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Isotopic Fingerprinting of Metals: From Environment to Human Body

A special issue of International Journal of Environmental Research and Public Health (ISSN 1660-4601). This special issue belongs to the section "Environmental Science and Engineering".

Deadline for manuscript submissions: closed (30 September 2018) | Viewed by 10218

Special Issue Editors


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Guest Editor
Department of Geological Sciences, University of Florida, Gainesville, FL 32611, USA
Interests: George Kamenov’s research is focused on using ICP-MS and MC-ICP-MS instrumentation to decipher geochemical cycle of a number of elements, including heavy metals such as Pb.

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Guest Editor
Department of Earth Sciences, University of Arkansas at Little Rock, Little Rock, AR 72204, USA
Interests: Laura Ruhl’s research focuses on environmental geochemistry issues with special emphasis on water and sediment related issues.

Special Issue Information

Dear Colleagues,

We mine and use vast amounts of metals and other raw materials at present. As a result, the natural geochemical cycles of a number of metals in the modern environment are altered, or even dominated, by anthropogenic activities. Recent developments in mass-spectrometry, in particular MC-ICP-MS and TIMS, allow us to measure isotope abundances of a number of metals with unprecedented precision and accuracy in various environmental and biological samples. The goal of this special issue is to create a forum to highlight new developments in using traditional (e.g., Sr, Pb, Nd) and non-traditional (e.g., Li, Mg, Si, Ca, Cr, Fe, Cu, Zn, Mo, Hg, U) isotopes for tracing metals from the environment to the human body. These recent advances can be highlighted with publications of new research findings on the following topics:

  1. Novel use of traditional radiogenic isotopes such as high-precision Pb isotopes or Sr or Nd isotopes for exploring exposure and metal sources to humans.
  2. Use of Hg and U isotopes for source identification and pathways for human exposure.
  3. Use of non-traditional isotopes, such as Li, Si, Mg, Cr, Fe, Zn, Cu, Mo for deciphering metal sources and pathways from the environment to humans.
  4. Analytical advances in measurements of traditional and non-traditional isotopes in environmental and biological samples.
  5. Theoretical considerations examining fractionation of non-traditional metal isotopes in environmental and biological samples.

In addition, reviews on any of the above topics are also welcomed. The ultimate goal of this Special Issue is to show how we can use isotope information to decipher what controls the abundance and isotopic composition of metals in the modern environment, and ultimately, how these metals enter the human body.

Dr. George D. Kamenov
Dr. Laura S. Ruhl
Guest Editors

Manuscript Submission Information

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Keywords

  • radiogenic isotopes
  • non-traditional metal isotopes
  • isotope tracing
  • environmental exposure
  • metal sources to humans
  • medical geology
  • geology and health
  • isotopic fingerprints

Published Papers (2 papers)

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15 pages, 2199 KiB  
Article
Tracing Copper Migration in the Tongling Area through Copper Isotope Values in Soils and Waters
by Jingwen Su, Ryan Mathur, Glen Brumm, Peter D’Amico, Linda Godfrey, Joaquin Ruiz and Shiming Song
Int. J. Environ. Res. Public Health 2018, 15(12), 2661; https://doi.org/10.3390/ijerph15122661 - 27 Nov 2018
Cited by 11 | Viewed by 3557
Abstract
Copper mining in Tongling has occurred since the Bronze Age, and this area is known as one of the first historic places where copper has been, and is currently, extracted. Multiple studies have demonstrated, through concentrated work on soils and waters, the impact [...] Read more.
Copper mining in Tongling has occurred since the Bronze Age, and this area is known as one of the first historic places where copper has been, and is currently, extracted. Multiple studies have demonstrated, through concentrated work on soils and waters, the impact of mining in the area. Here we present copper isotope values of 13 ore samples, three tailing samples, 20 water samples (surface and groundwater), and 94 soil samples (15 different profiles ranging in depth from 0–2 m) from proximal to distal (up to 10 km) locations radiating from a tailings dam and tailings pile. Oxidation of the copper sulfide minerals results in isotopically heavier oxidized copper. Thus, copper sourced from sulfide minerals has been used to trace copper in mining and environmental applications. At Tongling, higher copper isotope values (greater than 1 per mil, which are interpreted to be derived from copper sulfide weathering) are found both in waters and the upper portions of soils (5–100 cm) within 1 km of the source tailings. At greater than 1 km, the soils do not possess heavier copper isotope values; however, the stream water samples that have low copper concentrations have heavier values up to 6.5 km from the source. The data suggest that copper derived from the mining activities remains relatively proximal in the soils but can be traced in the waters at greater distances. Full article
(This article belongs to the Special Issue Isotopic Fingerprinting of Metals: From Environment to Human Body)
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18 pages, 27122 KiB  
Commentary
Concerns about Quadrupole ICP-MS Lead Isotopic Data and Interpretations in the Environment and Health Fields
by Brian Gulson, George D. Kamenov, William Manton and Michael Rabinowitz
Int. J. Environ. Res. Public Health 2018, 15(4), 723; https://doi.org/10.3390/ijerph15040723 - 11 Apr 2018
Cited by 31 | Viewed by 6321
Abstract
There has been a massive increase in recent years of the use of lead (Pb) isotopes in attempts to better understand sources and pathways of Pb in the environment and in man or experimental animals. Unfortunately, there have been many cases where the [...] Read more.
There has been a massive increase in recent years of the use of lead (Pb) isotopes in attempts to better understand sources and pathways of Pb in the environment and in man or experimental animals. Unfortunately, there have been many cases where the quality of the isotopic data, especially that obtained by quadrupole inductively coupled plasma mass spectrometry (Q-ICP-MS), are questionable, resulting in questionable identification of potential sources, which, in turn, impacts study interpretation and conclusions. We present several cases where the isotopic data have compromised interpretation because of the use of only the major isotopes 208Pb/206Pb and 207Pb/206Pb, or their graphing in other combinations. We also present some examples comparing high precision data from thermal ionization (TIMS) or multi-collector plasma mass spectrometry (MC-ICP-MS) to illustrate the deficiency in the Q-ICP-MS data. In addition, we present cases where Pb isotopic ratios measured on Q-ICP-MS are virtually impossible for terrestrial samples. We also evaluate the Pb isotopic data for rat studies, which had concluded that Pb isotopic fractionation occurs between different organs and suggest that this notion of biological fractionation of Pb as an explanation for isotopic differences is not valid. Overall, the brief review of these case studies shows that Q-ICP-MS as commonly practiced is not a suitable technique for precise and accurate Pb isotopic analysis in the environment and health fields. Full article
(This article belongs to the Special Issue Isotopic Fingerprinting of Metals: From Environment to Human Body)
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