离子色谱法测定浴盐中的阴、阳离子

用离子色谱法测定浴盐中的Na^ 、K^ 、Mg^2 、Ca^2 、Cl^-、Br^-、SO4^2-时，分离阳离子的色谱柱为ICS-C25阳离子交换柱，淋洗液为2.0mmol/L均苯四甲酸溶液，流速为0.6mL/min；分离阴离子时的色谱柱为shim-pack IC-Al阴离子交换柱，淋洗液为2.5mmol/L邻苯二甲酸溶液－2.4mmol/L三羟基氨基甲烷溶液（体积比为1：1），流速为1.0mL/min。所测离子Na^ 、K^ 、Mg^2 、Ca^2 、Cl^-、Br^-、SO4^2-在较宽浓度范围内有良好的线性关系，回收率为94.7%-102.4%，检出限为0.001-0.02mg/L，相对标准偏差为1.03%-1.63%。     

细胞内游离离子及离子通道的核磁共振研究

生物细胞内游离离子及离：子通道(Ca^2 、Mg^2 、Na^ 、K^ 以及Na^ ／Ca^2 和Na^ ／Li^ 交换等)在生理病理过程中起着重要作用。用于这些方面研究的生物核磁共振方法主要包括有：^31PNMR、^19NMR、^7Li NMR及^23Na NMR等。^31P NMR主要用于对细胞内小分子代谢物、pH及游离Mg^2 的分析测定；^19F NMR是利用氟代指示剂间接地测定细胞内游离Mg^2 和Ca^2 的浓度，进而对钙镁离子通道进行分析研究；^7Li NMR、^23Na NMR等方法分别用于研究Li^ 、Na^ ／Li^ 交换、Mg^2 ／Li^ 交换、Na^ 及K^ 等。为了更好地理解和阐释细胞内离子的调控机制，本文对近几年核磁共振技术在这些方面的应用进行了综述。     

啤酒酵母生理代谢过程中钠、钾、镁、钙离子含量变化的跟踪检测

采用空气-乙炔火焰原子吸收光谱法分别测定了啤酒酵母发酵液中的Na^ 、K^ 、Mg^2 、Ca^2 离子动态变化中的含量,用La^3 盐消除P对Ca^3 的干扰,以Sr^2 盐作为Na^ 、K^ 的消电离剂。本实验室采用配制培养基,通过对不同种类及不同发酵阶段培养的发酵液样品进行测定,以研究在啤酒酵母生长代谢过程中Na^ 、K^ 、Mg^2 、Ca^2 离子代谢动态变化。方法的Na^ 、K^ 、Mg^2 、Ca^2 相对标准偏差(RSD)分别为0．31％,0．73％。1．78％,0．28％;样品加标回收率为98％-107％;检出限：Na^ 为0．159mg／L,K^ 为0．789nag／L,Mg^2 为0．039mg／L,Ca^2 为0．029mg／L。该方法简便快速,具有很好的精密度。     

广西车田红辉沸石对不同离子吸附性的初步研究

研究表明,不同粒度的红辉沸石在不同的温度条件下对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 等离子具有不同的吸附容量。在30℃时,8μm的红辉沸石对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 的吸附量分别为：10.90mg/g、10.01mg/g、7.64mg/g、5.50mg/g、108.70mmol/100g;45μm的红辉沸石对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 的吸附量分别为：10.10mg/g、9.80mg/g、6.90mg/g、5.08mg/g、101.10mmol/100g;246μm的红辉沸石对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 的吸附量分别为：2.66mg/g、2.20mg/g、1.86mg/g、1.26mg/g、28.00mmol/100g;在2℃时,8μm的红辉沸石对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 的吸附量分别为：10.60mg/g、9.82mg/g、6.90mg/g、5.07mg/g、99.60mmol/100g。在常温25-30℃,湿度82%条件下,246μm、45μm、8μm的红辉沸石含水率为7.06%、7.25%、7.78%。     

