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DC Field | Value | Language |
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dc.contributor.author | Bahia, O. | - |
dc.contributor.author | Moreno, MMT | - |
dc.contributor.author | Nardy, AJR | - |
dc.contributor.author | deOliveira, MAF | - |
dc.contributor.author | daSilva, J. A. | - |
dc.date.accessioned | 2014-05-20T15:29:29Z | - |
dc.date.accessioned | 2016-10-25T18:04:45Z | - |
dc.date.available | 2014-05-20T15:29:29Z | - |
dc.date.available | 2016-10-25T18:04:45Z | - |
dc.date.issued | 1996-01-01 | - |
dc.identifier | http://www.scielo.br/scielo.php?script=sci_issues&pid=0100-4670 | - |
dc.identifier.citation | Ecletica Química. São Paulo: Editora Unesp, v. 21, p. 19-42, 1996. | - |
dc.identifier.issn | 0100-4670 | - |
dc.identifier.uri | http://hdl.handle.net/11449/39071 | - |
dc.identifier.uri | http://acervodigital.unesp.br/handle/11449/39071 | - |
dc.description.abstract | The main variables found on procedure of the dissolution silicate rocks using acid dissolution in teflon open vessel for analysis of micro elements by ICP-AES has been determined. The results obtained for some samples showed strong dependence of the rock mineralogical composition, then it was recommended an alkaline fusion step after acid dissolution. The decomposition procedure use 20 mi of an acid mixture of HF:HNO3 in the proportion 3:1 for a fraction of 250 mg pulverized sample. The recommended temperatures were 60 degrees C for attack and 90 degrees C for acid volatilization. The fusion step with 50 mg LiBO2 at 1000 degrees C may be used if non-attacked residue is observed in the solution. The whole time was 6 h per sample. Nine types os silicate rocks that show mineralogical and chemical different compositions were chosen for obtaining the optimization of the variables. The elements used were Ce, Y, Yb and Zr. In addition, ultrassonic nebulization has been used. The percentual standard deviations obtained for five determinations were 0.7 and 1.4 for triplicate samples. The mineralogical and textural information from the petrographical analysis of the samples indicated the need of increasing the fusion step on the optimized procedure. | en |
dc.format.extent | 19-42 | - |
dc.language.iso | por | - |
dc.publisher | Editora Unesp | - |
dc.source | Web of Science | - |
dc.subject | inductively coupled plasma atomic emission spectrometry | pt |
dc.subject | ultrasonic nebulization | pt |
dc.subject | silicate rock analysis | pt |
dc.subject | dissolution of geological matrix | pt |
dc.subject | analytical geochemistry | pt |
dc.title | Procedure optimization of silicate rocks dissolution in open vessels for ICP-AES analysis. | en |
dc.type | outro | - |
dc.contributor.institution | Universidade Estadual Paulista (UNESP) | - |
dc.description.affiliation | UNESP,INST GEOCIENCIAS & CIENCIAS EXATAS,DEPT PETROL & METALOGENIA,BR-13500230 RIO CLARO,SP,BRAZIL | - |
dc.description.affiliationUnesp | UNESP,INST GEOCIENCIAS & CIENCIAS EXATAS,DEPT PETROL & METALOGENIA,BR-13500230 RIO CLARO,SP,BRAZIL | - |
dc.identifier.wos | WOS:A1996WH62900002 | - |
dc.rights.accessRights | Acesso restrito | - |
dc.relation.ispartof | Eclética Química | - |
Appears in Collections: | Artigos, TCCs, Teses e Dissertações da Unesp |
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