植物角质层的蜡质组分对甲萘酚的吸附作用

采用批量平衡法,比较研究了苹果角质结合蜡质、分离蜡质和重建蜡质对极性有机污染物甲萘酚的吸附作用,并探讨了不同负载量的重建蜡质的吸附性能,以期为准确预测有机污染物在不同状态蜡质组分上的吸附行为提供依据.结果表明,甲萘酚在苹果角质层、脱蜡角质层、分离蜡质(IW)、重建蜡质(BW)上的等温吸附线呈非线性,符合Freundlich方程.植物蜡质对甲萘酚的吸附作用与蜡质所处状态密切相关,吸附能力(Koc)大小顺序为:重建蜡质(321.2) > 分离蜡质(190.4) > 角质结合蜡质(128.4),表明植物角质层进入土壤后发生演化过程中,其中不易降解的蜡质的吸附能力逐渐增大.重建蜡质(BW)的吸附系数(Kd)与甲萘酚的浓度呈负相关,与蜡质的负载量呈正有关.在低浓度时,甲萘酚的有机碳标化吸附系数Koc值随有机碳含量(foc)增大先增大后减小,存在一些强的特殊作用;而高浓度时, Koc-基本为一常数,不随蜡质负载量而变化,主要吸附机理为分配作用.角质结合蜡质(CW)对角质层的总吸附作用的贡献较小,但随甲萘酚平衡浓度的增大而逐渐增大,并于高浓度时, CW的吸附能力与IW相当.     

Sorption of chlorophenols onto fruit cuticles and potato periderm

To better understand the interaction mechanisms of plant surfaces with polar organic compounds, sorption of 4-chlorophenol, 2,4- dichlorophenol, and 2,4,6-trichlorophenol by fruit cuticles (i.e., tomato, apple, and pepper), and potato tuber periderm were investigated. The roles of cuticular components (waxes, cutin, cutan and sugar) on sorption of chlorophenols are quantitatively compared. Cutin and waxes govern the sorption capacity of bulk apple cuticle by hydrophobic interactions. Potato periderm with highest sugar content exhibits the lowest sorption capability for the chlorophenols. With the increase of hydrophobicity (i.e., K_ow ) of sorbate, the relative contribution of lipophilic components (wax, cutin and cutan) on total sorption increases, however, the ratios of K_oc to K_ow decreases due to increasing ionization degree of sorbates.     

Sorption of pyrene on two paddy soils and their particle-size fractions

In the present study, the sorption of pyrene on two kinds of bulk paddy soils, Gleyic Stagnic Anthrosols, and Ferric accumulic Stagnic Anthrosols as well as their particle-size fractions was investigated. The sorption isotherms fitted well with Freundlich equation. For both soils, the clay fraction（ 〈 2μm） and coarse sand fraction（2000-250μm） had higher sorption capacity than fine sand fraction（250-20 μm） and silt fraction（20-2 μm）. The IogKoc values obtained of each soil and its particle-size fractions were similar, proving that SOM content was a key factor affecting pyrene sorption. The Kd values showed a significant correlation with contents of dithionite-extractable Fe in both paddy soils and a good relationship with CEC in Gleyic Stagnic Anthrosols, indicating possible effects of surface properties of particle-size fractions on the sorption of pyrene.     

源自腐殖土的溶解性有机质组分对棕壤和黑土吸附苯并三唑的影响

溶解性有机质(DOM)影响着有机污染物在土壤中的吸附行为.将从腐殖土中提取的DOM(DOMbulk)用XAD-8树脂和阴/阳离子交换树脂进行分级,用红外光谱、元素分析、紫外分光光度计和电位滴定的方法对DOM不同组分特征进行分析.用吸附批次实验方法研究了DOM不同组分对棕壤和黑土吸附苯并三唑(BTA)的影响.结果表明,DOMbulk中疏水酸性(HOA)、疏水中性(HON)、亲水酸性(HIA)、亲水碱性(HIB)和亲水中性(HIN)组分比例分别为61%、17%、6%、2%和14%.由于黑土有机碳(OC)含量高于棕壤,黑土对BTA和DOM组分的吸附能力均大于棕壤.相对于黑土,棕壤吸附DOM的标化分配系数Koc较高,其原因是棕壤中含有较多的对吸附DOM起重要作用的黏粒和粉砂.由于水分子占据DOM结合点位,DOM组分与BTA在溶液中结合较弱.DOMbulk中HIN在土壤上吸附最强.HIN的吸附增加了土壤吸附BTA的点位,增加点位的促进吸附作用大于HIN与BTA的竞争吸附作用,最终表现为促进吸附.疏水组分在土壤上的吸附较弱,产生的新吸附点位较少,主要通过竞争吸附作用抑制土壤对BTA的吸附.DOMbulk由78%的疏水组分构成,对土壤吸附BTA的影响与疏水组分相似.     

