The determination of metals at ppb levels by thin-film x-ray fluorescence spectrometry after coprecipitation with a molybdenum carrier complex

A method is described for the determination of iron, cobalt, nickel, copper, zinc, cadmium and lead in water at μg 1^-1 levels, in which the metals are coprecipitated with a molybdenum—pyrrolidinedithiocarbamate carrier complex. The precipitate is collected as a thin film on a membrane filter (0.4-μm pore-size) and analysed directly by x-ray fluorescence spectrometry. Detection limits, for 100-ml water samples and counting times of 200 s per element, are 1 μg metal l^-1 or lower. Total dissolved metal concentrations are obtained without boiling or u.v. irradiation of the water sample. The method is applicable to river and estuarine waters and is not affected by dissolved organic matter.     

Uranium determination at ppb levels by X-ray fluorescence after its preconcentration on polyurethane foam

A sensitive method based on the preconcentration of uranium on powdered polyurethane foam (PUF) has been developed to determinate this element in water samples by X-ray florescence. Uranium at ppb levels was sorbed as the salicylate complex on powdered PUF at pH 4.0. The resulting PUF was filtered through a filter paper and used for X-ray fluorescence measurements. For 50 μg/l of uranium the coefficient of variation for five measurements is 5% and the detection limit is 5.5 μg/l. The interference level of various ions and ligands was studied and optimum conditions were developed to determine uranium in reference materials, waste water, mine drainage, and sea water.     

The determination of antimony in nodular cast iron by wavelength-dispersive x-ray fluorescence spectrometry

Antimony is determined in cast irons by wavelength-dispersive x-ray fluorescence spectrometry. Excitation and detection conditions are evaluated for the three most intense x-rays of antimony, i.e., the K_α, L_α and L_β lines. Standard samples were obtained by precise determination of the antimony content of some specimen cast irons by neutron activation analysis. Calibration graphs are linear from 0 to 200 mg kg^?1. The precision of the determination by means of the most sensitive Sb L_α line, using a chromium tube and a 5-min measuring time, ranges from 6% for samples containing 20 mg kg^?1 antimony, to 1% for samples containing 200 mg kg^?1.     

The coprecipitation of an organophosphate fraction from harbour water for x-ray fluorescence spectrometry

The film x-ray fluorescence spectrum of a cobalt pyrrolidinedithiocarbamate carrier complex, precipitated in harbour-water samples, contains a previously unreported peak at the wavelength of the first-order K_α line of phosphorus. The coprecipitated phosphorus is an organophosphate fraction of biological origin, constituting approximately 10% of the dissolved organophosphorus in the waters.     

Preconcentration by coprecipitation of arsenic and tin in natural waters with a Ni-pyrrolidine dithiocarbamate complex and their direct determination by solid-sampling atomic-absorption spectrometry

A method for the determination of trace amounts of arsenic and tin in natural waters is described. Trace amounts of arsenic and tin were preconcentrated by coprecipitation with a Ni-ammonium pyrrolidine dithiocarbamate (APDC) complex. The coprecipitates obtained were directly analyzed by graphite-furnace atomic-absorption spectrometry (GFAAS) using the Ni-APDC complex solid-sampling technique. The coprecipitation conditions used for the trace amounts of arsenic and tin in natural water were investigated in detail. It was found that arsenic and tin at sub-ng mL(-1) levels were both coprecipitated quantitatively by Ni(PDC)2 in the pH range 2-3. The concentration factors by coprecipitation reached approximately 40,000 when 2 mg nickel was added as a carrier element to 500 mL of the water sample. The proposed method has been applied to the determination of trace amounts of arsenic and tin in river water and seawater reference materials, and the detection limits for arsenic and tin, which were calculated from three times of the standard deviation of the procedural blanks, are 0.02 ng mL(-1) and 0.04 ng mL(-1), respectively, for 500-mL volumes of water sample.     

The determination of dissolved chromium(III) and chromium(VI) and particulate chromium in waters at μg l-1 levels by thin-film x-ray fluorescence spectrometry

A method is described for the determination of particulate chromium and dissolved chromium(III) and (VI) in water at μg l^-1 levels. Particulate material is collected by filtration of the water sample through a membrane filter (0.4-μm pore-size). Chromium(III) and chromium(VI) are then coprecipitated, separately and in that order, with iron(III) hydroxide (at pH 8.5) and a cobalt—pyrrolidinedithiocarbamate carrier complex (at pH 4.0). Both precipitates are collected as thin films on membrane filters and, with the particulate material, analysed directly for chromium by x-ray fluorescence spectrometry. Detection limits, for a 100-ml water sample and counting times of 100 s, are 0.1 μg Cr l^-1. The method is unaffected by sea salt and is applicable, without modifications, to river and estuarine waters.     

