一种评估阳离子交换吸附活化能的方法（英文）

离子和带电粒子之间的相互作用受纳米/胶体颗粒表面上离子吸附控制,同时它决定着颗粒的微观性质、界面反应过程以及颗粒间相互作用。现有的离子界面反应理论没有考虑到离子特异性对离子-表面相互作用的影响。本研究建立了带电颗粒表面离子吸附模型。结果表明蒙脱石胶体表面离子吸附平衡存在着强烈的离子特异性效应。离子和表面之间的吸附能随离子浓度的增加而降低,随着粒子电荷密度(绝对值)升高而增加。根据建立的模型还可预测吸附反离子在扩散层中的位置,进而可计算出离子的吸附能与活化能。活化能直接决定了离子的吸附饱和度,且不同的离子遵循相同的规律。本研究表明建立的离子-表面相互作用模型在固/液界面反应中具有普适性的应用。     

螯合物调控蒙脱石电动电位及其吸附铬离子性能

采用改变pH值、电解质浓度和各种金属离子插层的方法, 调整对蒙脱石胶体的ζ电位, 研究了ζ电位变化与吸附金属铬离子性能的关系, 并用螯合物调控蒙脱石的ζ电位, 探索提高吸附铬离子性能的有效方法. 研究结果表明, 蒙脱石对铬离子的吸附性与ζ电位有关, 随着ζ电位的增大, 吸附量明显增大; 螯合物改性能使蒙脱石ζ电位发生明显变化, 经邻菲罗啉螯合物改性的蒙脱石电性由负变正; 对于离子交换吸附, 蒙脱石吸附前ζ电位的绝对值必须大于吸附后ζ电位的绝对值, 并且吸附前后ζ电位差值越大, 越有利于提高对低浓度铬离子的吸附; 用邻菲罗啉与铬离子的螯合物调控蒙脱石的ζ电位, 能使对铬离子的吸附量增大1倍以上, 因此, 采用螯合物调控蒙脱石ζ电位的方法有利于提高离子交换吸附的效果.     

蒙脱石化学修饰电极的制备与电化学特性

用预交换法和掺入法将某些荷阳电物(NR, MB)与荷阴电物[IC, Fe(CN)~6^3-]吸附在蒙脱石膜中制备化学修饰电极(CME)。对不同电性的吸附物, 用预交换法制备的CME在支持电解质溶液中显示不同的伏安响应。被吸附物在蒙脱石膜内的电活性浓度(c*)和总浓度(c~t)之比值较小, 说明被吸附物中只有小部分表现有电化学特性。X衍射实验表明荷阳电的吸附物可能通过离子交换吸附而嵌入蒙脱石层间。吸收光谱实验亦表明荷阳电物与蒙脱石间有强的化学吸附作用。根据蒙脱石中各种不同的吸附位置, 讨论了被吸附物对电化学响应的不同贡献。     

Eu(Ⅲ)在蒙脱石上的吸附及碳酸根和磷酸根对其吸附的影响

锕系核素在处置库围岩和缓冲回填材料中的吸附和迁移参数是处置库安全评价的重要数据模块之一，而Eu(Ⅲ)由于其与三价锕系元素An(Ⅲ)相似的离子半径和化学性质常被用于模拟三价锕系元素的化学行为。本文通过批式吸附实验研究了固液比、接触时间、离子强度、pH、碳酸根及磷酸根等对Eu(Ⅲ)在蒙脱石上吸附的影响，重点关注了吸附机理和表面种态。研究结果表明，低pH时Eu(Ⅲ)在蒙脱石上的吸附方式为外层配位吸附，近中性时为内层配位吸附，高pH时则以表面沉淀的方式被吸附。离子强度的增大对Eu(Ⅲ)在低pH时的吸附产生抑制作用。低pH时碳酸根对Eu(Ⅲ)吸附的影响不明显，但在高pH时其会改变Eu(Ⅲ)的表面吸附种态。尽管磷酸根本身的吸附非常弱，但磷酸根会显著增强Eu(Ⅲ)的吸附。X射线光电子能谱结果和磷酸根吸附实验说明Eu(Ⅲ)在蒙脱石表面上形成了EuPO₄沉淀。本工作研究了蒙脱石/Eu(Ⅲ)二元体系和蒙脱石/Eu(Ⅲ)/阴离子三元体系的吸附行为，并用光谱技术探究了其吸附种态，为理解三价锕系核素在蒙脱石上的吸附行为提供了重要参考。     

