水分子在高岭石中插层行为的量子化学研究

采用密度泛函理论B3LYP方法,在B3LYP/6-31G(d)理论水平上,构建高岭石的层间团簇模型Si6Al6O42H42(层间距为0.844 0和1.000 0nm),并对高岭石层间及其与n(n=1～3)个水分子相互作用的团簇的各种性质进行研究,如优化的几何构型、电子密度、氢键、能量、NBO电荷分布、振动频率等.结果表明,随着水分子个数n(n=1～3)的增加,体系的能量逐渐降低.水分子通过多种类型的氢键插层于高岭石层间,其中水分子间的氢键强度最强,其次是水分子与铝氧层之间形成的氢键,再次是水分子与硅氧层之间的氢键;层间距随着插层分子的增多而增大,但高岭石层间的活性位点依然存在,且位置较插层前没有明显变化.     

氟置换高岭石层间羟基的能量最小化模拟

为了进一步澄清高岭石中结构无序的成因以及氢键对它们的影响程度,利用补充了氟参数的CLAYFF力场,对层间羟基不同分数的氟置换进行了能量最小化模拟.结果发现:四面体底氧起皱的原因是四、八片层不匹配引起的Al—O(连接氧)键拉伸以及维持四面体自身外形的需要;四面体旋转的原因与Newnham的解释类似.八面体上下三原子对旋转是由于:(1)四、八面体层的不匹配,具体地说是连接氧/内部羟基氧与八面体铝之间的O—Al—O键角(θ1)和Al—O—Al键角(θ2),层间羟基氧与八面体铝之间的O—Al—O键角(θ4)和Al—O—Al键角(θ5)的增大,以及八面体共棱O—Al—O键角(θ3)的减小;(2)铝硅斥力引起的θ1、θ2变小和θ3变大;(3)(1)和(2)中所有键角变化引起的结构调整;(4)高岭石特殊的网状结构共同引起的.八面体O-O共享棱的缩短和铝更靠近层间羟基氧同样也是(1)-(4)作用的结果;θ1、θ2、θ4和θ5增大和θ3减小还引起了八面体展平.层间氢键对四面体底氧起皱、八面体展平和八面体上下三原子对旋转起阻碍作用,而对四面体旋转起促进作用.此外,当氟对层间羟基的置换摩尔分数较低时(xF=0-0.7),高岭石层间距并不明显随氟的增加而增加,这说明了高岭石的水合过程可能并不需要氟化铵的加入.     

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.     

尿素-富马酸根-水分子为主体晶格的四乙基铵离子包合物的合成与晶体结构

合成一种新的尿素-阴离子复合主体晶格包合物,(C₂H₅)₄N⁺[C₄H₂O₄^2-]1/2·CO(NH₂)₂·H₂O,并进行了X射线晶体结构分析.晶体为单斜晶系,C₂/_c(No.15)空间群,a=1.7909(5)nm,b=1.4431(4)nm,c=1.4443(3)nm,β=126.76(2)°,V=2.9905(13)nm³,Z=4,R₁=0.0647,_wR=0.0735.包合物中,两个尿素分子通过一对N-H…O氢键以通常的“肩并肩”方式连接起来,形成一个二聚体.这些二聚体沿c轴方向依次排列,每两个相邻二聚体间生成的氢键将它们连接成一个沿(001)方向延伸的锯齿形扭带.由c滑移面相关连的富马酸阴离子以水分子为桥,由O(W)-H…O氢键连成一条宽带,沿c轴方向延伸.这些富马酸根-水分子复合氢键宽带与尿素纽带交替平行排列,由此形成了一个平行于ac面的氢键层.四乙基铵离子层填充在b=1/4和b=3/4处的主体晶格的层间空隙处,构成“三明治”式夹层结构的包合物.     

高岭石/APTES插层复合物的表征及其脱嵌反应动力学

以高岭石/甲醇(K/M)复合物为前驱体,利用置换法制备出了高岭石/γ-氨丙基三乙氧基硅烷插层复合物(K/APTES),并应用XRD、FTIR、TEM、TG-DSC分析等表征手段对复合物进行了分析。结果表明:APTES分子的氨基与前驱体K/M的四面体硅氧烷基、嫁接在铝氧八面体表面上的甲氧基均发生键合作用形成氢键,APTES分子为两层倾斜排列于高岭石层间,倾角大小与温度有关。插层剂APTES破坏了高岭石层间的氢键,加剧了高岭石自身结构中硅氧四面体片层与铝氧八面体片层之间存在的错位,使得K/APTES插层复合物的部分片层卷曲变形。还针对复合物的插层剂APTES的脱嵌反应,采用Satava积分法和AcharBrindley-Sharp-Wendworth微分法相结合的动力学方法计算得到了完整的动力学三因子:活化能E=197.8 k J·mol-1,指前因子的对数lg(A/s-1)=14.60,最概然机理函数为:f(α)=[-ln(1-α)]-1,G(α)=α+(1-α)ln(1-α)。     

