用原位红外光谱研究低硅铝比ZSM—5沸石中的新型B酸

在反应下付里叶变换红外光谱技术的研究，揭示了高晶格铝含量的沸石ＸＳＭ－５有新类型的Ｂ酸。基于甲醇和甲醇脱水物二甲基醚和Ｂ酸的相互作用，在红外差谱中，原来表征Ｂ酸在ＯＨ伸缩频率区的特征吸收谱带３６１０ｃｍ＾－１不再出现，代之以两个负吸收谱带，分别为３６１５与３５８５ｃｍ＾－１，这是以往的研究中未报导过的红外吸收谱带。     

带压水热处理对HZSM-5沸石结构和性质的影响

利用ＸＲＤ，＾２７ＡｌＭＡＳＮＭＲ，ＮＨ３－ＴＰＤ吡啶吸附ＩＲ等技术考察了带压水热处理温度对直接法ＨＺＳＭ－５沸石骨架铝的迁脱和表面酸性质的影响规律，实验发现，随着水处理温度的升高，沸石骨架铝的迁脱量增加，在带压水热处理条件（４００－６００℃）下，直接法ＨＺＳＭ－５的骨架结构稳定，其架铝不能迁脱，对ＨＺＳＭ－５（３８），于５００℃，和水蒸气压力为１．０ＭＰａ条件下热处理１２ｈ后，只能使３０．０％的     

β-沸石骨架铝化改性的红外光谱

β沸石是以有机胺为模板剂合成的高硅沸石．为在孔道中进行吸附和催化反应,通常是在空气中 (５５０℃ )进行焙烧,将有机胺脱除并使质子酸中心形成．但这种脱模板剂方法,会造成骨架脱铝［１ -４］,使质子酸中心显著减少．β沸石固有结构中存在着孔道位错和结构空穴,空气中焙烧脱有机胺可能会进一步损伤沸石的骨架结构［４,５］．沸石骨架改性已发展了多种铝化方法［６ -８］．有的研究工作表明,通常用红外光谱和ＭＡＳＮＭＲ表征的非骨架铝,在温和的条件下,例如回馏温度下的离子交换或者在较低温度下 (１００℃或室温 )与碱反应就可…     

无粘结剂ZSM-5沸石催化剂骨架脱铝改性的研究

对比了无粘结剂和有粘结剂ZSM-5沸石催化剂的吸附性质, 证实前者的优良品质. 以27Al固体核磁共振(MAS NMR)考察了盐酸处理、水蒸气处理及水蒸气-盐酸相结合处理后无粘结剂ZSM-5沸石催化剂的骨架脱铝行为以及非骨架铝的状态. 以X射线粉末衍射(XRD), X射线荧光光谱(XRF), 低温氮吸附, NH3-TPD和吡啶吸附原位红外光谱(in situ IR)等详细表征了骨架脱铝对其晶体、元素组成及孔结构、表面强(S)酸与弱(L)酸、Brönsted(B)酸与Lewis(L)酸酸量分布等影响. 揭示了水蒸气处理的深度骨架脱铝强烈地调变沸石的结构和表面酸性的本质, 证明了该处理方式对调变S酸和B酸起主导作用.     

CXN天然沸石的研究VII. 骨架高硅超稳化改性

以高硅超稳化辉沸石(STI)为基底沸石, 分别经盐酸脱铝或氟硅酸铵脱铝补硅处理后制备的改性H-STI沸石, 其非骨架铝含量明显减少, 而后者骨架硅铝比进一步提高. X射线荧光散射光谱(XRF), ²⁷Al高分辨率魔角旋转固体核磁共振(MAS NMR), 红外(FT-IR)光谱等表征证明改性后的沸石骨架硅铝原子比分别为6.8和11.4. 低温氮吸附表明, 经盐酸处理的高硅STI沸石孔道开放完美, 但经氟硅酸铵处理的样品孔道被部分堵塞. 分段程序升温焙烧表明前者骨架热稳定性略差, 1000 ℃焙烧后结构基本被破坏, 而后者热稳定性较好, 经相同温度段焙烧后仍保持较高的结晶度和热稳定性, 其结构基本实现超稳化.     

CXN天然沸石的研究Ⅶ.骨架高硅超稳化改性

以高硅超稳化辉沸石(STI)为基底沸石,分别经盐酸脱铝或氟硅酸铵脱铝补硅处理后制备的改性H-STI沸石,其非骨架铝含量明显减少,而后者骨架硅铝比进一步提高.X射线荧光散射光谱(XRF),27Al高分辨率魔角旋转固体核磁共振(MAS NMR),红外(FT-IR)光谱等表征证明改性后的沸石骨架硅铝原子比分别为6.8和11.4.低温氮吸附表明,经盐酸处理的高硅STI沸石孔道开放完美,但经氟硅酸铵处理的样品孔道被部分堵塞.分段程序升温焙烧表明前者骨架热稳定性略差,1000℃焙烧后结构基本被破坏,而后者热稳定性较好,经相同温度段焙烧后仍保持较高的结晶度和热稳定性,其结构基本实现超稳化.     

