基于三维荧光与绝对主成分算法的河滨带土壤腐殖酸组分及来源特性分析

Analysis of humus components and source characteristics from riparian soils based on excitation-emission matrix spectroscopy and absolute principal component analysis

  • 摘要: 分别采集蒲河生态区、城市区、城镇区和农村区河滨带不同深度土壤样品,基于三维荧光光谱结合绝对主成分分析和平行因子分析识别河滨带土壤腐殖酸的光谱特征,利用二维相关光谱分析其组分空间变化,并通过偏最小二乘法结构方程揭示土壤腐殖酸来源、组成与理化性质的响应关系。结果表明:1)生态区、城镇区和农村区河滨带土壤中,腐殖酸荧光强度随土壤深度的增加而增加,而城市区腐殖酸荧光强度的垂向变化无明显规律。2)土壤腐殖酸光谱中包含5个荧光组分(C1~C5),其中C1和C2分别为紫外光区和可见光区的类富里酸,C3为微生物代谢产物,C4和C5分别为紫外光区和可见光区的类胡敏酸。生态区以C3和C4(54.71%±4.74%)为主,城市区和城镇区以C3和C2(51.57%±3.09%)为主,农村区以C3和C5(52.96%±12.69%)为主。3)城市区紫外光区的类富里酸和类胡敏酸含量随土层深度优先发生变化,这主要归因于工业源、生活源等面源污染的影响;其他3个区域的荧光组分变动趋势与城市区的相反,均受到植物代谢、陆源土壤和农田退水等多因素作用。4)生态区和城镇区河滨带土壤新鲜有机质较多,腐殖化程度相对较高〔腐殖化指数(HIX)为21.25±1.92〕;城市区和农村区土壤腐殖酸自生源相对较弱,腐殖化程度较低(HIX为19.55±3.24)。5)腐殖酸来源、组成与土壤理化性质显著相关,腐殖酸组成对土壤理化性质的影响高于其来源。研究揭示了不同土地利用类型下河滨带土壤腐殖酸的空间分布规律及其与土壤环境的响应机制,可为河滨带生态修复与建设提供科学依据。

     

    Abstract: In this study, soil samples at different depths were collected from riparian zones of Puhe ecological area, urban area, town area and rural area. Using excitation-emission matrix spectroscopy (EEMs) combined with absolute principal component analysis (APCA) and parallel factor analysis (PARAFAC), the spectral characteristics of soil humus in riparian zones were identified. Two-dimensional correlation spectroscopy was used to analyze the spatial variation of their components, and partial least squares structural equation modeling (SEM) to reveal the response relationships between the sources, composition and physicochemical properties of soil humus. The results showed: 1) The fluorescence intensity of humus increased with the increase of soil depth in the riparian soils of the ecological area, town area and rural area, while the vertical variation showed no obvious pattern in the urban area. 2) The soil humus spectrum contained five fluorescent components (C1-C5), with C1 and C2 being ultraviolet fulvic-acid and visible fulvic-acid, C3 being microbial metabolite, and C4 and C5 being ultraviolet humic acid and visible humic acid. The ecological area was mainly composed of C3 and C4 (54.71%±4.74%), while the urban area and town area were dominated by C3 and C2 (51.57%±3.09%), and the rural area was primarily made up of C3 and C5 (52.96%±12.69%). 3) The ultraviolet fulvic-acid and ultraviolet humic acid changed preferentially with soil depth in the urban area, mainly due to the influence of non-point source pollution (e.g. industrial and domestic sources), while the variation trends of fluorescence components in the other three areas were opposite to those in the urban area, affected by multiple factors including plant metabolism, terrestrial soil and agricultural runoff. 4) The riparian soils in the ecological area and town area had more fresh organic matter and relatively higher degree of humification (HIX=21.25±1.92), whereas the soil humus in the urban area and rural area had relatively weaker autochthonous sources and lower humification (HIX=19.55±3.24). 5) The sources and compositions of humus were significantly correlated with soil physicochemical indicators, and the latter had a greater impact on these properties than the former. This study unraveled the spatial distributions of soil humus in riparian across diverse land-uses, along with their response mechanisms to the soil environment, thus offering a scientific foundation for the ecological restoration and development of riparian zones.

     

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