溴化十四烷基吡啶对膨润土吸附萘的增强效应及机理

研究了溴化十四烷基吡啶(MPB)对膨润土吸附萘的增强效应、机理及影响因素,试图为有机膨润土在污染环境修复中的应用提供新的技术路线.结果表明,MPB能显著增强膨润土对萘的吸附作用,增强效应及机理与MPB浓度有关.当MPB平衡浓度(X)在0～1/10CMC之间,MPB几乎全部被膨润土吸附,对萘产生分配作用,其表观分配系数(K_d^*)随MPB加入量的增大而急剧增大;当X在1/10CMC～ICMC之间,由于表面活性剂的吸附作用及其单体的增溶作用,K_d^*值则缓慢减小;当X大于1CMC,由于增加的表面活性剂主要起胶束增溶作用,K_d^*值则急剧减小.引入了标化表观分配系数(K_oc^*)探讨萘在表面活性剂-膨润土-水体系中的吸附机理,其倒数(1/K_oc^*)与X呈线性关系;由线性斜率和截距可求得K_oc、K_mn、K_mc参数.     

Effects of temperature and surfactants on naphthalene and phenanthrene sorption by soil

Adsorption experiments were carried out to investigate the sorption behaviors of naphthalene and phenanthrene in six different soils and to determine the effects of temperature, linear alkylbenzene sulfonate (LAS) and cetylrimethyl ammonium bromide (CTAB) on sorption. The results show that for a given sorbent phenanthrene exhibited greater nonlinear and stronger sorption than naphthalene. There was a strong negative correlation for the Koc values with organic carbon content (foc). The increase of temperature was not favorable to sorption. Sorption decreased along with the increasing aqueous LAS concentration from 0 to 1000 mg/L. At low CTAB concentration (＜ 100 mg/L), the adsorption increased as CTAB hemimicelles formed on the soil surface. At high concentration, CTAB decreased the adsorption by occupying active hydrophobic adsorption sites and solubilization of naphthalene and phenanthrene.     

Effect of organic fractions on sorption properties of organic pollutants in sediments

Humic substrates are a major fraction of sediment organic matters, and the sorption of hydrophobic organic chemicals by humic substrates influences their behavior and fate in sediment. In this paper, organic matters were divided into non-humic substrates and humic substrates. Non-humic substrates include acid leaching fraction, acid extracted fraction, and lipid; humic substrates were fractionated into Ca-binding-FA(fulvic acid), Ca-binding-HA (humic acid), oxide-FA, oxide-HA, and humin. To study the effect of organic fractions on sorption properties, sorption kinetic and equilibrium sorption experiments of phenanthrene and pentachlorophenol(PCP) in five sediments were carried out. The results showed that the contents of acid leaching fraction and oxide-binding-HA were the main fractions to affect the sorption rate constant, and for the sorption capacity of phenanthrene, humin was the major fraction, followed by oxide-binding-HA, oxidebinding-FA, and so on. While for PCP, the factors of influence on sorption capacity were mainly CEC, Ca-binding-FA, and Ca-binding-HA.     

Effects of free iron oxyhydrates and soil organic matter on copper sorption-desorption behavior by size fractions of aggregates from two paddy soils

