Samples of sediments taken from the River Saale at different locations
were investigated by thermogravimetry, differential thermal analysis,
mass spectrometry and FTIR spectroscopy. The thermal behaviour of the
se sediments varied significantly depending on contents of organic and
inorganic compounds. The variable organic loading resulted from the d
ifferent degrees of treatment of communal or industrial waste water. M
ass spectrometric investigations in the lower temperature ranges demos
trated humic substances as essential components. The mineral component
s in the river sections of the slate mountains differed significantly
from those of the shell limestone. The results of FTIR analysis of the
se samples confirmed well with the findings of thermoanalytical invest
igations.