Analysis of cast iron by x-ray fluorescence spectrometry

It is shown that a wide range of cast irons can be analysed on one calibration if the sample surfaces are prepared to a mirror finish with diamond paste. Polishing the samples with any abrasive material results in preferential removal of the softer constituents from the sample matrix. If coarser abrasives than diamond paste are used, the increased depth of the introduced sample inhomogeneity leads to unacceptable error limits for the determination of light elements.     

Spectrophotometric determination of uranium in natural waters

A method for the spectrophotometric determination of uranium in samples of natural water is described. Ion exchange with Amberlite IR-120 (H⁺) to concentrate the metal was used. The absorption properties of the complex formed between uranium and the chromogenic reagent Arsenazo III, its stability over several hours, the effect of the pH on the ability of the resin to retain uranium, the reproducibility of the method and the effects of ionic interferences were considered. The sensitivity was 0.67 and 0.05 μg l^?1 of uranium for the direct and the addition methods, respectively. Uranium concentrations for the samples analysed were between 0.10 and 0.50 μg l^?1.     

Determination of dissolved arsenic in waters at μg l−1 levels by precipitation and energy-dispersive x-ray fluorescence spectrometry

Arsenic is precipitated as magnesium ammonium arsenate with magnesium ammonium phosphate as carrier. The precipitate is collected on a glass-fibre filter and arsenic is measured by energy-dispersive x-ray fluorescence spectrometry with a silver secondary target. With 200-ml water samples and 100-s counting times, the limit of detection is 0.7 μg As l^?1. The method is applicable to all types of natural water including sea waters.     

Determining of trace metals in nuclear-grade uranium dioxide by x-ray fluorescence spectrometry

A method is described for the simultaneous determination of low concentration of Ca, Cr, Cu, Fe, Mn and Ni in nuclear-grade uranium dioxide by x-ray fluroescence spectrometry, without the use of chemical treatment. The lower limits of detection range from 2 μg g^?1 for nickel and manganese to 5 μg g^?1 for copper. Samples are prepared in the form of double-layer pellets with boric acid as a binding agent. Standards are prepared in a U₃O₈ matrix, which is more chemically stable than UO₂ and has similar matrix behaviour. The correlation coefficients for calibration curves are better than 0.999. Errors range from 2.4% for chromium to 6.8% for nickel.     

The determination of sulphate in natural waters by inductively-coupled plasma emission spectrometry

Sulphate is determined simultaneously with other constituents by using inductively-coupled plasma emission spectrometry; the intensity of the 180.73-nm sulphur line is monitored. At a forward power of 1100 W, under compromise conditions, a 3 s detection limit of 0.08 mg l^-1 sulphate and a precision of 0.8% RSD at the 200 mg l^-1 sulphate level were obtained. A small spectral interference from calcium is overcome by software corrections, and good agreement is demonstrated between the proposed method and spectrophotometric sulphate measurements for a variety of natural waters including seawater.     

The simultaneous determination of gold,silver and cadmium at ppb levels in silicate rocks by atomic absorption spectrometry with electrothermal atomization

A method for the determination of Au, Ag and Cd at ppb-levels in silicate rocks by flameless atomic absorption spectrometry after separation with an anion-exchange resin is described. The final test solutions are simple and calibration graphs can be prepared with pure salt solutions. The detection limits allow the determination of as little as 0.2, 0.05 and 0.03 ppb for Au, Ag and Cd, respectively, in 1-g rock samples.     

Ion pair-based dispersive liquid-liquid microextraction for gold determination at ppb level in solid samples after ultrasound-assisted extraction and in waters by electrothermal-atomic absorption spectrometry

A new methodology was developed for the determination of ultratrace levels of gold in water samples, soils and river sediments. Dispersive liquid-liquid microextraction was used to preconcentrate the ion pair formed between AuCl₄⁻ and [CH₃(CH₂)₃]₄N⁺ in a microliter-range volume of chlorobenzene using acetone as disperser solvent. When solid samples were analyzed, the method consisted of a combination of ultrasound-assisted extraction and dispersive liquid-liquid microextraction with final detection by electrothermal-atomic absorption spectrometry. Since an HCl medium was required for the formation of the AuCl₄⁻ complex, HCl together with HNO₃ was used as extractants for ultrasound-assisted extraction. After optimization, the enrichment factor obtained was 220 for water samples. Moreover, the extraction efficiency was around 96%. The repeatability, expressed as relative standard deviation ranged from 3.6% to 9.7%. The instrumental detection limit was 8.4 ng L⁻¹, whereas the procedural detection limits were 42 ng L⁻¹ for water samples and 1.5 ng g⁻¹ for environmental solid samples.     

