We report on two recent X-ray observations of the intermediate polar T
X Col made with ASCA and ROSAT, From a consideration of the power spec
tra of their light curves, we show that the system was accreting predo
minantly via a disc in 1994 October, but had reverted to a discover fl
ow mode of accretion by 1995 October, at which time a substantial amou
nt of the accretion was directly via a stream. We discuss possible rea
sons for this change, By considering the relative phases of the spin a
nd beat pulsations seen in the ROSAT data, as well as their orbital ha
rmonics, we demonstrate that the stream-fed accretion regions on the w
hite dwarf surface remain fixed at about orbital phase 0.7, and thus m
igrate around the white dwarf, We suggest that the observed orbital mo
dulation results from a combination of two effects: first, attenuation
of emission sites by material located at the stream-disc boundary at
orbital phase 0.8, and, secondly, the changing visibility of the strea
m-fed accretion sites which are always on the side of the white dwarf
facing the stream.