Effects of free iron oxyhydrates (Fed) and soil organic matter (SOM) on copper (Cu2+) sorption-desorption behavior by size fractions of aggregates from two typical paddy soils (Ferric-Accumulic Stagnic Anthrosol (Soil H) and Gleyic Stagnic Anthrosol (Soil W)) were investigated with and without treatment of dithionite-citrate-bicarbonate and of H2O2. The size fractions of aggregates were obtained from the undisturbed bulk topsoil using a low energy ultrasonic dispersion procedure. Experiments of equilibrium sorption and subsequent desorption were conducted at soil water ratio of 1:20, 25℃. For Soil H, Cu2+ sorption capacity of the DCB-treated size fractions was decreased by 5.9% for fine sand fraction, by 40.4% for coarse sand fraction, in comparison to 2.9% for the bulk sample. However, Cu2+ sorption capacities of the H2O2-treated fractions were decreased by over 80% for the coarse sand fraction and by 15% for the clay-sized fraction in comparison to 88% for bulk soil. For Soil W, Cu2+ sorption capacity of the DCB-treated size fraction was decreased by 30% for the coarse sand fraction and by over 75% for silt sand fraction in comparison to 44.5% for the bulk sample. Cu2+ sorption capacities of the H2O2-treated fractions were decreased by only 2.0% for the coarse sand fraction and by 15% for the fine sand fraction in comparison to by 3.4% for bulk soil. However, Cu2+ desorption rates were increased much in H2O2-treated samples by over 80% except the clay-sized fraction (only 9.5%) for Soil H. While removal of SOM with H2O2 tendend to increase desorption rate, DCB- and H2O2-treatments caused decrease in Cu2+ retention capacity of size fractions. Particularly, there hardly remained Cu2+ retention capacity by size fractions from Soil H after H2O2 treatment except for clay-sized fraction. These findings supported again the dominance of the coarse sand fraction in sorption of metals and the preference of absorbed metals bound to SOM in differently stabilized status among the size fractions. Thus, enrichment and turnover of SOM in paddy soils may have great effects on metal retention and chemical mobility in paddy soils.     

水体冻结过程中卤乙酸前体物在水-冰体系中的分配研究

通过室内模拟试验,研究了水体冻结过程中,水体中溶解性有机物(DOM)和卤乙酸前体物在水-冰体系中的分配规律.按照DOM在XAD树脂上的吸附特性将其分为5个部分:疏水性有机酸(HPO-A),疏水性中性有机物(HPO-N),过渡亲水性有机酸(TPI-A),过渡亲水性中性有机物(TPI-N)和亲水性有机物(HPI).结果表明:在水体冻结过程中,5种DOM组分在水相中的DOC浓度均随冷冻时间的增长而增加,呈现冷冻浓缩效应.与溶解性有机碳(DOC)所表征的整体有机物相比,5种DOM组分中的卤乙酸(HAAs)前体物更倾向于停留在水相中浓缩.在5种DOM组分中,HPI是主要的HAAs前体物.5种DOM组分在未冻结水中的UV-254与HAAFP均表现出一定相关性,其中HPO-A, TPI-A和HPI的UV-254与HAAFP达到极显著水平.然而在融冰水中,这5种DOM组分的UV-254与HAAFP的相关性均不显著.     

二级处理出水中溶解性有机物的荧光特性

为研究二级处理出水中溶解性有机物的荧光特性,以沈阳市B污水处理厂为研究对象,利用XAD树脂对二级处理出水中的溶解性有机物(DOM)进行分级分离。按照DOM在不同树脂上的吸附特性将其分为5个部分:疏水性有机酸(HPO-A)、疏水性中性有机物(HPO-N)、过渡亲水性有机酸(TPI-A)、过渡亲水性中性有机物(TPI-N)和亲水性有机物(HPI)。研究结果表明,DOM组分中含有类腐植酸荧光团、类富里酸荧光团、类芳香族蛋白质荧光团和类溶解性微生物代谢产物荧光团,此外,还含有具有多环芳香结构的荧光物质。DOM中的荧光物质主要集中在HPO-N和TPI-N中。类腐植酸荧光团、类富里酸荧光团和类溶解性微生物代谢产物荧光团在TPI-N中的含量最高,而类芳香族蛋白质荧光团在HPO-N中的含量最高。对于HPO-A、TPI-A和TPI-N来说,类富里酸荧光峰的强度最高;类芳香族蛋白质荧光峰是HPO-N的最强峰;类溶解性微生物代谢产物荧光峰是HPI的最强峰。     

重金属污染的长春水田黑土对菲的吸附作用

以菲为多环芳烃(PAHs)代表物,研究了Pb、Zn、Cu污染后黑土对PAHs的吸附作用.结果表明,分配作用是黑土吸附菲的主要机制,无论重金属污染与否,黑土对菲的等温吸附曲线均呈线性.实验条件下,重金属污染后黑土对菲的吸附作用明显增强,且随重金属含量提高,黑土对菲的吸附系数(Kd)和有机碳标化的吸附系数(Koc)增大.由于重金属的“键桥”作用,黑土吸附菲的平衡溶液中水溶性有机质(DOM)浓度降低,土壤固相有机质含量略有增加(不超过原有有机质含量的0.53%).计算了这部分增加的固相有机质对菲的吸附系数K_Ph/soc,并分析了溶液中DOM对土壤吸附菲的影响.结果显示,溶液中DOM浓度变化及其与菲的结合作用对重金属影响土壤吸附菲的贡献甚微;而K_Ph/soc值则比土壤原有有机质对菲的吸附系数K_d值大2～3个数量级,这是重金属污染导致土壤吸附作用增强的根本原因.     

