高原湿地草海不同覆被土壤中溶解性有机质光谱特征

Spectral Characteristics of Dissolved Organic Matter in Different Land Cover Soils in Caohai Plateau Wetland

  • 摘要: 土地覆被类型差异会影响土壤有机质的生物地球化学循环,为探究高原湿地不同覆被类型土壤溶解性有机质(DOM)的分布特征及影响因素,以我国亚热带高原湿地生态系统的典型代表−贵州草海湿地为研究对象,基于紫外-可见吸收光谱(UV-Vis)、三维荧光光谱(3D-EEMs)及平行因子分析(PARAFAC)方法,解析草海湿地林地、耕地、草地、灌丛和滩涂等5种覆被土壤DOM的组成及特征。结果表明:①草海湿地土壤有机质平均含量为(51.11±10.58)g/kg,DOM含量为0.37~1.02 g/kg。DOM以植物源等陆源输入为主,呈弱腐殖化、较强自生源特征。土壤DOM共解析出3种组分,即类富里酸(C1)、陆源类腐殖质(C2)和类蛋白(C3)。②土地覆被类型影响土壤DOM特征,滩涂和灌丛土壤中C1组分占优势,林地和耕地土壤中C2组分相对占优,草地土壤中以C3组分为主。不同覆被土壤中DOM含量表现为滩涂>灌丛>耕地>草地>林地,林地土壤中DOM含量最低;耕地和草地土壤中DOM呈现较低的芳香化程度,滩涂和灌丛土壤中则有较高的芳香性,且DOM光谱参数呈表聚性。③共现网络分析和主成分分析(PCA)显示,C1组分与陆源输入密切相关,C2和C3组分与微生物活动联系紧密。冗余分析(RDA)和方差分解分析(VPA)表明,pH和总氮(TN)浓度是影响草海湿地土壤DOM光谱特征变化的关键因子。研究显示,高原湿地不同土地覆被通过植物资源输入、微生物转化及人类活动等多重因素对土壤DOM组成产生重要影响,其中pH和TN浓度是关键环境影响因子,研究结果可为高原湿地土壤碳循环提供基础数据。

     

    Abstract: The variation in land cover significantly affects the biogeochemical processes of soil organic matter. This study takes Caohai Wetland in Guizhou, a typical representative of subtropical plateau wetland ecosystems in China, as the research object to explore the distribution characteristics and influencing factors of dissolved organic matter (DOM) in plateau wetland soils under different land covers. Ultraviolet-visible absorption spectroscopy (UV-Vis), three-dimensional fluorescence spectroscopy (3D-EEMs), and parallel factor analysis (PARAFAC) were applied to reveal the composition and source of DOM in soils from forestland, cultivated land, grassland, shrubland and mudflat in Caohai Wetland. The results indicated that the average content of soil organic matter in the Caohai Wetland was (51.11±10.58) g/kg, and the soil DOM concentration ranged from 0.37 g/kg to 1.02 g/kg. The DOM in soil predominantly originated from terrestrial sources, such as plant inputs, showing weak humification and relatively strong autochthonous characteristics. Three fluorescence components were identified in DOM by PARAFAC: fulvic-like component C1, terrestrial humic-like component C2, and protein-like component C3. Land cover types influenced the characteristics of soil DOM. Specifically, the C1 component was predominant in the mudflat and shrubland soils, the C2 component was dominant in the forestland and cultivated land soils, and the C3 component dominated in grassland soils. The DOM content in forestland was the lowest, with the order of DOM content from highest to lowest as: mudflat > shrubland > cultivated land > grassland > forestland. Cultivated land and grassland exhibited a low degree of aromatization, while mudflat and shrubland demonstrated relatively high aromaticity. The DOM spectral parameters displayed surface accumulation patterns. Co-occurrence network analysis and principal component analysis (PCA) revealed that the C1 component was closely related to terrestrial inputs, while the C2 and C3 components were closely related to microbial activities. Redundancy analysis (RDA) and variance partitioning analysis (VPA) indicated that pH and total nitrogen (TN) were the key factors influencing the variations of DOM components in Caohai Wetland soil. The research indicated that land cover types in plateau wetlands exerted a vital influence on soil DOM composition through multiple factors such as plant resource input, microbial transformation, and human activities, with pH and TN emerging as crucial environmental factors. These findings offer fundamental insights into the carbon cycle in plateau wetland soils.

     

/

返回文章
返回