projections, due to lesser integration: a 1D projection on a plane fills an entire plane in the 3D Radon and Fourier spaces REDUNDANCY OF PROJECTIONS ON ALL PLANES 1. Projections planes are 2 (azimuth and polar angle). In each plane 2 integration lines can be defined. Hence 4 values are found; i.e., each Radon Transform point is found in ways. Indeed, the same can be computed on the family of projection planes containing axis t and fill the corresponding axis in the Full Radon Transform and in the 3D Fourier space. 2. Equivalently, the Central Section Th. (in the Partial Radom Transform version), says that by transforming a planar projection an entire plane (2 points) is filled in the 3D Fourier space. Given the 2 planar projections we obtain a redundancy of 3 over 4 , again. In conclusion, a set of 1 directions filling the Radon Space and the Fourier space is sufficient for the reconstruction. Passing from parallel projections to cone beam projections an appropriate trajectory of the focal spot passing through 1 points can cover the entire 3D transform spaces if it satisfies proper conditions (see Tuy Smith sufficient condition in the next slide). SUFFICIENT SET OF DATA IN 3D FOR CONE BEAM Tuy-Smith sufficient condition (1985): A cone-beam projection permits to derive the integral of each plane passing through the source S. Hence, if the source in its trajectory encounters each plane through the object a sufficient set is obtained Explanation: Any plane (,,t) through S is filled by X-rays and we know the integral (1D projection) along them; the 2D projection of the plane (i.e., integral over the plane) can be derived by summing up the 1D projection values giving a 3D Radon sample Rf(,,t). Note that 2 planes pass through a point S, which multiplied by positions of S on the trajectory can fill all the 3D Radon space, if a proper trajectory is chosen. trajectory of S z t S plane (,,t) touched by S y x corresponding point of Radon Transform Rf(,,t) ALMOST SUFFICIENT SET OF DATA IN 3D FOR CONE BEAM A cone-beam projection permits to derive the integral of each plane passing through the source. Hence, if the source in its trajectory encounters each plane through the object a sufficient set is obtained. This is the Tuy-Smith sufficient condition (1985). A circular trajectory, most often used, satisfies this condition only partially: planes parallel to the trajectory are never encountered. Hence, a torus is filled in Radon space with a hole, called shadow zone, close to the rotation axis z. z z shadow zone x y x x TRAJECTORIES SATISFYING TUY-SMITH CONDITION 1. helics (used in multislice “spiral” CT) 2. two non parallel circles (possibly used in C arm cone beam) 3. circle and line (just theoretical)