碱熔-标准物质法-电感耦合等离子体发射光谱(ICP-AES)法测定硅酸盐岩中10种主量元素

硅酸盐岩元素的准确测定是其地球化学分析研究的基础,其主量元素含量通常可以采用电感耦合等离子体发射光谱(ICP-AES)法测定,但其测定方法的系统性研究相对缺乏,尤其是样品前处理和基体干扰的有效消除两方面。前处理过程中,考察不同熔剂用量对硅酸盐岩样品的分解能力,发现当熔剂与样品比例达到6:1后,熔珠为纯色透明,经稀硝酸提取后溶液澄清,确定了硅酸盐岩前处理时熔剂与样品的最佳配比。测定过程中,通过考察基体匹配法和标准物质法两种基体干扰消除方法对测定结果的影响,发现当采用与岩性一致或者接近的标准物质绘制校准工作曲线时,基体干扰消除效果更好,更适用于测定硅酸盐岩10种主量元素含量。据此,建立了硅酸盐岩经偏硼酸锂熔融,稀硝酸振荡提取处理,以标准物质法绘制校准工作曲线,采用ICP-AES法同时测定SiO2、Fe2O3、Al2O3、CaO、K2O、MgO、Na2O、TiO2、P2O5、MnO 10种成分含量的方法。对岩石标准物质GBW07107进行分析测定,方法的相对标准偏差(RSD)为0.17%～0.75%,方法检出限为0.001%~0.016%,满足硅酸盐岩样品元素定量分析的要求,而且操作简单快速,环境污染小,适用于大批量样品分析。     

Direct ICP-MS determination of trace and ultratrace elements in geological materials after decomposition in a microwave oven. Part II. Quantitation of Ba, Cs, Ga, Hf, In, Mo, Nb, Pb, Rb, Sn, Sr, Ta and Tl

A new method has been developed for the rapid determination of traces of Ba, Cs, Ga, Hf, In, Mo, Nb, Pb, Rb, Sn, Sr, Ta and Tl in silicate rocks and lake, stream and river sediments. The method involved dissolution of samples in a microwave oven by heating in a pressure decomposition Teflon vessel with a mixture of HF + HNO₃ + HCl + H₃BO₃ + EDTA followed by direct multielement determination using inductively coupled plasma-mass spectrometry (ICP/MS). The method is faster than conventional dissolution of samples by open vessel acid digestion and fusion and determination by instrumental methods. The accuracy and precision of the developed method were tested by replicate analyses of a number of international geochemical reference samples of established trace element contents. Satisfactory correlation with the “recommended” or “consensus” values was found and recoveries were in most cases 95–100%. New values for Ga, In, Nb and Tl in several international geochemical reference materials are first reported in this paper.     

The separation of platinum, palladium and gold from silicate rocks by the anion exchange separation of chloro complexes after a sodium peroxide fusion: an investigation of low recoveries

A series of experiments was undertaken to measure the recovery efficiency of platinum, palladium and gold from silicate rocks using a sodium peroxide fusion followed by anion exchange separation of the analytes as chloro complexes. Results obtained by graphite furnace atomic absorption spectrometric analysis of standard solutions prepared in dilute HCl or HCl-acidified sodium peroxide solution showed that recoveries were near quantitative. However, when standard solutions were added to an alkaline sodium peroxide solution, which was then acidified, low results were obtained for platinum and gold (46% and 76% respectively). Low and variable results were also obtained when standard solutions were added to a peridotite sample that had been dissolved by the state procedure, and in the analysis of the South African Bureau of Standards certified reference material, SARM 7. Various experiments were undertaken to investigate these low recoveries, but the reason proposed here is the formation of hydroxychloro compounds in alkaline solution which are not, on acidification with HCl, converted quantitatively to the chloro complex necessary for quantitative anion exchange separation. It is concluded that a sodium peroxide fusion followed by an anion-exchange separation does not appear to form the basis of a successful technique for the determination of platinum, palladium and gold in silicate rocks.     

Determination of nickel in standard rocks and glasses by photon activation analysis with 30-MeV bremsstrahlung

The determination of nickel in various silicate rocks and glasses by photon activation analysis with a linear electron accelerator is described. Simultaneous irradiation of the sample and comparative standards produces the ⁵⁸Ni(γ, n)⁵⁷Ni reaction, and a post-irradiation chemical separation is used in conjunction with Ge(Li) γ-spectrometry. Nickel abundances for ten standard silicate rocks and two elementally doped glasses are presented and compared with the data previously published. The method is quite simple and gives good reproducible results for nickel down to sub-p.p.m. levels.     

