TODGA树脂小柱分离-多接收电感耦合等离子体质谱（MC-ICP-MS）法测定岩石样品中Nd同位素比值

通过改进岩石样品分析物Nd的化学分离,实现Nd同位素比值的准确分析,为研究青藏高原岩石成因,揭示物质来源提供技术支持。采用TODGA萃淋树脂分离基体及其与Nd相邻的稀土元素,多接收电感耦合等离子体质谱（MC-ICP-MS）法测定Nd同位素比值,建立了简捷实用的地质样品Nd同位素分析方法。样品HF-HNO3分解, HNO3(3 mol/L )- H3BO3(0.12 mol/L)提取,上柱后,先用6 mL HCl(2.8 mol/L)淋洗干扰轻稀土,再用6 mL HCl(2.2 mol/L)淋洗分析物Nd,Nd淋洗液由MC-ICP-MS测定其同位素比值。分析国际岩石标准物质BCR-2、BHVO-2和AGV-2,所得143Nd/144Nd同位素比值（平均值 ± 2σ）分别为0.512638 ± 0.0000007、0.512990 ± 0.0000012和0.512792 ± 0.000016,这些同位素数据在误差范围内,与推荐值和文献值完全一致。方法适合各种类型地质样品,为西藏不同地区不同岩石提供了可靠的Nd同位素分析数据。     

离子色谱法L-组氨酸/盐酸淋洗体系同时分离一价和二价阳离子

1前言 关于利用离子色谱分离技术测定一价和二价阳离子的工作,国内外已有报道。然而,由于二价阳离子对离子交换树脂的亲合力明显强于一价阳离子,使用单一组分淋洗液难于同时获得一价和二价阳离子的较好分离。国外有人采用DAP(2,3-二氨基丙酸)/HCI淋洗体系,配合其它分析技术,成功地同时分离了一价和二价阳离子。但其淋洗体系中使用的DAP试剂价格十分昂贵,难于在我国推广。本文提出用L-组氨酸/盐酸为淋洗的新淋洗体系用于一价和二价阳离子的分离。方法试用于多种样品的分析,得到满意的结果。 2实验部分     

土壤铵态氮中氮稳定同位素比值测定前处理方法优化研究

土壤氮素在土壤养分供给和植物生长发育中起着重要作用。利用氮稳定同位素自然丰度或富集标记技术,开展土壤氮循环转化、化肥利用效率和生物有效性等方面的研究,涉及NH4+-N稳定同位素比值的精准测定。本研究在前人基础上,开发了一种快速高通量的铵态氮蒸馏分离方法,并使用次氯酸盐替代了次溴酸盐优化了铵态氮化学转化条件,将转化效率由原方法的25%左右,提高至60%以上。利用新建立的前处理方法结合气体预浓缩装置与稳定同位素质谱仪（PreCon-IRMS）联用系统,分析了不同浓度条件下自然丰度、15N富集和标记的NH4+-N标准溶液中的氮稳定同位素比值。结果表明,新的反应体系下,当铵态氮浓度为0.5 μmol /mL以上时,所有NH4+-N标准样品均能获得较理想的分析精度,其中自然丰度和15N富集参比溶液的NH4+-N的δ15N的精度可控制在0.5‰以内,而15N标记的标准溶液的15N atom%测试精度为0.001~0.006 atom%（CV在0.1~0.3%之间）。所有NH4+-N标准样品的15N测定值与参考值一致,无分馏现象发生。将该方法应用于两种不同土地类型的旱地和稻田土壤浸提液中NH4+-N稳定同位素丰度的测定,也可获得较好的重现性（CV<0.5%）,与原方法测定结果基本一致,且精度更优。优化后的前处理方法操作简单,耗时短,重复性好,适用于土壤溶液铵态氮15N丰度测定的快速、批量前处理。     

利用锶特效树脂分离富集岩石样品中的锶及测定~(87)Sr/~(86)Sr

本研究以Sr-Spec树脂作为分离锶的特效树脂,以HNO3为淋洗液,通过改变HNO3的浓度,将地质岩石样品中的锶分离富集.实验结果表明,Sr与基质元素和Rb能很好地分离.利用Sr-Spec树脂分离国际标准物质SRM607、日本岩石标样JA-2、JB-2、JF-2和国家标准物质GBW04111后, 测得同位素比值87Sr/86Sr结果及误差(2σ)分别为1.200660±22, 0.706350±17, 0.703640±16, 0.709692±22和0.700008±23.相对于常规的阳离子树脂分离方法,此方法所用淋洗试剂量少,分离流程短,可以降低实验空白并提高工作效率.因此,Sr-Spec树脂分离法是快速分离富集不同岩性地质样品的Sr并测定87Sr/86Sr的有效方法.     