CXN天然沸石的研究VII. 骨架高硅超稳化改性

以高硅超稳化辉沸石(STI)为基底沸石,分别经盐酸脱铝或氟硅酸铵脱铝补硅处理后制备的改性H-STI沸石,其非骨架铝含量明显减少,而后者骨架硅铝比进一步提高.X射线荧光散射光谱(XRF),27Al高分辨率魔角旋转固体核磁共振(MASNMR),红外(FT-IR)光谱等表征证明改性后的沸石骨架硅铝原子比分别为6.8和11.4.低温氮吸附表明,经盐酸处理的高硅STI沸石孔道开放完美,但经氟硅酸铵处理的样品孔道被部分堵塞.分段程序升温焙烧表明前者骨架热稳定性略差,1000℃焙烧后结构基本被破坏,而后者热稳定性较好,经相同温度段焙烧后仍保持较高的结晶度和热稳定性,其结构基本实现超稳化.     

新试剂3,5—二溴—4—偶氮8—羟基喹啉苯基荧光酮光度法测定微量铝

在溴化十六烷基三甲胺（ＣＴＭＡＢ）存在下，ＰＨ６，０的ＨＡｃ－ＮａＡｃ缓冲介质中，铝与新试剂３，５－二溴－４－偶氮８－羟基喹啉苯基荧光酮形成红色三元胶束配合物，最大吸收波长位于５６４ｎｍ，表观摩尔吸光系数ε为１．３５×１０＾５．ｍｏｌ＾－１．ｃｍ＾－１，铝浓度在０～５μｇ／２５ｍＬ范围内符合比耳定律，拟定的方法用于铝铁黄铜中微量铝的测定，结果满意。     

HY沸石上的两种结构羟基的红外光谱研究

用红外光谱测定了碱度相近、构型不同的分子,如:氨、三乙胺和三正丁胺等及构型接近、碱度不同的分子,如:吡啶、2,6-二甲基吡啶和哌啶等在HY沸石的两种结构羟基上的吸附.通过升温热脱附的IR谱,观察了吸附分子的碱度和构型对质子酸强度的影响. 用红外光谱测定了HY沸石上HF和LF两种表面结构羟基吸附氨后的脱附热分别为22.2kcal/mol和18.9kcal/mol.     

红外光谱法考察活性纤维状氧化铝表面酸性质

本文用红外光谱和升温脱附的方法,考察了活性纤维状氧化铝的表面酸性质。吸附了吡啶蒸气的红外光谱表明,活性纤维状氧化铝的表面酸主要以非质子酸形式存在。作者根据升温脱附和共吸附水时吸附态光谱的变化,探讨了表征络合吡啶的吸收峰位移原因。     

高岭石结构缺陷的 1H MAS NMR和Raman研究

The structure default of kaolinites was characterized with ¹H MAS NMR and Raman spectra. Although the HI indexes of Suzhou and Maoming kaolinite are similar, their ¹H MAS NMR and Raman spectra are very different. ¹H MAS NMR showed that the hydroxyl proton chemical shifts of Suzhou kaolinite are in the higher field and with larger different between the inner surface hydroxyls protons and inner hydroxyls proton chemical shifts than Maoming kaolinite. Raman spectra showed that the surface hydroxyls stretching vibration bands of Suzhou kaolinite are in the high frequency region, and the half height widths of the bands are 7.0～14 cm^-1. The area ratio S_z/(S_z+S_A), where S_Z and S_A are the areas of bands 3685 cm^-1 and 3695 cm^-1 respectively, is 0.23. But the surface hydroxyls stretching vibration bands of Maoming kaolinite are in the low frequency region, and the half height widths of the bands are 8.9～15.1 cm^-1. The area ratio S_z/(S_z+S_A) is 0.77. Those data proved that Suzhou kaolinite has lower structure default than Maoming kaolinite and ¹H MAS NMR and Raman spectra are effective method for study of kaolinite structure default.     

