Dm. Mcknight et al., Spectrofluorometric characterization of dissolved organic matter for indication of precursor organic material and aromaticity, LIMN OCEAN, 46(1), 2001, pp. 38-48
We studied the fluorescence properties of fulvic acids isolated from stream
s and rivers receiving predominantly terrestrial sources of organic materia
l and from lakes with microbial sources of organic material. Microbially de
rived fulvic acids have fluorophores with a more sharply defined emission p
eak occurring at lower wavelengths than fluorophores in terrestrially deriv
ed fulvic acids. We show that the ratio of the emission intensity at a wave
length of 450 nm to that at 500 nm, obtained with an excitation of 370 nm,
can serve as a simple index to distinguish sources of isolated aquatic fulv
ic acids. In our study, this index has a value of similar to1.9 for microbi
ally derived fulvic acids and a value of similar to1.4 for terrestrially de
rived fulvic acids. Fulvic acids isolated from four large rivers in the Uni
ted States have fluorescence index values of 1.4-1.5, consistent with predo
minantly terrestrial sources. For fulvic acid samples isolated from a river
, lakes, and groundwaters in a forested watershed, the fluorescence index v
aried in a manner suggesting different sources far the seepage and streamfe
d lakes. Furthermore, we identified these distinctive fluorophores in filte
red whole water samples from lakes in a desert oasis in Antarctica and in f
iltered whole water samples collected during snowmelt from a Rocky Mountain
stream. The fluorescence index measurement in filtered whole water samples
in field studies may augment the interpretation of dissolved organic carbo
n sources for understanding carbon cycling in aquatic ecosystems.