多接收器电感耦合等离子质谱精确测定钕同位素组成

报道了本实验室近两年来Neptune MC-ICP-MS测试Nd同位素的结果。测试结果显示样品化学分离中伴随的大量铈对钕同位素组成测定没有影响;而分离后残余少量钐,在一定范围内(钐/钕<0.04)可以直接扣除,获得准确的Nd同位素组成。Neptune MC-ICP-MS和热电离质谱(TIMS)平行测定实际地质样品表明,Neptune MC-ICP-MS可以精确测定Nd同位素组成,与经典的TIMS技术相比,MC-ICP-MS可以获得与TIMS相媲美的数据精度,而且分析时间缩短,效率明显提高。     

HEDTA-H_3Cit体系阳离子交换色层法分离镱和镥的研究

用N-羟乙基乙二胺-N,N′,N′-三乙酸(HEDTA)-柠檬酸(H3Cit)体系作淋洗剂,阳离子交换色层法分离Yb,Lu。通过红外光谱分析和电位滴定法确定Yb-HEDTA-H3Cit三元配合物的形成;研究室温条件下HEDTA-H3Cit体系淋洗剂对Yb,Lu分离的效果,通过ICP-AES测定洗脱液中稀土离子的浓度,绘制淋洗曲线,根据曲线中交叉区洗脱液体积占含稀土离子总洗脱液体积的比例衡量分离效果。结果表明,用HEDTA-H3Cit体系淋洗剂分离Yb,Lu,当HEDTA与H3Cit摩尔比为1∶1时,比HEDTA淋洗剂具有更好的分离效果和更短的淋洗周期。     

天然样品中锂的分离及其同位素比值的测定

以锂元素标准样品和K、Na、Ca、Mg元素标准样品的混合溶液为主要研究对象,采用阳离子交换树脂AG-50W X8(0.032~0.098 mm粒径)来分离富集L i,探索不同淋洗介质(包括盐酸、硝酸以及与甲醇、乙醇的混合)对L i分离纯化的最佳效果。在对比研究的基础上,建立了一种有效分离提纯天然样品中L i的方法。用本方法分离了水体、土壤、岩石等天然样品中的L i,并用MC-ICP-MS准确测定了L i同位素组成。研究结果表明,该方法的精度在0.1‰~1.0‰,与目前文献报道的分析方法具有相似的精度。经过流程前后单元素标准L i同位素比值(7δL i)的比较,发现化学处理过程所产生的同位素分馏约为0.3‰,化学处理的流程空白可以忽略不计。该方法测定海水7δL i值为(31.6±1.0)‰,与前人的分析结果吻合。因此,本方法可用于测定天然样品中的L i同位素组成。     

高效毛细管电泳分离/电导检测麻黄碱和伪麻黄碱

采用高效毛细管电泳电导检测法分离麻黄碱和伪麻黄碱，初步探讨了分离机理，建立了检测方法。以柠檬酸－柠檬酸钠为缓冲体系，铜盐为络合剂，在pH值为4．5、电压13.5kV的条件下，盐酸麻黄碱和伪麻黄碱得到了较好的分离，加入适量乙醇可改善峰形和分离效果。用该法以水杨酰胺为内标，对含盐酸麻黄碱和伪麻黄碱的实际样品进行检测，回收率为97.3%-101.1%，结果令人满意。     

离子色谱法测定电子烟烟液中氨的含量

建立了测定电子烟烟液中的氨含量离子色谱法。样品经10 mol·L-1盐酸溶液萃取10 min后,采用Dionex Ion Pac CS16A阳离子交换柱分离,以MSA为淋洗液进梯度洗脱,用电化学检测器检测。氨的质量浓度在0.05~1.0 mg·L-1范围内与峰面积呈线性关系,检出限(3S/N)为0.035μg·g-1,测定下限(10S/N)为0.12μg·g-1。方法用于12种市售品牌电子烟烟液中氨的测定,加标回收率在93.2%~106%之间,测定值的相对标准偏差(n=5)小于4%。     

微量黄铁矿单矿物中痕量碲、铊、钴、镍的分离及碲、钴的动力学法测定

本文研究用732型阳离子交换树脂,一次上柱后,以盐酸、丙酮混合淋洗剂定量分离毫微克量碲、铊、钴和镍,同时,干扰元素在淋洗中也被分离。用微型交换柱,淋洗剂量少,盐酸和丙酮易提纯,降低了测试本底;本装置可避免丙酮挥发。试验了钴-钛铁试剂-过氧化氢催化体系测定钴的条件,特别是使催化反应稳定,手续简便。对诱导法测碲的条件作了适当改变,使灵敏度提高。     

镁离子存在下乙醇-水混合溶液中碳酸钙结晶行为的研究

通过对不同反应体系中合成样品的物相及镁含量变化规律的分析, 认为水溶液中碳酸钙的结晶遵循溶解重结晶机理, 乙醇-水溶液中则以聚集重构为主, 碳酸根阴离子的溶剂化作用对碳酸钙的沉积产生显著影响. 采用XRD, IR等手段对醇水混合溶液中合成的碳酸钙样品进行分析, 认为形成了含镁方解石及具有类白云石结构的过渡相同时存在的混合物相, 醇水溶液中含镁方解石趋于白云石化.     