饱和锌的粘土矿物吸附半胱氨酸的机理

用红外光谱、X射线衍射（XRD）和热分析研究了饱和过渡金属锌的粘土矿物吸附半胱氨酸的机理；XRD结果显示吸附了半胱氨酸后的粘土矿物的d(001)方向的距离明显增大，说明被吸附的半胱氨酸进入了粘土的层状结构之中；饱和了锌的粘土矿物吸附半胱氨酸有两种方式，其一为弱相互作用，另一种强相互作用；后一种方式吸附的半胱氨酸与粘土的过渡金属之间形成了配合结构，结合力比较强，在热作用下，它们一直到395℃左右才分解；强相互作用吸附的半胱氨酸主要是以去质子的两性离子和阴离子形式存在于粘土矿物上，与过渡金属形成螯合的六元环结构。     

苯硫酚及其衍生物在银电极表面的吸附取向

采用表面增强拉曼光谱技术研究了苯硫酚及其功能衍生物，对巯基苯胺和对苯硫酚在粗糙银电极上的吸附取向特征。结果表明：虽然3种分子的结构类似，但对位取代基直接影响各分子在电极上的吸附取向。3种分子都通过硫原子与银电极形成S-Ag键吸附在电极表面。苯硫酚采用倾斜的方式吸附，使得苯环与基底间表现一定程度的相互作用；吸附的对巯基苯胺则因质子化氨基间的静电相互作用而完全垂直于电极表面；而对苯硫酚则采用平躺于电极表面的方式吸附，致使苯环π体系与基底银之间具有较强的相互作用。     

蒙脱石对Y~(3+)的吸附特性及机制研究

研究了提纯后蒙脱石对Y~(3+)的吸附行为,考察接触时间、固液比、初始浓度、 pH、离子强度、共存NH~+_4和温度对吸附过程的影响,并进行吸附等温模型拟合和热力学计算。研究结果表明:蒙脱石对Y~(3+)的吸附在1.5 min内可以达到平衡。固液比和Y~(3+)初始浓度的增大会减小Y~(3+)吸附量而增大吸附率;溶液pH的增大和离子强度的减小会促进Y~(3+)的吸附。离子交换是Y~(3+)吸附过程中存在的一种作用方式,随着pH增大,离子交换作用减弱,表面配位作用增强。Y~(3+)在蒙脱石上的吸附较好地符合Langmuir, Freundlich和Dubinin-Radushkevich吸附等温模型。根据吸附热力学参数, Y~(3+)在蒙脱石上的吸附自发进行,提高温度会促进Y~(3+)的吸附。     

Ni－Cu和TiO_2－SiO_2间的相互作用及其对催化性能的影响

用表面反应改性法制备了ＴｉＯ２－ＳｉＯ２（ＴＳＯ）表面复合物载体．采用ＴＰＲ，ＩＲ，ＴＰＤＭＳ和ＴＰＳＲ－ＭＳ等技术研究了ＮＩ－Ｃｕ／ＴＳＯ间的相互作用及其对ＣＯ加氢反应的催化性能．结果表明，ＮｉＯ－ＣｕＯ与ＴＳＯ间的相互作用导致ＣｕＯ的还原温度降低和ＮｉＯ的还原温度升高，并有少量表面物种生成；还原后的Ｎｉ－Ｃｕ／ＴＳＯ催化剂表面上存在着两类活性中心，即合金相中的Ｎｉ及载体相中的Ｔｉｎ＋（或Ｔｉｎ＋－Ｏ）；ＣＯ在催化剂表面存在孪生、线式、桥式和卧式等４种吸附态；Ｈ２在催化剂表面上发生解离吸附形成Ｎｉ－Ｈ和Ｔｉｎ＋－Ｈ，前者比较活泼，是加氢反应的主要Ｈ源；卧式吸附态极易在催化剂表面裂解形成Ｎｉ－Ｃ和Ｔｉｎ＋－Ｏ，前者是加氢反应的Ｃ源，使ＣＯ加氢生成烃类的反应在Ｎｉ中心上按＂表面碳＂机理进行，其生成乙烯的选择性大于６０％．Ｈ２Ｏ的生成反应在Ｔｉｎ＋中心上按Ｔｉｎ＋－Ｏ与Ｔｉｎ＋－Ｈ或Ｎｉ－Ｈ反应的途径进行．     

