苯分子与Si_6O_18H_12和Al_6O_24H_30团簇模型相互作用的理论研究(英文)

粘土矿已经被广泛用来去除有机物,修复和净化被石油碳氢化合物污染的土壤和地下水.我们选择高岭石作为研究对象,构造了Si6O18H12和Al6O24H30两个团簇模型分别代表高岭石的硅氧层表面和铝氧层表面,在MP2/6-31G(d,p)//B3LYP/6-31G(d,p)的理论水平上系统地研究了气态下苯分子和高岭石团簇模型的相互作用.并进一步分析了苯分子和高岭石表面相互作用的各种气态性质,比如:优化的几何构型、结构参数、吸附能、自然键轨道电荷分布、振动频率变化、静电势、电子密度性质(次级氢键的电子密度和拉普拉斯算符值)和电子密度差分等.优化的几何构型表明苯分子吸附在高岭石表面的本质可能是次级氢键的形成.其他性质的结果进一步验证了次级氢键的存在,并指出苯更倾向于吸附在高岭石的铝氧层表面,且苯环和铝氧层表面形成近似90°的夹角.     

光学活性偶氮苯自组装膜的制备及其蛋白吸附行为

研究了在紫外光作用下, 牛血清白蛋白(BSA)在偶氮苯自组装膜上光控可逆的吸附行为. 首先合成羧基偶氮苯衍生物, 并在金膜表面制备偶氮苯自组装膜, 采用紫外吸收光谱(UV)、原子力显微镜(AFM)观察偶氮苯衍生物的光学顺反异构现象以及偶氮苯自组装膜表面形貌的变化. 同时利用等离子体表面谐振仪(SPR)考察偶氮苯光学异构对牛血清白蛋白(BSA)在自组装膜表面上的吸附行为的影响. 结果表明, BSA在偶氮苯自组装膜表面的吸附作用主要来自于BSA分子与自组装膜之间的静电作用及亲疏水作用. 在紫外光作用下, 偶氮苯自组装膜可以实现光控可逆的牛血清白蛋白分子吸附行为.     

N_2O在Cu/t-ZrO_2(101)表面的吸附与解离

运用广义梯度密度泛函理论结合周期性平板模型方法研究了N2O在完整及负载Cu的四方相ZrO2(101)表面的吸附与解离.结果表明,N2O在完整ZrO2(101)表面的吸附均为物理吸附,Cu在其完整表面的次表层第一氧位为最稳定吸附位,且覆盖度为0.25ML时的吸附最为稳定,吸附能为155.8kJ/mol;N2O分子中O端弱物理吸附于Cu/ZrO2(101)表面,其N端及平行吸附方式得到的稳定吸附能分别为121.6和66.8kJ/mol.频率及电荷布居计算表明,吸附后对称和反对称伸缩振动频率均发生红移,电子由Cu负载底物表面转移给N2O分子.对N2O分子的解离考虑了N端垂直吸附和平行吸附两种解离反应过程,发现平行吸附过程的解离更易发生.     

苯在CuCl（111）表面吸附的密度泛函理论研究

采用量子化学的密度泛函理论方法,探讨了苯分子在CuCl(111)表面上不同覆盖度下不同吸附位上的平行吸附行为. 计算结果表明,随覆盖度的减小,吸附作用增强, Cl位上的吸附是稳定的吸附模式,在低覆盖度下吸附能约为74 kJ/mol, 在顶位和穴位上的吸附属于较弱的物理吸附. 同时对吸附前后的电子布居和态密度进行了分析. 吸附过程中,苯分子的π电子向底物转移,同时Cu的 3d轨道的电子反馈给苯的反键π轨道.     

