城郊关键带土壤中溶解性有机质的光谱特性及其时空变异

溶解性有机质(DOM)作为地球关键带中物质与能量循环的重要活性组分,其与关键带中诸多重要环境过程有着密切关系.本研究以宁波樟溪流域作为城郊关键带的典型代表区域,采集土壤样品,结合紫外可见光谱(UV-Vis)、三维荧光光谱(3D-EEM)进行特征表征,分析不同类型土壤中DOM的分布特征、影响因素和季节性变化规律.主要结果如下:林地DOC平均含量均大于耕地,其中林地秋季(15.4 mg·L~(-1))林地春季(12.5 mg·L~(-1));耕地秋季(11.9 mg·L~(-1))耕地春季(11.4 mg·L~(-1));DOM结构在紫外可见光谱下表现为耕地DOM芳香化程度(SUVA_(254))、疏水性组分(SUVA_(260))和分子量(S_R)较林地大,其中耕地秋季最为突出;三维荧光光谱结合平行因子分析(PARAFAC)把土壤DOM分为5种组分,主要以富里酸类物质为主(C_1、C_3、C_5),也含有色氨酸、酪氨酸类蛋白质(C_4)和腐殖酸(C_2)等物质,其中耕地春季的腐殖化程度最大,耕地秋季比春季含有较多类蛋白质,林地较耕地含有更多的类蛋白质,林地春秋两季中DOM结构变化不大.     

长江重庆段溶解性有机物的荧光特性分析

利用三维荧光光谱(EEMs),并结合平行因子分析(PARAFAC)及主成分分析(PCA),研究了长江重庆段溶解有机物(DOM)的荧光组分特征及其污染来源,并探讨了荧光强度同溶解性有机碳(DOC)及溶解氧(DO)的相关性.结果表明,PARAFAC模型识别出长江重庆段DOM由2类6个荧光组分组成,即类腐殖质荧光组分C1(350/422 nm)、C4(245,305/395 nm)、C5(260,340/420 nm)、C6(260/480 nm)及类蛋白荧光组分C2(275/300 nm)、C3(227,278/329 nm).在DOM来源组成中,陆源的类腐殖质含量占62.56%,类蛋白物质含量占31.31%.类腐殖质组分的荧光强度同DOC的含量存在明显的线性正相关(r=0.73),类蛋白组分的荧光强度同DO的含量呈明显的线性负相关(r=0.80).EEMs-PARAFAC不仅可以表征长江重庆段DOM的光谱特征,示踪长江重庆段的有机污染程度,还可以为三峡库区水体保护提供依据.     

焦化废水生物出水溶解性有机物特性光谱表征

利用非离子型DAX-8树脂和离子型交换树脂对某焦化废水二级生物出水溶解性有机物(DOM)进行组分分离,从溶解性有机碳(DOC)、紫外-可见光谱、三维荧光光谱、傅立叶变换红外光谱(FT-IR)等4个方面对组分进行光谱学分析与特征识别.结果显示,疏水性酸性物质(Ho A)、亲水性酸性物质(Hi A)和亲水性中性物质(Hi N)为DOM的主要组分,其DOC含量占总DOC的39.88%、20.85%、25.38%;DOM主要含有单环芳香族化合物或共轭双键类化合物成分,类腐殖质物质和类富里酸物质是DOM的特征有机物;低分子量有机物在亲水性物质组分(HIS)中含量最高,E2 54/E3 65=3.89,E445/E665=1.91,SR=0.926均证明了这一点;亲水性碱性组分(Hi B)组分UV254占比为32%,SUVA值为49.94 L·mg-1·cm-1,不饱和物质和芳香性物质含量最高,芳香化程度最高;Ho A的E300/E400值为2.58,腐化程度最高,组分中含有类富里酸物质.DOM光谱分析能够提供组分中亲疏水性物质的比例、芳香性高低、分子量、发色团及有机基团等信息,可以作为判断废水特征的参考依据.     