HMS和NaY固载酒石酸钛配合物的研究

利用化学键合和“瓶中造船”方法,成功地将酒石酸钛配合物接枝到HMS(heragonal mesoporous silicas)上或包络合于微孔NaY内.FT-IR表征表明酒石酸钛在HMS上是通过与载体表面羟基发生交换作用而被固载的;在NaY载体上则是通过包络合被封装在载体的超笼内.UV-Vis可见漫反射表征表明两类固载型催化剂有着相似的钛配位环境.在催化肉桂醇环氧化反应中,HMS键合型催化剂的反应转化率比NaY包络型催化剂的高;但后者在环氧化选择性上要高于前者.回收样品的重复使用实验结果表明,两类固载型催化剂在重复使用过程中均存在不同程度的失活.     

Infrared evidence of three distinct acidic hydroxyls in defect-free HY faujasite

Trimethylamine (TMA) and ammonia (NH(3)) were coadsorbed over a free extraframework aluminum (EFAL) HY zeolite, which allowed us to distinguish at least three different acidic hydroxyls in the faujasite structure.     

Time-resolved photoluminescence spectra of Si species encapsulated in zeolite supercages

Photoluminescence (PL) spectra of Si species encapsulated in zeolite supercages are studied. It is reported that the chained Si species terminated partially with phenyl groups and with some unsaturated bonds are formed in zeolite supercages by the reaction with phenylsilane and they show PL around 4 eV (J. Phys. Chem. 2004, 108, 2501-2508). In the present paper they are reduced with hydrogen to prepare Si chained species terminated and saturated with hydrogen atoms. The PL spectra are deconvoluted to be four components at 1.9, 2.2, 2.6, and 3.7 eV, which can tentatively be assigned to Si nanocrystals and Si quantum wires in addition to defects in SiO2 and uncontrolled organic impurities in zeolite, respectively. At elevated temperatures the Si quantum wires in zeolite pores seem to change the Si nanocrystals with the size larger than that of the zeolite pore diameter. It is the first case in which the PL decay lifetime of oxygen vacancies in zeolite can be detected to be quite short to be about 16 ns. The detected lifetimes of Si quantum wires are significantly very short, about 12 ns. The Si species encapsulated zeolite is solvated with hydrofluoric acid solution to separate the Si quantum wires by dissolving zeolite lattice. The Si quantum wires in the HF solution show intense PL spectra peaked at 2.33 eV and broad UV spectra around 2.8-3.5 eV. They will have different shapes and lengths. The HF solvated zeolite shows still PL spectra characteristic of oxygen vacancies and the absorption edge at 3.6 eV. The result means that zeolite lattice is solvated in HF solution as clusters with a band gap of 3.6 eV and they can still have some oxygen vacancies. Oxygen vacancies situate about 1.0 eV below the zeolite conduction band minimum, and the absorbed energy can be dissipated as PL between the valence band maximum and the oxygen vacancies. It is concluded that the excitation photon energy can be absorbed in zeolite and the Si quantum wires and then the absorbed energies are competitively relaxed in zeolite and the Si quantum wires.     

原位红外光谱法研究脱铝Y型沸石表面羟基及异丙苯裂解反应

本文用原位红外光谱法, 以自行设计的红外池, 采用流动体系研究了NH4Y及用EDTA配位脱铝的Y型沸石上的表面羟基, 苯及异丙苯在不同温度下的吸附, 以及用脉冲进样原位红外研究了异丙苯裂解反应。发现在脱铝Y型沸石(DAIY)中除Y型沸石有的3620和3535cm^-^1表面羟基峰外, 在3724cm^-^1处又出现一个与脱铝“空穴"Si-OH有关的吸收峰, 且此峰随脱铝量增加而增加, 脱氨过程的研究表明超笼中羟基具有酸性, 苯及异丙苯Y型或DNIY型沸石上均与超笼中羟基作用。在360℃时异丙苯裂解反应的活性中心主要是超笼中羟基, 催化剂失活主要是由于炭沉积在活性位上所致。     

ZnHZSM-5上丙烷芳构化的研究─丙烷的活化

研究了HZSM－5、ZnHZSM－5和ZnNaZSM－5上的羟基振动光谱和一氧化碳吸附的红外光谱，以及丙烷的芳构化反应．红外光谱中发现表征强B酸的3610cm－1羟基振动峰相对强度由于锌离子的引入和浸渍氢氧化钠而减小，说明了锌离子和钠离子均进入了分子筛的阳离子位；一氧化碳在锌离子上的吸附峰位在2232cm－1，说明进入阳离子位的锌离子是一种强L酸．反应结果表明，锌离子的引入大大地促进了丙烷的转化和芳烃选择性的提高；在一定范围内，随浸渍氢氧化钠量的增加，丙烷转化率下降，而丙烯的选择性和产率增加，说明了锌组份直接参与了丙烷的脱氢过程．Zn－L酸是丙烷活化脱氢的中心，丙烷在该中心上异裂活化直接脱氢．     

