Fluorescence and Absorbance Indices for Dissolved Organic Matter from Wildfire Ash and Burned Watersheds
Sarah J. Fischer,
Timothy S. Fegel,
Paul J. Wilkerson
et al.
Abstract: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, whi… Show more
“…In addition, based on the small heating temperature interval, we found that the fluorescence index (FI) increased, the biological index first increased and then decreased, and the humification index (HIX) first decreased and then increased with heating temperature (Figure S3). Such results complemented a recent study that found wildfires elevated the FI and HIX values of DOM …”
Heating
temperature (HT) during forest fires is a critical factor
in regulating the quantity and quality of pyrogenic dissolved organic
matter (DOM). However, the temperature thresholds at which maximum
amounts of DOM are produced (TTmax) and at which the DOC
gain turns into net DOC loss (TT0) remain unidentified
on a component-specific basis. Here, based on solid-state 13C nuclear magnetic resonance, absorbance and fluorescence spectroscopies,
and Fourier transform ion cyclotron resonance mass spectrometry, we
analyzed variations in DOM composition in detritus and soil with HT
(150–500 °C) and identified temperature thresholds for
components on structural, fluorophoric, and molecular formula levels.
TTmax was similar for detritus and soil and ranged between
225 and 250 °C for bulk dissolved organic carbon (DOC) and most
DOM components. TT0 was consistently lower in detritus
than in soil. Moreover, temperature thresholds differed across the
DOM components. As the HT increased, net loss was observed initially
in molecular formulas tentatively associated with carbohydrates and
aliphatics, then proteins, peptides, and polyphenolics, and ultimately
condensed aromatics. Notably, at temperatures lower than TT0, particularly at TTmax, burning increased the DOC quantity
and thus might increase labile substrates to fuel soil microbial community.
These composition-specific variations of DOM with temperature imply
nonlinear and multiple temperature-dependent wildfire impacts on soil
organic matter properties.
“…In addition, based on the small heating temperature interval, we found that the fluorescence index (FI) increased, the biological index first increased and then decreased, and the humification index (HIX) first decreased and then increased with heating temperature (Figure S3). Such results complemented a recent study that found wildfires elevated the FI and HIX values of DOM …”
Heating
temperature (HT) during forest fires is a critical factor
in regulating the quantity and quality of pyrogenic dissolved organic
matter (DOM). However, the temperature thresholds at which maximum
amounts of DOM are produced (TTmax) and at which the DOC
gain turns into net DOC loss (TT0) remain unidentified
on a component-specific basis. Here, based on solid-state 13C nuclear magnetic resonance, absorbance and fluorescence spectroscopies,
and Fourier transform ion cyclotron resonance mass spectrometry, we
analyzed variations in DOM composition in detritus and soil with HT
(150–500 °C) and identified temperature thresholds for
components on structural, fluorophoric, and molecular formula levels.
TTmax was similar for detritus and soil and ranged between
225 and 250 °C for bulk dissolved organic carbon (DOC) and most
DOM components. TT0 was consistently lower in detritus
than in soil. Moreover, temperature thresholds differed across the
DOM components. As the HT increased, net loss was observed initially
in molecular formulas tentatively associated with carbohydrates and
aliphatics, then proteins, peptides, and polyphenolics, and ultimately
condensed aromatics. Notably, at temperatures lower than TT0, particularly at TTmax, burning increased the DOC quantity
and thus might increase labile substrates to fuel soil microbial community.
These composition-specific variations of DOM with temperature imply
nonlinear and multiple temperature-dependent wildfire impacts on soil
organic matter properties.