焦化废水中溶解性有机物组分的特征分析

焦化废水是典型的具有复杂有机质的工业废水,其复杂的有机构成制约了水处理的水质达标,且可能对排入水体构成危害.为了探明其溶解性有机物的组成,采用XAD-8大孔树脂将焦化废水中的溶解性有机物分为亲水性组分(HIS)、疏水酸性组分(HOA)、疏水碱性组分(HOB)和疏水中性组分(HON),分析了各组分的溶解性有机物(DOC)、紫外-可见光谱、色度,并采用GC/MS对各组分中有机物进行定性分析.结果表明,焦化废水中的有机物主要为HIS和HOA组分,其DOC含量分别占总DOC的44.3%和32.4%;焦化废水在200—250 nm和300—400 nm范围内有特征吸收峰,且吸收光强度顺序为HIS>HOA>HON>HOB;焦化废水的色度主要由HOA和HON构成,其在525 nm和436 nm处的吸光度分别占焦化废水吸光度的42.9%(HON)、42.1%(HON)和21.4%(HOA)、15.8%(HOA);焦化废水中亲水性物质主要是苯胺、苯酚、喹啉、异喹啉,疏水酸性物质中主要是各种甲基取代的酚类物质,疏水碱性物质主要是各种胺类和含氮杂环化合物,疏水中性物质主要是吲哚及其衍生物.     

洱海沉积物不同分子量溶解性有机氮空间分布及光谱特征

利用超滤技术对洱海沉积物溶解性有机氮(DON)进行分子量分级,探究了DON各组分空间分布特征,并运用紫外-可见吸收光谱和三维荧光光谱对其结构进行了表征.结果表明,洱海沉积物总DON含量ω(DON)为23.46—61.40 mg·kg-1,平均值为37.19 mg·kg-1,空间分布总体呈现南部>北部>中部的趋势;分子量大于1K Da的大分子组分ω(>1KDa)占ω(DON)的比例为79.1%—93.0%,即洱海沉积物DON是以大分子为主.沉积物DON各组分的芳香性及腐殖化程度较高,芳香环取代基中活性官能团种类较多,且南部芳香性及腐殖化程度最高,北部芳香环取代基种类最多;大分子组分DON含有类富里酸荧光物质,其来源于陆源输入和微生物降解共同作用.由此可见,洱海沉积物DON主要由大分子物质组成,其腐殖化程度较高且含类富里酸荧光物质,而此类DON对藻类的生物有效性较低,这可能是洱海沉积物氮含量较高而上覆水氮浓度较低的原因之一,即沉积物DON分子组成及其结构特征可在一定程度上作为湖泊营养水平的衡量指标.     

印染外排废水中溶解性有机质的荧光特性

通过三维荧光(EEM)光谱技术,结合平行因子分析(PARAFAC)及荧光区域积分法(FRI),对我国珠三角的五家印染废水处理厂外排废水的溶解性有机质(DOM)进行定性及定量表征.五组水样DOM的EEM光谱中类蛋白荧光峰最为明显,结合荧光指数(FI),自生源指标(BIX)及腐殖化指标(HIX),发现DOM的腐殖质主要来源...     

渗滤液中溶解性荧光有机物与铅的作用

采用荧光光谱和猝灭滴定实验,结合二维相关分析和区域体积积分分析,研究了生活垃圾渗滤液不同处理阶段样品中溶解性荧光有机物(DFOM)络合Pb(Ⅱ)的特性.结果显示:渗滤液中无机阴离子对Pb(Ⅱ)猝灭DFOM荧光影响较大,它们的存在致使Pb(Ⅱ)对DFOM的荧光猝灭效果不明显.在渗滤液DFOM的各种荧光基团中,Pb(Ⅱ)对类蛋白类物质的荧光猝灭效率高,而对类腐殖质物质的荧光猝灭效率低,这种猝灭特征不随渗滤液处理进行而改变;但Pb(Ⅱ)对调节池和厌氧处理中可溶性微生物降解副产物的荧光猝灭效率低而对氧化沟和MBR出水中DFOM的荧光猝灭效率高.分析结果表明,渗滤液DFOM中类蛋白物质络合Pb(Ⅱ)能力大于类腐殖质物质,经好氧生物处理后,可溶性微生物降解副产物络合Pb(Ⅱ)的能力有所提高.     

