Determination of phosphorus in waste-waters by inductively-coupled plasma atomic emission spectrometry

Inductively coupled plasma—atomic emission spectrometry offers a simple and rapid method for the determination of total phosphorus in waste-waters: the optimum operating conditions are described. The detection limits are 0.02, 0.04, and 0.11 μg ml^-1 at the 213.618, 214.914, and 253.565-nm lines, respectively. Interferences by other elements are negligible at the concentration levels of these elements in environmental and waste-waters, except for the spectral interference of copper on the lines at 213.618 and 214.914 nm. Differences in emission response for various inorganic and organic phosphorus compounds are small. Analytical results for phosphorus in municipal and industrial waste-waters agree well with those obtained by standard methods.     

The preparation of iron-free solutions from geological materials for the determination of boron (and other elements) by inductively-coupled plasma emission spectrometry

A procedure based on successive fusions with potassium dihydrogenphosphate and potassium hydroxide is described which yields an iron-free solution for the determination of boron in a wide variety of geological matrices. Data obtained for boron and other trace elements in geological reference materials are presented.     

Determination of traces of boron in semiconductor amorphous silicon film by filament-vaporization inductively-coupled plasma/atomic emission spectrometry

Silicon is dissolved from the platinum substrate by nitric/hydrofluoric acids. The recovery of boron on direct analysis was poor, but was increased to >95% by the addition of 500–5000 μg ml^?1 phosphorus as phosphoric acid. The results compared well with the molar ratio of the gases (B₂H₆/(Ar + H₂) used to form the film and the intensity ratio of ¹¹B⁺ and ³⁰Si⁺ obtained by secondary-ion mass spectrometry.     

Determination of trace elements in sea water by inductively-coupled plasma emission spectrometry

Pb, Zn, Cd, Ni, Mn, Fe, V and Cu in sea water are determined by extraction of their complexes with sodium diethyldithiocarbamate into chloroform, decomposition of the chelates and inductively-coupled plasma emission spectrometry. When 1-l water samples are used, the lowest determinable concentrations are: 0.063 μg Mn l^-1, 0.13 μg Zn l^-1, 0.25 μg Cd l^-1, 0.25 μg Fe l^-1, 0.38 μg V l^-1, 0.5 μg Ni l^-1, 0.5 μg Cu l^-1, and 2.5 μg Pb l^-1. Above these levels, the relative standard deviations are better than 12% for the complete procedure.     

Determination of the rare-earth elements in geological materials by thin-film X-ray fluorescence and inductively-coupled plasma atomic-emission spectrometry

Thin-film XRF and ICP-AES analytical procedures for the determination of the rare-earth elements (REE) in rocks, involving preconcentration by ion-exchange and co-precipitation with Fe(OH)(3) for thin-film preparation, and matrix modification, are described. The REE in five international reference rocks have been determined, with correction for spectral line overlap whenever necessary. The results obtained by using X-ray fluorescence spectrometry compare well with those of inductively-coupled plasma atomic-emission spectrometry, and with other values reported in the literature.     

Simultaneous determination of boron,phosphorus and sulphur in some biological and soil materials by inductively-coupled plasma emission spectrometry

Atomic emission lines at 249.678 nm, 214.911 nm and 180.735 nm are used simultaneously to determine total concentrations of boron, phosphorus and sulphur respectively, in plant and soil sample digests by means of inductively-coupled plasma emission spectrometry. The digestion procedures chosen enable these elements to be determined simultaneously on a single digest. Analytical data are compared after using various digestion procedures on standard reference materials. Actual and potential interelement interferences in the plasma are discussed together with attempts to overcome these interferences. Limitations for simultaneous determinations of boron, phosphorus and sulphur remain in the digestion and dissolution procedures.     

Determination of traces of zirconium in silicate rocks by inductively-coupled plasma emission spectrometry

The sample is fused with a mixture of sodium and potassium carbonates. Zirconium is separated from the large amounts of sodium and potassium by precipitation of hydrated oxides before nebulization. The detection limit is 0.32 μg Zr g^-1. Results for seven standard rocks are in accord with recommended values.     

Determination of sulfur in biological samples by vacuum-ultraviolet inductively-coupled plasma atomic emission spectrometry

Sulfur is most sensitively determined at 180.7 nm, the detection limit being 10 μg l^?1. A comparison of digestion procedures shows that acid digestion in a teflon bomb gives least loss of analyte. Only calcium interferes spectrally at this wavelength. Results for various reference materials are presented.     

