煤吡啶抽提过程中柱色谱与索氏提取法对富集物组成的影响

为考察柱色谱分离和索氏提取两种固体样品提取方法对提取物组成的影响,探索操作条件温和、溶剂使用量经济的固体样品提取方法。本研究以吡啶为溶剂,对准葛尔黑岱沟、平朔、潞安常村3种不同变质程度的煤样进行了柱色谱分离和索氏抽提。提取物用凝胶色谱、电喷雾质谱和同步荧光光谱进行分析,比较和确定不同提取方法对煤提取物中组分分子量分布和结构的影响。分析发现,柱色谱分离与索氏提取相比,抽提率略有增加,但柱色谱提取物组分中缺失了提取样品中结构稳定的超大分子结构片断;质谱结果显示柱色谱抽提物中主要存在5个组分,提取物组分相对于索氏提取物单一、富集度高;同步荧光显示柱色谱提取物中芳香化合物的基本组成为3~5个环的芳香化合物。实验结果表明:如仅分析质量数小于1000 amu的化合物,柱色谱法可替代索氏提取法。     

8-羟基喹啉-5-磺酸纤维微柱分离富集电感耦合等离子体原子发射光谱法同时测定多种痕量元素

本文合成了8-羟基喹啉-5-磺酸纤维滤纸片,以此做为微柱填充物同时富集了10种痕量元素,并分离了样品中的高盐组分.本方法可使痕量组分的分离与富集同步进行,因而特别适用于原子光谱测定前样品的预处理.     

同位素稀释高分辨气相色谱-高分辨质谱法检测烟道气中的低氯代二恶英

建立了同位素稀释高分辨气相色谱-高分辨质谱检测烟道气中痕量低氯代二恶英的分析方法。采用索氏提取富集烟道气样品中的目标物,提取液经过复合硅胶柱和碱性氧化铝柱净化后,进行高分辨气相色谱-高分辨质谱检测。采用DB-5MS毛细管色谱柱（30 m×0.25 mm×0.25 μm）分离,以保留时间和同位素特征离子丰度比定性,以与同位素的峰面积比值定量。实验结果表明,方法的回收率为66.6%~112.5%,相对标准偏差（RSD）的范围为19.9%~40.5%（n=5）,方法的检出限（LOD）为0.027~0.485 μg/L。应用该方法检测了3个焚烧炉烟道气样品,回收率在85.7%~137.0%范围内,样品中目标物含量分布在11.4~9183 pg/Nm³之间。结果表明该方法适合用于烟道气中痕量低氯代二恶英的检测。     

吹扫捕集-原子荧光光谱与同位素稀释质谱法结合测定海水中痕量汞

建立了吹扫捕集-原子荧光光谱,结合同位素稀释质谱法测定海水中痕量汞的高准确度的分析方法,以HNO3消解样品,通过吹扫捕集、金柱吸附的方式实现痕量汞与高盐基体的分离并进一步富集,与电感耦合等离子体质谱联用,采用同位素稀释质谱法进行准确测定.对影响样品准确测定结果的消解用HNO3体积、消解时间、SnCl2用量、基体影响、本...     

体液的在线样品前处理技术及其小分子化合物的液相色谱-质谱分析

在线样品前处理液相色谱-质谱联用技术为体液中痕量小分子化合物提供了高灵敏度、高选择性和高通量的分析方法。该文以在线固相萃取柱为主线,总结了不同种类富集柱的特点及其近5年来在相关领域的应用,并简要介绍了在线液相色谱-质谱分析的流路系统。     

