APPLICATION OF A SEQUENTIAL EXTRACTION SCHEME TO 10 GEOLOGICAL CERTIFIED REFERENCE MATERIALS FOR THE DETERMINATION OF 20 ELEMENTS

Citation
Gem. Hall et al., APPLICATION OF A SEQUENTIAL EXTRACTION SCHEME TO 10 GEOLOGICAL CERTIFIED REFERENCE MATERIALS FOR THE DETERMINATION OF 20 ELEMENTS, Journal of analytical atomic spectrometry, 11(9), 1996, pp. 787-796
Citations number
24
Categorie Soggetti
Spectroscopy
ISSN journal
02679477
Volume
11
Issue
9
Year of publication
1996
Pages
787 - 796
Database
ISI
SICI code
0267-9477(1996)11:9<787:AOASES>2.0.ZU;2-0
Abstract
Methods are described for a sequential extraction scheme to dissolve s electively elements bound in soils and sediments in the following nomi nal forms: (1) adsorbed, exchangeable, carbonate (AEC); (2) amorphous iron oxyhydroxide (am Fe ox), including manganese oxides; (3) crystall ine iron oxides (cry Fe ox); (4) organics and sulfides; and (5) residu al.(mainly silicates). This scheme has been applied in triplicate to a suite of ten international CRMs, ie., soils SRM 2709-2711 and the SO- 1-4 series, marine mud MAG-1, lake sediment LKSD-4 and the till sample TILL-2. Elements determined comprise: As (by HG-quartz tube AAS, HG-Q TAAS); Be, Ca, Co, Cr, Cu, Ni, P, Ti and V (by ICP-AES); Mn, Fe and Zn (by FAAS); and Cd, Ce, Li, Li, Tl Pb and U (by ICP-MS). The precision obtained is excellent, generally in the range 2-10% RSD, at concentra tions 10 x higher than detection limits. Most results for the element concentrations summed over the five phases agree, within statistical u ncertainties, with the recommended total values for the CRMs. Those wh ere recoveries are significantly below 90% are for elements such as Cr and V, which are known to be present in refractory minerals and would require fusion for complete dissolution. The results presented herein for samples SO-1-4 and MAG-1 do not agree well with those recently pu blished using a scheme purported to dissolve similar phases. This high lights the need to be more definitive in describing the nature and ext ent of the phases actually extracted so that comparisons can be made b etween different laboratories and studies.