水合Pb(OH)~+在高岭石(001)晶面的吸附机理(英文)

采用密度泛函理论广义梯度近似平面波赝势法,结合周期平板模型,探讨了水体环境中Pb(OH)+在高岭石铝氧八面体(001)晶面的吸附行为和机理,确定了吸附配合物的结构、配位数、优势吸附位和吸附类型.结果表明,Pb(II)与高岭石铝氧(001)面的氧原子形成单齿或双齿配合物,其配位数为3-5,均为半方位构型.高岭石表面存在含"平伏"氢原子的表面氧(Ol)位和含"直立"氢原子的氧(Ou)位,后者更易与Pb(OH)+单齿配位,该吸附配合物具有较高的结合能(-182.60 kJ·mol-1),为优势吸附物种;高岭石表面位于同一个Al原子上的"OuOl"位可形成双齿配合物.表面Ol与水分子配体形成氢键,对配合物的稳定性起到关键作用.Mulliken布居和态密度分析表明,高岭石单齿配合物中Pb―O成键机理主要为Pb 6p轨道与Pb 6s―O 2p反键轨道进行耦合,电子转移到反键轨道.双齿配合物"Pb―Ol―H"共配位结构中,受配位氢原子影响,Pb―Ol成键过程成键态电子填充占主导地位.     

CO在α-U(001)表面的吸附

采用密度泛函理论中的广义梯度近似,计算了CO在α-U(001)表面的吸附、解离和扩散.结果表明:CO分子以CU3OU2构型化学吸附在α-U(001)表面,吸附能为1.78-1.99eV;吸附后表层U原子向上迁移,伴随着褶皱的产生;CO分子与表面U原子的相互作用主要是U原子的电子向CO分子最低空轨道2π*转移,以及CO2π*/5σ/1π-U6d轨道间杂化而生成新的化学键;CO解离吸附较分子吸附在能量上更为有利,h1(C)+h2(O)和h1(C)+h1(O)(h:空位)解离态吸附能分别为2.71和3.08eV;近邻三重穴位之间C、O原子的扩散能垒分别为0.57和0.14eV,预示O原子较C原子更易在U(001)表面扩散迁移.     

吸附O的Cu(110)c(2×1)表面原子结构和电子态

采用第一性原理的密度泛函理论方法计算了清洁Cu(110)表面和吸附O原子的Cu(110) c(2×1)表面的原子结构, 结构弛豫和电子结构, 得到了各种表面结构参数. 分别计算了O原子在Cu(110)表面三个可能吸附位置吸附后的能量, 并给出了能量最低的吸附位置上各层原子的弛豫特性和态密度. 结果表明O吸附后的Cu(110)表面有附加列(added-row)再构的特性, O原子吸附在最表层铜原子上方, 与衬底Cu原子的垂直距离为0.016 nm, 以氧分子为能量基准的吸附能为－1.94 eV; 同时由于Cu 3d- O 2p态的杂化作用使得低于费米能级5.5~6.0 eV的范围内出现了局域的表面态. 计算得到清洁的和氧吸附的Cu(110)表面的功函数分别为4.51 eV和4.68 eV. 电子态密度的结果表明：在Cu(110) c(2×1) 表面O吸附的结构下, 吸附O原子和金属衬底之间的结合主要是由于最表层Cu原子3d态和O原子2p态的相互作用.     

O3分子在CuO(110)面吸附的密度泛函理论研究

应用密度泛函理论研究了O3分子在2×1 CuO(110)面(S1)和掺杂一个Fe原子的2×1 CuO(110)面(S2)的吸附过程和电子特性. 计算结果表明, O3分子与表面S1和S2有很强的相互作用, O3分子在表面吸附反应的活化能和反应能均为负值, 反应很容易进行. 态密度和电荷密度分析结果进一步证实了O3分子在S1上吸附是桥位化学吸附, 形成表面臭氧化物, 在S2上吸附分解为1个被吸附的表面氧原子和1个自由氧分子. 电子特性分析表明, O3分子与S1和S2相互作用的本质是O3分子的价轨道2p与CuO(110)表面杂化轨道的相互作用.     

