Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/25208
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dc.contributor.authorLal, Roshan-
dc.contributor.authorSharma, N D-
dc.date.accessioned2013-12-30T06:48:55Z-
dc.date.available2013-12-30T06:48:55Z-
dc.date.issued2003-07-
dc.identifier.issn0975-1041 (Online); 0019-5596 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/25208-
dc.description559-561en_US
dc.description.abstract57Fe Mössbauer spectroscopy has been used to characterize the iron-bearing minerals from Dagsheri (Himachal Pardesh, India). An interesting feature of this sample is, the presence of large amount of haematite and small amount of Jarosite, which decompose into oxide phase, i.e. into haematite, which is likely to have volcanic origin. The decomposition behaviour of these minerals on combustions studied by Mössbauer technique, after heating the samples at different temperatures. The decomposition route is significantly different from that normally observed in coal samples.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJPAP Vol.41(07) [July 2003]en_US
dc.subjectIron bearing mineralsen_US
dc.subjectMineralsen_US
dc.subjectHaematiteen_US
dc.subjectJarosithen_US
dc.titleCharacterization of iron bearing minerals from Dagsheri and study of their decomposition behaviour during combustion using 57Fe Mossbauer spectroscopyen_US
dc.typeArticleen_US
Appears in Collections:IJPAP Vol.41(07) [July 2003]

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