A direct method for the determination of carbonate and non-carbonate carbon in geological materials by infrared spectrometry

A simple and direct infrared method for determining carbonate and non-carbonate carbon in geological samples is described. To determine carbonate carbon, hydrochloric acid is added directly to the heated samples; non-carbonate carbon is determined by combustion after digesting the samples with hydrochloric acid. The limit of detection is 2 ppm for carbonate carbon and 10 ppm for non-carbonate carbon; the relative standard deviations are 4% or less for 100–1000 μg of carbonate and non-carbonate carbon. The method has been applied to standard rocks, NBS minerals and geological exploration reference samples.     

New evidence from stable isotope for the uplift of mountains in northern edge of the Qinghai-Tibetan Plateau

New data of oxygen and carbonate isotope in calcite cements from Cenozoic rocks inthe Jianggelesayi area to reconstruct the uplift history of mountains in northern edge of the Qing-hai-Tibetan Plateau are presented. Analyses results show that rapid changes of δ~(18)O and δ~(13)C inthe calcite cement occurred in both the Early Oligocene and Early Miocene. Studies on sedimen-tary features indicate that a rapid up-coarsing of the sediments size occurred in the Early Miocene,and sedimentary velocity increased rapidly during the Pliocene and Early Quaternary. Thus, it issuggested that the uplift of mountains in the northern edge of the Qinghai-Tibetan Plateau initiatedfrom the Early Oligocene, and a rapid uplift occurred in the early stage of the Miocene, while thesharp difference in topography between the northern plateau and the Tarim Basin predominatelyformed later than the Miocene.     

New evidence from stable isotope for the uplift of mountains in northern edge of the Qinghai-Tibetan Plateau

New data of oxygen and carbonate isotope in calcite cements from Cenozoic rocks in the Jianggelesayi area to reconstruct the uplift history of mountains in northern edge of the Qing-hai-Tibetan Plateau are presented. Analyses results show that rapid changes of δ¹⁸O and δ¹³C in the calcite cement occurred in both the Early Oligocene and Early Miocene. Studies on sedimentary features indicate that a rapid up-coarsing of the sediments size occurred in the Early Miocene, and sedimentary velocity increased rapidly during the Pliocene and Early Quaternary. Thus, it is suggested that the uplift of mountains in the northern edge of the Qinghai-Tibetan Plateau initiated from the Early Oligocene, and a rapid uplift occurred in the early stage of the Miocene, while the sharp difference in topography between the northern plateau and the Tarim Basin predominately formed later than the Miocene.

     

Sequential and rapid determination of Po-210, Bi-210 and Pb-210 in natural waters

A sequential and rapid separation method for the determination of radon daughter nuclides, Pb-210, Bi-210 and Po-210 has been developed for application to natural waters. Rapid separation is attained by the use of the same hydrochloric acid solution. After isolation of the three radionuclides from the sample by co-precipitation with added Fe³⁺, polonium isotopes are first spontaneously deposited onto a silver disc from a 0.5N hydrochloric acid solution. Next, bismuth isotopes are electrodeposited onto a platinum net cathode coupled with a platinum coil anode at 1.2 V. Finally, lead isotopes are electrodeposited onto a platinum net cathode at 1.8 V from the remaining solution by adding hydroxylamine hydrochloride as an anodic depolarizer. This method can be applied to meteorological precipitation samples where these three nuclides are separated within 10 hr after the sampling with chemical yields of more than 80% for Po-210 and Bi-210 and more than 70% for Pb-210. This method is applicable to other environmental water samples.     