Simultaneous determination of fluorine and chlorine in silicate rocks by a rapid spectrophotometric method

A rapid accuiate method is described for simultaneous determination of fluorine and chlorine in silicate rocks by taking, separate aliquots of the single sample dissolution. Fluorine, without separation, was determined by means of the zirconium-criochrome cyanine R complex, whereas chlorine was determined by means of the stable iron (III) thiocyanate complex. The mctliod was tested with standard rocks. Results with geochemical standards were comparable with analyses reported by others. Application to several acidic, mafic, and ultramafic rock samples, gave results with a relative standard deviation of less than 5 %.     

Determination of Copper in Silicates Using Chelating Resin After Decomposition With Teflon Vessel

Abstract

By the combined use of a decomposition vessel, chelating resin, and atomic absorption spectrometry, a simple method for the determination of copper in silicate rocks was devised. A sample was digested overnight at room temperature with small amounts of hydrofluoric acid and aqua regia in the Teflon vessel having a sealing stopper. In the presence of citrate, only the supernatant of the digested sample solution was passed through a small column of the chelating resin, Dowex A-1, at pH 4. After elution with nitric acid, copper was determined by ordinary atomic absorption spectrometry. The recovery, reproducibility, and accuracy of the method were quite satisfactory. The analytical results obtained for the standard rocks agreed well with reported results.     

PVC matrix membrane electrodes based on cobalt and nickel phenanthroline complexes for selective determination of cobalt(II) and nickel(II) ions

Potentiometric sensors for determining cobalt and nickel ions are described. They are based on the use of cobalt and nickel tris(1,10-phenanthroline)-TPB as electroactive compounds dispersed in plasticized poly(vinyl chloride) matrix. The sensors exhibit fast, near-Nernstian responses for cobalt and nickel-phenanthroline cations over the pH range 3–11 with a slope of 30.3 ± 0.3 mV/concentration decade. In the presence of excess 1,10-phenanthroline reagent, cobalt(II) and nickel(II) ions at concentration levels as low as 4 × 10^–6 M are accurately determined. The results show an average metal ion recovery of 98.5% with a mean standard deviation of 0.5%. Cobalt in organometallic compounds and nickel in silicate rocks are determined by these sensors and results agreeing fairly well with atomic absorption spectrometry are obtained.     

Practical aspects of neutron activation determination of the platinum metals

Triple gamma coincidence counting of¹⁹²Ir allowed the determination of Ir by instrumental neutron activation analysis down to 1 ppb in ultrabasic rocks and down to ca. 20 ppb in some high-furnace slags; the limiting factor for the latter matrix was the presence of¹²⁴Sb. Radiochemical neutron activation analysis of the USGS standard rocks revealed that the Ir contents are up to three orders of magnitude lower than previously reported, except for the ultrabasic rocks. The factor of merit of several scintillation and semiconductor, gamma-ray detectors was determined for the neutron activation determination of Pd, Pt and Os. In the case of radiochemically pure sources, a NaI(Tl) wafer was preferred; in the presence of high-energy gamma-emitters, a Ge(Li) low-energy photon detector was superior.     

Quantitative Determination of Iron and Aluminium in Some Alloys and Silicate Rocks After a Cation Exchange Separation on Zirconium(IV) Phospho and Silico Arsenates

Abstract

A rapid and quantitative method has been developed for the analysis of some iron and aluminium based alloys and silicate rocks using zirconium(IV) based arsenophosphate and arsenosilicate cation exchangers. The method is simple, reproducible and precise with a standard deviation <3%, for the direct determination of iron and aluminium in rocks and alloys. The low standard deviation values suggest that the method should be useful for the standardization purposes.     

Interference-free determination of thallium in aqua regia leaches from rocks, soils and sediments by D(2)-ETAAS method using mixed palladium-citric acid-lithium chemical modifier

The mixture of palladium (chloride) with citric acid and lithium is proposed as a new chemical modifier for the elimination of interference occurred during the determination of Tl in aqua regia extracts from rocks, soils and sediments by electrothermal atomic absorption spectrometry using instrumentation with deuterium-lamp background correction (D₂-ETAAS). Palladium was preferred to rhodium and platinum as to analyte stabilization, citric acid served as an effective reducing agent facilitating formation of Pd-Tl stable covalent bonds playing an important role in the analyte stabilization. Citric acid in addition helps to remove most of interfering chloride at low temperature. The further addition of Li increased significantly the robustness of chemical modifier against strongly interfering ZnCl₂ matrix by binding free chlorine into a more stable LiCl molecule. In the presence of the proposed chemical modifier the temperature for the final step of pyrolysis was adjustable up to 1000 °C, without any noticeable loss of volatile Tl species and the interference of the rest chloride matrix was significantly reduced. The application of the modifier to direct determination of Tl in aqua regia extracts from rocks, soils and sediments has ensured the characteristic mass and LOD value for the original sample 13 pg and 0.043 μg g⁻¹, respectively (10-μL aliquots of sample) and has enabled the use of matrix-free standard solutions for attaining accurate analysis. The accuracy was verified by the analysis of certified reference samples and by the comparison of results with those found by an inductively coupled plasma orthogonal acceleration time-of-flight mass spectrometer (ICP-oa-TOFMS) method.     