广西车田红辉沸石对不同离子吸附性的初步研究

研究表明，不同粒度的红辉沸石在不同的温度条件下对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 等离子具有不同的吸附容量。在30℃时，8μm的红辉沸石对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 的吸附量分别为：10.90mg/g、10.01mg/g、7.64mg/g、5.50mg/g、108.70mmol/100g；45μm的红辉沸石对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 的吸附量分别为：10.10mg/g、9.80mg/g、6.90mg/g、5.08mg/g、101.10mmol/100g；246μm的红辉沸石对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 的吸附量分别为：2.66mg/g、2.20mg/g、1.86mg/g、1.26mg/g、28.00mmol/100g；在2℃时，8μm的红辉沸石对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 的吸附量分别为：10.60mg/g、9.82mg/g、6.90mg/g、5.07mg/g、99.60mmol/100g。在常温25－30℃，湿度82％条件下，246μm、45μm、8μm的红辉沸石含水率为7.06%、7.25%、7.78%。     

离子色谱法测定水利工程水样中的5种无机阳离子北大核心CSCD

提出新型高通量离子色谱仪快速测定水利工程水样中5种阳离子Na^+、NH_4^+、Mg^(2+)、Ca^(2+)和K^+的含量的方法。采用TSKgel Super IC-CR阳离子交换柱,以2.2 mmol·L^(-1)甲基磺酸和1.00 mmol·L^(-1)18冠醚6的混合液为淋洗液,流量为0.7 mL·min^(-1),柱温为40℃,凝胶抑制电导检测,可在18 min内完成对5种阳离子的分析。5种无机阳离子的质量浓度在一定范围内与其峰面积呈线性关系,Na^+、NH_4^+、Mg^(2+)、Ca^(2+)和K^+的检出限(3S/N)分别为7.1,6.3,9.5,10.0,8.3μg·L^(-1),水样的加标回收率为95.3%~104%,相对标准偏差(n=5)为0.26%~4.0%。     

紫外光降解-离子色谱法测定液晶材料中有机分子上的碱、碱土金属和铵

采用紫外光降解－离子色谱法测定了液晶材料中的阳离子。研究了样品光降解的条件，H2O2及酸的影响，样品基体有机物的去除，并对直接水溶样品，超声提取样品和光解样品和光解样品测定结果进行了对比。结果表明：3种样品中均含有Na^ ,NH4^ ,K^ ,Mg^2 ,Ca^2 5种阳离子，但光解样品中5种阳离子的含量分别是超声提取及直接水溶样品中含量的3．5－19．7倍和10．6－46．6倍。对液晶样品进行光解测定阳离子时无需加入H2O2氧化，光解后无需对样品进行酸化。Na^ ,NH4^ ,K^ 在光解1.5h时响应值达到最大，Mg^2 ,Ca^2 在2h时光解最完全。5种阳离子加标回收率为71．5％－107．6％。本方法对测定有机化合物上结合的阳离子有一定的参考价值。     

离子色谱法测定酸雨中的阳离子

用离子色谱法测定酸雨中的Na^ 、NH4^ 、K^ 、Mg^2 、Ca^2 等阳离子，并同时用原子吸收分光光度法进行了对比实验。结果表明，利用离子色谱法测定阳离子，方法简便、快捷，能一次同时测定多种离子，测定结果和原子吸收法相符。     

高脂饲料对长爪沙鼠血脂和血清电解质的影响

目的观察高脂饲料对长爪沙鼠血清脂质4项和血清电解质K^＋、Na^＋、Cl^-、Ca^2＋、Mg^2＋含量的影响。方法选取雄性长爪沙鼠40只,随机分为两组,分别给予普通饲料和高脂饲料（含1%胆固醇、10%猪油）。喂养12周后颌下静脉丛采血,用日立7180型全自动生化分析仪检测血清TC、TG、HDL-C、LDL-C及Ca^2＋、Mg^2＋含量,用美国Easy Lyte Plus型电解质分析仪检测血清K^＋、Na^＋、Cl^-含量。结果与正常饲料组相比,高脂饲料喂养后沙鼠血清TC、TG、HDL-C、LDL-C含量显著升高（P〈0.01）,以TC、LDL-C水平升高最为明显。沙鼠血清电解质K^＋、Mg^2＋含量在不同饲料组差异有显著性（P〈0.01或P〈0.05）,而Na^＋、Cl^-、Ca^2＋含量在不同饲料喂养组的差异不显著（P〉0.05）。结论高脂饲料能明显升高长爪沙鼠血清脂质4项,并改变其血清电解质K^＋、Mg^2＋水平。     

