Aluminum-induced aggregates of terrestrial and aquatic humic acid standards
from the International Humic Substances Society are shown to be fluorescen
t by means of a multiwavelength fluorescence anisotropy experiment in which
the data was treated with a model for nonspherical particles. While aggreg
ates of aquatic humic acids appear in the fluorescence signal at both short
and long excitation wavelengths, aggregates of terrestrial humic acids are
detected only at the long wavelength. Furthermore, the results indicate th
at emission obtained at longer excitation wavelengths is representative of
smaller particles. At pH 4, the aquatic humic acids appear to exist in an e
xtended conformation, whereas the terrestrial humic acids show less extensi
on. The size and shape of the fluorescent particles display a complex depen
dence on Al concentration. Both enhancement and quenching of fluorescence a
re observed in the total luminescence spectra upon Al addition. However, qu
enching is shown to be the result of decreased humic acid concentration due
to precipitation by Al rather than photophysical processes.