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不同粒径黄河沉积物中可提取腐殖质的含量分布及光谱特性
引用本文:孙莉英,倪晋仁,孙卫玲. 不同粒径黄河沉积物中可提取腐殖质的含量分布及光谱特性[J]. 环境科学, 2007, 28(6): 1324-1331
作者姓名:孙莉英  倪晋仁  孙卫玲
作者单位:北京大学环境工程系水沙科学教育部重点实验室,北京,100871;北京大学环境工程系水沙科学教育部重点实验室,北京,100871;北京大学环境工程系水沙科学教育部重点实验室,北京,100871
基金项目:国家自然科学基金项目(40501063)
摘    要:测定了黄河表层沉积物3种粒径组分(Ⅰ:100~300 μm;Ⅱ: 63~100 μm;Ⅲ: <63 μm)中总有机碳和可提取腐殖质的含量,分析了可提取腐殖质的紫外-可见吸收光谱、红外光谱和三维荧光光谱特征,探讨了不同粒径组分沉积物中可提取腐殖质含量分布及其化学组成特性.结果表明,沉积物有机质主要为粘土矿物吸附的天然腐殖质成分,总有机碳中可提取腐殖质的比例随沉积物有机质与矿物质相互作用的增强而降低,顺序为Ⅰ>Ⅱ>Ⅲ.3种粒径组分沉积物中可提取腐殖质的紫外-可见吸收光谱相似但相对峰强不同;红外光谱主要有5个吸收峰,各吸收峰面积百分含量的计算结果表明酚、醇及羧酸类官能团为主要的活性官能团,占可提取腐殖质组成的75%以上;三维荧光光谱主要有3个荧光峰,除了典型的类腐殖质荧光峰(峰A和峰C)外,还有源于小分子类蛋白或酚类物质的荧光峰(峰T′).比较3种粒径组分沉积物中可提取腐殖质的紫外-可见、红外及三维荧光光谱的特征参数,发现Ⅰ、Ⅱ组分沉积物中可提取腐殖质的芳香度高,脂肪族和芳香族含量高于Ⅲ组分,而Ⅲ组分沉积物可提取腐殖质中酚、醇及羧酸类活性基团含量相对较高.

关 键 词:沉积物  腐殖质  粒径  光谱特性
文章编号:0250-3301(2007)06-1324-08
收稿时间:2006-08-16
修稿时间:2006-08-162006-10-13

Concentration and Spectrum Characteristic of the NaOH Extracted Humic Substances in Three Size Fractions of Sediments from the Yellow River
SUN Li-ying,NI Jin-ren and SUN Wei-ling. Concentration and Spectrum Characteristic of the NaOH Extracted Humic Substances in Three Size Fractions of Sediments from the Yellow River[J]. Chinese Journal of Environmental Science, 2007, 28(6): 1324-1331
Authors:SUN Li-ying  NI Jin-ren  SUN Wei-ling
Affiliation:The Key Laboratory of Water and Sediment Sciences, Ministry of Education, Department of Environmental Engineering, Peking University, Beijing 100871, China
Abstract:The concentrations of total organic carbon (TOC) and the NaOH extracted humic substances were analyzed in three size fractions (I : 100 - 300 microm, II : 63 - 100 microm and III : < 63 microm) of sediments sampled in the middle Yellow River. Moreover, UV-visible absorption spectra, fourier transform infrared spectra (FTIR) and three-dimensional excitation emission matrix fluorescence spectra (3DEEM) were used to characterize the chemical structures of the NaOH extracted humic substances in three sediment size fractions. The results show that sediment organic matter in all the size fractions of the collected sediments is dominated by humic substances absorbed on the clay minerals. The proportions of the NaOH extracted humic substances to TOC decrease with decreasing sediment grain size ( I > II > III). This may result from the stronger interaction of the humic substances with clay minerals in finer size fractions of the colleted sediments. Similar UV-visible spectra with different absorbance intensity are observed for the NaOH extracted humic substances in three sediment size fractions. The infrared spectra of the NaOH extracted humic substances show five strong peaks in all fractions of the samples. The area ratios of FTIR peaks suggest that the contents of the phenolic, alcoholic and carboxylic groups account for more than 75% in the NaOH extracted humic substances. Three characteristic excitation-emission peaks present in the 3DEEM of the NaOH extracted humic substances: peak A (UV humic-like compounds), peak C (visible humic-like compounds) and peak T'(phenolic compounds or protein like compounds). UV-visible, FTIR and 3DEEM results imply that the aromatic degree of the NaOH extracted humic substances is higher in fractions I and II than in fraction III. The results also indicate that the aliphatic and aromatic contents are higher in fractions I and II, whilst the phenolic, alcoholic and carboxylic contents are higher in fraction III.
Keywords:sediment   humic substances   grain size   spectrum characteristic
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