甲基对硫磷和西维因在粘土矿物表面的吸附解吸特性

研究了甲基对硫磷和西维因在蒙脱石、高岭石和针铁矿表面的吸附 解吸特征。结果表明,Langmuir方程能较好的描述甲基对硫磷和西维因在３种矿物表面的等温吸附过程,且蒙脱石对农药的最大吸附量大于高岭石和针铁矿。用动力学方程对2种农药的吸附过程进行拟合,Elovich方程、双常数方程和一级动力学方程均得到较好的结果,其中Elovich方程为最佳模型,相关系数（R²）在0.93～0.98之间,说明该吸附为非均相扩散过程。3种矿物对甲基对硫磷和西维因的吸附强度均为蒙脱石＞高岭石＞针铁矿。     

GC-MS在微生物降解农药机制研究中的应用

农药的微生物降解及代谢已有不少报道,但国内对微生物降解农药的机理研究报道较少[1].甲基对硫磷(化学名称O,O-二甲基-O-(4-硝基苯基)硫逐磷酸酯)为高效有机磷杀虫剂,甲基对硫磷(MP)降解菌DLL-1在实验室中的分离、鉴定见文献[2].本研究采用GC-MS联用技术对DLL-1菌降解甲基对硫磷农药的中间产物进行了定性鉴定,同时应用GC-MS对DLL-1菌降解甲基对硫磷及其中间产物的特性进行了动态分析.     

高效液相色谱与飞行时间质谱联用技术研究

用青岛曹家汶河口沉积物中分离出的细菌L-10(希瓦氏菌属)进行了水体中甲基对硫磷的细菌降解研究.研究表明,该菌对甲基对硫磷具有显著的降解性.采用高效液相色谱/飞行时间质谱(HPLC-TOF-MS)联用技术对甲基对硫磷及其细菌降解产物进行了分析.样品经SPE-C18小柱富集分离后,进行液相色谱和在线电喷雾飞行时间质谱分析.采用C18反相色谱柱(15 cm×4.6 mm i.d. 5 μm), 线性梯度为0 min 乙腈/水(30/70),5 min 乙腈/水(30/70),20 min 乙腈/水(80/20),25 min 乙腈/水(80/20);流速0.8 ml/min,甲酸铵缓冲溶液浓度为0.1% (V/V);电喷雾正离子(ESI)模式,m/z扫描范围50～1000进行TOF-MS扫描、测定,测定结果用Analyst QS软件进行分析.结果表明,与甲基对硫磷光降解产生甲基对氧磷和对硝基酚不同,在降解菌L-10的存在下,甲基对硫磷发生了取代、氧化、还原等一系列反应,产生了相应的降解产物.降解过程的机理很复杂,从甲基对硫磷及其降解产物的分子结构式来分析,推断可能与细菌本身的代谢有关.     

高效液相色谱与飞行时间质谱联用技术研究甲基对硫磷的细菌降解产物

用青岛曹家汶河口沉积物中分离出的细菌L-10(希瓦氏菌属)进行了水体中甲基对硫磷的细菌降解研究。研究表明,该菌对甲基对硫磷具有显著的降解性。采用高效液相色谱/飞行时间质谱(HPLC-TOF-MS)联用技术对甲基对硫磷及其细菌降解产物进行了分析。样品经SPE-C18小柱富集分离后,进行液相色谱和在线电喷雾飞行时间质谱分析。采用C18反相色谱柱(15 cm×4.6 mm i.d.5μm),线性梯度为:0 m in乙腈/水(30/70),5 m in乙腈/水(30/70),20 m in乙腈/水(80/20),25 m in乙腈/水(80/20);流速0.8 m l/m in,甲酸铵缓冲溶液浓度为0.1%(V/V);电喷雾正离子(ESI)模式,m/z扫描范围50~1000进行TOF-MS扫描、测定,测定结果用AnalystQS软件进行分析。结果表明,与甲基对硫磷光降解产生甲基对氧磷和对硝基酚不同,在降解菌L-10的存在下,甲基对硫磷发生了取代、氧化、还原等一系列反应,产生了相应的降解产物。降解过程的机理很复杂,从甲基对硫磷及其降解产物的分子结构式来分析,推断可能与细菌本身的代谢有关。     

