Thomas C Meisel

Dr. Thomas C Meisel

orcid

Research Focus & Metrics

Academic Career Length

37Years (1990-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 April 2001 in Geochimica et Cosmochimica Acta
Verified
Journal Article
Closed access
TMThomas C Meisel
Thomas C Meisel
RWRichard J Walker
Richard J Walker
AIAnthony J Irving
Anthony J Irving
JLJean-Pierre Lorand
Jean-Pierre Lorand

10 October 1996 in Nature
Verified
Journal Article
Closed access
PDF file
TMThomas C Meisel
Thomas C Meisel
RWR. J. Walker
R. J. Walker
JMJ. W. Morgan
J. W. Morgan


1 February 2012 in Lithos
Verified
Journal Article
Closed access
IUİbrahim Uysal
İbrahim Uysal
YEYalçın E. Ersoy
Yalçın E. Ersoy
OKOrhan Karslı
Orhan Karslı
YDYildirim Dilek
Yildirim Dilek
MSM. Burhan Sadıklar
M. Burhan Sadıklar
TMThomas C Meisel
Thomas C Meisel

4 April 2009 in Contributions to Mineralogy and Petrology
Verified
Journal Article
Closed access
PDF file
IUIbrahim Uysal
Ibrahim Uysal
MTMahmud Tarkian
Mahmud Tarkian
MSM. Burhan Sadiklar
M. Burhan Sadiklar
FZFederica Zaccarini
Federica Zaccarini
TMThomas C Meisel
Thomas C Meisel
SHStefanie Heidrich
Stefanie Heidrich

9 May 2003 in Journal of Analytical Atomic Spectrometry
Verified
Journal Article
Closed access
PDF file
TMThomas C Meisel
Thomas C Meisel
NFNorbert Fellner
Norbert Fellner
JMJohann Moser
Johann Moser
A simple and highly selective analytical procedure is presented here for the concentration determination of Ru, Rh, Pd, Re, Os, Ir and Pt via isotope dilution, which is suitable for the investigation of geological and environmental materials. Sample preparation consists of a sample digestion step in a high pressure asher (HPA-S) with concentrated HNO3 and HCl and drying down of the sample solution after the Os concentration was determined via sparging OsO4 into an ICP-MS. After drying and redissolution of the remaining solution the other PGEs are separated on-line from their matrix in a simple cation-exchange column that is coupled to a quadrupole ICP-MS. Through this technique it is possible to monitor in every sample the isotopes of the analytes as well as of those elements that cause isobaric interferences or that potentially cause interferences through molecular species. Concentrations of the two or more isotopic elements can be calculated through isotope ratios, whereas Rh is calculated via the peak area. Data for ultramafic reference materials UB-N and GP13 with concentrations lower than 8 ng g−1 show excellent reproducibilities (n = 9) for Re, Pd and Pt (2.5–3.9% RSD) and Pt, Ru, Rh, Os and Ir (4.5–7% RSD). It can be demonstrated that a large portion of the higher standard deviations is caused by sample heterogeneity. Road dust (BCR-723) was included to demonstrate the strength of this procedure for the determination of environmental samples. Reproducibilities (n = 5) for Re, Pt and Os were between 1.2 and 2.3% RSD, 5.2% RSD for Pd and 11% RSD for Rh. Data for Ru and Ir are presented for the first time.