三维荧光光谱表征膜污染物

本文探讨三维荧光光谱表征天然湖水中膜污染物质的可行性.选取天然湖水中的4种溶解性有机组分,进行膜过滤试验,探讨水样的荧光峰位置、强度和分布等特征参数与其分子量、亲疏水性质的关系,从而达到用三维荧光光谱参数定性、定量表征膜污染程度的目的.经研究发现,EEM谱图上与膜污染关系最密切的两个区域是:λex=220-250nm/λcm=350-380nm和λex=230-280nm/λem=380-500nm,其对应的小分子蛋白类和腐殖类有机物是造成膜污染的主要成分.此外,EEM谱图上的荧光强度还可用来表征过膜前后有机物的截留效率.经研究认为,采用三维荧光光谱反映膜污染成因和膜截留效率,具有实际应用意义.     

土壤溶解性有机质的生态环境效应

土壤生态环境是一个复杂的多介质多界面体系。现有的研究表明，DOM作为环境中重要的天然配位体和吸着载体，是一种非常活跃的化学物质，它将土壤中的矿物质、有机质与生物成分联系在一起，通过物理或化学作用改变金属与外源性化合物的环境行为，促进温室气体的排放，调节土壤养分流失，指示土壤质量，并对成土过程、微生物的生长代谢过程、土壤有机质分解和转化过程有着重要作用，已经成为土壤科学、生态科学和环境科学交叉领域的研究热点。文章系统地评述了DOM的组成特点及其环境效应，同时介绍了未来的研究方向及一些有待于进一步研究的问题。     

夏季渭河西安段溶解性有机质(DOM)的特征、分布及来源分析

通过紫外吸收光谱,三维荧光光谱结合平行因子分析(EEMs-PARAFAC)方法及主成分分析(PCA),研究了夏季渭河西安段水体中的溶解性有机质(DOM)的组成、来源,及其与水质指标的相关性.在研究区域共检出2种类别5个不同的DOM组分,分别为类腐殖质荧光组分C1、C2、C3、C5和1个类蛋白类荧光组分C4,5个组分具有...     

Three-dimensional fluorescence spectral characterization of soil dissolved organic matters in the fluctuating water-level zone of Kai County, Three Gorges Reservoir

Three-dimensional fluorescence spectroscopy was used to investigate the fluorescent properties of soil dissolved organic matter (DOM) in the water-level-fluctuation zone (WLFZ) of Kai County, Three Gorges Reservoir (TGR). Most of the soil DOM analyzed in this study was found to contain four fluorescence peaks. Peaks A and C represent humic-like fluorescence, whereas peaks B and D represent tryptophan-like fluorescence. Peaks E and F, which represent tyrosine-like fluorescence, only appeared in certain soils. Soil humus was the main source of DOM in soil, and higher concentration of soil DOM was found in the exposed soil than submerged soil. Compared to the peaks A and B, the fluorescence intensities of peaks C and D were strongly influenced by the fluctuating water level. Analysis of fluorescence intensities of different peaks in soil DOM showed that WLFZ soil was not contaminated significantly. Soil DOM contained at least two types of humic-like fluorescence groups and two types of protein-like fluorescence groups. The proportion of the content of peak A in soil organic matter was quite stable. The soil DOM in exposed soil had relatively high humification and aromaticity, and periodic submerging and exposure of soil had an impact on the humification of soil DOM.     

可溶性有机物对土壤中主要有机污染物环境行为的影响

概括了环境中可溶性有机物的特点，并系统总结了当前国内外关于可溶性有机物对土壤中主要污染物环境行为的影响的研究进展。阐述了可溶性有机物对农药、多环芳烃在土壤中的吸附、解吸及分配等环境行为所起的作用。最后指出了该方面研究存在的问题及今后应加强的方向。     

Fluorescence spectroscopic studies of the effect of granular activated carbon adsorption on structural properties of dissolved organic matter fractions

