Spectrofluorometric characterization of dissolved organic matter for indication of precursor organic material and aromaticity

Citation
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
Citations number
43
Categorie Soggetti
Aquatic Sciences
Journal title
LIMNOLOGY AND OCEANOGRAPHY
ISSN journal
00243590 → ACNP
Volume
46
Issue
1
Year of publication
2001
Pages
38 - 48
Database
ISI
SICI code
0024-3590(200101)46:1<38:SCODOM>2.0.ZU;2-I
Abstract
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.