Ni－Cu和MgO－SiO_2间的相互作用及其对催化性能的影响

本文用ＴＰＲ，ＩＲ，ＴＰＤ和ＴＰＳＲ等技术研究了以表面改性法制备的ＭｇＯ－ＳｉＯ２（ＭＳＯ）表面复合物担载的Ｎｉ－ＣＵ合金间的相互作用及其对ＣＯ加氢反应催化性能的影响．结果表明，ＮｉＯ－ＣｕＯ与ＭＳＯ间的相互作用导致部分ＭＯ与ＭＳＯ形成表面物种从而使金属组分氧化物还原温度明显升高；还原后的Ｎｉ－Ｃｕ／ＭＳＯ表面上存在着两类活性中心，即合金相中的Ｎｉ与载体相中的Ｍｇ２＋（或Ｍｇ２＋－Ｏ）；在两类活性中心的协同作用下，ＣＯ吸附除有孪生、线式和桥式吸附态物种外，还有一种新的卧式吸附态（Ｎｉ．．．Ｃ＝Ｏ→Ｍｇ２＋）．这种吸附态的活化程度较高，易在表面上发生裂解形成Ｎｉ－Ｃ和Ｍｇ２＋－Ｏ，其中Ｎｉ－Ｃ是加氢反应的碳源；Ｈ２在催化剂表面上发生解离吸附形成Ｎｉ－Ｈ和Ｍｇ２＋－ＯＨ，前者比较活泼，是加氢反应的氢原．ＣＯ加氢生成烃类的反应在Ｎｉ中心上按＂表面碳＂机理进行，其生成ＣＺＨ４的选择性高于８０％；Ｈ２Ｏ的生成反应按２（Ｍｇ２＋－ＯＨ）－→Ｍｇ２＋＋（Ｍｇ２＋－Ｏ）＋Ｈ２Ｏ方式进行．     

示波极谱法测定膨润土的吸蓝量

膨润土是一种以含蒙脱石类矿物为主的粘土,由于蒙脱石具有独特的矿物结构和结晶化学性质,使膨润土具有很大的实用价值。膨润土分散于水溶液中具有吸附次甲基蓝的能力,其吸附的量被称为吸蓝量,膨润土中蒙脱石含量越高,吸蓝量越多。因此,吸蓝量可成为粗略估计膨润土矿中蒙脱石相对含量的技术指标。示波极谱法测定膨润土的吸蓝量,基于经蒙脱石吸附后的水悬胶液中,用极谱法测定剩余的次甲基蓝量,该设想立意新颖,是继patterson和Boenisch创立晕环法后唯一能获得准确结果的新方法。     

Modification and characterization of montmorillonite fillers used in composites with vulcanized natural rubber

Parent Ca-montmorillonite (Jelšovy Potok, Slovakia, Ca-JP) and Na-montmorillonite Kunipia-F (Japan, Na-KU) were ion-exchanged with octadecyltrimethylammonium (ODTMA) cations. Characteristics of the samples were studied by X-ray diffraction (XRD), Fourier transform infrared spectroscopy (IR) and thermogravimetry (TG). Surface areas were measured by sorption of N₂ and ethyleneglycol monoethyl ether. Scanning electron microscopy photographs (SEM) were used to characterize the texture of samples. The XRD patterns show that, upon intercalation, the basal spacing of montmorillonite is expanded and corresponds to the pseudotrimolecular arrangement of organic cations in the interlayers. The IR spectra of organically modified montmorillonite show C-H stretching and bending bands of both CH₃ and CH₂ groups in the 3000–2800 cm⁻¹ and 1500–1400 cm⁻¹ region, respectively. Modification of montmorillonite by organic cations decreased the hydrophilicity of their mineral surface and adsorbed water evaporated at lower temperatures. The SEM photographs reveal a tendency towards lump formation and agglomeration of the ODTMA-montmorillonite particles. The modification introducing organic moiety lead to a substantial decrease in the surface area of both montmorillonites; however, it remained remarkably high, being at the level typical for silica. Completely characterized fillers were used to prepare rubber compositions with enhanced physical properties, as described in Hrachová et al. (2008).     

