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Related Concept Videos

Inductively Coupled Plasma–Mass Spectrometry (ICP–MS): Overview01:19

Inductively Coupled Plasma–Mass Spectrometry (ICP–MS): Overview

In inductively coupled plasma–mass spectrometry (ICP–MS), an inductively coupled plasma (ICP) torch is used as an atomizer and ionizer. Solid samples are dissolved and volatilized before being introduced into the high-temperature argon plasma, while solution samples are nebulized and passed through the high-temperature argon plasma. Plasma dissociates the analytes and ionizes their component atoms to form a mixture of positive ions and molecular species. The positive ions are then passed on to...
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Inductively Coupled Plasma-Mass Spectrometry (ICP-MS): Interferences

Inductively coupled plasma–mass spectrometry (ICP–MS) is a highly selective and sensitive technique for accurate elemental analysis. Though the analysis of ICP–MS mass spectra is comparatively straightforward, it is affected by spectroscopic and non-spectroscopic interferences. Spectroscopic interferences arise when the plasma contains ionic species with an m/z value the same as the analyte ion. Spectroscopic interference can be categorized as isobaric, polyatomic ions, and refractory oxide ion...
High-Resolution Mass Spectrometry (HRMS)01:15

High-Resolution Mass Spectrometry (HRMS)

The resolution of a mass spectrometer depends on the efficiency of separating ions with different ion masses. The mass of an atom is approximated to the sum of the masses of protons and neutrons inside, considering the masses of protons and neutrons as equal. However, the masses of the proton (1.6726 × 10−24 g) and neutron (1.6749 × 10−24 g) are not truly equal. There is a minor error in the expression of atomic masses relative to the simplest atom of hydrogen. For example, the mass of helium...
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Most elements exist in nature as a mixture of isotopes. The isotopes differ in weight due to their respective number of neutrons. The molecular weight of a molecule is different depending on the specific isotope of its elements involved. As a result, the mass spectrum of the molecule exhibits peaks from the same fragment at multiple positions. The positions of these mass signals depend on the mass differences between isotopes. Furthermore, the intensity of these signals is dependent on the...
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The probability of having two carbon-13 atoms next to each other is negligible because of the low natural abundance of carbon-13. Consequently, peak splitting due to carbon-carbon spin-spin coupling is not observed in spectra. However, protons up to three sigma bonds away split the carbon signal according to the n+1 rule, resulting in complicated spectra.
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Carbon-13 (¹³C) NMR: Overview01:10

Carbon-13 (¹³C) NMR: Overview

Carbon-13 is a naturally occurring NMR-active isotope of carbon with a low natural abundance of 1.1%. In contrast, carbon-12 is the most abundant isotope of carbon with zero nuclear spin. Therefore, it is NMR inactive. The gyromagnetic ratio of carbon-13 is smaller than that of protons. As a result, carbon-13 resonance is about 6000 times weaker than proton resonance. For a given magnetic field strength, the resonance frequency of carbon-13 is about one-fourth of the resonance frequency for...

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Precise and traceable (13)C/(12)C isotope amount ratios by multicollector ICPMS.

Rebeca Santamaria-Fernandez1, David Carter, Ruth Hearn

  • 1LGC, Queens Road, Teddington, Middlesex, TW11 0LY, UK. rsf@lgc.co.uk

Analytical Chemistry
|June 21, 2008
PubMed
Summary

A new method uses multicollector inductively coupled mass spectrometry (MC-ICPMS) for precise SI-traceable carbon isotope measurements. This technique simplifies sample preparation and offers accurate analysis of carbon isotope ratios in diverse materials.

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Area of Science:

  • Analytical Chemistry
  • Geochemistry
  • Environmental Science

Background:

  • Accurate measurement of carbon isotope amount ratios is crucial for various scientific disciplines.
  • Existing methods, like gas source isotope ratio mass spectrometry, can be complex and require extensive sample preparation.
  • The need for a simpler, more direct method for SI-traceable carbon isotope analysis is evident.

Purpose of the Study:

  • To introduce and validate a novel method for measuring SI-traceable carbon isotope amount ratios using multicollector inductively coupled mass spectrometry (MC-ICPMS).
  • To demonstrate the accuracy and reliability of the MC-ICPMS method across a range of carbon isotope ratios.
  • To highlight the advantages of the new method over conventional techniques.

Main Methods:

  • Utilized multicollector inductively coupled mass spectrometry (MC-ICPMS) for carbon isotope ratio measurements.
  • Employed internal normalization using boron (11)B/(10)B isotope ratios to correct for instrumental mass bias.
  • Calculated full uncertainty budgets using the Kragten approach for absolute ratio determination.

Main Results:

  • Successfully measured carbon (13)C/(12)C isotope amount ratios for four NIST reference materials with high accuracy (0.06-0.20% deviation from reference values).
  • Achieved excellent linearity (R = 0.9997) across the measured range, suitable for natural variations in carbon compounds.
  • Demonstrated excellent agreement with conventional dual inlet isotope ratio mass spectrometry (IRMS) measurements for a CO2 gas sample.

Conclusions:

  • The developed MC-ICPMS method provides accurate, SI-traceable carbon isotope amount ratios with uncertainties < 0.1%.
  • The method simplifies sample preparation by allowing direct measurement of organic compounds without derivatization or combustion.
  • This novel technique offers a versatile and efficient approach for analyzing carbon isotope ratios in a wide array of samples.