Optimization of silicate rock decomposition for determination of major elements by atomic-absorption spectrophotometry

A rapid method for sample decomposition of silicate rocks and further accurate determination of major elements by atomic-absorption spectrometry is described. The solutions obtained were stabilized so that the measurements were comparable with those made on standard rocks solutions. Interferences were avoided. The most important methods of silicate rock decomposition were applied, and the useful characteristics from each were combined, and in some cases improved, to obtain the final procedure.     

Determination of Mercury and Thallium in Seawater by Electrothermal Vaporization Inductively Coupled Plasma Mass Spectrometry

Electrothermal vaporization inductively coupled plasma mass spectrometry (ETV‐ICP‐MS) has been applied to the determination of Hg and Tl in seawater samples. Various modifiers were tested for the best signal of these elements. After preliminary studies, 0.3% EDTA, 0.1%m/vTAC and 1% v/v HCl were added to the sample solution to work as the modifier. Since the sensitivities of Hg and Tl in various seawater matrices and aqueous standard solutions were quite different, standard addition method and isotope dilution method were used for the determination of Hg and Tl in these seawater samples. This method was applied to the determination of Hg and Tl in NASS‐4 and CASS‐3 reference seawater samples and seawater samples collected from the Kaohsiung area. Results obtained by isotope dilution method and method of standard additions agreed satisfactorily. Detection limits were in the range of 5‐15 and 0.4‐0.5 ng l^?1 for Hg and Tl in seawater, respectively, with the ETV‐ICP‐MS method. The precision between sample replicates was better than 18%) for all the determinations.     

Determination of gallium in geological materials by graphite-furnace atomic-absorption spectrometry

A graphite-furnace atomic-absorption spectrometric method has been worked out for the determination of traces of gallium in silicate rocks and minerals. The samples are opened up by fusion with a lithium carbonate-boric acid mixture and the cake is taken up with 2M nitric acid. Addition of nickel nitrate to this solution elminates the severe matrix effects allowing gallium solutions in nitric acid to be used as calibration standards. No separations are necessary. Results are quoted for 14 standard silicate rocks and two minerals. The RSD is 2.9%, and the sensitivity is 27 pg of gallium for 1% absorption.     

Kinetic spectrophotometric determination of iron oxidation states in geological materials

Summary A kinetic spectrophotometric approach is applied to the determination of iron oxidation states in geological materials. Silicate rock samples were sealed in a Teflon vial under argon atmosphere and were decomposed with a mixture of hydrofluoric acid and sulphuric acid by the microwave digestion technique. The absorbance of iron(III)-Tiron complex was followed at 560 nm and the absorbance/time relation was analyzed by non-linear least squares fitting. The FeO and Fe₂O₃ determinations in silicate rocks by the proposed kinetic method agree with those done by the static o-phenanthroline method. The analytical results for standard igneous rock samples are compared with published data.     

Flow-injection analysis of silicate rocks for total iron and aluminium

A flow-injection method is described for the spectrophotometric determination of total iron and aluminium in silicate rocks. Rock samples are opened up by fusion with a mixture of lithium carbonate and boric acid, the melt is taken up in 1M hydrochloric acid and the resulting solution is used for the determination of both iron and aluminium. The flow system for the determination of iron needs no particular reagents, involving simply measurement of the absorbance of the chloro-complex of iron(III) at 335 nm. The system for aluminium consists of the reduction of iron(III) to iron(II), colour development with Xylenol Orange (XO), destruction of XO-chelates other than that of aluminium by addition of EDTA and subsequent measurement of the absorbance of the aluminium-XO complex at 506 nm. The systems permit semi-automatic, rapid analysis of silicate rocks for iron and aluminium. Results obtained for standard rocks were in good agreement with the recommended values. The precision ranged from 0.1 to 0.9% for iron and from 0.3 to 0.7% for aluminium.     

The determination of some elements in rocks by instrumental photon activation analysis

This text describes the instrumental determination of some elements in silicate samples of ≃1 g by photon activation. The following elements can be determined: In acidic rocks: Mg, Ca, Ti, Mn, Sr, Zr and Nb, in ultramafic rocks: Mg, Cr, Ni, and Mn. The relative standard deviation is a few percent.     