Molecular dynamics simulation of TCDD adsorption on organo-montmorillonite

In this work, molecular dynamics simulation was applied to investigate the adsorption of Tetrachlorodibenzo-p-Dioxin (TCDD) on tetramethylammonium (TMA) and tetrapropylammonium (TPA) modified montmorillonite, with the aim of providing novel information for understanding the adsorptive characteristics of organo-montmorillonite toward organic contaminants. The simulation results showed that on both outer surface and interlayer space of TPA modified montmorillonite (TPA-mont), TCDD was adsorbed between the TPA cations with the molecular edge facing siloxane surface. Similar result was observed for the adsorption on the outer surface of TMA modified montmorillonite (TMA-mont). These results indicated that TCDD had stronger interaction with organic cation than with siloxane surface. While in the interlayer space of TMA-mont, TCDD showed a coplanar orientation with the siloxane surfaces, which could be ascribed to the limited gallery height within TMA-mont interlayer. Comparing with TMA-mont, TPA-mont had larger adsorption energy toward TCDD but smaller interlayer space to accommodate TCDD. Our results indicated that molecular dynamics simulation can be a powerful tool in characterizing the adsorptive characteristics of organoclays and provided additional proof that for the organo-montmorillonite synthesized with small organic cations, the available interlayer space rather than the attractive force plays the dominant role for their adsorption capacity toward HOCs.     

Sorption interactions of volatile organic compounds with organoclays under different humidities by using linear solvation energy relationships

Organoclays are usually used as sorbents to reduce the spread of organic compounds and to remove them at contaminated sites. The sorption equilibrium and the mechanisms of volatile organic compounds (VOCs) on organoclays under different humidities are helpful for developing efficient organoclays and for predicting the fate of VOCs in the environment. In this study, the organoclay was synthesized through exchanging inorganic cations by hexadecyltrimethyl ammonium (HDTMA) into montmorillonite, resulting in 12?% of organic content. The surface area of organoclay was smaller than the unmodified clay due to the incorporation of organic cations into the interlayer. Both adsorption on organoclay surface and partition into the incorporated HDTMA in organoclay played roles on the sorption process. Compared the sorption coefficients in montmorillonite and different modified clays, the incorporated organic cations overcame the inhibition effect of hydrophilic surface of clay on the sorption process of hydrophobic organic compounds from water. The sorption coefficients of VOC vapors on organoclay were further characterized using a linear solvation energy relationship (LSER). The fitted LSER equations were obtained by a multiple regression of the sorption coefficients of 22 probe chemicals against their solvation parameters. The coefficients of the five-parameter LSER equations showed that high HDTMA-content montmorillonite interacts with VOC molecules mainly through dispersion, partly through dipolarity/polarizability and hydrogen-bonds as well as with negative π-/n-electron pair interaction. The interaction analysis by LSERs suggests that the potential predominant factors governing the sorption of VOCs are dispersion interactions under all tested humidity conditions, similar with the lower level modified clay. The derived LSER equations successfully fit the sorption coefficients of VOCs on organoclay under different humidity conditions. It is helpful to design better toxic vapor removal strategy and evaluate the fate of organic contaminants in the environment.     

Thermal behavior of Cu(II)-, Cd(II)-, and Hg(II)-exchanged montmorillonite complexedwith cysteine

The thermal behavior of montmorillonite and organically modified montmorillonite, both treated with heavy metal cations [Cu(II), Cd(II) and Hg(II)], was characterized via thermal analyses (TG, DTG and DTA) combined with evolved species gas mass spectrometry (MS-EGA), and X-ray diffraction at in situ controlled temperature (HTXRD). The reactions involving Cu(II)- and Cd(II)-montmorillonite samples are mostly related to H₂O and OH loss, unlike Hg(II)-montmorillonite, where effects associated to Hg(II) loss are also present. Finally reactions related to dehydration, dehydroxylation and to organic matter decomposition can be observed in montmorillonite samples treated with cysteine.     

聚苯乙烯/蒙脱土纳米复合材料的制备及结构研究

以可与苯乙烯发生共聚的阳离子表面活性剂乙烯苄基二甲基十八烷基氯化铵(VOAC)为插层处理剂改性蒙脱土(VC18-MMT),有机蒙脱土在超声波强剪切作用以及乳化剂作用下预分散在乳化剂溶液中,然后引入苯乙烯单体进行原位乳液聚合制备聚苯乙烯/蒙脱土纳米复合材料.采用XRD和TEM对纳米复合材料的结构进行了表征.结果表明,绝大多数的蒙脱土被剥离成单个片层均匀的分散在聚合物基体中;动态力学分析表明,纳米复合材料的储能模量和玻璃化温度均有所增加,而动态损耗有所降低;接枝在蒙脱土片层上的聚合物通过与锂离子进行阳离子交换反应提取下来,采用GPC和NMR对接枝聚合物的结构进行了表征,结果表明,接枝聚合物是较基体分子量低且分布很宽的苯乙烯和乙烯苄基二甲基十八烷基氯化铵的共聚物,计算表明每一个共聚物分子链上平均含有大约25个乙烯苄基二甲基十八烷基氯化铵分子.     

