Isotope-ratio mass spectrometry

Isotope-ratio mass spectrometry
Magnetic sector mass spectrometer used in isotope ratio analysis, through thermal ionization.
AcronymIRMS
Classificationmass spectrometry

Isotope-ratio mass spectrometry (IRMS) is a specialization of mass spectrometry, in which mass spectrometric methods are used to measure the relative abundance of isotopes in a given sample.[1][2]

This technique has two different applications in the earth and environmental sciences. The analysis of 'stable isotopes' is normally concerned with measuring isotopic variations arising from mass-dependent isotopic fractionation in natural systems. On the other hand, radiogenic isotope analysis[3] involves measuring the abundances of decay-products of natural radioactivity, and is used in most long-lived radiometric dating methods.

  1. ^ Paul D, Skrzypek G, Fórizs I (2007). "Normalization of measured stable isotopic compositions to isotope reference scales - a review". Rapid Commun. Mass Spectrom. 21 (18): 3006–14. Bibcode:2007RCMS...21.3006P. doi:10.1002/rcm.3185. PMID 17705258.
  2. ^ Stellaard F, Elzinga H (2005). "Analytical techniques in biomedical stable isotope applications: (isotope ratio) mass spectrometry or infrared spectrometry?". Isotopes in Environmental and Health Studies. 41 (4): 345–61. doi:10.1080/10256010500384333. PMID 16543190.
  3. ^ Dickin, A.P. (2005). Radiogenic Isotope Geology. Cambridge University Press. Archived from the original on 2014-03-27. Retrieved 2008-10-09.

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