热带亚热带植物学报2024,Vol.32Issue(5):611-619,9.DOI:10.11926/jtsb.4831
增温对亚热带常绿阔叶林凋落物溶解性有机质的影响
Effect of Warming on Dissolved Organic Matter in Litter of Subtropical Evergreen Broad-leaved Forest
摘要
Abstract
In order to understand the effect of warming on litter decomposition,the litter collected in subtropical evergreen broad-leaved forest was distributed in control and warming(+4℃)plots,respectively.The changes in the quantity and spectral characteristics of dissolved organic matter during litter decomposition under warming were studied.The results showed that the mass residual rate of litter decreased significantly with decomposition process,rapidly decreased by 20.08% to 23.32% in 0-60 days,and slowly decreased by 6.35% to 10.98% in 60-210 days.Along decomposition process,the dissolved organic carbon content of litter source showed a decreasing trend of first fast and then slow,and the overall decrease was 94.15% .The content of dissolved organic nitrogen fluctuating decreased by 81.82% overall.The spectral characteristics of dissolved organic matter(SUVA254,SUVA260,SUVA280 and SUVA370)showed an increase-decrease-increase tendency.The warming did not significantly affect the mass residual rate of litter and the spectral characteristics of dissolved organic matter,but the contents of dissolved organic carbon and organic nitrogen decreased by 16.72% and 25.10% .Therefore,the decomposition of litters decreased the mass residual rate of litters and the contents of dissolved organic carbon and organic nitrogen,and changed the spectral characteristics of dissolved organic matter.Although warming decreased the contents of dissolved organic carbon and organic nitrogen in litters,it did not significantly change the mass residual rate and spectral characteristics of dissolved organic matter in litters.关键词
增温/凋落物分解/可溶性有机碳/可溶性有机氮/光谱特征Key words
Warming/Litter decomposition/Dissolved organic carbon/Dissolved organic nitrogen/Spectral characteristics引用本文复制引用
王云,张宇辉,冉佳鑫,毛超,熊德成,陈仕东,杨智杰..增温对亚热带常绿阔叶林凋落物溶解性有机质的影响[J].热带亚热带植物学报,2024,32(5):611-619,9.基金项目
国家自然科学基金项目(31930071,32201354)资助This work was supported by the National Natural Science Foundation of China(Grant No.31930071,32201354). (31930071,32201354)