"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。     

苯氧羧酸类农药在高岭石表面吸附的理论研究

构建了高岭石铝氧八面体层表面模型Al₁₃O₄₈H₅₇和硅氧四面体层表面模型Si₁₃O₃₇H₂₂,采用B3LYP/6-31G(d,p)方法, 对其与2,4-二氯苯氧乙酸(2,4-D)、 2,4-二氯苯氧丙酸(2,4-DP)、 2,4-二氯苯氧丁酸(2,4-DB)、 2-甲基-4-氯苯氧乙酸(MCPA)、 2-甲基-4-氯苯氧丙酸(MCPP)和2-甲基-4-氯苯氧丁酸(MCPB)等苯氧羧酸类农药分子间的相互作用及吸附性质进行了研究, 包括优化的几何构型、 结构参数、 吸附能及自然键轨道(NBO)电荷. 八面体层表面的中心原子(OH2, OH3及OH11)与四面体层表面的中心原子(O2, O3及O11)并未表现出明显的吸附活性. 相较于侧链为乙酸基的分子, 含有丙酸基或丁酸基的分子因带有更多的吸附位点而具有较强的吸附性. 研究发现MCPP的吸附性高于MCPA. 结合2,4-D的吸附性高于MCPA的结论, 可以推断2,4-D与MCPA更倾向于吸附在高岭石的硅氧层表面. 因此在农药施用的过程中, 应充分考虑各分子的活性及其与高岭石表面的作用强弱, 确保淋洗对去除农药在土壤中残留的可行性.     

Photochemical phase transition behaviour of polymer azobenzene liquid crystals with flexible siloxane units as a side-chain spacer

The influence of the spacer structure on the photochemical phase transition behaviour was explored for azobenzene polymer liquid crystals (azo-PLCs) possessing siloxane spacers in the polymer side chain, and for analogue without the siloxane spacer. The photochemical phase transition of the azo-PLC with the siloxane spacer was found to proceed less effectively than that of the azo-PLC without the siloxane spacer. It was also confirmed that the spacer structure does not affect the trans-cis photoisomerization behaviour of the azobenzene moieties. These results were interpreted in terms of stabilization of the alignment of the mesogens in the liquid crystalline phase by the siloxane spacer, since the siloxane chain is one of the most flexible spacers and decouples the motion of the polymer backbone from that of the aligned mesogens. Furthermore, the response of the azo-PLCs in the photochemical phase transition was evaluated by means of a laser pulse. The phase transition occurred in 300 mus for both samples.     

Adsorption of oleic acid and triolein onto various minerals and surface treated minerals

A systematic investigation of the adsorption of oleic acid was under-taken with various minerals and surface treated minerals, viz., kaolinite, treated kaolinites, montmorillonites, talcs, gibbsites, calcites and a treated calcite. Adsorption onto kaolinite, two of the treated kaolinites (amine and MgSiO₃ treated), talcs and gibbsites was well correlated by the Langmuir model, while adsorption on the treated calcite was well correlated by the Freundlich model. Adsorption on a cationic polymer-treated kaolinite was explained in terms of a cooperative mechanism. Adsorption onto montmorillonites was explained in terms of a penetrative mechanism involving exchangeable cations.Oleic acid adsorption was compared with triolein adsorption on one of the montmorillonites, two adsorbents produced by the surface treatment of this montmorillonite, and one of the talcs. The triolein adsorption of the montmorillonite was considerably less than its oleic acid adsorption, and was explained in terms of a cooperative mechanism. Triolein adsorption of the treated montmorillonites, and the talc was well correlated by the Langmuir model. Larger amounts of triolein were taken up by the treated montmorillonites than by the untreated montmorillonite. The triolein adsorption of the talc was greater than its oleic acid adsorption.     

