  The Lyman edge at 912 \AA is an important diagnostic region for studying
quasi-stellar objects (QSOs). In particular, it reveals a great deal about the
physical conditions within the atmospheres of accretion disks, a ubiquitous
component of QSO theories. A robust prediction of accretion disk models is a
significant polarization due to electron scattering just longward (in
wavelength) of the Lyman edge because of the wavelength dependence of the
Hydrogen absorption opacity. Observations of the Lyman edge regions of QSOs
have shown scant evidence for the predicted features-few QSOs show the broad,
partial Lyman edges expected to be common according to most theories, and none
show the high polarizations expected longward of the Lyman edge. Still,
polarization spectra of a small number of QSOs have shown a rising polarization
(up to 20%) at wavelengths shortward of the Lyman edge. We have now doubled our
sample of intermediate-redshift QSOs observed with the HST/FOS
spectropolarimeter to determine the amount of polarization on both sides of the
Lyman limit. For this new sample of six objects, polarizations are low and
mostly consistent with zero below the Lyman edge.
  Another important result of the new data is that it strengthens the
conclusion that quasars are generally not polarized significantly just longward
of the Lyman edge at $\sim 1000 \AA. There is no significant statistical
wavelength dependence to the polarization longward of the Lyman edge indicating
that simple plane-parallel atmospheres with scattering-dominated opacity are
not significant sources of UV flux in quasars.