This work investigated the effect of granular activated carbon adsorption (GACA) on fluorescence characteristics of dissolved organic matter (DOM) in secondary effluent, by means of excitation–emission matrix (EEM) spectra, the fluorescence regional integration (FRI) method, synchronous spectra, the fluorescence index defined as the ratio of fluorescence emission intensity at wavelength 450 nm to that at 500 nm at excitation (λ_ex)=370 nm, and the wavelength that corresponds to the position of the normalized emission band at its half intensity (λ_0.5). DOM in the secondary effluent from the North Wastewater Treatment Plant (Shenyang, China) was fractionated using XAD resins into 5 fractions: hydrophobic acid (HPO–A), hydrophobic neutral (HPO–N), transphilic acid (TPI–A), transphilic neutral (TPI–N) and hydrophilic fraction (HPI). Results showed that fluorescent materials in HPO–N and TPI–N were less readily removed than those in the other fractions by GACA. The relative content of fluorescent materials in HPO–A, TPI–A and HPI decreased whereas that in HPO–N and TPI–N increased as a consequence of GACA. Polycyclic aromatics in all DOM fractions were preferentially absorbed by GACA, in comparison with bulk DOM expressed as DOC. On the other hand, the adsorption of aromatic amino acids and humic acid-like fluorophores exhibiting fluorescence peaks in synchronous spectra by GACA seemed to be dependent on the acid/neutral properties of DOM fractions. All five fractions had decreased fluorescence indices as a result of GACA. GACA led to a decreased λ_0.5 value for HPO–A, increased λ_0.5 values for HPO–N, TPI–A and HPI, and a consistent λ_0.5 value for TPI–N.     

Influence of dissolved organic matter from corn straw on Zn andCusorption to Chinese loess

The interaction of Zn and Cu with dissolved organic matter (DOM) is a significant physicochemical process affecting their sorption as well as mobility in soil. The objective of this study was to examine the influence of DOM from corn straw on the sorption of Zn and Cu by loess through batch adsorption technique. The sorption isotherms of Zn and Cu could be well described by the Freundlich equation, and the partition distribution coefficient (k) in the presence of DOM was reduced by 86% for Zn and 58% for Cu, as compared to the control receiving no DOM, suggesting that DOM had a stronger inhibitory effect on Zn sorption than that of Cu. In addition, the sorption of metal increased with an increase in pH for loess, with maximum inhibition on metal sorption observed at pH > 7.6 for Zn and pH > 5.5 for Cu in the absence ofDOM but Cu sorption of DOM was suddenly decreased with an increase of pH at pH > 7.9 in the presence of DOM. At a DOM concentration of <200 mg L^?1, sorption of Zn and Cu was reduced by 46% for Zn and 32% for Cu with an increase in DOM concentration.     

红树植物凋落叶分解对土壤可溶性有机质的影响

研究红树林湿地土壤可溶性有机质（DOM）的来源、性质及其归宿对于揭示 DOM 在红树林湿地生物地球化学循环中的作用具有重要意义。采集了木榄（Bruguiera gymnoihiza）、秋茄（Kandelia candel）和桐花树（Aegiceras corniculatum）3种红树植物的新近落叶进行室内48 d分解实验,探讨了凋落叶分解过程对土壤可溶性有机碳（DOC）和可溶性总氮（TDN）含量、C/N比（DOC/TDN）及紫外-可见（UV-Vis）光谱特征（A280、A240/A420和A250/A365比值）的影响。在48 d分解期间,3种红树植物凋落叶的输入均明显增加了土壤DOC的含量,其变化在分解第6 d最为显著,各凋落叶添加组比对照组平均增加了149%（秋茄）~196%（桐花树）,随后各凋落叶添加组土壤DOC含量呈下降趋势。与土壤DOC的变化不同,凋落叶输入后土壤TDN的变化与对照组的差异不明显,但木榄和桐花树添加组的C/N比在分解初期（第6天）显著高于对照组（P<0.05）。凋落叶的输入亦在不同程度上增大了土壤DOM的A280值,降低了DOM的A240/A420和A250/A365比值。与土壤DOC的变化相似,凋落叶输入使DOM的UV-Vis光谱特征在分解初期（第6天）的变化最明显,其中桐花树凋落叶的影响最大,秋茄凋落叶的影响最小。结果表明：凋落叶输入使培养初期土壤DOM的含量和性质发生明显改变,DOM中大分子及芳香类组分增多、团聚化程度增加,DOM 的生物可降解性变小。然而,随着分解的进行,不同凋落叶处理组之间土壤DOM的变化差异性逐渐缩小,并在分解后期与对照组趋近。