"中性"粘土矿物对非水溶液中有机碱的吸附

理想品格中无同晶转换，因而不带层电行的中性粘土矿物（即：1：1型的高岭石，板状蛇纹石和2：1型的叶蜡石，滑石）对非极性有机溶剂中有机碱（偶氮苯化合物，pKa＝1.5-5.0）的吸附等温线均属于Langmuir型，且吸附在矿物表面的有机碱均由其碱型变为酸型.偶氮苯化合物的pKa越大，被吸附的量越多在溶剂为正己烷和二硫化碳时粘土的吸附能力比溶剂为苯时高.这些结果说明不带层电行的粘土矿物表面存在着酸位.蒙脱石的酸位数量明显地储存于阳离子种类，但在Na＋、Ca2＋、Mg2＋饱和的条件下高岭石的改位数量几乎相同.随着相对湿度的增加;两矿物对甲基黄的吸附量均减少，但减少的方式明显不同、因此1：1型高岭石和2：1型叶蜡石一样，也具有与蒙脱石不同的表面酸性起源。     

红壤可变电荷矿物的酸碱缓冲能力及表面络合模型

氧化铁和高岭石是红壤中可变电荷的主要来源,对红壤的酸碱变化起到缓冲作用.本研究基于红壤矿物的表征和酸碱滴定实验结果,采用1-site/2-pK表面络合模型获得了其表面活性位点浓度H_s、密度D_s、酸碱平衡常数pK_a^int以及电荷零点pH_pzc等相关参数,定量解析了氧化铁和高岭土的酸碱缓冲能力.结果表明：该模型能较好地适用于分析针铁矿、赤铁矿及高岭石的表面酸碱性质;针铁矿、高岭石表面活性位点浓度H_s较高,说明其对酸具有较好的缓冲效果.根据上述酸碱性质参数,模拟计算了不同pH下的矿物表面化学物种,揭示了矿物表面反应缓冲土壤酸碱变化的机制.采用上述酸碱滴定方法及模型计算方法,分析实际林地红壤样品的酸碱缓冲能力,并采用表面络合模型计算了其表面化学物种,验证了该方法用于林地红壤酸碱缓冲能力分析的可行性.     

针铁矿对焦磷酸根的吸附特征及吸附机制

为深入了解自然水体中焦磷酸盐的迁移转化行为,以表生环境中广泛存在的稳定矿物-针铁矿为研究对象,系统研究了其对焦磷酸根的吸附过程,探索了不同实验条件下(pH值、电解质、时间、温度)针铁矿对焦磷酸根吸附的影响。 结果表明,溶液pH值从6.27升至10.99时,总磷吸附量从3.00 mg/g降低至0.75 mg/g;电解质浓度越低越有利于针铁矿对焦磷酸根的吸附;吸附剂对焦磷酸根的吸附量在最初1 h内增长较快,随后渐渐达到吸附平衡;溶液温度的升高对吸附量提高具有增强作用。 用动力学和热力学模型对吸附过程进行拟合,发现准二级动力学和Langmuir模型具有更好的适用性。 结合材料吸附焦磷酸根前后的表征,推导出针铁矿对焦磷酸根的吸附机制可能是以表面配合和物理吸附为主导。     

石英微天平定量分析纳米Pd/TiO2对农药的吸附与降解

采用压电石英微天平(QCM)技术研究了有机农药甲基对硫磷在经钯(palladium,Pa)掺杂和软脂酸(palmic acid)改性前后的纳米TiO2上的吸附和降解行为。研究表明Pd和PA均能提高纳米TiO2对非极性有机农药的吸附量,复合纳米TiO2和Pd/TiO2的最大吸附量Г∞分别为6.18×10-4mol/g和7.54×10-4mol/g,吸附常数k分别为5.72×103L/mol和1.79×103L/mol。光降解和毒力实验结果表明复合纳米TiO2和Pd/TiO2农药制剂可在太阳光照下自行降解,在农作物体内的残留期大大缩短,且复合纳米TiO2和Pd/TiO2农药制剂的毒力有明显的提高,5%的纳米TiO2和Pd/TiO2乳液的毒力分别是95%原药毒力的1.68倍和2.19倍。     