Determination of rare earths in lanthanum oxide by inductively-coupled plasma emission derivative spectrometry

Rare-earth elements (REE) at ppm levels in lanthanum oxide can be determined without prior separation and preconcentration by use of high-resolution inductively-coupled plasma emission derivative spectrometry (ICPEDS). The calibration graphs are all linear and pass through the origin, even in the presence of large amounts of lanthanum, except those for dysprosium, holmium and ytterbium. The detection limit for each REE is 1-10 mug g in lanthanum oxide. Investigation of various physical and/or spectral interferences shows that good selectivity is obtained by ICPEDS.     

Determination of minor and trace elements in silicate rocks by inductively-coupled plasma emission spectrometry

Samples (0.5 g) are decomposed with mixed acids in a sealed teflon vessel. After suitable treatment, barium, cobalt, chromium, copper, lithium, nickel, scandium. strontium, vanadium and zirconium are determined sequentially. The method is satisfactory for a variety of standard silicate materials.     

Characterization of noise in inductively-coupled plasma emission spectrometry

The nebulizing process in inductively-coupled plasma emission spectrometry is a major source of the instrumental variability; an attempt has been made to isolate this source so that its influence on the final result could be evaluated. Direct measurements of the time-dependent variations of the sample supply to the plasma were achieved by using a device based on the light-scattering property of nebulized test solutions. The noise from the nebulizer and of the emission signal was characterized by autocovariance functions and power spectral densities. The types of noise observed showed f^{-$\text{1}\text{2}$} and f^{-$\text{1}\text{4}$} character, depending on the concentration of the test elements employed. Cross-covariance revealed a strong correlation between the noise sources considered. The applicability and limitations of possible correction and electronic filtering procedures are indicated.     

Determination of cadmium by suction-flow liquid-liquid extraction combined with inductively-coupled plasma atomic emission spectrometry

The flow manifold described permits suction-flow liquid-liquid extraction of cadmium in a discrete aqueous sample as its diethyldithiocarbamate into carbon tetrachloride. The organic extract is fed into the nebulizer of an inductively-coupled plasma atomic emission spectrometer by a peristatic pump. An increase in sensitivity of ca. 250-fold is achieved in comparison with direct aspiration of the aqueous solution. The sampling frequency is 20 h^?1 and the consumption of carbon tetrachloride and 5% (w/v) sodium diethyldithiocarbamate solution are each 0.6 ml min^?1. The 3σ detection limit is 0.4 ng ml^?1 cadmium, and the calibration is linear up to 300 ng ml^?1. The relative standard deviation for 10 replicate measurements is 1.5% for 50 ng ml^?1 cadmium. The flow interferences observed can be decreased or eliminated by the addition of citrate to the buffer solution. Results of analysis of some certified biological reference materials are given.     

Determination of boron,beryllium and lithium in coal ash and geological materials by spark optical emission spectrometry

A method is described for the accurate and precise determination of boron, beryllium and lithium in coal ash and geological materials by a point-to-plane high-voltage spark optical emission spectrometric technique. A 200-mg sample is crushed and blended with graphite, copper oxide internal standard and cellulose powders, and briquetted. Synthetic calibration standards are prepared from spectrographically pure materials blended into graphite. Corrections are made for spectral interference by iron and silicon on boron. Accurate results are presented for certified reference materials. The precision of the method, about 5%, is superior to that obtained by d.c. arc optical emission.     

Determination of rare earth elements in geological samples by inductively-coupled plasma atomic emission spectrometry after oxalate coprecipitation and cation-exchange column separation

A method for separation and determination of traces of 14 rare earth elements (REEs) in geological samples is described. Determination by inductively-coupled plasma atomic emission spectrometry follows oxalate coprecipitation of the REEs with calcium as carrier and cation- exchange column separation in nitric acid. The combination of the two separation techniques improved the low recoveries found for Sm, Eu, and Gd when only ion-exchange was used, especially for iron- and aluminum-rich samples. The method was applied to the analysis of geological standard materials NBS SRM 688 (basalt), NBS SRM 278 (obsidian), GSJ JB-1 (basalt), GSJ JA- 2 (andesite), and CCRMP SY-3 (syenite). The results were evaluated on the basis of chondrite- normalized rare earth element distribution patterns.     

