Spectrofluorometric properties of dissolved organic matter from Central and Southern Ontario streams and the influence of iron and irradiation.

Fluorescence measurements were used to compare characteristics of dissolved organic matter (DOM) from distinctly different origins: boreal, agricultural and urban streams as well as a storm runoff pond and the outlet of a tertiary wastewater treatment plant. The primary goal was to determine if differences among stream types could be detected using DOM fluorescence in lieu of isolated fulvic acids (FA). Differences in peak excitation and peak emission wavelengths, fluorescence integrated over the 3-D matrix volume integrated fluorescence (VIF), and in a fluorescence index (FI) were examined. In general, peak fluorescence excitation and emission wavelengths as well as FI best distinguished DOM from the various origins. Results suggested that DOM from the boreal streams was of a higher molecular weight and more complex than that of agricultural and urban streams. The effects of irradiation as well as Fe on fluorescence of natural stream waters were also investigated, both of which decreased the ability of optical properties to distinguish DOM source.