  We present the first analysis of an EUV selected sample of hot DA white
dwarfs using a new type of atmospheric models. These models take into account
the interplay between gravitational settling and radiative acceleration to
predict the chemical stratification from an equilibrium between the two forces
while self-consistently solving for the atmospheric structure. In contrast to
atmospheric models with the assumption of chemical homogeneity, the number of
free parameters in the new models is reduced to the effective temperature and
surface gravity alone. The overall good reproduction of observed EUV spectra
reveals that these models are able to describe the physical conditions in hot
DA white dwarf atmospheres correctly. A comparison with previous analyses
highlights the improvements as well as the limits of our new models.