轻烃中碳、氢同位素组成特征

本文收集了我国10个含油气区46个凝析油、轻质油样品,进行了全烃和部分饱和烃的碳、氢同位素分析,结合各地区地质背景,讨论了成气母质和沉积环境。从全油和饱和烃碳、氢同位素组成特征看,与煤系有关的凝析油常富集~(13)C,与Ⅰ,Ⅱ型母质(生油岩系)相关的凝析油则富集~(13)C。总体而言,碳同位素组成主要与母质的同位素继承效应相关,而氢同位素组成的变化则主要反映与沉积环境及水介质盐度的相关性。基于现有资料,提出δD值小于-150‰者为淡水-微咸水;大于-150‰者为半咸水-海水环境。研究表明,沉积相控制了有机母质,而不同有机母质又显示出稳定同位素组成的差异。     

氧化石墨烯/壳聚糖微球吸附-电感耦合等离子体质谱法测定地质样品中痕量钽EI北大核心CSCD

建立了氧化石墨烯/壳聚糖微球吸附-电感耦合等离子体质谱法测定地质样品中痕量Ta的方法。合成了氧化石墨烯/壳聚糖微球,将其应用于地质样品中痕量Ta的分离富集,采用电感耦合等离子体质谱对富集后的试液进行测定。对氧化石墨烯含量、配体种类和浓度、pH、吸附时间、吸附剂用量等吸附条件和洗脱剂类型、体积、洗脱时间等洗脱条件进行了优化,在优化的条件下,对地质样品标准物质进行测定,Ta的方法检出限为2.0 ng/g,富集倍数为26.7倍。     

液相色谱-同位素比值质谱法研究桔橙汁中柠檬酸碳同位素比值

以国际原子能机构提供的蔗糖(δ13C为-10.449‰)作为溯源标准,建立了液相色谱-同位素比值质谱联用法(LC-IR MS)分析天然柑桔、橙汁中柠檬酸碳同位素比的方法,对不同产地个柑桔、橙子中有机酸碳同位素情况进行了研究。基于建立天然水果的柠檬酸碳同位素δ13C值的数据,提出了柑桔、橙子样品的δ13C值范围。方法将果汁用水稀释后,液相色谱-钙离子交换色谱在线制备柠檬酸,氢型离子交换柱分离柠檬酸后采用液相色谱-稳定同位素比质谱分析,柠檬酸方法检出限为5μg/m L,在2.00~100μg/m L水平时,柠檬酸响应与浓度成线性关系,相关系数为0.9997。方法日内、日间和人员比对结果相对标准偏差小于0.82%。收集不同产地161个橙子、167个柑桔测得天然桔汁中柠檬酸δ13C值在-32.87‰~-27.07‰之间,橙汁柠檬酸δ13C值在-32.73‰~26.01‰之间。采集40个市售柑桔、橙汁样品进行鉴定,检出17个掺有C4植物柠檬酸的的阳性样品,新方法可提高勾兑柠檬酸掺假果汁的鉴别能力。     

飞秒激光剥蚀-多接收等离子体质谱原位分析玄武岩玻璃样品Mg同位素组成

建立了飞秒激光剥蚀多接收等离子体质谱(fsLA-MC-ICP-MS)原位微区分析玄武岩玻璃中Mg同位素的方法.溶液进样-干气溶胶条件下浓度匹配实验表明,样品和标准样品中Mg浓度比在0.4 ～3.0时,可获得准确样品Mg同位素组成.激光剥蚀条件对Mg同位素的准确测定有明显的影响,激光剥蚀斑束和扫描速率变化,使得质谱仪的质量歧视效应随进样负载量不同而产生较大的变化,并影响样品Mg同位素组成;激光剥蚀频率与δ25 Mg正相关,与δ26 Mg负相关,当剥蚀频率大于4 Hz时,δ25 Mg和δ26 Mg趋于平稳;超快激光的能量密度对Mg同位素组成影响较小.利用本方法对国际标准样品的分析结果与参考值在误差范围内一致.本方法具有制样简单、快速的特点,且测试结果准确可靠,为火山玻璃中Mg同位素分析提供了有效的分析手段.     

