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Please use this identifier to cite or link to this item: http://scholars.ntou.edu.tw/handle/123456789/20773
DC FieldValueLanguage
dc.contributor.authorJyh-Jaan Huangen_US
dc.contributor.authorLudvig Löwemarken_US
dc.contributor.authorQueenie Changen_US
dc.contributor.authorTzu-Yu Linen_US
dc.contributor.authorHuei-Fen Chenen_US
dc.contributor.authorSheng-Rong Songen_US
dc.contributor.authorKuo-Yen Weien_US
dc.date.accessioned2022-02-17T05:29:26Z-
dc.date.available2022-02-17T05:29:26Z-
dc.date.issued2016-04-
dc.identifier.issn1525-2027-
dc.identifier.urihttp://scholars.ntou.edu.tw/handle/123456789/20773-
dc.description.abstractX-ray fluorescence (XRF) core-scanning is a fast and nondestructive technique to assess elemental variations of unprocessed sediments. However, although the exposure time of XRF-scanning directly affects the scanning counts and total measurement time, only a few studies have considered the influence of exposure time during the scan. How to select an optimal exposure time to achieve reliable results and reduce the total measurement time is an important issue. To address this question, six geological reference materials from the Geological Survey of Japan (JLK-1, JMS-1, JMS-2, JSD-1, JSD-2, and JSD-3) were scanned by the ltrax-XRF core scanner using the Mo- and the Cr-tube with different exposure times to allow a comparison of scanning counts with absolute concentrations. The regression lines and correlation coefficients of elements that are generally used in paleoenvironmental studies were examined for the different exposure times and X-ray tubes. The results show that for those elements with relatively high concentrations or high detectability, the correlation coefficients are higher than 0.90 for all exposure times. In contrast, for the low detectability or low concentration elements, the correlation coefficients are relatively low, and improve little with increased exposure time. Therefore, we suggest that the influence of different exposure times is insignificant for the accuracy of the measurements. Thus, caution must be taken when interpreting the results of elements with low detectability, even when the exposure times are long and scanning counts are reasonably high.en_US
dc.language.isoen_USen_US
dc.publisherAMER GEOPHYSICAL UNIONen_US
dc.relation.ispartofGEOCHEM GEOPHY GEOSYen_US
dc.subjectRAY-FLUORESCENCE ANALYSISen_US
dc.subjectREFERENCE SAMPLESen_US
dc.subjectMARINE-SEDIMENTSen_US
dc.subjectITRAXen_US
dc.subjectOPTIMIZATIONen_US
dc.subjectCALIBRATIONen_US
dc.subjectSCANNERSen_US
dc.subjectRECORDSen_US
dc.subjectCLIMATEen_US
dc.subjectAFRICAen_US
dc.titleChoosing optimal exposure times for XRF core-scanning: Suggestions based on the analysis of geological reference materialsen_US
dc.typejournal articleen_US
dc.identifier.doi10.1002/2016GC006256-
dc.identifier.isiWOS:000379523900018-
dc.relation.journalvolume17en_US
dc.relation.journalissue4en_US
dc.relation.pages1558-1566en_US
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
item.cerifentitytypePublications-
item.languageiso639-1en_US-
item.fulltextno fulltext-
item.grantfulltextnone-
item.openairetypejournal article-
crisitem.author.deptCollege of Ocean Science and Resource-
crisitem.author.deptInstitute of Earth Sciences-
crisitem.author.deptNational Taiwan Ocean University,NTOU-
crisitem.author.orcid0000-0003-0188-9342-
crisitem.author.parentorgNational Taiwan Ocean University,NTOU-
crisitem.author.parentorgCollege of Ocean Science and Resource-
Appears in Collections:地球科學研究所
14 LIFE BELOW WATER
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