内含式化合物X@Al12P12的结构与稳定性研究

采用B3LYP／6—31G*方法,对内含式化合物X@Al12P12(X=Li^0/ ,Na^0/ ,K^0/2 ,Be^0/2 ,Mg^0/2 ,Ca^0/2 ,H和He)的不同对称性构型进行计算,讨论其最稳定构型的几何参数、布居分析、偶极矩、电离势、包含能、频率、HOMO—LUMO能隙和自旋密度．发现X@Al12P12化合物中,客体X=Na^0/ ,K^0/ ,Mg和He几乎处在笼的中心,Be和Ca^0/2 处在中心附近0．033nm的半径内,Li^0/ ,Be^2 ,Mg^2 和H很大程度上偏离笼的中心位置．大部分金属内含式化合物的C3对称性构型稳定．Li^0/ 。,Be^0/2 ,Mg^2 ,Ca^2 和H与其它离子相比更易嵌入笼内形成稳定的内含式化合物．     

氧化石墨阳离子交换容量测定过程中结构的变化

氧化石墨(GO)结构层上的碳羟基(―C―OH)和边缘羧基(―COOH)在水介质中发生质子化反应解离出的H+具有阳离子可交换性。实验采用甲醛缩合法测量了GO的阳离子交换容量(CEC),用X射线衍射(XRD)、傅里叶变换红外(FTIR)光谱和X射线光电子能谱(XPS)分析测试手段对GO阳离子交换过程中间产物的结构变化进行了分析。结果表明,GO的CEC高达541.48 mmol/100 g。NH_4~+和Ca~(2+)交换后的GO,保持稳定的层状结构,c轴方向层间距分别增大了0.1499和0.2905 nm。NH_4+和Ca~(2+)主要以层间可交换阳离子形式存在于层间域中,并与水分子形成可交换水化阳离子层,部分以[NH_4(H_2O)_6]+和[Ca(H_2O)_6]_2+的形式存在于结构层的边缘附近,共同平衡结构层水解产生的负电荷。     

Use of the Second Derivative of TG Curves for Investigation of the Exchanged Interlayer Cation in Montmorillonite

Various cation-exchanged montmorillonites (Li+, Na+, Ba2+, Mg2+, Ca2+, Mn2+, Co2+, Cu2+, Ag+, Cd2+, Hg2+, Al3+, Pb2+ and NH4+) were prepared from calcium montmorillonite and their properties were studied by means of X-ray diffraction and thermal analysis. The two methods give information on the cation exchange in the interlayer space only. X-ray diffraction studies at room temperature are mainly suitable for estimation of the exchange of cations of different valencies. At 500°C, when the structure is completely collapsed, the d value of montmorillonite depends on the non-hydrated ionic radius of the interlayer cation, but the measurement interval is limited for fine interpretation. The thermoanalytical method is suitable for a better distinction of different exchangeable cations of higher hydration energy on the basis of the DTG or DDTG curve. This revised version was published online in July 2006 with corrections to the Cover Date.     

Adsorption isotherms of homologous alkyldimethylbenzylammonium bromides on sodium montmorillonite

The adsorption of homologous alkyldimethylbenzylammonium bromides, [C(6)H(5)CH(2)N(CH(3))(2)R]Br, on sodium montmorillonite from aqueous NaCl solutions at room temperature has been studied. R stands for the methyl-, butyl-, hexyl-, octyl-, decyl-, and dodecyl-group, and the corresponding ammonium cations will be denoted as C1+, C4+, C6+, C8+, C10+, and C12+, respectively. C1+, the reference cation, attains the plateau region of adsorption at a level close to the cation exchange capacity (CEC) of the clay. The chain-length dependence on adsorptivity of the homologous cations exhibits an unexpected peculiarity. In the case of short-chain homologues of C1+ their adsorption onto sodium montmorillonite decreases in the order C1+>C4+>C6+. This behavior is due, presumably, to the growing steric hindrances at the surface of clay, which occur because of the limited area available for the bulky organic cations at the exchange sites. These limitations appear to be out-balanced in the case of higher homologues for which the increasingly growing hydrophobic effects lead to the expected sequence of adsorptivity of the cations, i.e., C1+相似文献   

Effect of exchangeable cation on the swelling property of 2:1 dioctahedral smectite--a periodic first principle study