用于综合录井技术的在线快速气相色谱-四极杆质谱联用仪研制

研制了一种用于综合录井技术的在线快速气相色谱-四极杆质谱联用仪。采用隔膜泵直接抽取泥浆中脱出的气体样品直接引入气相色谱,通过气驱十通阀实现自动进样;快速分离后,样品中各组分依次进入四极杆质谱进行检测;四极杆质谱采用电子轰击源电离及选择离子扫描的方式,提供对碳氢化合物检测所需要的高灵敏度;仪器通过精确的时序控制实现周期循环进样分析,满足录井现场的实时监测需求。仪器采用安全易得的氮气作载气,对C1-C8烷烃、苯、甲苯、环己烷和甲基环己烷等油气组分进行快速在线分析,结果表明,C1-C5分析周期小于30 s,C1-C8周期小于85 s,最低检测浓度为0.0001%(V/V),线性范围高于5个数量级,适合于录井技术中油气组分分析。     

三通道气相色谱法测定炼厂气组成

炼厂气是炼油工艺产生的各种气体的混合物,采用四阀六柱将炼厂气分离分解为3部分,以双TCD+FID检测器3通道气相色谱法快速分析炼厂气.FID通道用于分析烃类,一个TCD通道分析永久性气体和硫化物,另一个TCD通道分析氢气,采用面积归一化法定量计算分析结果.用该法测定了3种标准气体,测定值与标准值基本一致,测定结果的相对标准偏差小于8％.该法适用于测定包括液化气、烟气、裂解气等组分相近的样品组成.     

A simple, practical methodology for routine VSMOW/SLAP normalization of water samples analyzed by continuous flow methods

Normalization of stable isotope data is important for meaningful inter-laboratory comparisons of data, especially for waters where there may be large natural variations in isotope ratios of oxygen and hydrogen. As a result, large, systematic errors may arise in continuous flow applications without correction, whereas normalization to the VSMOW/SLAP scale can facilitate inter-laboratory comparison and can be accomplished by a simple procedure in which secondary laboratory standards, carefully calibrated, are analyzed along with unknown samples. Delta values for these standards, as analyzed, are plotted against the calibrated values and a linear regression is performed. The resulting equation is applied to unknown samples to achieve the normalization. The one-sigma [1sigma] standard deviation for replicate samples by this normalization method using a Finnigan Gasbenchll should be 相似文献   

Experimental studies on the hydrogen isotope recovery using low-pressure palladium membrane diffuser

In this paper, we introduce a set of low-pressure palladium membrane diffuser designed to recover hydrogen isotopes from inert mixture gases. Several gaseous mixtures (D₂/Ar and D₂/He) with different deuterium concentration have been used for cleanup test of the low-pressure palladium membrane diffuser at 723 K. Effect of the composition of feed gas on the pressure of permeate side has been observed by gas chromatography (GC) and pressure sensor. With the feed flow rate of the mixture gases increasing, the D₂ permeate pressure is increasing as well. Decontamination factor (DF) of more than 1000 and recovery efficiency greater than 99.9% have been obtained by controlling the feed gas flow rate. The same palladium membrane diffuser was used to process helium-3 gas with more than 10% hydrogen isotope and about 0.3% tritium gas. The pure helium-3 (above 99.4%) with low content of hydrogen isotopes (about 0.084%) has been obtained. Recovery efficiency of all hydrogen isotopes is 99.5% above.     

An online method combining a thermal conversion elemental analyzer with isotope ratio mass spectrometry for the determination of hydrogen isotope composition and water concentration in geological samples

