Stokes-V and I spectra of sunspot structures have been observed simult
aneously in the lines Fe 6843 and Ca 6103 originating from layers whic
h differ by more than 350 km. The Fe line is totally split thus allowi
ng to deduce the field strength from the Stokes-I and V profiles. Both
splitting values yield a field strength reduction up to 20% in bright
er (peripheral) dots at the umbral border. This reduction is not seen
in the higher layer where the Ca line originates. The faint (central)
dots do not exhibit a field strength difference with respect to their
darker surroundings. Using the ratio of pi to sigma depressions of the
totally split Fe 6843 line as a measure for the field inclination, th
e field lines are found to be essentially flatter in a light bridge th
an in its neighbourbood. Flatter fields are also found in some of the
peripheral dots. The Doppler shifts of the Fe and of the Ca line devia
te significantly from each other but do not show a relation to the umb
ral structures.