We describe fits to the Ginga LAC and ASCA GIS and SIS X-ray spectra of the
intermediate polar V1223 Sgr using a multi-temperature emission model and
including reflection from the white dwarf surface. Shock temperatures of T-
S = 30(-4)(+12), 54(-15)(+26) and 47(-12)(+30)keV were obtained for the Gin
ga LAC, ASCA GIS and SIS instruments, respectively, giving a mean value of
47(-12)(+13)keV. The data reveal significant amounts of reflection as well
as a heavy metal underabundance by a factor of similar to 2.
Multiple absorption components are required to successfully model the obser
ved X-ray spectra at low energies, suggesting the presence of complex intri
nsic absorption. All data sets reveal a low-energy spectral hardening at th
e minimum in the spin cycle caused by an increase in the amount of absorpti
on at this phase. The requirement of such complex absorption is becoming in
creasingly common in the good quality X-ray spectra from magnetic cataclysm
ic variables.