A procedure was developed for the graphite furnace atomic absorption spectrometnc determmatlon of galhum m high-iron geological matenals such as iron meteontes To overcome severe interference from iron, gallium 1s extracted as a chloro complex from 5 M hydrochloric aad mto lsobutyl methyl ketone Iro
Quantification of thallium in rocks and meteorites by graphite furnace atomic absorption spectrometry
β Scribed by Xun Guo; Maki Hoashi; Robert R. Brooks; Roger D. Reeves
- Publisher
- Elsevier Science
- Year
- 1992
- Tongue
- English
- Weight
- 412 KB
- Volume
- 266
- Category
- Article
- ISSN
- 0003-2670
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β¦ Synopsis
A procedure was developed for the quanhficatlon of thalbum at the ultratrace level (ng g-l) m geoloacal matenals The sample 1s dissolved m 3 M H2S04 to which IS added KI and K,HP04 The thalhum IS then extracted as its mdo complex mto methyhsobutyl ketone (MIBK), leavmg behind most of the n-on The remamder of the iron IS removed from the organic layer by back-extra&on mto 3 M H,SO, The added K,HPO, enhances the extraction of thalhum mto the MIBK layer which 1s then analysed by graphite furnace atonuc absorption spectrometry The hnut of detection (30) was about 2 ng g-' m the ongmal sobd sample, though this could be reduced by further multiple loadmgs Precmon and accuracy were determmed by analysts of the standard reference rocks G-l, W-l and CAAS Sulphlde Ore The precmon ranged from 3 03-10 5% dependmg on the thalhum content of the rocks, and the relative error (accuracy) ranged from 2 l-6 7%
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