Wildfires
generate significant amounts of ash and burned soils
that can leach altered dissolved organic matter (DOM) to watersheds.
In this work, we analyzed the absorbance and fluorescence spectrum
of DOM leached from 40 ash and soil samples collected from two conifer
forest burn scars. DOM fluorescence quantum yield at 350 nm (ϕf350) was elevated in all ash and burned soil leachates. Wildfire
DOM fluorescence was also consistently shifted toward the ultraviolet
(UV) region relative to unburned materials, which limited the utility
of several pre-defined optical indices, such as the humification index
(HIX) and SUVA254, for wildfire DOM differentiation. In
contrast, E2:E3 and ϕf350 resolved
differences between ash, burned mineral soil, and unburned soil DOM
across an assortment of physical settings. Mixtures of a freshwater
DOM reference material and wildfire ash leachate confirmed that specific
fluorescence peaks A and C, ϕf350, and E2:E3 were well correlated (R
2 > 0.92) to mass increases of ash-derived DOM. These findings
were
compared to 31 surface water samples collected from burned tributaries
within the Cameron Peak Fire burnscar. Surface waters draining from
the burn scar were also elevated in ϕf350, E2:E3, SUVA254, FI, and UV-shifted fluorescence
peaks A and C at intensities comparable to ash mixing experiments.