scholarly journals Determination of lead isotope ratios in archeological products by ion microanalyzer.

1985 ◽  
Vol 1 (3) ◽  
pp. 227-230
Author(s):  
Shigenori MAEDA ◽  
Junko TAKASE ◽  
Yoshinori SUGITANI ◽  
Kozo NAGASHIMA
Keyword(s):  
Lead Isotope ◽  
Isotope Ratios ◽  
Lead Isotope Ratios

Evaluation of the accuracy of the determination of lead isotope ratios in wine by ICP MS using quadrupole, multicollector magnetic sector and time-of-flight analyzers

Talanta ◽  
2001 ◽  
Vol 54 (2) ◽  
pp. 307-317 ◽  
Author(s):  
Mireille Barbaste ◽  
Ludwik Halicz ◽  
Albert Galy ◽  
Bernard Medina ◽  
Hakan Emteborg ◽  
...  
Keyword(s):  
Lead Isotope ◽  
Time Of Flight ◽  
Isotope Ratios ◽  
Magnetic Sector ◽  
Lead Isotope Ratios ◽  
Icp Ms

Application of lead isotope ratios for pollution source investigation in the marine environment

2020 ◽  
Author(s):  
Emiliya Vassileva ◽  
Anna Maria Orani ◽  
Sergey Assonov
Keyword(s):  
Isotopic Composition ◽  
Lead Isotope ◽  
Isotope Ratios ◽  
Environmental Matrices ◽  
Total Uncertainty ◽  
Lead Isotope Ratios ◽  
Icp Ms ◽  
Seawater Samples ◽  
Biota Samples

<p><span><span>Lead is a non-essential toxic element that at high levels of human exposure causes damage to many organs of the human body. This element naturally occurs in the Earth crust, but its biogeochemical cycle has been altered by anthropogenic activities, which have introduced high amount of this element from different sources. Among inorganic contaminants, Pb is perhaps the most studied, but the determination of its total concentration only is not sufficient for a proper evaluation of contamination sources. Discrimination of anthropogenic and geogenic lead sources requires both precise and accurate isotope ratio determination as well as high versatility due to the complexity of environmental matrices, such as sediments, biota and seawater. This element has a partially radiogenic isotopic composition with 208Pb, 206Pb and 207Pb originating from the radioactive decay of 238U, 235U and 232Th respectively and 204Pb representing the only natural stable isotope. This characteristic isotopic composition represents a powerful analytical tool as it allows to trace the sources, fate and effects of possible Pb contamination. The most common way to express the Pb isotopic composition is using the ratio 206Pb/207Pb, because of the easy interference-free determination and isotopes’ abundance. The determination of 204Pb by ICP-MS is quite challenging as this is also the least abundant among Pb isotopes (about 1.4%) and it is also affected by isobaric interference from 204Hg. The latter derives from both sample matrices and from plasma/sweep gas supplies and it represents a big analytical challenge, especially for marine biota samples, where the amount of Hg can be up to 100 times higher than Pb. </span></span></p><p><span><span>In this work we present the development and the application of analytical methodology for the accurate and precise determination of Pb isotope ratios by HR-ICP-MS in different marine environmental matrices (sediments, seawater and biota). Analytical procedures are involving a separation of Pb from the sample matrix and mercury, present in the sample. For seawater samples, the use of the SeaFAST automated system allowed simultaneous matrix separation and analyte pre-concentration before ICP-MS analysis. A comparison of results for lead isotope ratios obtained with MC-ICP-MS and HR ICP-MS in the same samples, in all cases, showed very good agreement . The total uncertainty associated to each result was estimated and all major contributions to the combined uncertainty of the obtained results were identified. As all such studies involve companions of different datasets, the uncertainty estimation is critical to ensure correct companions.  The developed methodology was applied to different marine samples, namely sediments from Caribbean, Baltic and Namibian coasts, biota samples from French Polynesia, seawater samples from Mediterranean and Arctic seas.</span></span><span><span> </span></span></p>

A fast atom bombardment study of the lead isotope ratios in early nineteenth century Niagara Peninsula pottery glazes

1986 ◽  
Vol 64 (3) ◽  
pp. 488-491 ◽  
Author(s):  
Jack M. Miller ◽  
Timothy R. B. Jones ◽  
Tina Kenney ◽  
David W. Rupp ◽  
Brian N. Green ◽  
...  
Keyword(s):  
Nineteenth Century ◽  
Lead Isotope ◽  
Fast Atom Bombardment ◽  
Acid Leaching ◽  
Direct Analysis ◽  
Isotope Ratios ◽  
Local Source ◽  
Lead Isotope Ratios ◽  
Sedimentary Deposits

The application of fast atom bombardment (FAB) mass spectrometry to the determination of lead isotope ratios in nineteenth century pottery glazes from the Niagara Peninsula has been investigated with the aim of determining the source of the lead used in the glazes. Methods of sampling have been compared, including direct analysis of glass chips, analysis of powdered glaze scrapings, analysis of acid extracts of the former, and simple acid leaching of the surface of a piece of pottery. The latter method gave the best results. The FAB data, as obtained on an older mass spectrometer, can distinguish lead from igneous vs. sedimentary deposits, but is not adequate to determine specific mining locations. Although newer FAB instrumentation can narrow this range, the overlap of data from the Niagara Peninsula and England precludes a simple answer to the archeological question as to English vs. Canadian origin of the lead used in the Jordan pottery glazes. However, the data do suggest that the potter used a local source for the lead.

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