Radiometric determination of uranium in natural waters after enrichment and separation by cation-exchange and liquid-liquid extraction

Preconcentration of uranium from natural water samples using Chelex-100 cation-exchange resin, its selective extraction by tributylphosphate and electrodeposition on stainless steel discs is reported. The validity of the separation procedure and the chemical recoveries were checked by addition of uranium standard solution as well as by tracing with ²³²U. The average uranium yield for the cation-exchange was (97±2)%, for the liquid-liquid extraction was (95±2)% and for the electrodeposition was more than 99%. Employing high-resolution a-spectroscopy, the measured activity of ²³⁸U and ²³⁴U radioisotopes was found to be ~7 mBq^.l^-1 and ~35 mBq^.l^-1 for ground- and seawater samples, respectively. The energy resolution (FWHM) of the α-peaks was 22 keV, the minimum detectable activity (MDA) was estimated to be 1 mBq^.l^-1 (at 95% confidence limit). This revised version was published online in July 2006 with corrections to the Cover Date.     

Rapid sequential determination of inorganic mercury and methylmercury in natural waters by flow injection-cold vapour-atomic fluorescence spectrometry

A novel method for the rapid sequential determination of inorganic mercury and methylmercury in natural waters at the ng/l. level has been developed. Trace enrichment and separation of mercury species are achieved using a microcolumn of sulphydryl cotton which has a relatively high affinity for methylmercury. The limit of detection for methylmercury based on processing of a 0.5-ml sample volume was 6 ng/l. Application to river waters is demonstrated.     

Preconcentration and spectrophotometric determination of chromium(vi) in natural waters by coprecipitation with barium sulfate

A selective preconcentration of chromium(VI) is proposed for analysis of natural waters. Chromium(VI) is quantitatively separated from chromium(III) by coprecipitation with barium sulfate; salicylic acid is used as a masking agent for iron(III), aluminum(III) and chromium(III). The precipitate is fused with alkali carbonate, and the chromium(VI) in the melt is isolated with hot water and determined spectrophotometrically with diphenylcarbazide. The detection limit is 0.02 μg l^-1 the relative standard deviation for chromium(VI) in river water is less than 5%.     

Spectrophotometric determination of uranium in natural waters after preconcentration on TBP-plasticized dibenzoylmethane-loaded polyurethane foams

A method is presented for the spectrophotometric determination of uranium in natural waters after a preconcentration step involving percolation of a suitable aliquot of the water sample whose pH is adjusted to 6.0–6.5 through a TBP-plasticized dibenzoylmethane-loaded polyurethane foam bed. Uranium on the foam is eluted with 0.6M HCl solution and then determined spectrophotometrically using arsenazo III as a chromogenic reagent.     

Fluorimetric method for the determination of uranium in natural waters

A method is described for the fluorimetric determination of uranium in natural waters. The limit of detection is 0.3 ppM. Ion-exchange is used to preconcentrate the uranium by a factor of 22 and separate it from quenching ions in the sample. The fluorescence is measured in a medium that is 1.35M in both sulphuric and phosphoric acids. The uranyl ions are excited by radiation of wavelength 280 nm and bandwidth 40 nm. The emitted signal is scanned from 470 to 510 nm. After spiking of the sample solution with a small volume of standard uranium solution, the fluorescence signal is scanned again and the uranium content of the sample calculated from the two readings. The coefficient of variation is 8.5% for determinations of U in a synthetic water sample having a uranium content of 1.9 ppM. Destruction of organic matter in the eluates gives 0.1 ppM detection limit.     

Determination of uranium in natural waters after anion-exchange separation

A method is described for the determination of uranium by fluorimetry and spectrophotometry in samples of natural non-saline waters. After acidification with hydrochloric acid, the water sample is filtered and, following the addition of ascorbic acid and potassium thiocyanate, passed through a column of the strongly basic anion-exchange resin Dowex 1-X8 (thiocyanate form). On this exchanger uranium is adsorbed as an anionic thiocyanate complex. After removal of iron and other coadsorbed elements by washing first with a mixture consisting of 50 vol.% tetrahydrofuran, 40 vol.% methyl glycol and 10 vol.% 6 M hydrochloric acid, and then with pure aqueous 6 M hydrochloric acid, the uranium is eluted with 1 M hydrochloric acid. In the eluate, uranium is determined fluorimetrically or by means of the spectrophotometric arsenazo III method. The procedure was used for the routine determination of uranium in water samples collected in Austria.