The Adsorption of Herbicides and Pesticides on Clay Minerals and Soils. Part 1. Isoproturon

The adsorption of isoproturon and two model compounds, N,N-dimethylurea and4-isopropylaniline, on clay minerals (bentonite,montmorillonite and kaolinite), organic matter (humic acid) and soil (with and without organic matter) has been studied using FT-infrared spectroscopy (IR), thermogravimetric analysis (TGA), high pressure liquid chromatography (HPLC) and X-ray diffraction (XRD).N,N-dimethylurea interacted with bentonite and montmorillonite by the coordination of the carbonyl group, directly or indirectly through water molecules, with exchangeable cations. Adsorption on humic acid was due to hydrogen bonding with the active sites of the adsorbent. The amino group ofN,N-dimethylurea appears tobe relatively inactive during adsorption. The mechanisms involved in the adsorption of 4-isopropylaniline were hydrogen bonding and protonation. No adsorption of 4-isopropylaniline was observed on kaolinite. The investigation of isoproturon suggested that both the carbonyl and amino groups of isoproturon were involved in interactions with the active sites of the adsorbents. Both the clay minerals and organic matter of soil contribute to the adsorption of organic compounds on soil but the clay minerals bentonite and montmorillonite play a major role in their adsorption on soil.     

Formability and properties of self-standing clay film by montmorillonite with different interlayer cations

Influences of exchangeable interlayer cations were investigated on self-standing film formability, film morphology, and properties of the clay films such as flexibility and gas barrier property. Ion-exchanged montmorillonite samples were prepared by a cation exchange from naturally bearing cation, mostly Na⁺, to Li⁺, Mg²⁺, Ca²⁺, Al³⁺, and Fe^{2+, 3+}. Self-standing films were prepared from aqueous colloidal dispersions of these montmorillonite samples with no additives. The montmorillonite samples with monovalent or divalent cation formed flat self-standing films while the Al-montmorillonite sample produced a distorted film. The Fe-montmorillonite sample formed many separated reddish-brown rod-shaped pieces. Clay film microstructures were different with interlayer cations. The films with monovalent interlayer cations were constructed by the stacking of units with delicately waved thin clay sheets in the whole film, but other films show different morphologies between the upper side and lower side; the upper side is laminated with thin sheets; the lower side is laminated with large thick sheets.The self-standing films’ flexibility and gas barrier property differed according to the interlayer cations. These properties were good in cases of samples with monovalent cations. The innumerable short wave and sheet thinness are considered to foster good flexibility and gas barrier properties. The differences in film formability and properties of the films are attributable to different swellability among samples with different interlayer cations. The montmorillonite samples with monovalent cations swell sufficiently by water, but those with polyvalent cations swell poorly. In the latter case, clay crystals aggregate in water, then the aggregate grows into large particles, creating a film with large particles.     

Preconcentration of phenols by adsorption on organo-clay followed by capillary electrophoretic determination

The organo-clay adsorbent used was prepared by modification of montmorillonite from Kurşunlu, Turkey with the cationic surfactant cetyltrimethlyammonium bromide. The modification process involves replacing the inorganic exchange cations of the clay by organic cations containing long chain alkyl groups. The retention of phenolic compounds from aqueous solution on the organo-clay was studied. The analytes are quantitatively retained on the proposed adsorbent at pH 7 and recovered by elution with ethanol. The determination of phenols was performed by capillary electrophoresis. Received: 28 July 1997 / Revised: 15 December 1997 / Accepted: 8 January 1998     

Preparation and characterization of microporous SiO2-ZrO2 pillared montmorillonite

SiO₂-ZrO₂ pillared montmorillonite (SZM) was prepared by the reaction of Na-montmorillonite with colloidal silica-zirconia particles which were prepared by depositing zirconium hydroxy cations on silica particles. By pillaring with the colloidal particles, the basal spacing of montmorillonite was expanded to ca. 45 Å and the calcined SZM samples showed large specific surface areas up to 320 m²/g at 400 °C. In spite of large interlayer separation, adsorption results indicated the presence of micropores generated between the colloidal particles. The microporous structure was maintained at least up to 600 °C and exhibited specific shape selectivity for the adsorption of large organic molecules, especially between toluene and mesitylene. According to the temperature-programmed-desorption (TPD) spectra of ammonia, the calcined SZM showed weakly acidic sites.