Use of a large quartz spectrograph for the determination of thorium, yttrium and the rare earths in silicates

Studies were carried out on the optimum conditions for the successful use of a large quartz spectrograph for the determination of thorium, yttrium and the rare earths in silicate rocks. The best line-to-background ratios were achieved by arcing samples in a matrix of 4 % sodium chloride in carbon powder. An atmosphere of 20 % argon and 80% oxygen was used to reduce background and eliminate cyanogen band interference. An anion-exchange procedure was used to separate the rare earths from other elements. The resultant enrichment allowed use to be made of less sensitive rare earth lines in the ultraviolet end of the spectrum where the spectrographic dispersion is greater. Line interferences were studied and necessary corrections for these interferences were calculated. The technique was tested by analysing the standard rocks, G-1, W-1 and CAAS syenite. Good agreement with recommended values was obtained.     

3,4-Dihydroxybenzoic Acid As A Reagent for the Spectrophotometric Determination of Titanium

Abstract

The reaction between titanium(IV) and 3,4-dihydroxybenzoic acid in aqueous media results in an intensely colored complex which is stable for at least 8h. It allows the spectrophotometric determination of titanium in silicate rocks. The proposed method, in pH 4.0–6.0, shows a molar absorptivity of 1.43.10⁴ L.mole^?1.cm^?1 at 380 nm. Beer's Law is obeyed up to 3.0 μg/mL of titanium(IV). The interference of iron(III) can be eliminated by reduction to iron(II) with hydroxylamine hydrochloride. The method was applied to the determination of titanium in various standard rocks and the results indicated that the accuracy and precision are satisfatory.     

Spurenbestimmung von Thallium in Gesteinen durch Flammen oder flammenlose Atomabsorptions-Spektralphotometrie nach Vorkonzentrierung durch Extraktion

Zusammenfassung Die beschriebene Methode für die Bestimmung von Tl in Zement und dessen Ausgangsmaterialien eignet sich auch für die Spurenbestimmung in Gesteinen, Lösungen, usw. Spuren von Tl können aus großen Gehalten von Ca oder Fe durch Maskieren der Fremdelemente in mineralsaurer Lösung mit großen Mengen Citronensäure, Ascorbinsäure, wenn nötig auch mit KCN, und Extrahieren bzw. Konzentrieren des Tl als Diethyldithiocarbaminat-Komplex mit kleinen Mengen Methylisobutylketon bei pH 10,5 abgetrennt werden. Tl⁺ und auch Tl³⁺ werden erfaßt. Der Methylisobutylketon-Extrakt kann direkt in die Flamme eingesprüht werden. Die Empfindlichkeit ist in Methylisobutylketon-Lösung etwa um 30% besser als in rein wäßriger Lösung. Ein Zusatz von Cd, welches unter den gegebenen Bedingungen ebenfalls mitextrahiert wird, verbessert die Empfindlichkeit durch Interferenzeffekt nochmals um weitere 30 %. Wird eine Proben-Einwaage von 1 g zur Extraktion verwendet, so kann noch 0,1 ppm Tl im Ausgangsmaterial nachgewiesen werden. 60 untersuchte Kationen und etwa 20 Anionen stören in weiten Grenzen nicht. Mit der flammenlosen Atomisierung im Graphitrohrofen können noch 20–100mal kleinere Mengen Tl bestimmt werden, wenn das Tl im Methylisobutyl-Extrakt mit HNO₃ in die Nitratform gebracht und mit Alkohol verdünnt wird. Die Methoden wurden mit Standardgesteinen und Zementproben mit zugesetztem Tl überprüft.

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Trace determination of thallium in rocks by flame or flameless atomic absorption spectrophotometry following pre-concentration by extraction

Summary A sensitive method for the trace analysis of Tl in cement raw materials, rocks and other samples by AAS is described. To the aqueous sample solutions, containing mainly Ca or Fe, large amounts of citric and ascorbic acid were added for masking interfering cations. Tl is extracted and concentrated as the diethyldithiocarbamate complex in methyl-isobutylketone at pH 10.5. This extract can directly be injected into the flame. The sensitivity was found to be 30% higher than for aqueous solutions and can be enhanced by another 30% by addition of some Cd. For a 1 g-sample the sensitivity is about 0.1 ppm Tl. Some 60 cations and 20 anions may be present in rather large amounts without disturbing the Tl-determination. A procedure for the flameless AAS is also described leading to a 20–100 times higher sensitivity. The methods were tested with standard rocks and with cement samples to which defined amounts of Tl had been added.

Für die Überprüfung des Manuskriptes möchte ich den Herren Dr. P. Baertschi und O. Antonsen herzlich danken.     

Chemical Analyses of Canadian Reference Samples: SY-2 and SY-3

Abstract

Chemical analyses of the major and some of the minor constituents are reported for two new Canadian silicate rock standards recently introduced by the Department of Energy, Mines and Resources. To date quantitative chemical analyses have not yet been reported for these samples. The compositions of these rocks offer a useful range of values that are not currently covered by existing silicate rock standards.