同时测定海水中K+、Na+、Ca2+、Cl-的流动注射离子选择电极分析

建立了一种用于海水中K+、Na+、Ca2+、Cl-同时快速、自动测定的流动注射离子选择电极自动方法(FI-ISE-M),优化了方法的最佳条件:总离子强度调节液(TISAB)的组成为0.3 mmol/L K+、6.0 mmol/L Na+、1.4 mmol/L Ca2+、21.0 mmol/L Cl-及pH8.0的80 mmol/L的tris-H3BO3缓冲溶液,其流量为1.25mL/min;每次测定的样品用量仅为160μL,载流流量为1.42 mL/min,混合盘管长度为30cm(I.D.0.5 mm)。本方法的分析速度为100样/h,相对标准偏差为2.0%(n=11),标准添加回收率为94.9%～104.3%,测定范围分别为1.0～8.0 mmol/L K+、50～290 mmol/L Na+、3.2～16.0 mmol/L Ca2+、70～430 mmol/LCl-。本方法已应用于反渗透海水淡化系统的水质检测。     

酶荧光毛细管分析法测定微量血清中乳酸脱氢酶活性

基于丙酮酸/还原型辅酶I/乳酸脱氢酶(LDH)/乳酸/氧化型辅酶I荧光猝灭体系和荧光毛细管分析技术,建立了可用于微量样品中LDH酶活性测定的方法。优化的测定条件为:激发及发射波长分别为350和460nm;测定温度为25℃;酸度为pH 6.5;NADH浓度为300μmol/L;丙酮酸浓度为1.2mmol/L。本方法的测定范围为50～1500IU/L,检出限为30IU/L,相对标准偏差2.1%～2.2%(n=10),回收率在96.4%～105%范围内。本方法操作简单,每次测定仅需样品2.0μL、试剂18.0μL,分析速度约为30样/h,利用本方法测定了微量血清中LDH的活性。     

流动注射-固相萃取-分光光度法检测半导体工业用水中痕量硅

硅酸盐在酸性介质中与钼酸铵反应生成硅钼黄,硅钼黄还原为硅钼蓝后,可被HLB小柱定量萃取.在此基础上,建立了流动注射-固相萃取-分光光度(FI-SPE-Vis)测定水中痕量硅酸盐的新方法.反应生成的硅钼蓝经HLB小柱萃取后,用水清洗去除杂质,NaOH溶液洗脱,分光光度法检测.实验对各参数进行了优化,优化后的参数为:洗脱剂浓度0.01 mol/L;试样上柱流速28.0 mL/min;洗脱流速3.5 mL/min;反应温度45 ℃;硅钼黄与硅钼蓝反应时间均为5 min;钼酸铵混合溶液、草酸溶液、抗坏血酸溶液的用量分别为3.5,3.5和1.75 mL.本方法具有良好的重现性和灵敏度,测定含硅9.33 μg/L的硅酸盐水样7次,RSD值为1.8%;选取不同的试样富集时间,可将定量分析的线性范围扩展为0.47～117 μg/L;检出限0.18 μg/L;回收率为96.8%～105%.可满足特殊工业用水中痕量硅检测的需要.     

流动注射-微型流通式离子选择性电极测定地热水中高浓度钙(Ⅱ)

采用流动注射-微型流通式钙(Ⅱ)选择电极测定地热水中高浓度钙(Ⅱ)的含量,并对各种影响因素进行了研究。优化的试验条件为:混合盘管长度30cm,载流流量为0.99mL.min-1,采样体积60μL,总离子强度调节缓冲溶液(pH 9.7)由0.02mol.L-1硼砂、0.02mol.L-1氢氧化钠、10mg.L-1钙(Ⅱ)和0.6mol.L-1氯化钠溶液组成,其流量为0.88mL.min-1。方法的线性范围为0.16～20.00g.L-1。对1.00,2.00g.L-1钙标准溶液分别连续测定11次,所得结果的相对标准偏差分别为2.8%,1.8%。方法用于地热水样的分析,加标回收率在102%～111%之间。     

电感耦合等离子体串联质谱法测定实验室纯水中痕量硅

建立电感耦合等离子体串联质谱法测定实验室纯水中痕量硅的方法。优化电感耦合等离子体串联质谱仪工作条件,两个四极杆质量过滤器Q1,Q2质量数均为28,碰撞/反应模式为H_2原位质量模式,采用标准加入法进行定量分析。硅的质量浓度在0～100μg/L范围内与响应信号呈良好的线性关系,线性相关系数大于0.999 9,检出限为0.109μg/L。测定结果的相对标准偏差为1.6%～4.5%(n=7),样品加标回收率为96.2%～103.7%。该方法灵敏度高,测定结果准确、可靠,可用于实验室纯水中痕量硅分析。     