聚脲多孔材料的简单制备及在酶固定和手性拆分中的应用

以甲苯二异氰酸酯(TDI)为单体,在水与丙酮混合溶剂中通过沉淀聚合一步法制备了富含胺基的聚脲多孔材料(PPU),通过扫描电镜和压汞法对其表面形貌和孔结构进行了表征.PPU经戊二醛(GA)活化后用于荧光假单胞菌脂肪酶(PFL)的固定,考察了GA活化过程中GA浓度对酶固定量及固定酶活性的影响.结果表明,PPU是一种粒子尺寸分布在30~50μm范围的形状不规则的多孔粒子,孔径在2 nm~100μm之间呈连续分布.在pH=8.0的缓冲溶液中用0.17 mol/L的GA对PPU进行改性,将改性后的PPU用于PFL的固定,当酶溶液浓度为2.56 mg/m L时,得到酶的最大固定量为95.2 mg/g,固定酶的活性为375 U/mg,相对活性为76%.将此固定酶作为催化剂,用于1-苯乙醇外消旋化合物的手性拆分,并与游离酶催化的结果相比较.结果表明,固定酶的反应活性和立体选择性都明显优于游离酶.通过沉淀聚合制备的聚脲多孔材料在酶固定及手性分子拆分方面具有应用前景.     

STXM-NEXAFS研究铁(Ⅲ)离子诱发柠檬酸在高岭石表面的固定机制

热带地区土壤有机碳的稳定性受有机碳与高岭石、三价铁离子[Fe(Ⅲ)]交互作用的强烈影响.低分子量有机酸(LMWOAs)是土壤有机碳中最易被微生物降解的组分,研究LMWOAs在高岭石-Fe(Ⅲ)-LMWOAs三相系统中的固定机制对于理解热带地区土壤有机碳循环具有重要意义;然而LMWOAs在该三相系统中固定机制仍不清楚,并缺乏分子水平上的直接证据.本研究以柠檬酸(CA)为LMWOAs的典型代表,通过采集Fe/CA初始物质的量比2.0条件下获取的吸附样品,利用同步辐射X射线扫描透射显微术(STXM)在亚微米尺度上表征C,Fe和Si的分布特征,发现C-Fe分布的相关性与C-Si分布相当;并在高C,Fe微区中利用C的K边和Fe的L3边X射线近边吸收精细结构谱(NEXAFS)在分子水平上揭示了Fe在不同富集微区分别以水铁矿和高岭石-Fe(Ⅲ)-CA三元配合体形式存在,从而表明水铁矿诱发的吸附/共沉淀以及以Fe(Ⅲ)为架桥形成高岭石-Fe(Ⅲ)-CA三元配合作用是CA固定的重要机制.本研究成果对于理解热带地区土壤中CA稳定性和低分子量有机酸的碳固定和循环机制提供了重要科学依据.     

Preferential adsorption of extracellular polymeric substances from bacteria on clay minerals and iron oxide