ZnHZSM-5上丙烷芳构化的研究-丙烷的活化

研究了HZSM－5、ZnHZSM－5和ZnNaZSM－5上的羟基振动光谱和一氧化碳吸附的红外光谱，以及丙烷的芳构化反应．红外光谱中发现表征强B酸的3610cm－1羟基振动峰相对强度由于锌离子的引入和浸渍氢氧化钠而减小，说明了锌离子和钠离子均进入了分子筛的阳离子位；一氧化碳在锌离子上的吸附峰位在2232cm－1，说明进入阳离子位的锌离子是一种强L酸．反应结果表明，锌离子的引入大大地促进了丙烷的转化和芳烃选择性的提高；在一定范围内，随浸渍氢氧化钠量的增加，丙烷转化率下降，而丙烯的选择性和产率增加，说明了锌组份直接参与了丙烷的脱氢过程．Zn－L酸是丙烷活化脱氢的中心，丙烷在该中心上异裂活化直接脱氢．     

Investigation of sodium cations in dehydrated zeolites LSX, X, and Y by 23Na off-resonance RIACT triple-quantum and high-speed MAS NMR spectroscopy.

We investigated by two-dimensional 23Na ORIACT MQMAS NMR and one-dimensional 23Na high-speed MAS NMR spectroscopy a homologous series of dehydrated zeolites with faujasite structure. The framework silicon to aluminum ratios varied between 1.06 and 2.60. In the case of zeolites Y (nSi/nAl = 2.60), we studied materials with sodium exchange degrees between 0 and 95%. The recently introduced ORIACT method (Caldarelli, S.; Ziarelli, F. J. Am. Chem. Soc. 2000, 122, 12015) significantly improved the resolution of the MQMAS spectra, in comparison with earlier studies. It was thus possible to extract meaningful quadrupole parameters by MQMAS NMR, which were used as a starting point for the simulation of 1D MAS NMR spectra to obtain more accurate values of the NMR parameters and site occupancy. We were able to show by this approach that in zeolite NaLSX the SI positions in the hexagonal prisms are occupied by sodium cations. For the homologous series of zeolites Y, it was found that sodium cations located at SII positions are the easiest to be substituted by ammonium ions through the exchange process.     

杂原子(B、Ti、Fe)进入Y型分子筛骨架的表征

应用X射线粉末衍射(XRD)、傅立叶变换红外光谱(FT-IR)、固体核磁共振(NMR)、紫外可见漫反射(UV-Vis-DRS)和热重(TG)等多种表征方法对合成的杂原子Y分子筛(BY、TiY、FeY)的结构进行了表征. 根据引入杂原子后分子筛的晶胞常数、骨架伸缩振动吸收峰、杂原子的特征电子跃迁峰、还原的热重曲线以及杂原子所处的微观配位环境等多种性质的变化, 得出结论：杂原子B、Ti、Fe均已进入Y分子筛骨架.     

Understanding the dissolution of zeolites

Scientific knowledge of how zeolites, a unique classification of microporous aluminosilicates, undergo dissolution in aqueous hydrochloric acid solutions is limited. Understanding the dissolution of zeolites is fundamental to a number of processes occurring in nature and throughout industry. To better understand the dissolution process, experiments were carried out establishing that the Si-to-Al ratio controls zeolite framework dissolution, by which the selective removal of aluminum constrains the removal of silicon. Stoichiometric dissolution is observed for Type 4A zeolite in HCl where the Si-to-Al ratio is equal to 1.0. Framework silicon dissolves completely during Type 4A dissolution and is followed by silicate precipitation. However, for the zeolite analcime which has a Si-to-Al ratio of 2.0 dissolves non-stoichiometrically as the selective removal of aluminum results in partially dissolved silicate particles followed by silicate precipitation. In Type Y zeolite, exhibiting a Si-to-Al ratio of 3.0, there is insufficient aluminum to weaken the structure and cause silicon to dissolve in HCl. Thus, little or no precipitation is observed, and amorphous undissolvable silicate particles remain intact. The initial dissolution rates of Type Y and 4A zeolites demonstrate that dissolution is constrained by the number of available reaction sites, and a selective removal rate parameter is applied to delineate the mechanism of particle dissolution by demonstrating the kinetic influence of the Si-to-Al ratio. Zeolite framework models are constructed and used to undergird the basic dissolution mechanism. The framework models, scanning electron micrographs of partially dissolved crystals, and experimentally measured dissolution rates all demonstrate that a zeolite's Si-to-Al framework ratio plays a universal role in the dissolution mechanism, independent of framework type. Consequently, the unique mechanism of zeolite dissolution has general implications on how petroleum reservoir stimulation treatments should be designed.