银黄冲剂中黄芩甙和绿原酸的毛细管电泳分离分析

摘要：用毛细管电泳法分离并测定了银黄冲剂中黄芩甙和绿原酸。以对硝基苯甲酸为内标,未涂层融硅毛细管（50μmi.d.,370μmo.d.,总长47cm,有效分离长度40cm）为分离通道,25mmol/L硼砂缓冲液（pH8.5）为电泳介质,17kPa·s压力进样,25kV恒压电泳,310nm检测。黄芩甙和绿原酸线性范围分别为160～960mg/L(r=0.9993,RSD=1.76％～2.33％）和80～960mg/L（r=0.9989,RSD=1.07％～2.51％）,加入回收率：黄芩甙为（102.09±1     

夹管电磁阀定量-流动注射分析系统测定海水中亚硝酸盐和硝酸盐氮

采用3个夹管电磁阀联用代替传统六通阀的样品定量方法,自制一套多通道流动注射分析仪,并优化了仪器的最佳测试条件,实现了海水中硝酸盐氮和亚硝酸盐氮含量的测定。本分析系统结构简单,性能可靠,测定频率为28个/h。测试结果表明,亚硝酸盐氮和硝酸盐氮的线性范围(以氮含量计)分别为25～1000μg/L和50～1000μg/L(R≥0.999),检出限分别为1.8和4.8μg/L;加标回收率在94.5%～105.3%之间;加标200.0μg/L的回收实验的相对标准差在1.3%～4.5%之间(n=6)。经t检验分析,本方法与国标方法测定数据无显著性差异,可适用于海水中微量亚硝酸盐氮和硝酸盐中氮的快速测定分析。     

液液萃取-GC-MS法测定水中硝基苯质量控制指标研究

采用液液萃取–气相色谱–质谱法测定水中硝基苯,通过统计全国多家实验室的测定数据,对平行样测定结果相对偏差、空白加标回收率、样品加标回收率、空白加标回收率相对偏差及样品加标回收率相对偏差5个质控指标进行分析,得出质控指标评价标准。在概率P,γ均为0.90时,平行样测定结果允许最大相对偏差应控制在11.0%;当空白加标浓度为0.2～30μg/L时,回收率控制范围为59%～113%;当样品未检出、加标浓度在0.25～50μg/L时,样品加标回收率控制范围为56%～110%;空白加标、样品加标回收率最大相对偏差应分别控制在10.0%和11.1%。在概率P和γ均为0.95时,平行样测定结果允许最大相对偏差应控制在13.5%;当空白加标浓度为0.2～30μg/L时,回收率的控制范围为50%～122%;当样品未检出、加标浓度在0.25～50μg/L时,样品加标回收率控制范围为49%～117%;空白加标、样品加标回收率最大相对偏差应分别控制在12.6%和14.6%。     

乳酸的液态酶荧光毛细分析法研究

基于乳酸脱氢酶(LDH)和烟酰胺腺嘌呤二核苷酸(NADH)氧化还原体系,提出了乳酸的液态酶荧光毛细分析方法(LE-FCA).在激发波长350nm、发射波长460nm奈件下,用LE-FCA法对乳酸进行了测定;其线性范围为0.2～1.0 mmol/L,r>0.9932,检出限为0.022 mmol/L,RSD<4.2%.LE-FCA能节省贵重的酶试剂,样品用量仅为18μL;可用于医药、卫生、工业、食品等含乳酸样品的测定.     

微波消解-双通道原子荧光光谱法同时测定家禽内脏中的硒和汞

最佳分析条件下,采用微波消解样品,以HCl为预还原剂和测定介质,用氢化物发生-原子荧光法同时测定了家禽内脏中硒汞的含量。硒、汞的质量浓度分别在12.00～24.00μg/L范围与相应的荧光强度呈线性关系,方法的检出限分别为0.065μg/L和0.010μg/L,相对标准偏差(RSD)分别在1.3%～2.8%和2.4%～4.3%(n=5)之间,回收率范围分别为93.6%～101.1%和92.2%～98.6%。     

流动注射光度法测定地热水中可溶性硅

提出了基于正硅酸与钼酸铵的显色反应和流动注射分析装置的流动注射光度法测定地热水中可溶性硅量的方法。对仪器的各项工作参数,包括显色反应所需钼酸铵溶液的浓度及要求的酸度条件,各反应圈的长度,试剂环的定量体积,流动注射系统出口的流量等做了试验并予以优化,所提出的装置可达到每小时60个样品的进样频率。测定二氧化硅的线性范围为20~800 mg.L-1。应用此法对实样的测定结果与国家标准方法(GB/T 12148-2006)测得的结果相符。     