Determination of phosphorous in organic compounds and metal complexes by inductively-coupled plasma atomic emission spectrometry

Phosphorus is determined by inductively-coupled plasma atomic emission spectrometry at 213.618 nm. Different types of organic and inorganic phosphorus compounds and metal complexes were examined after direct dissolution in water, aqueous ethanol or acid, or after decomposition by oxygen flask combustion or Kjeldahl digestion; results were within the usual limit of precision and accuracy for such determinations. The effect of small (<20%) ethanol concentrations in the aqueous solution on the signals obtained from a low-power (1200 W) argon plasma is examined and discussed.     

Determination of rare-earth elements and yttrium in silicate rocks by sequential inductively-coupled plasma emission spectrometry

An ICP—AES method for determination of rare-earth elements (REE) and yttrium at trace levels in silicate rocks is described. The method involves decomposition of the rock sample by heating with a mixture of hydrofluoric and perchloric acid, followed by precipitation of the REE and Y as oxalates, with calcium as carrier. The oxalate precipitate is ignited to the oxide, which is then dissolved in dilute nitric acid and the solution is used for ICP—AES measurements, with use of pure REE solutions as calibration standards. The method has been applied to the determination of REE in a number of standard reference materials and the results have been compared with the reported values. Three other silicate rock samples have also been analysed for REE and Y by this method.     

Determination of rare-earth elements by high-performance liquid chromatography/inductively-coupled plasma/atomic emission spectrometry

Liquid chromatography coupled on-line to a sequential ICP/AES system is applied for the determination of 14 rare-earth elements (REEs) in samples with widely different concentrations of REEs and matrix elements. The REEs are separated on a cation-exchanger by applying an α- hydroxyisobutyric acid gradient. The determination limits were the same as those obtained by continuous nebulization of single-element standard solutions. The chromatographic separation precludes mutual spectral interferences between the REEs. The practical value of the method developed is demonstrated by the determination of REE impurities in Specpure rare-earth oxides, by its demonstrated potential to evaluate real spectral interferences, and by the analysis of geological samples (natural phosphates) with relatively low total REE contents. The detection limits of REEs in these natural phosphates ranged between 0.005 and 0.4 μg g^?1.     

Determination of arsenic by inductively-coupled plasma atomic emission spectrometry enhanced by hydride generation from organized media

A method is described for the determination of arsenic, which combines a continuous flow hydride generation technique with an inductively coupled plasma atomic emission detection system. Some atomic absorption preliminary studies are described as well. Arsine is generated with NaBH(4) from a didodecyldimethylammonium bromide (DDBA) vesicular medium. The analytical performance of this vesicles-enhanced method is superior to the generation of the hydride from aqueous media: the detection limit (0.6 ppb) is improved by a factor of 2 and greater tolerance to interferences is observed for arsine generation from DDBA vesicles. Precision of As determinations is also improved. The proposed method has been validated for low As levels determinations in two Certified Reference Materials (CRM) sediments with satisfactory results. The potential of organized media to improve hydride generation is addressed.     

Determination of boron in engine coolants by direct current plasma atomic emission spectrometry

Boron in unused engine coolants is determined by direct current plasma atomic emission spectrometry with a relative standard deviation of approximately 1%. Ethane-1,2-diol is added to calibration solutions to match the concentrations in the samples being analyzed. Results obtained are within 1% of the amount of boron in an engine coolant of known composition. The time needed for a batch of 10 samples is approximately 3 h.     

Determination of boron in boron-alloyed steels by inductively coupled plasma atomic emission spectrometry

An inductively coupled plasma atomic emission spectrometry (ICP-AES) procedure has been developed and examined for the determination of boron content (0.01 up to about 2% B) in boron-alloyed steels such as POLDI ATA BOR (65% Fe, 19%Cr, 12% Ni, 1.5% Mn, 1% B), POLDI ATA BOR EXTRA (62% Fe, 18% Cr, 13% Ni, 2.5% Mo, 1.5% Mn, 1% B) and POLDI ATA BOR-R (75% Fe, 18% Cr, 3.5% Ti, 1.8% B). The steel sample is dissolved with a mixture of hydrochloric, nitric, sulfuric and phosphoric acids in a quartz vessel. Borides of alloyed metals, especially of iron and chromium, are quantitatively decomposed. The presence of phosphoric acid in a sample solution reduces the volatility of boric acid with water vapour.Presented in part at the 1989 European Winter Conference on Plasma Spectrochemistry, Reutte, Austria