/******************************************************************************* * * McStas, version 1.0, released October 26, 1998 * Maintained by Kristian Nielsen and Kim Lefmann, * Risoe National Laboratory, Roskilde, Denmark * * Component: Mon_2foc * * %Identification * Written by: PL * Date: Feb. 12,1999 * Origin: Uni. Gottingen (Germany) * version: 1.0 * * Double bent monochromator with multiple slabs * * %Description * Double bent monochromator which uses a small-mosaicity approximation as well * as the approximation vy^2 << vz^2 + vx^2. * Second order scattering is neglected. * For an unrotated monochromator component, the crystal plane lies in the y-z * plane (ie. parallel to the beam). * * Added double bent feature by: Peter Link Feb. 12,1999 * corrected bug in rotation of v-coords: Peter Link Sep. 24. 1999 * * %Parameters * INPUT PARAMETERS: * * zwidth: horizontal width of an individual slab (m) * ywidth: vertical heigth of an individual slab (m) * gap: typical gap between adjacent slabs (m) * NH: number of slabs horizontal (columns) * NV: number of slabs vertical (rows) * mosaich: Horisontal mosaic FWHM (arc minutes) * mosaicv: Vertical mosaic FWHM (arc minutes) * R0: Maximum reflectivity (1) * Q: Scattering vector (AA-1) * RV: radius of vertical focussing (m) * RH: radius of horizontal focussing (m) * * %Link * Additional note from Peter Link. * * %End *******************************************************************************/ DEFINE COMPONENT Mon_2foc DEFINITION PARAMETERS (zwidth, ywidth, gap, NH, NV, mosaich, mosaicv, r0, Q, RV, RH) SETTING PARAMETERS () STATE PARAMETERS (x,y,z,vx,vy,vz,t,s1,s2,p) DECLARE %{ #define DIV_CUTOFF 2 /* ~ 10^-5 cutoff. */ %} TRACE %{ double dphi,tmp1,tmp2,tmp3,tmp4,vratio,phi,theta0,theta,v,cs,sn; double zmin,zmax,ymin,ymax,zp,yp,row,col; double tilth,tiltv; /* used to calculate tilt angle of slab */ double sna,snb,csa,csb,vxp,vyp,vzp; double old_x = x, old_y = y, old_z = z, old_t = t; double dt; if(vx != 0.0 && (dt = -x/vx) >= 0.0) { zmax = ((NH*(zwidth+gap))-gap)/2; zmin = -1*zmax; ymax = ((NV*(ywidth+gap))-gap)/2; ymin = -1*ymax; y += vy*dt; z += vz*dt; t += dt; x = 0.0; zp = fmod ( (z-zmin),(zwidth+gap) ); yp = fmod ( (y-ymin),(ywidth+gap) ); /* hit a slab or a gap ? */ if (z>zmin && zymin && y DIV_CUTOFF) { x = old_x; y = old_y; z = old_z; t = old_t; } else { p *= r0*exp(-tmp3*tmp3*4*log(2)); /* Use mosaics */ tmp1 = 2*theta; cs = cos(tmp1); sn = sin(tmp1); tmp2 = cs*vxp - sn*vzp; vyp = vyp; /* vz = cs*vz + sn*vx; diese Zeile wurde durch die folgende ersetzt */ tmp4 = vyp/vzp; /* korrigiert den schrägen Einfall aufs Plättchen */ vzp = cs*(-vyp*sin(tmp4)+vzp*cos(tmp4)) + sn*vxp; vxp = tmp2; /* Second: scatering out of plane. Approximation is that Debye-Scherrer cone is a plane */ phi = atan2(vyp,vzp); /* out-of plane angle */ dphi = (MIN2RAD*mosaicv)/(2*sqrt(2*log(2)))*randnorm(); /* MC choice: */ /* Vertical angle of the crystallite */ vyp = vzp*tan(phi+2*dphi*sin(theta)); vratio = v/sqrt(vxp*vxp+vyp*vyp+vzp*vzp); vzp = vzp*vratio; vyp = vyp*vratio; /* Renormalize v */ vxp = vxp*vratio; } /* rotate v coords back */ vx = vxp*csb*csa-vyp*snb*csa+vzp*sna; vy = vxp*snb+vyp*csb; vz = -vxp*csb*sna+vyp*snb*sna+vzp*csa; v=sqrt(vx*vx+vy*vy+vz*vz); } else { x = old_x; y = old_y; z = old_z; t = old_t; } } %} MCDISPLAY %{ double zmin,zmax,ymin,ymax; int ih,iv; magnify("xy"); for(ih = 0; ih < NH; ih++) { for(iv = 0; iv < NV; iv++) { zmin = (zwidth+gap)*(ih-NH/2.0)+gap/2; zmax = zmin+zwidth; ymin = (ywidth+gap)*(iv-NV/2.0)+gap/2; ymax = ymin+ywidth; multiline(5, 0.0, (double)ymin, (double)zmin, 0.0, (double)ymax, (double)zmin, 0.0, (double)ymax, (double)zmax, 0.0, (double)ymin, (double)zmax, 0.0, (double)ymin, (double)zmin); } } %} END