Evaluation of capillary electrophoresis for determining the concentration of dissolved silica in geothermal brines

The determination of silica concentrations in geothermal brines is widely recognized as a difficult analytical task due to its complex chemical polymerization kinetics that occurs during sample collection and chemical analysis. Capillary electrophoresis (CE) has been evaluated as a new reliable analytical method to measure silica (as silicates) in geothermal brines. Synthetic and geothermal brine samples were used to evaluate CE methodology. A capillary electrophoresis instrument, Quanta 4000 (Waters-Millipore) coupled with a Waters 820 workstation was used to carry out the experimental work. The separation of silicates was completed in approximately 5.5 min using a conventional fused-silica capillary (75 microm i.d. x 375 microm o.d. x 60 cm total length). A hydrostatic injection (10 cm for 20 s at 25 degrees C) was employed for introducing the samples. The carrier electrolyte consisted of 10 mM sodium chromate, 3 mM tetradecyltrimethyl-ammonium hydroxide (TTAOH), 2 mM sodium carbonate, and 1 mM sodium hydroxide, adjusted to a pH 11.0 +/- 0.1. Silicates were determined using an indirect UV detection at a wavelength of 254 nm with a mercury lamp and with a negative power supply (-15 kV). A good reproducibility in the migration times (%R.S.D. approximately 1.6%) based on six non-consecutive injections of synthetic brine solutions was obtained. A linear response between silica concentration and corrected peak area was observed. Ordinary (OLR) and weighted (WLR) linear regression models were used for calculating silica concentrations in all samples using the corresponding fitted calibration curves. The analytical results of CE were finally compared with the most probable values of synthetic reference standards of silica using the Student's t-test. No significant differences were found between them at P = 0.01. Similarly, the atomic absorption spectrometry (AAS) results were also compared with the most probable concentrations of the same reference standards, finding significant differences at P = 0.01.     

Estimation of Silica Species’ Concentrations in Lithium and Magnesium Chloride Solutions from the Peak Intensities Observed by FAB-MS

The concentrations of dissolved silica species in electrolyte solutions were derived from the relative intensities of silica species, obtained from FAB-MS measurements (fast atom bombardment mass spectrometry), and the total concentration of dissolved silica. Generally, silica species in aqueous solutions form various complexes with cations such as sodium (Na⁺) or calcium (Ca²⁺), and it has been difficult to determine the concentration of each species. From the observed results from FAB-MS, the chemical species of silica dissolved in lithium chloride (LiCl) and magnesium chloride (MgCl₂) solutions do not include complexes with these cations, and thus Li⁺ and Mg²⁺ do not replace protons of the silanol groups in silica. Therefore, in LiCl and MgCl₂ solutions, all of the simple structures of silicate species can be identified. The concentration of each silica species was estimated on the basis of its mass spectra peak intensities and the total concentration of silica as determined by colorimetry. This study yields the concentration of each silica species within small errors, whereas conventional methods (such as ²⁹Si-NMR) have not yielded the concentrations of individual silica species. From these results, dimers and cyclic tetramers are concluded to be the main species in silica solutions with concentrations of at most 0.1 to 0.2 μmol⋅dm⁻³. This tendency should also occur in NaCl and CaCl₂ solutions, which are major electrolytes in natural waters.     

Vibrational and 29Si NMR spectroscopies of soluble silicate oligomers

Vibrational spectroscopy has been used to correlate the features of silicate solution spectra with ²⁹Si NMR spectra, as a function of SiO₂:Na₂O ratio and SiO₂ concentration. Assignments of infrared and Raman component bands have been made for different anion types and are consistent with results reported for crystalline silicates and silicate glasses. The extent of depolymerization of larger anions has been found to differ, depending on both the degree of dilution and alkalinity. The relative amounts of polymeric (Q⁴) silica and larger three dimensional (Q³_4R) anions are greater for the more siliceous solutions (3.3 and 2.95 ratio) at high concentrations. These large anions continue to be major contributors to the anion distribution even at 15 to 50 fold dilution. In the case of more alkaline solutions, especially below 2.5 ratio, the relative contribution of the large anions to the distribution drops rapidly, even with 2 or 3 fold dilution. At low concentrations, in very alkaline solutions, the anion distribution is mainly monomer, dimer and cyclic trimer. Vibrational spectroscopies show great promise for observing changes in anion distribution on a much shorter time scale than is possible with ²⁹Si NMR and can be useful for following reactions involving silicate solutions.     