“…GDS-1 shows the lowest yield (1.1 g DOC kg –1 char C) followed by GDS-4 (2.1 g DOC kg –1 char C) and then GDS-30 (3.4 g DOC kg –1 char C). The low DOC yields are similar to those previously observed for laboratory-produced , and natural , chars and reflect the dominance of low solubility ConAC structures in the solid char samples.…”
An extensive body of research demonstrates that the molecular composition of pyrogenic organic matter (PyOM, also known as "black carbon") and dissolved PyOM (PyDOM) influences its properties and fate in the environment. The properties of PyOM and PyDOM are also well-known to be governed by their production conditions (e.g., combustion temperature). However, numerous physical and oxidative aging processes in the environment influence PyOM's chemical properties with unclear impacts on its cycling and fate. Here, the solid and aqueous leachate chemical characteristics of wildfire-derived chars aged 1, 4, and 30 years from the Great Dismal Swamp, USA, were examined to explore the effects of environmental aging. Solid-state 13 C NMR spectroscopic and elemental analyses show the most aged char to have the highest H/C and O/C ratios and lowest aromatic contents, yet it also had the highest benzene polycarboxylic acid (BPCA) marker compound yield and degree of aromatic condensation. In PyDOM leachates, increased char aging correlated with increased dissolved organic carbon and BPCA yields as well as with lower H/C and O/C ratios derived from molecular formulas obtained by ultrahigh-resolution mass spectrometry. These results are inconsistent with established combustion continuum molecular-level relationships, suggesting that aging processes govern long-term PyOM and PyDOM molecular compositions. We suggest that hydrological and oxidative aging processes of PyOM selectively remove an oxygenated, less aromatic fraction yielding lower H/C and O/C ratios in residual PyOM. Subsequently, only the most highly condensed aromatic compounds are available for oxidation and transport as PyDOM. Thus, while a combustion continuum describes the initial PyOM and PyDOM molecular characteristics, an aging continuum may better describe those characteristics on annual to decadal time scales, and PyOM losses as PyDOM are likely greater than those estimated from laboratory or fresh chars.
“…Dissolved organic carbon (DOC) and total dissolved nitrogen (TDN) were simultaneously measured on a Shimadzu TOC-L Total Organic Carbon Analyzer in precombusted amber vials within a week of leaching and filtering. Leached C and N in mg g C –1 were calculated as in eq of Fischer et al: Leachable.25emDOC.25em(mggC−1)=DOC.25em(mgL−1)×leaching.25emvolume.25em(L)/mass.25emof.25emdry.25emmaterial.25em(g)×normalC.25emcontent.25emof.25emdry.25emmaterial.25em(mgCg−1)…”
Section: Methodsmentioning
confidence: 99%
“…Dissolved organic carbon (DOC) and total dissolved nitrogen (TDN) were simultaneously measured on a Shimadzu TOC-L Total Organic Carbon Analyzer in precombusted amber vials within a week of leaching and filtering. Leached C and N in mg g C –1 were calculated as in eq of Fischer et al: …”
Wildfires
produce solid residuals that have unique chemical and
physical properties compared to unburned materials, which influence
their cycling and fate in the natural environment. Visual burn severity
assessment is used to evaluate post-fire alterations to the landscape
in field-based studies, yet muffle furnace methods are commonly used
in laboratory studies to assess molecular scale alterations along
a temperature continuum. Here, we examined solid and leachable organic
matter characteristics from chars visually characterized as low burn
severity that were created either on an open air burn table or from
low-temperature muffle furnace burns. We assessed how the different
combustion conditions influence solid and dissolved organic matter
chemistries and explored the potential influence of these results
on the environmental fate and reactivity. Notably, muffle furnace
chars produced less leachable carbon and nitrogen than open air chars
across land cover types. Organic matter produced from muffle furnace
burns was more homogeneous than open air chars. This work highlights
chemical heterogeneities that exist within a single burn severity
category, potentially influencing our conceptual understanding of
pyrogenic organic matter cycling in the natural environment, including
transport and processing in watersheds. Therefore, we suggest that
open air burn studies are needed to further advance our understanding
of pyrogenic organic matter’s environmental reactivity and
fate.
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