Molecular dynamics of foliar litter and dissolved organic matter during the decomposition process

• Published in: Biogeochemistry 2020-08, Vol.150 (1), p.17-30
• Main Authors: Chen, Huan, Liu, Xijun, Blosser, Gavin D., Rücker, Alexander Martin, Conner, William H., Chow, Alex T.
• Format: Article
• Language: English
• Subjects: Aquatic ecosystems; Aromatic compounds; Aromatic hydrocarbons; Biogeosciences; Carbohydrates; Chemical composition; Decomposition; Dissolved organic matter; Earth and Environmental Science; Earth Sciences; Ecosystems; Environmental Chemistry; Floodplains; Fluorescence; Forest watersheds; Hydrocarbons; Life Sciences; Lignin; Litter; Litters (births); Molecular dynamics; National parks; ORIGINAL PAPERS; Phenolic compounds; Phenols; Pyrolysis; Quercus alba; Spectrophotometry; Unsaturated hydrocarbons
• ISSN: 0168-2563; 1573-515X
• DOI: 10.1007/s10533-020-00684-5

Decomposing foliar litter organic matter (LOM) in forested watersheds is an essential terrestrial source of dissolved organic matter (DOM) to aquatic ecosystems. To evaluate the relationship of chemical composition between LOM and DOM, we collected freshly fallen leaves of white oak (Quercus alba) and conducted an 80-week field decomposition experiment along a small elevation gradient in a floodplain within the Congaree National Park, South Carolina. Foliar litters were collected for water extraction and instrumental analyses using pyrolysis GC/MS, UV/VIS and fluorescence spectrophotometry. Factor analyses of pyrolysates showed that fresh LOM was mainly composed of lignin compounds (LgC), phenolic compounds (PhC), and carbohydrate (Carb), and the change in composition was relatively small throughout the decomposition process. In contrast, there were two distinct chemical compositions of DOM in early (between 0–8 weeks) and late phases (between 16–80 weeks). The early phase had a higher percentage of PhC, but the late phase contained higher percentages of Carb, unsaturated hydrocarbon (UnSaH), aromatic hydrocarbon (ArH), and nitrogen-containing compounds (Ntg). The fluorescence emission-excitation matrix showed there was an increasing trend in humic and fulvic-like fractions in DOM over time, matching well with increases of UnSaH and ArH fractions from the results of pyrolysis GC/MS. Our study illustrated that the changes of chemical components in LOM and water extractable DOM were not parallel during the decomposition process and the degradation of lignin and phenolic compounds was one of the controlling factors on the production of DOM.