Xi'an University of Technology, Xi'an, 710048, People's Republic of China.
North China University of Water Resources and Electric Power, Zhengzhou, 450045, People's Republic of China.
Environ Sci Pollut Res Int. 2018 May;25(14):14197-14205. doi: 10.1007/s11356-018-1645-7. Epub 2018 Mar 9.
UV-visible absorption spectroscopy combined with principal component analysis (PCA) and two-dimensional correlation (2D correlation) is used to trace components of dissolved organic matter (DOM) extracted from soils in a larger estuarine delta and to investigate spatial variations of DOM fractions. Soil samples of different depths were collected from native halophyte soils along a saline gradient, i.e., Suaeda salsa Comm. (SSC), Chenopodium album Comm. (CAC), Phragmites australis Comm. (PAC), and Artemisia selengensis Comm. (ASC). Molecular weights of DOM within the SSC soil profile were the lowest, followed by the CAC, PAC, and ASC soil profiles. Humification degree of DOM within the ASC soil profile was the highest, followed by the PAC, SSC, and CAC soil profiles. DOM within the soil profiles mainly contained phenolic, carboxylic, microbial products, and aromatic and alkyl groups through the PCA, which presented the significant differentiation among the four native halophyte soil profiles. The 2D UV correlation spectra of DOM within the SSC soil profile indicated that the variations of the phenolic groups were the largest, followed by the carboxylic groups, microbial products, and humified organic materials according to the band changing order of 285 → 365 → 425 → 520 nm. The 2D UV correlation spectra of DOM within the CAC soil profiles determined that the decreasing order of the variations was phenolic groups > carboxylic groups > microbial products according the band changing order of 285 → 365 → 425 nm. The 2D UV correlation spectra of DOM within the PAC soil profile proved that the variations of the phenolic groups were larger than those of the carboxylic groups according to the band changing order of 285 → 365 nm. The 2D UV correlation spectra of DOM within the ASC soil profile demonstrated that the variations of the phenolic groups were larger than those of the other DOM fractions according to the broad cross-peak at 285/365-700 nm.
利用紫外可见吸收光谱结合主成分分析(PCA)和二维相关(2D 相关),对取自更大河口三角洲的土壤中提取的溶解有机质(DOM)的成分进行跟踪,并研究 DOM 分数的空间变化。从沿着盐度梯度的天然盐生植物土壤中采集了不同深度的土壤样品,即盐地碱蓬群落(SSC)、藜群落(CAC)、芦苇群落(PAC)和差巴嘎蒿群落(ASC)。SSC 土壤剖面中 DOM 的分子量最低,其次是 CAC、PAC 和 ASC 土壤剖面。ASC 土壤剖面中 DOM 的腐殖化程度最高,其次是 PAC、SSC 和 CAC 土壤剖面。通过 PCA,SSC 土壤剖面中 DOM 主要含有酚类、羧酸、微生物产物以及芳香族和烷基基团,这表明四个天然盐生植物土壤剖面之间存在显著差异。SSC 土壤剖面中 DOM 的 2D UV 相关光谱表明,酚类基团的变化最大,其次是羧酸基团、微生物产物和腐殖质有机物质,根据 285→365→425→520nm 的波段变化顺序。CAC 土壤剖面中 DOM 的 2D UV 相关光谱表明,根据 285→365→425nm 的波段变化顺序,酚类基团的变化顺序最大,其次是羧酸基团和微生物产物。PAC 土壤剖面中 DOM 的 2D UV 相关光谱表明,酚类基团的变化大于羧酸基团,根据 285→365nm 的波段变化顺序。ASC 土壤剖面中 DOM 的 2D UV 相关光谱表明,根据 285/365-700nm 的宽交叉峰,酚类基团的变化大于其他 DOM 分数。