We present results from X-ray observations of the intermediate polars
AO Pac and V1223 Sgr, taken with the ROSAT HRI and the Ginga LAG. Both
sources show sinusoidal modulation at the white dwarf spin period in
all energy bands, possibly with the exception of the highest. The dept
hs of these modulations increase at lower energy, but the rates at whi
ch they do so are not consistent with single column densities of absor
bing material. Neither source shows any significant pulse at the beat
period, which argues for a predominantly disc-fed accretion model in e
ach case. The AO Psc observations show a modulation at the orbital per
iod, which in the ROSAT data may indicate an extended absorbing struct
ure, with a dip at orbital phase similar to 0.5-0.8 superimposed. The
V1223 Sgr ROSAT data show short dips which occur intermittently at aro
und orbital phase 0.8. These dips vary in duration and phase of commen
cement and suggest that the system inclination angle is just sufficien
t for our line of sight to graze the upper extent of the material thro
wn out of the disc plane.