水的密度随温度的变化

水的密度在4℃时最大,而不是在熔点温度时。水究竟为什么会有这样特殊的性质呢?这完全是由水分子的特殊结构引起的。气态水分子键角为104°52'′,由于氧为 sp~3杂化,有两对孤对电子,而氢原子显正电性,这样就形成了四面体取向的电荷分布,水分子就按这四个方向以四面体取向由氢键相连,构成了一个空旷的框架结构,但由于氢键键能为21 kJ·mol~(-1)远小于正常共价键(几百千焦每摩尔),所以这种框架结构很易破碎。     

水合肼在高岭石层间插层行为的量子化学研究

水合肼以其碱性及吸附性受到越来越多的关注,同时它在粘土中的污染问题也越来越受到重视.本工作构建了高岭石团簇模型为Al6Si6O42H42并在B3LYP/6-31G(d,p),MP2/6-31G(d,p)//B3LYP/6-31G(d,p)和MP2/6-31++G(d,p)//B3LYP/6-31G(d,p)水平下对一水合肼以及二水合肼在高岭石层间的插层性质(如:优化构型、结构参数、结合能、电荷分布、振动光谱、静电势等)进行探究.计算表明,当一水合肼进入层间后,水分子和肼分子之间的相互作用发生了改变.即水与肼分子分别以氢键的形式插层于高岭石层间,且肼与高岭石之间的相互作用要强于肼与水之间的相互作用,同时插层位点多位于高岭石四面体层和八面体层的重叠区域内,这些都是水合肼易进入高岭石层间而难以脱去的重要因素.当二水合肼进入层间后,随着层间距的不断扩大,肼分子与高岭石铝氧层之间的相互作用仍强于肼分子与水分子间的作用.但当层间距超过1.05 nm时,水分子与肼分子之间的作用则强于肼分子与高岭石的作用,这也印证了若要将肼脱附,需将层间距增大以减弱肼分子与高岭石的作用,再用溶剂将其脱附的可行性.     

高岭石/APTES插层复合物的表征及其脱嵌反应动力学

以高岭石/甲醇(K/M)复合物为前驱体,利用置换法制备出了高岭石/γ-氨丙基三乙氧基硅烷插层复合物(K/APTES),并应用 XRD、FTIR、TEM、TG-DSC分析等表征手段对复合物进行了分析.结果表明:APTES分子的氨基与前驱体K/M的四面体硅氧烷基、嫁接在铝氧八面体表面上的甲氧基均发生键合作用形成氢键,APTES分子为两层倾斜排列于高岭石层间,倾角大小与温度有关.插层剂APTES破坏了高岭石层间的氢键,加剧了高岭石自身结构中硅氧四面体片层与铝氧八面体片层之间存在的错位,使得K/APTES插层复合物的部分片层卷曲变形.还针对复合物的插层剂APTES的脱嵌反应,采用Satava积分法和Achar-Brindley-Sharp-Wendworth微分法相结合的动力学方法计算得到了完整的动力学三因子:活化能E=197.8 kJ·mol^-1,指前因子的对数lg(A/s^-1)=14.60,最概然机理函数为:f(α)=[-ln(1-α)]^-1,G(α)=α+(1-α)ln(1-α).     

三水合硝酸钪18-冠-6配合物的合成及其晶体结构

报道了[Sc(NO3)3(OH2)3].(18-冠-6)的合成及其晶体结构.Sc(III)离子同三个双齿配体硝酸根与三个水分子氧配位,构成九配位的配合物.配位多面体是稍有扭曲的单帽四方反棱柱.配位水分子的六个氢原子分别与上下两层冠醚环上的氧原子生成氢键,形成多层夹心分子缔合物.     

