黄河口湿地典型植被土壤溶解性有机质的特性及其季节变化

Spectral Properties and Seasonal Changes of Dissolved Organic Matter in Soils of Typical Vegetation in the Yellow River Estuary Wetland

  • 摘要: 为探究黄河口湿地典型植被土壤溶解性有机物(Dissolved Organic Matter, DOM)的特性,分别于2022年7月、9月和2023年2月采集了黄河口湿地3种典型植物(柽柳、芦苇和碱蓬)的根系表层土壤,分析了土壤的理化性质和DOM的光谱特征,探究了植被生长期和生长停滞期土壤DOM的特性及其与环境因素之间的关系。结果表明,3种植物的土壤溶解性有机碳(Dissolved Organic Carbon, DOC)和总溶解态氮(Total Dissolved Nitrogen, TDN)的含量排序为柽柳大于芦苇大于碱蓬;但其在不同生长期又有所差异:快速生长期表现为柽柳大于芦苇大于碱蓬,生长末期为柽柳大于碱蓬大于芦苇,生长停滞期则为碱蓬大于柽柳大于芦苇。基于三维荧光光谱-平行因子分析(EEMs-PARAFAC)技术,识别出土壤有色溶解有机质(Chromophoric Dissolved Organic Matter, CDOM)有3个类腐殖质组分(C1、C2和C3)和1个类蛋白质组分(C4),其中类腐殖质组分占86%以上。综合SUVA254SR、FI、BIX、HIX等光学指数的分析结果可知,研究区土壤DOM以疏水性物质为主,其腐殖化程度较高且具有芳香性,主要来源于陆源输入,自生源贡献较少。

     

    Abstract: In order to comprehensively examine the properties of dissolved organic matter (DOM) beneath typical vegetation in coastal wetland at Yellow River Estuary, we collected soil samples from the root surfaces of three dominant plants (Tamarix chinensis, Phragmites australis, and Suaeda salsa) in July and September 2022, as well as February 2023. These samples were analyzed to investigate the properties of soil DOM of different vegetation during the growing and stagnant periods, and to explore their associations with environmental factors. The results revealed significant differences in the concentrations of dissolved organic carbon (DOC) and total dissolved nitrogen (TDN) among the vegetation types, following an overall trend of T. chinensis>P. australis>S. salsa. There are also differences in different growth stages: during the rapid growth period, T. chinensis had the highest content, followed by P. australis and S. salsa; at the end of growth period, T. chinensis remained the highest, with S. salsa surpassing P. australis; whereas in the senescence phase, S. salsa exhibited the highest content, followed by T. chinensis and P. australis. Utilizing excitation-emission matrix spectroscopy combined with parallel factor analysis (EEMs-PARAFAC), we identified three humic-like components (C1, C2, C3) and one protein-like component (C4) in soil CDOM, with humic-like components accounting for the majority (over 86%). Comprehensive analysis using optical indices such as SUVA254, SR, FI, BIX, and HIX revealed that soil DOM in the study area was predominantly hydrophobic, characterized by high degrees of humification and aromaticity, primarily sourced from terrestrial inputs, with minimal autochthonous contributions.

     

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