The adsorption of extracellular polymeric substances (EPS) from Bacillus subtilis on montmorillonite, kaolinite and goethite was investigated as a function of pH and ionic strength using batch studies coupled with Fourier transform infrared (FTIR) spectroscopy. The adsorption isotherms of EPS on minerals conformed to the Langmuir equation. The amount of EPS-C and -N adsorbed followed the sequence of montmorillonite>goethite>kaolinite. However, EPS-P adsorption was in the order of goethite>montmorillonite>kaolinite. A marked decrease in the mass fraction of EPS adsorption on minerals was observed with the increase of final pH from 3.1 to 8.3. Calcium ion was more efficient than sodium ion in promoting EPS adsorption on minerals. At various pH values and ionic strength, the mass fraction of EPS-N was higher than those of EPS-C and -P on montmorillonite and kaolinite, while the mass fraction of EPS-P was the highest on goethite. These results suggest that proteinaceous constituents were adsorbed preferentially on montmorillonite and kaolinite, and phosphorylated macromolecules were absorbed preferentially on goethite. Adsorption of EPS on clay minerals resulted in obvious shifts of infrared absorption bands of adsorbed water molecules, showing the importance of hydrogen bonding in EPS adsorption. The highest K values in equilibrium adsorption and FTIR are consistent with ligand exchange of EPS phosphate groups for goethite surface. The information obtained is of fundamental significance for understanding interfacial reactions between microorganisms and minerals.     

Sorption of Cypermethrin Diastereoisomers to Quartz,Corundum, Goethite,Kaolinite and Montmorillonite

Differential sorption and degradation of different pesticide stereoisomers in soil may result in accumulation of the most strongly sorbed and the slowest degradable isomers. In this work the pyrethroid cypermethrin (8 isomers) has been used for test of stereochemical interactions with surfaces of the minerals quartz, corundum, goethite, kaolinite and montmorillonite. The sorption of three diastereoisomeric fractions denoted Cis A, Trans C and Cis B + Trans D were quantified by use of GC-ECD in batch experiments with initial cypermethrin concentrations in the range 1-9 µg/L. Correction for cypermethrin sorbed to surfaces of the shaking flasks were accomplished to obtain net sorption isotherms for the minerals, all of which were well fitted by the Freundlich equation. Bonding affinities per unit surface area decreased in the order: corundum > quartz > kaolinite > montmorillonite > goethite. The isotherms for sorption of all diastereoisomeric fractions to quartz, corundum and goethite were all linear, whereas non-linear isotherms were found for sorption of Cis A and Trans C fractions to kaolinite and montmorillonite. Corundum, quartz and goethite showed a significantly stronger sorption of Cis A than the other fractions, while kaolinite sorbed Cis B + Trans D most strongly. The observed differences predict less leaching and slower degradation of the Cis A fraction in subsoils low in organic carbon.     

Effects of low-molecular-weight organic ligands and phosphate on adsorption of Pseudomonas putida by clay minerals and iron oxide

Adsorption of Pseudomonas putida on kaolinite, montmorillonite and goethite was studied in the presence of organic ligands and phosphate. Citrate, tartrate, oxalate and phosphate showed inhibitive effect on P. putida adsorption by three minerals in a broad range of anion concentrations. The highest efficiencies of the four ligands in blocking the adsorption of P. putida on goethite, kaolinite and montmorillonite were 58–90%, 35–76% and 20–48%, respectively. The ability of organic ligands in prohibiting the binding of P. putida cells to the minerals followed the sequence of citrate > tartrate > oxalate > acetate. The significant suppressive effects on P. putida adsorption were ascribed to the increased negative charges by adsorbed ligands and the competition of ligands with bacterial surface groups for binding sites. The inhibitive effects on P. putida adsorption by organic ligands were also dependent on the steric hindrance of the molecules. Acetate presented promotive effect on P. putida adsorption by kaolinite and goethite at low anion concentrations. The results obtained in this study suggested that the adsorption of bacteria in soils especially in the rhizosphere can significantly be impacted by various organic and inorganic anions.     

Sorption of bisphenol A, 17alpha-ethynylestradiol and estrone to mineral surfaces

Sorption of the endocrine disrupting chemicals (EDCs) bisphenol A (BPA), 17alpha-ethynylestradiol (EE2) and estrone (E1) from 3 microM aqueous solutions in 10 mM KNO3 to goethite, kaolinite and montmorillonite was investigated at 25 degrees C. Uptake of the EDCs by goethite and kaolinite suspensions was <20%, and little affected by pH. Sorption by montmorillonite was greater, ranging from 20 to 60%, and steadily increased from about pH 7. The amount of EDC sorbed to the mineral phases generally increased in the order of decreasing solubility (BPA相似文献   