An online continuous-flow method, combining a thermal conversion elemental analyzer (TC/EA) with isotope ratio mass spectrometry (MS), is evaluated for the determination of both the hydrogen isotope composition and the water concentration of hydrous and nominally anhydrous minerals. The technique involves reduction of hydrous minerals or nominally anhydrous minerals by reaction with glassy carbon at 1450 degrees C in a helium stream. The product gases, H2 and CO, are separated on a gas chromatographic column prior to analysis in the mass spectrometer. Calibration curves for the H concentration analysis were generated from a standard of benzoic acid (C7H6O2) that has an H concentration of 5.0 wt%; the analytical uncertainties were better than +/-0.05% in our runs. Two standards of material with given D values, polyethylene IAEA-CH-7 and biotite NBS-30, were tested for the purpose of calibrating a natural garnet 04BXL02 representing nominally anhydrous minerals. Preheating at 90 degrees C for 12 h was found to be suitable for removing adsorption water on the sample surface. This results in constant D values and total H2O contents for the garnet, with weighted means of -94 +/- 1 and 522 +/- 11 ppm (wt), respectively. The TC/EA-MS technique allows routine analysis of sample sizes as small as 0.01 microL H2O. For natural minerals, absolute reproducibilities for D values are +/-0.5 to +/-2 (1) and relative uncertainties for total H2O concentrations are at levels of +/-1% to +/-3% (1). Therefore, this online method can be used for the quantitative determination of H isotope composition and H2O concentration of either hydrous or anhydrous minerals.     

FID/TCD并联气相色谱法测定天然气水合物的气体组成

建立了一种氢火焰离子化检测器（FID）与热导检测器（TCD）并联检测的气相色谱分析技术。该方法一次进样,即可实现天然气水合物中C1~C6、CO2、H2S、O2+N2 16种气体成分的同时测定。实验优化了色谱柱、升温程序、柱流速、进样口温度、检测器温度、TCD参考气和尾吹气流速等仪器分析参数。在优化条件下,16种气体分子在实验浓度范围内线性关系良好,r2为0.999 03~0.999 98,方法检出限为0.000 3~0.046 mol/mol,相对标准偏差（n=6）为1.6%~5.0%。对祁连山冻土区、南海神狐海域、人工合成水合物样品的分析表明,该方法简便实用、灵敏可靠,可满足天然气水合物气体组成的分析要求。     

Improved method for isotopic and quantitative analysis of dissolved inorganic carbon in natural water samples

We present here an improved and reliable method for measuring the concentration of dissolved inorganic carbon (DIC) and its isotope composition (delta(13)C(DIC)) in natural water samples. Our apparatus, a gas chromatograph coupled to an isotope ratio mass spectrometer (GCIRMS), runs in a quasi-automated mode and is able to analyze about 50 water samples per day. The whole procedure (sample preparation, CO(2(g))-CO(2(aq)) equilibration time and GCIRMS analysis) requires 2 days. It consists of injecting an aliquot of water into a H(3)PO(4)-loaded and He-flushed 12 mL glass tube. The H(3)PO(4) reacts with the water and converts the DIC into aqueous and gaseous CO(2). After a CO(2(g))-CO(2(aq)) equilibration time of between 15 and 24 h, a portion of the headspace gas (mainly CO(2)+He) is introduced into the GCIRMS, to measure the carbon isotope ratio of the released CO(2(g)), from which the delta(13)C(DIC) is determined via a calibration procedure. For standard solutions with DIC concentrations ranging from 1 to 25 mmol . L(-1) and solution volume of 1 mL (high DIC concentration samples) or 5 mL (low DIC concentration samples), delta(13)C(DIC) values are determined with a precision (1sigma) better than 0.1 per thousand. Compared with previously published headspace equilibration methods, the major improvement presented here is the development of a calibration procedure which takes the carbon isotope fractionation associated with the CO(2(g))-CO(2(aq)) partition into account: the set of standard solutions and samples has to be prepared and analyzed with the same 'gas/liquid' and 'H(3)PO(4)/water' volume ratios. A set of natural water samples (lake, river and hydrothermal springs) was analyzed to demonstrate the utility of this new method.     

