Mj. Pullin et Se. Cabaniss, PHYSICOCHEMICAL VARIATIONS IN DOM-SYNCHRONOUS FLUORESCENCE - IMPLICATIONS FOR MIXING STUDIES, Limnology and oceanography, 42(8), 1997, pp. 1766-1773
Synchronous fluorescence (SF) spectra of dissolved organic matter (DOM
) show promise for mixing studies and can resolve multiple river input
s to large water masses in a single fast measurement. This study exami
nes the effects of physicochemical variables on DOM SF; independent of
mixing. Our results show that changes in the pH and metal ion concent
ration do not affect SF in the alkaline Cuyahoga-Erie system. The effe
ct of temperature is small and correctable. Model predictions suggest
that photobleaching of DOM SF can limit the use of this method to shor
t periods (3-7 d, depending an conditions). SF spectra are sensitive e
nough to detect 1% river water mixed in Lake Erie water.