水滑石限域空间中Cl-与H2O的超分子作用

构建水滑石(LDHs-Cl-yH2O)周期性计算模型, 选用密度泛函理论-赝势平面波法对模型进行几何全优化, 从结构参数、Mulliken电荷布居、态密度(DOS)、能量等角度研究层间Cl-和水分子的分布形态以及与LDHs层板间的超分子作用. 计算结果表明, LDHs-Cl主客体间存在着较强的超分子作用, 主要包括静电和氢键作用. LDHs-Cl层间引入水分子后, 随着水分子数的增加, 层间距逐渐增大后趋于平衡. 水合过程中氢键作用比静电作用更占优势, layer-water型氢键要略强于anoin-water型氢键. 当y=1, 2时, Cl-与水分子所在平面以平行层板的方式存在于LDHs层板间, 并且与两层板的距离基本相等; 当y=3, 4时, Cl-与水分子则以偏向某一层的方式随机地存在于LDHs 层板间. 随着层间水分子增加, LDHs-Cl-yH2O由离子型晶体向分子型晶体转化, LDHs-Cl的水合具有饱和量.     

二维红外光谱研究聚碳酸酯薄膜中水的扩散

利用二维衰减全反射红外光谱方法,研究了水在聚碳酸酯(PC)薄膜中的扩散过程,发现水的羟基弯曲振动谱带中可以分辨出分别位于1672、1646和1621 cm-1的吸收峰,而羟基伸缩振动谱带中可以分辨出分别位于3560、3425和3255 cm-1的吸收峰,由此可知水分子在聚碳酸酯薄膜中存在3种状态,分别为与羰基形成强、中强氢键作用的水分子和进入PC微孔中的弱氢键作用的水分子。 经过二维相关分析得到水分子进入PC薄膜的顺序为首先形成中等强度的氢键,然后形成弱和强2种强度的氢键。     

Structural studies on the hydration of L-glutamic acid in solution

A combination of neutron diffraction augmented with isotopic substitution and computer modeling using empirical potential structure refinement has been used to extract detailed structural information for L-glutamic acid dissolved in 2 M NaOH solution. This work shows that the tetrahedral hydrogen bonding network in water is severely disrupted by the addition of glutamic acid and NaOH, with the number of water-water hydrogen bonds being reduced from 1.8 bonds per water molecule in pure water to 1.4 bonds per water molecule in the present solution. In the glutamic acid molecule, each carboxylate oxygen atom forms an average of three hydrogen bonds with the surrounding water solvent with one of these hydrogens being shared between the two oxygen atoms on each carboxylate group, while each amine hydrogen forms a single hydrogen bond with the surrounding water solvent. Additionally, the average conformation of the glutamic acid molecules in these solutions is extracted.     

THE SOLID STATE LUMINESCENCE OF ESTROGENS

Abstract. The luminescent behavior of certain estrogens in the solid state is discussed. Spectra of solid films of estradiol and estriol are red shifted compared to that in liquid solutions with estriol shifted to a lesser extent. The red shifts are attributed to intermolecular hydrogen bonding, this conclusion being based on IR spectra and X-ray data. The calculated distance over which hydrogen bonding takes place is 2.755 Å in estradiol and 2.638 Å in estriol. The increased shift in the spectrum of estradiol is believed to be due to an additional hydrogen bond with a water molecule present in the solid film (O—O distance 2.793 Å). In estrone the weak fluorescence present in liquid solution is absent in solid film, in contrast to 3-desoxyestrone where fluorescence is preserved. Out of three possible forms of crystalline estrone only two can form hydrogen bonds, based on O-O distance calculations. In equilenin, which is highly fluorescent in liquid solution, no fluorescence is detected in solid film. This again is attributed to hydrogen bonding between the hydroxyl group of the β-naphtholic chromophore and the carbonyl group in the C(17) position. Dihydroequilenin which lacks the carbonyl group and equilenin dissolved in a host crystal retain their fluorescence.     

二氟尼柳/水滑石插层组装结构、氢键及水合特性的分子动力学模拟

采用分子动力学方法模拟二氟尼柳插层水滑石(DIF/LDHs)的超分子结构, 研究复合材料主客体间形成的氢键以及水合膨胀特性.结果表明, 当水分子总数与DIF分子总数之比Nw≤3时, 层间距dc保持基本恒定, 约1.80 nm; 当Nw≥4时, 层间距逐渐增大, 且符合dc=1.2611Nw+13.63线性方程. 随着水分子个数增加, 水合能驻UH逐渐增大. 当Nw≤16时, 由于⊿UH<-41.84 kJ·mol-1, LDHs-DIF可以持续吸收水, 从而使材料层间距不断膨胀. 但当Nw≥24时, ⊿UH>-41.84 kJ·mol-1, 此时LDHs-DIF层间不能再进一步水合, 因此LDHs-DIF在水环境中膨胀具有一定的限度. 水滑石层间存在复杂的氢键网络. DIF/LDHs水合过程中, 水分子首先同步与层板和阴离子构成氢键; 当阴离子趋于饱和后, 水分子继续与层板形成氢键, 并逐步发生L-W型氢键取代L-A型氢键, 驱使阴离子向层间中央移动, 与层板发生隔离; 最后水分子在水滑石羟基表面形成有序结构化水层.     

