Abstract

A rapid and precise method for the determination of Pt in manganese nodules and crusts is presented. The sample of 0.1 g was decomposed with 8 ml of aqua regia and filtered. The filtrate was evaporated to dryness, then dissolved in 20 ml of 20% tartaric acid with heating. After the addition of 0.5 ml iron (III) chloride solution (20 mg Fe/ml) and 0.5 ml of 1% 1, 3-diphenylthiourea in acetone, the mixture was heated for 5 min at about 100°C. The solution was extracted with 1 ml of 1, 2-dichloroethane for 5 min. Platinum in the organic phase was determined by graphite furnace AAS. The limit of detection is 0.05 ppm, and the relative standard deviation in the determination of 0.01 μg to 1.0 μg of Pt is 4 to 16%. The method is satisfactorily applied to USGS manganese nodule reference samples and the manganese nodules and crusts collected from the Central Pacific Ocean, Antarctic Ocean and Ogasawara Plateau.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.