溶解性有机物在土壤含水层处理系统中的变化

通过实验室模拟土壤含水层处理(SAT)的土壤柱系统研究了二级处理出水中溶解性有机物(DOM)的荧光特性在SAT系统中的变化.利用XAD树脂将二级处理出水中的DOM分为5个部分:疏水性有机酸(HPO-A),疏水性中性有机物(HPO-N),过渡亲水性有机酸(TPI-A),过渡亲水性中性有机物(TPI-N)和亲水性有机物(HPI).结果表明,TPI-N中的类芳香族蛋白质荧光物质在SAT系统中优先去除.经过SAT系统处理后,类芳香族蛋白质荧光物质和类溶解性微生物代谢产物荧光物质在HPO-A,HPO-N,TPI-A和HPI中的相对含量升高.各组分中带有3~5个稠合苯环的荧光物质,以及激发波长/发射波长(λex/λem)=390~410nm/456~476nm的类腐殖酸荧光物质在SAT系统中的去除率低于相应组分中以溶解性有机碳(DOC)表征的整体有机物的去除率.不同组分中的其他荧光物质在SAT系统中去除行为不同.     

Binding of pyrene to dissolved organic matters: fractionation and characterization

Based on a modified Leenheer DOM fractionation scheme, fractionation of DOM from the paddy soil was conducted by using XAD-8 resin into hydrophobic bases ( HOB), hydrophobic acids ( HOA), acid-insoluble matter ( AIM), hydrophobic neutrals ( HON ) and hydrophilic matter(HIM). In total carbon content of DOM, 35.32% were the HIM and only 0.73% the HOB. However, HOA and AIM altogether occupied 53.45%, while the HON fraction represented 10%. The sorption experiments were conducted to determine the sorption capacity of pyrene on unfractionated DOM and its fractions. Elemental analysis, ^1H-NMR and FTIR spectra were carried out on unfractionated DOM and its fractions to examine the relationship between the structure of DOM and partition coefficients( Kac ). The results showed that HON had a greater affinity for binding pyrene than other fractions. While HON was characterized by large long-chain alkylate (aliphatic structure). AIM exhibited relative higher Kac values than HOA and HIM, due to much aromatic structure in AIM, while the high content of carboxylic groups of HOA and HIM depressed their binding capacity. This study demonstrated HON is a key subcomponents of DOM in binding of pyrene, in other words, aliphalic structure in DOM play an important role in binding of pyrene.     

水源水中有机物特性及其氯化活性研究

以西南某市一个地表水为水源水的M水厂为研究对象，对其原水中有机物进行富集，有机物按照操作定义分为6个部分，分别为：亲水性有机酸、亲水性有机碱、亲水中性物质、疏水性有机酸、疏水性有机碱和疏水性物质，通过富集、确定了原水中6种有机物的组成分布，研究各种有机物的消毒副产物形成潜力以及替代剂（氯胺、二氧化氯）对卤乙酸形成的影响，提出了控制消毒副产物的主要对策，研究结果表明：1）M水厂水源水属于腐殖质含量的天然水体，受污染较小；2）原水溶解性有机物中疏水性有机酸是卤乙酸的主要前体物；3）用氯胺和二氧化氯代替传统的消毒剂作为替代消毒剂，可大大降低THMs和HAAs的生成量。     

石化污水厂二级出水溶解性有机物分级解析研究

以某石化污水处理厂二级出水为研究对象,采用大孔吸附树脂将污水中溶解性有机物分离成亲水性物质、疏水酸性物质、疏水中性物质和疏水碱性物质4个组分,分析了各组分的有机物的组成特征、三维荧光光谱特征及红外光谱特征.结果表明,亲水性物质和疏水酸性物质分别占水样中溶解性有机碳的49%和29%,是该石化污水厂二级出水中的主要物质类别.亲水性物质中含有较多的生物源腐殖质类物质,疏水中性物质含有较多的芳香族蛋白质和溶解性微生物代谢产物类物质.4种组分的红外光谱图中600~1200cm-1波数的指纹区波峰数量最多,多为芳香类同分异构体化合物.     

