Overview
ABSTRACT
This article presents the modes of acquisition of noble gas signals in mono- and multi-collection based on the configurations of the latest generation of mass spectrometers. A treatment of the raw data, associated with isobaric interference corrections, is explained to enable calculating a noble gas concentration and isotopic composition in a sample. Several applications based on the measurement of elemental and isotopic compositions of noble gases are given as examples.
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Read the articleAUTHORS
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Laurent ZIMMERMANN: Design Engineer - CNRS - Center for Petrographic and Geochemical Research, Vandœuvre-lès-Nancy, France
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David BEKAERT: Postdoctoral researcher - Department of Marine Chemistry and Geochemistry - Woods Hole Oceanographic Institution - Woods Hole, MA 02543, United States
INTRODUCTION
Noble gases are extremely volatile elements found primarily in the Earth’s surface reservoirs, particularly in the atmosphere. Their elemental and/or isotopic compositions, which cannot be altered by chemical or biological reactions, thus depend on (i) their initial/inherited composition (in other words, the source), (ii) secondary contributions resulting from nuclear reactions (radioactivity, fission, spallation reactions), and/or (iii) mass-dependent fractionation linked to physical processes such as diffusion, evaporation, or condensation. Noble gas geochemistry is primarily used as a dating and tracing tool to shed light on geological processes that would otherwise be impossible to distinguish. It allows, for example, a thorough understanding of the physical processes during volcanic eruptions or the origin of certain fluids, rocks, or minerals. The isotopic composition of noble gases, when well characterized and quantified—whether in the atmosphere, the Earth’s crust, sediments, or the mantle—enables a thorough understanding of the evolution of a geological feature over time and highlights mixing phenomena between multiple reservoirs. Finally, they provide information on the origin and evolution of major volatile elements, such as water, carbon, and nitrogen, which are difficult to trace due to their involvement in chemical and biological reactions during geological processes. Determining when, and in what form(s), these volatile elements became available at the Earth’s surface is crucial for better understanding:
changes in the atmosphere;
the origin and fate of water on Earth;
the creation of conditions conducive to the development of life.
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KEYWORDS
dynamic mass spectrometry | monocollection | multicollection | isobaric interference | isotopic measurements
Analysis of noble gases by static mass spectrometry
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