Equilibrium studies and modeling on the removal of <Superscript>56</Superscript>Mn(II) by alumina and kaolinite

The removal of manganese from aqueous solutions on synthetic alumina and natural kaolinite was investigated in batch experiments as a function of pH. Experiments were carried out by using the radiotracer ⁵⁶Mn, produced by neutron activation. Theoretical analysis of manganese removal was performed considering the existence of a single type of surface sites, denoted as?≡?SOH°. The uptake of manganese on kaolinite is similar to that on alumina, indicating that adsorption occurred on the variable-charged aluminol sites. Adsorption experiments suggest that?≡?AlOH° group is the most probable edge site for complexing manganese cations through mononuclear surface complexes (≡?AlOMn⁺) and (≡?AlOMnOH).     

Theoretical estimates of the IR spectrum of water intercalated into kaolinite

Calculations at AM1, PM3, and HF/6‐31G levels of part of the IR spectrum of the water–kaolinite intercalated system based on a 96‐atom cluster of kaolinite with one water molecule are reported. Only the water molecule conformation is optimized. Frequencies and intensities for just the water vibrations and stretchings of four cluster hydroxyls were calculated through partial Hessian matrices and polar tensors obtained by numerical differentiation of energy gradients and dipole moment. The water molecule was found to attach to the cluster mainly through a double hydrogen bond to the siloxane inner surface, partially entering the siloxane ring hexagonal hole. Though the theoretical results predict that the water OH stretching frequencies decrease from the gas‐phase state to the intercalated state, they are still higher than expected with respect to the observed spectrum. © 2008 Wiley Periodicals, Inc. Int J Quantum Chem, 2009     

Effect of water on the formamide-intercalation of kaolinite

The molecular structures of low defect kaolinite completely intercalated with formamide and formamide-water mixtures have been determined using a combination of X-ray diffraction, thermoanalytical techniques, DRIFT and Raman spectroscopy. Expansion of the kaolinite to 10.09 A was observed with subtle differences whether the kaolinite was expanded with formamide or formamide-water mixtures. Thermal analysis showed that greater amounts of formamide could be intercalated into the kaolinite in the presence of water. New infrared bands were observed for the formamide intercalated kaolinites at 3648, 3630 and 3606 cm(-1). These bands are attributed to the hydroxyl stretching frequencies of the inner surface hydroxyls hydrogen bonded to formamide with water, formamide and interlamellar water. Bands were observed at similar positions in the Raman spectrum. At liquid nitrogen temperature, the 3630 cm(-1) Raman band separated into two bands at 3633 and 3625 cm(-1). DRIFT spectra showed the hydroxyl deformation mode at 905 cm(-1). Changes in the molecular structure of the formamide are observed through both the NH stretching vibrations and the amide 1 and 2 bands. Upon intercalation of kaolinite with formamide, bands are observed at 3460, 3344, 3248 and 3167 cm(-1) attributed to the NH stretching vibration of the NH involved with hydrogen bonded to the oxygens of the kaolinite siloxane surface. In the DRIFT spectra of the formamide intercalated kaolinites bands are observed at 1700 and 1671 cm(-1) and are attributed to the amide 1 and amide 2 vibrations.     

Modeling the adsorption of Cd(II) onto kaolinite and Muloorina illite in the presence of citric acid

The adsorption of cadmium onto kaolinite and Muloorina illite in the presence of citric acid has been measured as a function of pH and cadmium concentration at 25 degrees C. When citric acid is present in the systems cadmium adsorption is slightly enhanced below pH 5, but significantly suppressed between pH 5 and 8, for both substrates. At higher citric acid concentrations very little cadmium adsorbs onto kaolinite from pH 5 to 8. Above pH 8 adsorption of Cd(II) onto illite is enhanced in the presence of citric acid, especially at lower concentrations, but this does not occur for kaolinite. Adsorption and potentiometric titration data were fitted by simple extended constant-capacitance surface complexation models for the two substrates. Enhancement of adsorption at lower pH values was ascribed to the ternary reaction [X(-)--K(+)](0)+Cd(2+)+L(3-)+2H(+) right arrow over left arrow (0)+K(+) involving outer-sphere complexation with permanently charged X(-) sites on the "silica" faces of both clay minerals. The models suggested that suppression of adsorption in the intermediate pH range was due to the formation of a strong CdL(-) solution complex which adsorbed neither on the permanently charged sites nor on the surface hydroxyl groups at the edges of the clay crystals. At higher pH values the dominant solution complex, CdLOH(2-), apparently adsorbed as an outer-sphere complex at surface hydroxyl groups on illite, SOH+2Cd(2+)+L(3-) right arrow over left arrow [SOCd(+)--CdOHL(2-)](-)+2H(+), but not on kaolinite. This difference in behavior results from the presence of =FeOH groups on the illite surface which can form surface complexes with CdLOH(2-), while the =AlOH groups on the kaolinite surface cannot.     

