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SUEA2DF - SU version of (an)elastic anisotropic 2D finite difference forward modeling suea2df > outfile c11file= c55file [optional parameters] Required Parameters: c11file=c11_file c11 voigt elasticity parameter filename c55file=c55_file c55 voigt elasticity parameter filename Optional Parameters: rhofile=rho_file density filename Anisotropy parameters: aniso=0 =1 - include anisotropy parameters mode=0 =0 output particle velocity, =1 output stresses (snapshots only) ... the next 3 parameters become active only when aniso=1.... c13file=c13_file c13 voigt elasticity parameter filename c33file=c33_file c33 voigt elasticity parameter filename c15file=c15_file c15 voigt elasticity parameter filename c35file=c35_file c35 voigt elasticity parameter filename dt=0.001 time sampling interval (s) ft=0.0 first time (s) lt=1.0 last time (s) nx=200 number of values in slow (x-direction) dx=10.0 spatial sampling interval (m) x-coor fx=-1000 first x coor (m) nz=100 number of values in fast (z)-dimension dz=dx spatial sampling interval (m) z-coor fz=0 firstz coor (m) Source parameters: sx=0 source x position (m) sz=500 source location (m) stype='p' source type p: P-wave v: velocity pw: P plane-wave sang=0 for stype='pw': plane wave angle wtype='dg' wave type dg: Gaussian derivative ga: Gaussian ri: Ricker sp: spike, sp2: double spike ts=0.05 source duration (s) favg=50 source average frequency Attenuation parameters: ql= model q at xl,zl qsw=0 switch to include attenuation =1 - include Boundary condition parameters: bc=10,10,10,10 Top,left,bottom,right boundary condition =0 none =1 symmetry =2 free surface (top only) >2 absorbing (value indicates width of absorbing layer bc_a=0.95; bc initial taper value for absorbing boundary bc_r=0.; bc exponential factor for absorbing boundary variables are scaled by bc_a*pow(i,-bc_r) Output parameters: sofile= name of source file snfile= name of file containing for snapshots snaptime= times of snapshots i.e. snaptime=0.1,0.2,0.3 vsx= x coordinate of vertical line of seismograms hsz= z coordinate of horizontal line of seismograms vrslfile="vsp.su" output file for vertical line of seismograms[nz][nt] hsfile="hs.su" output file for horizontal line of seismograms[nx][nt] tsw=0 switch to use shear stress only in non-fluid media - may help reduce dispersion tsw=1. If tsw=0 then standard calculation verbose=0 =1 to print progress on screen Notes: 1) The outfile contains information generated by the input parameters, such as memory allocation, stability, etc. If your input file does not work, check this file first. The model is specified as binary files of stiffness parameters and densities. These may be created any way the user desires. The program unif2 or makevel may be used to generate densities, and the program unif2aniso may be used to generate the stiffnesses. You will need to transpose these files, as the input format for suea2df assumes that the fast dimesion is the horizontal or the x-dimension. You may do this via transp n1=nz < c11_file > transp_c11_file If qsw=1 a ql array specifies the values of the quality factor Q, to specify the attenuation of the medium. If aniso=1 then the program will expect the additional stiffnesss files. The epl and dsl are epsilon and delstar in Thomson (1986, Geophys.) anl is the angle the anisotropy makes with the horizontal. Output files (always generated) hsfile vrslfile hsfile.chd - header for hsfile vrslfile.chd - header for vrslfile hsfile.mod - model file Output files (if requested) sofile - ascii source file snfile - su format snapshots file Credits: UU GEOPHY Chris Juhlin 15 May 1999 Copyright (c) Uppsala University, 1998. All rights reserved. Parts of program use Seismic Unix Package - CSM Changes - C. Juhlin 1. Fixed upgrading of stresses. There was an error in the coding for the Tzz term, c15 was being used instead of c35. This only caused problems for dipping anisotropic layers 2. Added some header information for hutput of snapshots. 3. 2001-01-30: Added option to set absorbing bc constants bc_a and bc_r 4. 2001-02-23: Corrected bug in outputting model boundaries to standard output in routine get_econst 5. 2001-04-26: Added option for updating velocities to only use shear stress if material is non-fluid, this appears to reduce dispersion at near grazing angles for fluid-solid boundary. Set tsw=1 to invoke 6. 2001-05-14: Changed loop in free-surface boundary condition for velocties Thanks goes to Mike Holzrichter for pointing out this problem and the wrong scaling factor in the updating. 7. 2001-05-16: Changed set_layers function to avoid negative indexing. Thanks goes to Mike Holzrichter for pointing out this problem 8. 2001-05-17: Modified make_seis to take into account VSP geometry correctly and not store unnecessary data. 9. 2001-08-21: Fixed set_layers so mode fills properly in depth. Earlier versions were accessing incorrect array locations at last defined depth. 10. 2003-04-21: Fixed boundary conditions. 11. 2003-05-02: Extended the model area by half the grid spacing on the RHS. This makes the model area symmetric allowing a plane wave source to be introduced into the model (stype=pw). The w, txx and tzz grids contain now one more column than the u and txz grids. 12. 2003-05-02: Added routines to allow plane waves to be introduced at a specified angle (sang) into the model with functions add_pw_source_V and add_pw_source_S. 13. 15 Oct 2005 -- tossed all the model building stuff. Read models from binary files made by unif2aniso Alogrithm based on Juhlin (1995, Geophys. Prosp.) and Levander (1988, Geophysics) Attenuation included as in Graves (1996, BSSA)
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