http://scholars.ntou.edu.tw/handle/123456789/20773
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Jyh-Jaan Huang | en_US |
dc.contributor.author | Ludvig Löwemark | en_US |
dc.contributor.author | Queenie Chang | en_US |
dc.contributor.author | Tzu-Yu Lin | en_US |
dc.contributor.author | Huei-Fen Chen | en_US |
dc.contributor.author | Sheng-Rong Song | en_US |
dc.contributor.author | Kuo-Yen Wei | en_US |
dc.date.accessioned | 2022-02-17T05:29:26Z | - |
dc.date.available | 2022-02-17T05:29:26Z | - |
dc.date.issued | 2016-04 | - |
dc.identifier.issn | 1525-2027 | - |
dc.identifier.uri | http://scholars.ntou.edu.tw/handle/123456789/20773 | - |
dc.description.abstract | X-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.iso | en_US | en_US |
dc.publisher | AMER GEOPHYSICAL UNION | en_US |
dc.relation.ispartof | GEOCHEM GEOPHY GEOSY | en_US |
dc.subject | RAY-FLUORESCENCE ANALYSIS | en_US |
dc.subject | REFERENCE SAMPLES | en_US |
dc.subject | MARINE-SEDIMENTS | en_US |
dc.subject | ITRAX | en_US |
dc.subject | OPTIMIZATION | en_US |
dc.subject | CALIBRATION | en_US |
dc.subject | SCANNERS | en_US |
dc.subject | RECORDS | en_US |
dc.subject | CLIMATE | en_US |
dc.subject | AFRICA | en_US |
dc.title | Choosing optimal exposure times for XRF core-scanning: Suggestions based on the analysis of geological reference materials | en_US |
dc.type | journal article | en_US |
dc.identifier.doi | 10.1002/2016GC006256 | - |
dc.identifier.isi | WOS:000379523900018 | - |
dc.relation.journalvolume | 17 | en_US |
dc.relation.journalissue | 4 | en_US |
dc.relation.pages | 1558-1566 | en_US |
item.cerifentitytype | Publications | - |
item.openairetype | journal article | - |
item.openairecristype | http://purl.org/coar/resource_type/c_6501 | - |
item.fulltext | no fulltext | - |
item.grantfulltext | none | - |
item.languageiso639-1 | en_US | - |
crisitem.author.dept | College of Ocean Science and Resource | - |
crisitem.author.dept | Institute of Earth Sciences | - |
crisitem.author.dept | National Taiwan Ocean University,NTOU | - |
crisitem.author.orcid | 0000-0003-0188-9342 | - |
crisitem.author.parentorg | National Taiwan Ocean University,NTOU | - |
crisitem.author.parentorg | College of Ocean Science and Resource | - |
Appears in Collections: | 地球科學研究所 14 LIFE BELOW WATER |
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