Effects of low-molecular-weight organic ligands and phosphate on DNA adsorption by soil colloids and minerals

Adsorption of DNA on montmorillonite, kaolinite, goethite and soil clays from an Alfisol in the presence of citrate, tartrate and phosphate was studied. A marked decrease in DNA adsorption was observed on montmorillonite and kaolinite with increasing anion concentrations from 0 to 5 mM. However, the amount of DNA adsorbed by montmorillonite and kaolinite was enhanced when ligand concentration was higher than 5 mM. In the system of soil colloids and goethite, with the increase of anion concentrations, a steady decrease was found and the ability of ligands in depressing DNA adsorption followed the sequence: phosphate > citrate > tartrate. Compared to H2O2-treated clays (inorganic clays), a sharp decrease in DNA adsorption was observed on goethite and organo-mineral complexes (organic clays) with increasing ligand concentrations. The results suggest that the influence of anions on DNA adsorption varies with the type and concentration of anion as well as the surface properties of soil components. Introduction of DNA into the system before the addition of ligands had the greatest amount of DNA adsorption on soil colloids and goethite. Organic and inorganic ligands promoted DNA adsorption on montmorillonite and kaolinite when ligands were introduced into the system before the addition of DNA. The results obtained in this study have important implications for the understanding of the persistence and fate of DNA in soil environments especially rhizosphere soil where various organic and inorganic ligands are active.     

Adsorption of Pseudomonas putida on clay minerals and iron oxide

Adsorption of Pseudomonas putida on minerals including montmorillonite, kaolinite and goethite was studied. The adsorption isotherms of P. putida on the examined minerals conformed to the Langmuir equation. The amount of P. putida adsorbed followed the order: goethite > kaolinite > montmorillonite. A greater extent of P. putida adsorption on minerals was observed in the range of temperature from 15 to 35 °C. The adsorption of P. putida on minerals decreased with the increase of pH from 3.0 to 10.0. Magnesium ion was more efficient than sodium ion in promoting P. putida adsorption on minerals. The results suggest that electrostatic interactions play a vital role in P. putida adsorption by soil colloidal factions. The information obtained in this study is of fundamental significance for the understanding of the survival and transport of bacteria in soil systems.     

Copper and zinc removal from aqueous solution by mixed mineral systems II. The role of solution composition and aging

This study investigates Cu and Zn removal onto binary mixed mineral sorbents from simulated wastewater, relevant to streams impacted by acid mine drainage and effluents. Mixed suspensions of kaolinite/montmorillonite and kaolinite/goethite exhibited different sorption behavior from the single mineral components, reducing Cu and Zn removal (except Cu sorbed on montmorillonite/goethite) over the range of pH investigated. Cu and Zn removal by the electrolyzed systems showed a complex response to increased ionic strength, which increased solid concentration, leading to lower Cu and Zn sorption. Enhanced Cu sorption on the montmorillonite/goethite as age increased may be attributed to increased hydroxylation of the mineral surface resulting in the formation of new reactive sites.     

Adsorption of UO2 2+ on natural composite materials

The prediction of the adsorption behavior of natural composite materials was studied by a single mineral approach. The adsorption of U(VI) on single minerals such as goethite, hematite, kaolinite and quartz was fully modeled using the diffuse-layer model in various experimental conditions. A quasi-thermodynamic database of surface complexation constants for single minerals was established in a consistent manner. In a preliminary work, the adsorption of a synthetic mixture of goethite and kaolinite was simulated using the model established for a single mineral system. The competitive adsorption of U(VI) between goethite and kaolinite can be well explained by the model. The adsorption behavior of natural composite materials taken from the Koongarra uranium deposit (Australia) was predicted in a similar manner. In comparison with the synthetic mixture, the prediction was less successful in the acidic pH range. However, the model predicted well the adsorption behavior in the neutral to alkaline pH range. Furthermore, the model reasonably explained the role of iron oxide minerals in the adsorption of U(VI) on natural composite materials.