Crystal growth of aragonite and calcite in presence of citric acid, DTPA, EDTA and pyromellitic acid

The influence of four calcium complexing substances, i.e., citric acid (CIT), diethylenetriaminepentaacetic acid (DTPA), ethylenediaminetetraacetic acid (EDTA) and pyromellitic acid (PMA), on the crystal growth rate of the calcium carbonate polymorphs aragonite and calcite has been studied. Using a seeded constant supersaturation method supersaturation was maintained at 4 by keeping a constant pH of 8.5 through addition of sodium carbonate and calcium chloride solutions. The unique composition of each solution was calculated using chemical speciation. The growth rate was interpreted in terms of an overall growth rate. For both calcite and aragonite, the crystal growth rate is significantly reduced in the presence of the calcium complexing substances. The growth retarding effect depends on both the concentration and the polymorph. The relative crystal growth rate was correlated to the total complexing agent concentration using a Langmuir adsorption approach. Aragonite appeared fully covered for lower total concentrations than calcite. Furthermore, CIT very efficiently blocked aragonite growth contrary to what was observed for calcite. This is thought to be related to certain distinct features of the dominant aragonite crystal faces compared to the dominant calcite faces.     

Determination of calcium in biological material The use of calcein as an indicator in the edta titration

The EDTA titration of calcium using the change in fluorescence of Calcein indicator under ultraviolet illumination at the end-point was very satisfactory for essentially pure calcium chloride solutions. In order to use this method for biological samples, it was found best to separate the calcium by an oxalate precipitation at a pH of 4.7, convert the calcium oxalate to calcium carbonate, and dissolve the calcium carbonate in hydrochloric acid.     

From synthetic to biogenic Mg-containing calcites: a comparative study using FTIR microspectroscopy

The formation mechanism of the thermodynamically unstable calcite phase, very high Mg calcite, in biological organisms such as sea urchin or corallina algae has been an enigma for a very long time. In contrast to conventional methods such as KBr pellet Fourier Transform infrared (FTIR) spectroscopy and X-ray diffraction (XRD), FTIR microspectroscopy (FTIRM) provides additional information about a local disorder such as an amorphous phase or the occlusion of Mg ions in the calcite lattice. In this work, we characterise for the first time systematically synthetic and biogenic Mg-containing calcium carbonate samples (especially sea urchin teeth--SUT) in detail by using two FTIRM instruments and compare these samples with KBr pellet FTIR measurements. Furthermore, we present spectra from geogenic calcite and dolomite minerals, recorded with both FTIRM systems, as well as KBr pellet FTIR spectra as references. We analyse the spectra by applying multi-peak curve fitting on the in-plane-bending (ν(4)) and out-of-plane (ν(2)) bands. Based on the obtained results we attribute the two singlet bands at ～860-865 cm(-1) and ～695-704 cm(-1) observed in the SUT FTIRM spectra to the existence of amorphous calcium carbonate (ACC), and report for the first time the existence of ACC at the mature end of SUT. In the other three studied biominerals, however, we did not find any ACC. Also, based on the FTIRM results, we observe that not only ν(4), but also ν(2) shifts to higher wavenumbers if more calcium ions are replaced by magnesium ions in the calcite lattices.     

Influence of citric acid as chemical modifier for lead determination in dietary calcium supplement samples by graphite furnace atomic absorption spectrometry

Citric acid was used as a chemical modifier for Pb determination by graphite furnace atomic absorption spectrometry in dietary supplement samples (calcium carbonate, dolomite and oyster shell samples) and its efficiency was compared to the use of palladium. Pyrolysis and atomization curves were established without use of chemical modifier, with the addition of 20, 100 and 200 μg of citric acid, and with 3 μg of palladium. The citric acid modifier made possible the interference-free Pb determination in the presence of high concentrations of Ca and Mg nitrates. Acid sample digestion involving closed vessels (microwave-assisted and conventional heating) and acid attack using polypropylene vessels at room temperature were compared. All digestion procedures presented similar results for calcium carbonate and dolomite samples. However, for oyster shell samples accurate results were obtained only with the use of closed vessel systems. Analyte addition and matrix-matched standards were used for calibration. The characteristic mass for Pb using citric acid and palladium were 16 and 25 pg, respectively. The relative standard deviation (RSD) was always less than 5% when citric acid was used. The relative and absolute limits of detection were 0.02 μg g^− 1 and 8 pg with citric acid and 0.1 μg g^− 1 and 44 pg with the Pd modifier, respectively (n = 10, 3σ). The recovery of Pb in spiked calcium supplement samples (10 μg l^− 1) was between 98% and 105%. With the use of 100 μg of citric acid as chemical modifier, problems such as high background absorption and high RSD values were minimized in comparison to the addition of 3 μg of palladium.     

聚乙烯-双硫腙复膜树脂分离富集/原子吸收法测定地质样品中的痕量金

研究了聚乙烯双硫腙复膜树脂的合成及其分离富集痕量金的条件。于pH为2.0的HCl介质中,金离子被定量吸附在聚乙烯双硫腙复膜树脂上,并可用5%硫脲-0.1 mol/LHCl溶液洗脱,洗脱液用火焰原子吸收光谱法测定,金的回收率在91.5%~99.7%之间。本法可用于地质样品中痕量金的分离富集与测定。