TY - JOUR
T1 - Molecular heterogeneity in pyrogenic dissolved organic matter from a thermal series of oak and grass chars
AU - Wozniak, Andrew S.
AU - Goranov, Aleksandar I.
AU - Mitra, Siddhartha
AU - Bostick, Kyle W.
AU - Zimmerman, Andrew R.
AU - Schlesinger, Danielle R.
AU - Myneni, Satish
AU - Hatcher, Patrick G.
N1 - Funding Information:
This work was funded by the U.S. National Science Foundation - Geobiology and Low-Temperature Geochemistry Program ( EAR-1451452 ) and the ODU Frank Batten Endowment Fund. This research used beamline 8-BM (Tender Energy X-ray Absorption Spectroscopy, TES) of the National Synchrotron Lightsource II, a U.S. Department of Energy (DOE) Office of Science User Facility operated for the DOE Office of Science by Brookhaven National Laboratory under contract No. DE-SC0012704 . The authors thank the ODU COSMIC facility as well as Isaiah Ruhl and Jim Hall for assistance with FTICR-MS and NMR analyses. We additionally thank Drs. Rachel L. Sleighter and Hongmei Chen for assistance with FTICR-MS data processing and Dr. Alina Ebling for statistical assistance. Lastly, we thank Dr. Jason Curtis for assistance with elemental analyses, and Dow Van Arnam for the construction and maintenance of the pyrolysis system.
Funding Information:
This work was funded by the U.S. National Science Foundation - Geobiology and Low-Temperature Geochemistry Program (EAR-1451452) and the ODU Frank Batten Endowment Fund. This research used beamline 8-BM (Tender Energy X-ray Absorption Spectroscopy, TES) of the National Synchrotron Lightsource II, a U.S. Department of Energy (DOE) Office of Science User Facility operated for the DOE Office of Science by Brookhaven National Laboratory under contract No. DE-SC0012704. The authors thank the ODU COSMIC facility as well as Isaiah Ruhl and Jim Hall for assistance with FTICR-MS and NMR analyses. We additionally thank Drs. Rachel L. Sleighter and Hongmei Chen for assistance with FTICR-MS data processing and Dr. Alina Ebling for statistical assistance. Lastly, we thank Dr. Jason Curtis for assistance with elemental analyses, and Dow Van Arnam for the construction and maintenance of the pyrolysis system.
Publisher Copyright:
© 2020 Elsevier Ltd
PY - 2020/10
Y1 - 2020/10
N2 - Pyrogenic organic matter (Py-OM), generated via the incomplete combustion of biomass, is well studied due to the presence of slow-cycling, condensed aromatic compounds (ConAC) known to sequester in soils and sediments. Recently, dissolved Py-OM (Py-DOM) has received interest, due to its higher mobility and potential to be transferred through watersheds to aquatic systems. Py-DOM quantities, molecular identities and importance to global carbon budgets and cycles are only beginning to be understood. Fourier transform ion cyclotron resonance mass spectrometry (FTICR-MS) analyses were performed on Py-DOM isolated from oak and grass biochars produced over a range of temperatures (250–650 °C), and the data are compared to complementary 1H NMR spectroscopic and benzenepolycarboxylic acid biomarker (BPCAs) analyses. Py-DOM is revealed to be a heterogeneous mixture of compounds ranging in relative aromaticity and oxygenation. FTICR-MS analyses demonstrate a decrease in Py-DOM relative oxygen content and a concurrent increase in aliphatic character and heteroatomic (N, Cl) content. 1H NMR and BPCAs analyses detail low O/C dissolved ConAC not observed by FTICR-MS, demonstrating the necessity for a multiple proxy approach to Py-DOM characterization. Heterogeneous Py-DOM is explained as resulting from pyrolysis-initiated and radical-mediated functional group cleavage, aromatic condensation and aromatic ring-opening reactions. Oak biomass progresses faster along a char maturity continuum for a given pyrolysis temperature, perhaps due to its greater lignin content or radical quenching by grass cuticular material. Biomass species and pyrolysis temperature likely result in different Py-DOM compositions and fates and must be considered when evaluating the impacts of wildfires and biochar applications.
AB - Pyrogenic organic matter (Py-OM), generated via the incomplete combustion of biomass, is well studied due to the presence of slow-cycling, condensed aromatic compounds (ConAC) known to sequester in soils and sediments. Recently, dissolved Py-OM (Py-DOM) has received interest, due to its higher mobility and potential to be transferred through watersheds to aquatic systems. Py-DOM quantities, molecular identities and importance to global carbon budgets and cycles are only beginning to be understood. Fourier transform ion cyclotron resonance mass spectrometry (FTICR-MS) analyses were performed on Py-DOM isolated from oak and grass biochars produced over a range of temperatures (250–650 °C), and the data are compared to complementary 1H NMR spectroscopic and benzenepolycarboxylic acid biomarker (BPCAs) analyses. Py-DOM is revealed to be a heterogeneous mixture of compounds ranging in relative aromaticity and oxygenation. FTICR-MS analyses demonstrate a decrease in Py-DOM relative oxygen content and a concurrent increase in aliphatic character and heteroatomic (N, Cl) content. 1H NMR and BPCAs analyses detail low O/C dissolved ConAC not observed by FTICR-MS, demonstrating the necessity for a multiple proxy approach to Py-DOM characterization. Heterogeneous Py-DOM is explained as resulting from pyrolysis-initiated and radical-mediated functional group cleavage, aromatic condensation and aromatic ring-opening reactions. Oak biomass progresses faster along a char maturity continuum for a given pyrolysis temperature, perhaps due to its greater lignin content or radical quenching by grass cuticular material. Biomass species and pyrolysis temperature likely result in different Py-DOM compositions and fates and must be considered when evaluating the impacts of wildfires and biochar applications.
KW - Biochar
KW - Black carbon
KW - Dissolved organic matter (DOM)
KW - FTICR-MS
KW - H NMR
KW - Pyrogenic organic matter
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U2 - 10.1016/j.orggeochem.2020.104065
DO - 10.1016/j.orggeochem.2020.104065
M3 - Article
AN - SCOPUS:85088663679
SN - 0146-6380
VL - 148
JO - Organic Geochemistry
JF - Organic Geochemistry
M1 - 104065
ER -