Dissolved organic matter (DOM) is the most reactive and mobile fraction of forest soil organic matter, and it is increasingly impacted by wildfires worldwide. However, the changes in the dynamics, influencing factors, and environmental impacts of soil DOM following fire events remain insufficiently explored. In this study, carbon quantification and various spectroscopy and spectrometry techniques were applied to analyze DOM contents and characteristics in wildfire cases and laboratory-controlled burning experiments. The results showed that DOM exhibited significantly higher temporal variations compared to bulk soil organic matter (SOM) after fire, with carboxyl-rich compounds rapidly diminishing, while nitrogen-rich condensed aromatics persisted for an extended period. Heating temperature, fuel type, and oxygen availability were identified as key factors controlling the chemistry of pyrogenic DOM. Moreover, pyrogenic DOM was found to influence sulfamethoxazole degradation through different pathways, suggesting that fire can alter environmental quality. This study enhances the understanding of the temporal variations in the effects of fire on different soil DOM components, which can help inform future post-fire environmental management strategies.
National Natural Science Foundation of China Geobiology Society National Committee of Stratigraphy of China Ministry of Science and Technology Geological Society of China Paleontological Society of China Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (CAS) Institute of Vertebrate Paleontology and Paleoanthropology, CAS International Commission on Stratigraphy International Paleontological Association
承办单位
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (CUG, Wuhan)