土壤不同有机质组分对菲的吸附特征研究

采用批次实验,研究了三种不同类型土壤黄红壤、水稻土和草甸土的全土、重组、去松结态和紧结态4个组分对菲的吸附,结果表明,菲在不同土壤及其组分上的吸附等温线都能用Freundlich方程进行拟合,所有等温线都具有一定程度的非线性,指数N值的大小顺序基本都为全土>重组>去松结态>紧结态.除了黄红壤的紧结态比去松结态对菲的吸附容量KF值略小外,不同土壤及其组分对菲吸附的KF值以及有机碳归一化的KFoc值大小顺序都为紧结态>去松结态>重组>全土.不同类型土壤之间的KF值大小顺序为草甸土>水稻土>黄红壤,而KFoc值大小顺为水稻土>草甸土>黄红壤.KF值与有机碳含量之间呈显著性正相关(P<0.05),KFoc与N之间呈极显著负相关(P<0.001).土壤及其组分对菲的吸附强度与有机质的结构特征和聚合程度有关.     

溶解性有机质对芘在土壤中吸附解吸的影响

从腐解不同阶段的水稻秸秆提取溶解性有机质(DOM),用DAX-8树脂分组的方法分析了其亲疏水性,并研究了提取到的DOM对芘在土壤中吸附-解吸行为的影响.结果表明,随秸秆腐解时间的延长,产生DOM中亲水性组分减少,疏水性组分增多.在本试验所研究的吸附解吸实验条件下,芘在土壤中的吸附解吸均可用线性方程进行描述.加入DOM后,芘的吸附受到显著抑制(p0.01),并且随腐解时间延长,抑制作用增强;芘在土壤中存在解吸迟滞现象,加入DOM后迟滞现象减弱,促进了芘在土壤中的解吸.随腐解作用的进行,DOM促进芘解吸的作用增强,解吸迟滞系数减小.这是由于随秸秆腐解作用的进行,产生DOM中疏水性组分含量增多,其对芘的增溶作用增强所致.     

Partition of polycyclic aromatic hydrocarbons on organobentonites from water

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Sorption mechanism of naphthalene by diesel soot: Insight from displacement with phenanthrene/p-nitrophenol

The nonlinear sorption of hydrophobic organic contaminants (HOCs) could be changed to linear sorption by the suppression of coexisting solutes in natural system, resulting in the enhancement of mobility, bioavailability and risks of HOCs in the environment. In previous study, inspired from the competitive adsorption on activated carbon (AC), the displaceable fraction of HOCs sorption to soot by competitor was attributed to the adsorption on elemental carbon fraction of soot (EC-Soot), while the linear and nondisplaceable fraction was attributed to the partition in authigenic organic matter of soot (OM-Soot). In this study, however, we observed that the linear and nondisplaceable fraction of HOC (naphthalene) to a diesel soot (D-Soot) by competitor (phenanthrene or p-nitrophenol) should be attributed to not only the linear partition in OM-Soot, but also the residual linear adsorption on EC-Soot. We also observed that the competition on the surface of soot dominated by external surface was different from that of AC dominated by micropore surface, i.e., complete displacement of HOCs by p-nitrophenol could occur for the micropore surface of AC, but not for the external surface of soot. These observations were obtained through the separation of EC-Soot and OM-Soot from D-Soot with organic-solvent extraction and the sorption comparisons of D-Soot with an AC (ACF300) and a multiwalled carbon nanotube (MWCNT30). The obtained results would give new insights to the sorption mechanisms of HOCs by soot and help to assess their environmental risks.     

模拟根系分泌物对土壤吸附菲的影响

采用批量平衡试验方法,研究了模拟根系分泌物(ARE)对黄棕壤、棕红壤和红壤吸附菲的影响.结果表明,3种土壤对菲的等温吸附曲线均为线性,加入ARE后,土壤吸附菲的分配系数(Kd)和有机碳标化的分配系数(Koc)显著降低,且降低量随着ARE浓度的增加而增大,表明ARE抑制了土壤对菲的吸附.土壤有机质含量越低,ARE对土壤吸附菲的抑制作用越明显.分析土样吸附菲的平衡溶液中水溶性有机质(DOM)浓度,发现加入ARE后土壤有机质含量略有降低(1.64%),而DOM浓度增大,DOM与菲的结合作用对土壤吸附菲的抑制作用增强,这可能是ARE抑制土壤吸附菲的主要原因.