Effect of iron oxide coatings on zinc sorption mechanisms at the clay-mineral/water interface

Oxide surface coatings are ubiquitous in the environment, but their effect on the intrinsic metal uptake mechanism by the underlying mineral surface is poorly understood. In this study, the zinc (Zn) sorption complexes formed at the kaolinite, goethite, and goethite-coated kaolinite surfaces, were systematically studied as a function of pH, aging time, surface loading, and the extent of goethite coating, using extended X-ray absorption fine structure (EXAFS) spectroscopy. At pH 5.0, Zn partitioned to all sorbents by specific chemical binding to hydroxyl surface sites. At pH 7.0, the dominant sorption mechanism changed with reaction time. At the kaolinite surface, Zn was incorporated into a mixed metal Zn-Al layered double hydroxide (LDH). At the goethite surface, Zn initially formed a monodentate inner-sphere adsorption complex, with typical Zn-Fe distances of 3.18 A. However, with increasing reaction time, the major Zn sorption mechanism shifted to the formation of a zinc hydroxide surface precipitate, with characteristic Zn-Zn bond distances of 3.07 A. At the goethite-coated kaolinite surface, Zn initially bonded to FeOH groups of the goethite coating. With increasing aging time however, the inclusion of Zn into a mixed Zn-Al LDH took over as the dominant sorption mechanism. These results suggest that the formation of a precipitate phase at the kaolinite surface is thermodynamically favored over adsorption to the goethite coating. These findings show that the formation of Zn precipitates, similar in structure to brucite, at the pristine kaolinite, goethite, and goethite-coated kaolinite surfaces at near neutral pH and over extended reaction times is an important attenuation mechanism of metal contaminants in the environment.     

Reactivity of alkoxysilyl compounds: chemical surface modification of nano‐porous alumina membrane using alkoxysilylazobenzenes

In order to clarify the chemical adsorption properties of alkoxysilyl compounds to metal‐oxide surface quantitatively and to obtain the information on the reaction conditions for the efficient surface modification, the chemical surface modifications of nano‐porous alumina membranes (NPAMs) by typical alkoxysilyl compounds of 4‐(triethoxysilyl)azobenzene, 4‐(diethoxyphenylsilyl)azobenzene, 4‐(ethoxydiphenylsilyl)azobenzene and 4‐(methoxydimethylsilyl)azobenzene were examined. The chemical surface modifications were performed by immersing NPAMs into the solutions of the alkoxysilylazobenzenes. Especially for 4‐(triethoxysilyl)azobenzene, the modification was investigated precisely by changing the solvent, temperature, concentration and water content of the solutions to reveal the effects of the reaction conditions on the adsorption property of alkoxysilyl compounds to metal oxides. The NPAMs having chemically modified surface were prepared successfully by the immersing method, and the alkoxysilylazobenzenes were confirmed to be bound on the NPAM surface through Si? O? Al bonds, which were indicated to be formed mainly by the direct condensation reaction between the alkoxysilyl groups of the azobenzenes and the hydroxy groups on the NPAM surface. The amounts of the azobenzenes adsorbed on the NPAM surface were estimated quantitatively by a visible absorption spectroscopy, and the results showed that the solutions with non‐polar solvents, higher temperatures and higher concentrations are suitable for the efficient surface modification. Copyright © 2010 John Wiley & Sons, Ltd.     

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。