A portable automated system for trace gas sampling in the field and stable isotope analysis in the laboratory

A computer-controllable mobile system is presented which enables the automatic collection of 33 air samples in the field and the subsequent analysis for delta13C and delta18O stable isotope ratios of a carbon-containing trace gas in the laboratory, e.g. CO2, CO or CH4. The system includes a manifold gas source input for profile sampling and an infrared gas analyzer for in situ CO2 concentration measurements. Measurements of delta13C and delta18O of all 33 samples can run unattended and take less than six hours for CO2. Laboratory tests with three gases (compressed air with different pCO2 and stable isotope compositions) showed a measurement precision of 0.03 per thousand for delta13C and 0.02 per thousand for delta18O of CO2 (standard error (SE), n = 11). A field test of our system, in which 66 air samples were collected within a 24-hour period above grassland, showed a correlation of 0.99 (r2) between the inverse of pCO2 and delta13C of CO2. Storage of samples until analysis is possible for about 1 week; this can be an important factor for sampling in remote areas. A wider range of applications in the field is open with our system, since sampling and analysis of CO and CH4 for stable isotope composition is also possible. Samples of compressed air had a measurement precision (SE, n = 33) of 0.03 per thousand for delta13C and of 0.04 per thousand for delta18O on CO and of 0.07 per thousand for delta13C on CH4. Our system should therefore further facilitate research of trace gases in the context of the carbon cycle in the field, and opens many other possible applications with carbon- and possibly non-carbon-containing trace gases.     

二维气相色谱法分析天然气水合物区沉积物间隙水中示踪气体的浓度

利用微流路控制技术中心切割装置(Deans Switch)、两根色谱柱(PoraPLOT Q和Molsieve 5A)和3个检测器(脉冲氦离子化检测器、火焰光度检测器、热导检测器),建立了一种二维气相色谱分析系统,实现了海洋中多种示踪气体组分(氢气、甲烷、二氧化碳、硫化氢)的同时分析和精确测定。氢气、甲烷、二氧化碳、硫化氢的含量分别在2～1030、0.6～501、120～10500和0.2～49.1 μmol/mol范围内的校正曲线线性关系良好,检出限分别为0.51、0.17、82和0.08 μmol/mol,10次重复测定含量的相对标准偏差均小于10%。通过对南海天然气水合物区沉积物间隙水顶空气的测定,表明该方法方便、灵敏、可靠,易于实现海上现场测定;与以往采用多种分析方法分别测定示踪气体相比,大大节省了样品量。该方法适用于海洋天然气水合物、海底热液等资源的调查和海洋溶解态气体的研究等。     

Measurement of As,P, and S in the waste gases and water emitted from semiconductor processes by high-temperature hydrogen reduction gas chromatography

A quick, sensitive, and accurate method, high-temperature hydrogen reduction gas chromatography (GC) (1,2), for measuring arsenic (As), phosphorus (P), and sulfur (S) in the waste gases and water emitted from semiconductor processes is proposed in this paper. A high-temperature hydrogen reduction system that changes As, P, S, and their compounds into hydrides by atomic hydrogen has been designed. It is convenient to detect these elements in solid, liquid, and gaseous samples by high-temperature hydrogen reduction GC without pretreating samples. The lower detection limits of As, P, and S by this method are 0.01, 0.003, 0.02 mg/L, respectively, and the values of relative standard deviation are 6.2%, 8.6%, and 0.3%, respectively. Results determined by high-temperature hydrogen reduction GC are primarily accordant to those by conventional methods such as colorimetry and ion chromatography. The error statistics of this analysis method also show that high-temperature hydrogen reduction GC can be successfully used to determine trace As, P, and S in waste gases and wastewater emitted from semiconductor processes.     

气体同位素质谱与色谱结合分析天然气组成

建立了气体同位素质谱仪结合气相色谱测试天然气组成的新方法.气体同位素质谱仪能够解决色谱中热导检测器TCD分离非烃组分时,出现组合峰、个别峰不能实现基线分离及单个色谱峰有展宽的问题.通过不同方法测试了气体同位素质谱仪的稳定性,其相对标准偏差低于0.2%(n=6).将气体同位素质谱仪测得的非烃组分数据与色谱仪测得的烃类气体...