Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/6447
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dc.contributor.authorAthiray, P. S-
dc.contributor.authorSudhakar, M-
dc.contributor.authorTiwari, M. K-
dc.contributor.authorNarendranath, S-
dc.contributor.authorLodha, G. S-
dc.contributor.authorDeb, S. K-
dc.contributor.authorSreekumar, P-
dc.contributor.authorDash, S. K-
dc.date.accessioned2013-12-06T10:29:22Z-
dc.date.available2013-12-06T10:29:22Z-
dc.date.issued2013-12-
dc.identifier.citationPlanetary and Space Science, Vol. 89, pp. 183–187en
dc.identifier.issn0032-0633-
dc.identifier.urihttp://hdl.handle.net/2248/6447-
dc.descriptionRestricted Accessen
dc.description.abstractWe have developed an algorithm (x2abundance) to derive the lunar surface chemistry from X-ray fluorescence (XRF) data for the Chandrayaan-1 X-ray Spectrometer (C1XS) experiment. The algorithm converts the observed XRF line fluxes to elemental abundances with uncertainties. We validated the algorithm in the laboratory using high Z elements (20<Z<30) published in Athiray et al. (2013). In this paper, we complete the exercise of validation using samples containing low Z elements, which are also analogous to the lunar surface composition (ie., contains major elements between 11<Z<30). The paper summarizes results from XRF experiments performed on Lunar simulant (JSC-1A) and anorthosite using a synchrotron beam excitation. We also discuss results from the validation of x2abundance using Monte Carlo simulation (GEANT4 XRF simulation).en
dc.language.isoenen
dc.publisherElsevier B.V.en
dc.relation.urihttp://dx.doi.org/10.1016/j.pss.2013.08.022en
dc.rights© Elsevier B.V.en
dc.subjectX-ray Fluorescence (XRF)en
dc.subjectChandrayaan-1en
dc.subjectFundamental parameteren
dc.subjectC1XSen
dc.subjectLunar chemistryen
dc.titleExperimental validation of XRF inversion code for Chandrayaan-1en
dc.typeArticleen
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