Mass spectrometry application: relative atomic mass

Mass spectrometry plays a crucial role in determining relative atomic mass by accurately measuring the masses of isotopes in a sample, providing essential data for understanding elemental abundance and chemical properties.

As mention in an earlier article, the relative masses of isotopes can be determined by comparing the charge-to-mass ratio of an isotope of interest with that of carbon-12. For example, mass spectrometric data for the ratio of the mass-to-charge ratio (u/z) of 2H to that of 12C is 0.167842. Thus, the relative mass of 2H on the carbon-12 unified atomic mass unit scale is:

u\; of \; ^{2}H=\frac{u/z\; of\;\; ^2H}{u/z\; of\; \; ^{12}C}\; \times \; u\; of\; ^{12}C

u\; of \; ^{2}H=0.167842\times 12\, u

u\; of \; ^{2}H=2.014104\, u

Consequently, the relative atomic mass of an element can be calculated from its isotopic abundance spectrum.

With reference to the spectrum above, the relative atomic mass of chlorine is:

A_{r,Cl}=\frac{100\times 34.969}{100+31.96}+\frac{31.96\times 36.966}{100+31.96}=35.45

Question

With reference to the table below, deduce the spectrum for the chlorine gas ion, Cl2+.

Isotope

Relative isotopic mass

Relative abundance, %

35Cl

35

75.78

37Cl

37

24.22

Answer

Assuming a random distribution of isotopes in the sample of chlorine gas used and that no fragmentation occurred, the possible permutations of chlorine isotopes in a chlorine gas ion are:

Permutation, XClYCl+

Relative isotopic mass

No. of permutations

35Cl35Cl

70

1

35Cl37Cl or 37Cl35Cl

72

2

37Cl37Cl

74

1

The probability of observing each permutation is:

Permutation, XClYCl+

Probability = abundance X x abundance Y x no. of permutations

35Cl35Cl

0.7578 x 0.7578 x 1 = 0.5742

35Cl37Cl or 37Cl35Cl

0.7578 x 0.2422 x 2 = 0.3671

37Cl37Cl

0.2422 x 0.2422 x 1 = 0.0587

Hence, the spectrum has the following characteristics:

Permutation

Relative isotopic mass Relative abundance (%)

% of predominant peak

35Cl35Cl

70 57.42

100.00

35Cl37Cl or 37Cl35Cl

72 36.71

63.93

37Cl37Cl

74 5.87

10.22

The values for ‘% of predominant peak’ are calculated relative to the abundance of 35Cl35Cl.

 

Here’s another way to explain the permutation of isotopes in chlorine gas:

Chlorine gas is formed by the collision of two chlorine atoms. Consider an infinitesimal two-dimensional space in a vessel that is filled with chlorine atoms, with the space large enough to accommodate two chlorine atoms (see diagram below).

If we further consider a single axis of collision through that space, and that chlorine atoms are approaching the space along that axis from the left and from the right, we end up with four possible products: 35Cl35Cl, 35Cl37Cl, 37Cl35Cl and 37Cl37Cl. If the abundances of 35Cl and 37Cl are equal, we have twice as many chlorine molecules with mixed isotopes than 35Cl35Cl or 37Cl37Cl, i.e. in the ratio of 2:1:1. If the abundances of 35Cl and 37Cl are unequal, we multiply the numbers in the ratio with the respective abundances of isotopes to get the probabilities of occurrence of the three molecular species. The same result is obtained if we rotate the axis of collision in any direction in three dimensions, or if the collision happens at an angle.

 

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