柚皮素三乙胺盐一水合物的制备、晶体结构及溶解度

柚皮素是一种天然黄酮类化合物,几乎不溶于水。利用晶体工程学原理可以有效改善天然产物的溶解性。本文合成了柚皮素和三乙胺的有机盐一水合物[C_(15)H_(11)O_5]-·[C_6H_(16)N]+·H_2O,测定了其晶体结构。解析结果表明,有机盐水合物属于单斜晶系,P2_1/n空间群。柚皮素7取代位的羟基上的质子转移到了三乙胺的N原子上,并形成了N~+—H....O~-氢键。羟基阴离子与4'取代位上的羟基形成了O—H....O~-氢键,产生了一维的氢键链状结构。水分子通过两种氢键作用将一维的氢键链连接成二维的氢键网络。形成三乙胺盐一水合物后,柚皮素在水中的溶解度增加了20倍。     

High physisorption affinity of water molecules to the hydroxylated aluminum oxide (001) surface

The adsorption mechanism of water on the hydroxylated (001) plane of α-Al(2)O(3) was studied by measuring adsorption isotherms and GCMC simulations. The experimental adsorption isotherms for three α-Al(2)O(3) samples from different sources are typical type II, in which adsorption starts sharply at low pressures, suggesting a high affinity of water to the Al(2)O(3) surface. Water molecules are adsorbed in two registered forms (bilayer structure). In the first form, water is registered at the center of three surface hydroxyl groups by directing a proton of the water. In the second form, a water molecule is adsorbed by bridging two of the first-layer water molecules through hydrogen bonding, by which a hexagonal ring network is constructed over the hydroxylated surface. The network domains are spread over the surface, and their size decreases as the temperature increases. The simulated adsorption isotherms present a characteristic two-dimensional (2D) phase diagram including a 2D critical point at 365K, which is higher than that on the hydroxylated Cr(2)O(3) surface (319 K). This fact substantiates the high affinity of water molecules to the α-Al(2)O(3) surfaces, which enhances the adsorbability originating from higher heat of adsorption. The higher affinity of water molecules to the α-Al(2)O(3) (001) plane is ascribed to the high compatibility of the crystal plane to form a hexagonal ring network of (001) plane of ice Ih.     

Ions in water: the microscopic structure of concentrated NaOH solutions

A neutron diffraction experiment with isotopic H/D substitution on four concentrated NaOH/H(2)O solutions is presented. The full set of partial structure factors is extracted, by combining the diffraction data with a Monte Carlo simulation. These allow to investigate both the changes of the water structure in the presence of ions and their solvation shells. It is found that the interaction with the solute affects the tetrahedral network of hydrogen bonded water molecules in a manner similar to the application of high pressure to pure water. The solvation shell of the OH(-) ions has an almost concentration independent structure, although with concentration dependent coordination numbers. The hydrogen site coordinates a water molecule through a weak bond, while the oxygen site forms strong hydrogen bonds with a number of molecules that is on the average very close to four at the higher water concentrations and decreases to about three at the lowest one. The competition between hydrogen bond interaction and Coulomb forces in determining the orientation of water molecules within the cation solvation shell is visible in the behavior of the g(NaHw)(r) function     

Super-Molecular Interaction between Cl and H2O within the Restricted Space of Layered Double Hydroxides

A periodical interaction model of LDHs-Cl-yH₂O has been proposed. The geometry optimization and energy of the layered double hydroxides (LDHs) were calculated using CASTEP/LDA method at the CA-PZ level. The distribution of H₂O in the interlayer and the super-molecular interaction between host layer and guest anion have been investigated by analyzing the geometric parameters, charge population, energy, and density of state (DOS). The results showed that there was a strong super-molecular interaction between the host layer and the guest anion Cl⁻. In the system of LDHs-Cl-yH₂O, the interlayer distance increased gradually then tended to invariableness. And in the process of hydration of LDHs-Cl, hydrogen bonding was superior to electrostatic interaction, and layer-water type hydrogen bonding was a little stronger than anion-water type hydrogen bonding between H₂O and the rest of the structure. When y was 1 or 2, Cl⁻ and the plane of water were parallel to the layer; while y was 3 or 4, distribution of Cl⁻ and water was random. Moreover, the LDHs-Cl-yH₂O would change from ionic crystal to molecular crystal with the increase of number of water molecule. The hydration of LDHs-Cl would achieve a definite saturation state.