We used both localized and periodic calculations on a series of monovalent (Li+, Na+, K+, Rb+, Cs+) and divalent (Mg2+, Ca2+, Sr2+, Ba2+) cations to monitor their effect on the swelling of clays. The activity order obtained for the exchangeable cations among all the monovalent and divalent series studied: Ca2+ > Sr2+ > Mg2+ > Rb+ > Ba2+ > Na+ > Li+ > Cs+ > K+. We have shown that, in case of dioctahedral smectite, the hydroxyl groups play a major role in their interaction with water and other polar molecules in the presence of an interlayer cation. We studied both type of clays, with a different surface structure and with/without water using a periodic calculation. Interlayer cations and charged 2:1 clay surfaces interact strongly with polar solvents; when it is in an aqueous medium, clay expands and the phenomenon is known as crystalline swelling. The extent of swelling is controlled by a balance between relatively strong swelling forces and electrostatic forces of attraction between the negatively charged phyllosilicate layer and the positively charged interlayer cation. We have calculated the solvation energy at the first hydration shell of an exchangeable cation, but the results do not correspond directly to the experimental d-spacing values. A novel quantitative scale is proposed with the numbers generated by the relative nucleophilicity of the active cation sites in their hydrated state through Fukui functions within the helm of the hard soft acid base principle. The solvation effect thus measured show a perfect match with experiment, which proposes that the reactivity index calculation with a first hydration shell could rationalize the swelling mechanism for exchangeable cations. The conformers after electron donation or acceptance propose the swelling mechanism for monovalent and divalent cations.     

Decationization and dealumination of clinoptilolite tuff and ammonium exchange on acid-modified tuff

The paper presents results of investigation of exchange of the clinoptilolite tuff cations with hydrogen ions from HCl solution of concentration 0.1 mmol cm(-3) and ammonium ions solutions of concentrations 0.0071 to 2.6 mmol cm(-3). Molal concentrations, x (mmol g(-1)) of cations exchanged in acid solution and in ammonium ions solutions were compared with molal concentrations of cations obtained by determination of the cation-exchange capacity of clinoptilolite tuff. The obtained results show that at ammonium ion concentrations lower than 0.1 mmol cm(-3), with regard to exchange capacity for particular ions, best exchanged are Na+ ions, followed by Mg2+ and Ca2+ ions, while exchange of K+ ions is the poorest (Na+ > Mg2+ > Ca2+ > K+). At ammonium concentrations from 0.2 to 1 mmol cm(-3) the order is Na+ > Ca2+ > Mg2+ > K+. At concentrations higher than 1 mmol cm(-3) the order is Na+ > Ca2+ > K+ > Mg2+. The results are a consequence of the uptake of hydrogen ions by zeolite samples in ammonium ions solutions at concentrations lower than 1 mmol cm(-3) and indicate the importance of Mg2+ (besides Na+ ions) for the exchange between clinoptilolite cations and H+ ions, in contrast to K+ ions, whose participation in the reaction with H+ ions is the lowest. During decationization of the clinoptilolite in acid solution, best exchanged are Na+, Mg2+, and Ca2+ ions, while exchange of K+ ions is the poorest. Due to poor exchange of K+ and H+ ions and good exchange of Na+, Mg2+, and Ca2+ ions, it is to be assumed that preservation of stability of the clinoptilolite structure is caused by K+ ions present in the channel C. Clinoptilolite is dissolved in the clinoptilolite A and B channels where Na+, Mg2+, and Ca2+ ions are present. On the acid-modified clinoptilolite samples, exchange of ammonium ions is poorer than on natural zeolite. The longer the contact time of the zeolite and acid solution, the worse ammonium ions exchange. It can be assumed that H+ ions exchanged with zeolite cations are consumed for solution of aluminum in the clinoptilolite structure; therefore the concentration of H+ ions as exchangeable cations decreases. In the ammonium ion solution at a concentration of 0.0065 mmol cm(-3), from the acid-modified zeolite samples, Al3+ ions are exchanged best, followed by Na+, Mg2+, Ca2+, and K+ ions. Further to the results, it is to be assumed that exchangeable Al3+ ions available from clinoptilolite dissolution are best exchanged with H+ ions in acid solution.     