Bubble guidance of tubular growth in reaction-precipitation systems

Numerous types of reaction-precipitation systems involve the growth of tubular structures similar to those formed in "silica gardens". As a model case for this phenomenon, we investigate the rapid growth of hollow tubes in the reaction between sodium silicate and cupric sulfate. The latter solution is injected hydrodynamically at constant flow rates of 1-20 mL h(-1) into a large reservoir of waterglass. In this study, the growth is templated and guided by single, buoyant gas bubbles. The resulting tubes can be several decimetres long and have constant radii in the range of 100-600 microm. Systematic measurements show that bubble size governs the tube radius. According to this radius, the system selects its growth velocity following volume conservation of the injected solution. Moreover, scanning electron microscopy reveals intricate ring patterns on the tube walls. We also show evidence for the existence of a minimal and a maximal tube radius. Finally, we report an intriguing collapse of tubes created at high silicate concentrations, which yields twisted ribbon-like structures. Critical radii and tube collapse are discussed in terms of simple competing forces.     

Use of disposable clean-up columns for selective removal of humic substances prior to measurements with a nitrate ion-selective electrode

Measurements of nitrate in natural waters with a nitrate ion-selective electrode are seriously affected by the presence of humic substances. These can be removed quantitatively by a clean-up procedure with cheap disposable adsorption columns packed with chemically-bonded alkylamino silica. The method is applied to natural water samples with high contents of humic substances. The nitrate concentrations found were in good agreement with determination by ion chromatography.     

Use of radioactive thermal water after226Ra removal

The paper describes the possibility of efficient and safe use of geothermal water at a location in the town of Zagreb. Geothermal water is used exclusively for the purpose of sport and recreation. Due to elevated²²⁶Ra concentrations, the raw geothermal water must be used in limited proportions so as to exclude any potential health risk for the pool users. With application of adequate treatment methods, such as intense aeration (²²⁶Ra removal efficiency 13.7±3.5%) and filtration of aerated water with high pressure sand filters (removal efficiency 39.5±7.9%), the elevated²²⁶Ra content would be maximally reduced. The decrease of radioactivity enables that the proportion of geothermal water would be increased without any health risk, ensuring great cost reduction spent on the warming of pool waters.     

Use of radioactive thermal water after226Ra removal

The paper describes the possibility of efficient and safe use of geothermal water at a location in the town of Zagreb. Geothermal water is used exclusively for the purpose of sport and recreation. Due to elevated²²⁶Ra concentrations, the raw geothermal water must be used in limited proportions so as to exclude any potential health risk for the pool users. With application of adequate treatment methods, such as intense aeration (²²⁶Ra removal efficiency 13.7±3.5%) and filtration of aerated water with high pressure sand filters (removal efficiency 39.5±7.9%), the elevated²²⁶Ra content would be maximally reduced. The decrease of radioactivity enables that the proportion of geothermal water would be increased without any health risk, ensuring great cost reduction spent on the warming of pool waters.     

Depolymerization of polysilicic acid by tiron

As a preliminary experiment for the development of an effective silica scale inhibitor at geothermal power plants, the effect of tiron, a ligand to monosilicic acid, on the polymerization of silicic acid was investigated by gel chromatographic method. The experiments were carried out at Si concentration of 400 ppm (14 mM) and at pH 8 where are a similar condition to geothermal water. The tiron concentration was varied (0-50 mM). At 30 mM of tiron, the polymerization of silicic acid occurred rapidly within first 1 h in spite of the presence of tiron, however, polysilicic acids were depolymerized by tiron. The depolymerization mechanism of polysilicic acids was discussed based on zeta potentials for silica gel particles in the absence and presence of tiron.     

Study on Deactivation of Co/ZrO2/SiO2 Catalyst For Fischer-Tropsch Synthesis

A Co/ZrO₂ /SiO₂ catalyst active for synthesis of heavy hydrocarbons from syngas was subjected to a stability test of 500 h on a laboratory scale. The catalyst showed a considerable decrease in CO conversion, while the hydrocarbon distribution hardly changed with time on stream. The regeneration of deactivated catalyst with H₂ at 673 K partially restored the activity. XRD, FT-IR and TGA identified a hydrated cobalt silicate species in the catalyst near the reactor outlet. Thus, the cause of deactivation was proposed mainly to be the formation of inactive hydrated silicate between Co metal and silica in presence of high partial pressure of water.