Differences in coating mechanism of structurally different aluminosilicates observed through the thermal analysis

Systematic modification of three structurally different minerals (zeolite, mica, and vermiculite) was carried out with the aim of determining the modification mechanism and exposing the hydrophobic surface that can be used as a sorbent for many organic compounds. Mechanism of modification with cationic surfactant depends strongly on the mineral type. In order to identify the influence of aluminosilicates structural differences on the modification process, adsorption experiments with organic matter and water vapor, supplemented with the DTA/TG analysis, were performed. The cation exchange capacity (CEC) value was 1454?>?560?>?28 meq kg^?1 for zeolite (clinoptilolite), vermiculite, and mica (muscovite), respectively. Despite its CEC value, vermiculite adsorbed three times the amount of organic matter than did clinoptilolite due to the porous structure of zeolite, which acted to limit the adsorption only on the external exchangeable cations. If the loading amount is equal to the CEC or the external cation exchange capacity for clinoptilolite (ECEC?≈?10% CEC), the monolayer will form while mineral surface will have hydrophobic character. Only one active center exists at the surface of the clinoptilolite that was identified by DTA curves with a sharp and defined peak around 300 °C and by the mass loss at the TG diagrams. Two significant and equal active centers were observed in vermiculite, one for the exchange of the surface cations and the other for the interlayer cations and H₂O molecules. Muscovite CEC is negligible, and due to the absence of any other functional groups, the modification of this mineral was impossible.     

Natural vermiculite as an exchanger support for heavy cations in aqueous solution

The natural highly charged lamellar silicate vermiculite was investigated as an exchanger matrix in doubly distilled water solution to exchange magnesium inside the lamella with the heavy cations copper, nickel, cobalt, and lead at the solid/liquid interface. The extension of each exchange reaction was dependent on time of reaction, pH, and cation concentration. The maximum time presented the following order Pb2+ < Ni2+ < Cu2+ < Co2+, which corresponds to 12, 24, 48, and 72 h, respectively. The best performance was observed for nickel, as represented by the exchange capacity Nf, which gave values 0.59, 0.76, 0.84, and 0.93 mmol g(-1) for Pb2+ < Co2+ < Cu2+ < Ni2+, respectively. This capacity is dependent on pH interval variation from 1 to 9, being significantly increased in alkaline condition. The isotherm data were adjusted to a modified Langmuir equation and from the data the spontaneous Gibbs free energy was calculated. Linear correlations were obtained through Gibbs free energy or the maximum capacity against the cationic radius plot, with the lowest values for the largest cation lead. An exponential correlation was also observed for the maximum capacity versus enthalpy of hydration plot, indicating a difficulty of the less hydrated cation, lead, in exchanging with magnesium inside the lamellar space, as suggested by the proposed mechanism. The saturated matrices with cations presented a decrease in interlayer distance in comparison with the original vermiculite, which can be related to the hydrated phases, characteristic for each cation, with a lowest value for lead.     

离子交换与离子排斥色谱柱串联体系中阳离子的多峰现象及其机理

研究了串联柱体系中阳离子的“多峰现象”。在阳离子交换柱后面接上阴离子分析用的离子排斥柱构成一个串联柱体系,当以酒石酸（ＴＡ）和吡啶二羧酸（ＰＤＣ）的混合溶液作淋洗液时,每一种阳离子同时出现３个色谱峰。这是因为从阳离子交换柱流出的阳离子与有络合作用的两种淋洗剂阴离子形成络合物,使流动相中淋洗剂阴离子浓度减少以及两种淋洗剂阴离子在离子排斥柱中被保留且保留值不同。     

A comparative study of different methods of deter-mining exchangeable cations from clays and micas

A comparative study of the various methods of determining exchangeable cations was made in order to assess their relative applicability It seems that SCHOLLENBERGER'S method, is quite well suited for cation exchange studies as the ammonium thus adsorbed gives a fairly accurate measure of the cation exchange capacity at PH 7     

浸渍硅胶薄层色谱板分离钴和镍及数字图像分析法定量(英文)

Thin layer chromatography(TLC) of cobalt and nickel has been performed on silica gel layers induced with alkali mediated cellulose extract.A novel combination of 10% aqueous solutions of Tween-20 and potassium thiocyanate in 1∶1(v/v) was identified as the best mobile phase for the selective separation of Co2+from Ni2+on the impregnated Silica Gel G layers.The chromatographic characteristics of the cations were studied and the limits of detection as well as the limits of quantification for Co2+and Ni2+were determined.The quantitative estimation of the cations was achieved from the digital image analysis of respective chromatograms.The proposed quantitative method was successfully applied with 0-0.50% error for the determination of Co2+from Ni2+in spiked samples of bauxite,soil and rock containing common cations such as Al3+,Fe2+,Ti4+,Zn2+,Mn2+,Cu2+,Cr6+,Mg2+,etc.under the optimized chromatographic conditions.