1.8-1.10 - Mass Spectra And Relative Mass

1.8-1.10 - Mass Spectra And Relative Mass

Read the positions and relative heights of mass-spectrum peaks, calculate weighted mean masses and work backwards to isotope abundances. Combining isotope probabilities predicts the molecular-ion pattern of a diatomic molecule; a stated singly charged molecular ion gives its relative molecular mass.

Reading A Mass Spectrum

Peak position identifies mass-to-charge ratio; peak height measures relative abundance. Keep these two readings separate.

The problem

A sample of an element gives two peaks in a mass spectrum:

m/zRelative peak height
3575
3725

The instrument is not saying that one atom has a mass of 35.5. It is saying that two kinds of atom are present, and their ions are detected at different m/zm/z values.

What the instrument data means

For the singly charged isotope ions used here:

  • each peak represents ions of one isotope
  • m/zm/z is mass-to-charge ratio
  • for singly charged ions, m/zm/z has the same numerical value as the isotope mass used in the calculation
  • peak height or peak area represents relative abundance

So a peak at m/z=35m/z = 35 with height 75 means that isotope-35 contributes 75 relative parts to the sample. A peak at m/z=37m/z = 37 with height 25 means isotope-37 contributes 25 relative parts. The relative atomic mass is the weighted mean of those isotope masses, not the middle of the two masses.

Relative atomic mass from a mass spectrum

Ar=∑(isotope mass×relative abundance)∑relative abundanceA_r=\frac{\sum(\text{isotope mass}\times\text{relative abundance})}{\sum\text{relative abundance}}

Use the m/zm/z value of each singly charged isotope peak as the isotope mass and its height or area as the relative abundance. With percentage abundances the denominator is 100; with relative peak heights such as 100 and 32 it is 100+32100 + 32. ArA_r has no units.

Peak position and peak height do different jobs

Each isotope peak's m/zm/z gives the mass of that isotope; its height gives how common it is. A decimal ArA_r is the weighted mean of a mixture of isotope masses (rounded to whole numbers in these examples), not evidence of atoms with fractional numbers of protons or neutrons.

Calculating Relative Atomic Mass

Weight each isotope mass by its abundance, add the contributions and divide by the total abundance.

Worked example: magnesium isotope data

A sample of magnesium contains three isotopes.

IsotopeMass used in calculationRelative abundance / %
X24X2224Mg\ce{^{24}Mg}2478.99
X25X2225Mg\ce{^{25}Mg}2510.00
X26X2226Mg\ce{^{26}Mg}2611.01

Calculate the relative atomic mass of magnesium from these data.

The chemical model is a weighted mean: the most abundant isotope should pull the answer closest to its mass. Here X24X2224Mg\ce{^{24}Mg} is much more common than the other two, so the answer should be just above 24, not near 25.

Ar=[(24×78.99)+(25×10.00)+(26×11.01)]/100A_r = [(24\times 78.99) + (25\times 10.00) + (26\times 11.01)] / 100

Ar=(1895.76+250.00+286.26)/100A_r = (1895.76 + 250.00 + 286.26) / 100

Ar=2432.02/100A_r = 2432.02 / 100

Ar=24.3202A_r = 24.3202

To a sensible number of significant figures:

Ar(Mg)=24.32A_r(\ce{Mg}) = 24.32

The sense check matters. The answer is close to 24 because almost 79% of the atoms are X24X2224Mg\ce{^{24}Mg}.

Same calculation from peak heights

A mass spectrum of element X has these isotope peaks:

m/zRelative peak height
1019.9
1180.1

The heights happen to sum to 100, so the calculation is:

Ar=[(10×19.9)+(11×80.1)]/100A_r = [(10\times 19.9) + (11\times 80.1)] / 100

Ar=(199.0+881.1)/100A_r = (199.0 + 881.1) / 100

Ar=10.801A_r = 10.801

If the heights had been 50 and 201 instead, the chemical mixture would be similar, but the denominator would be 251251.

Arithmetic mean of repeat results

Three equally weighted repeat determinations give relative atomic masses 10.80, 10.84 and 10.82. Their arithmetic mean is (10.80+10.84+10.82)/3=10.82(10.80+10.84+10.82)/3=10.82. Divide by the number of measurements. This is different from weighting isotope masses by unequal isotope abundances; a simple mean of isotope masses works only when their abundances are equal.

Finding Abundance From Relative Atomic Mass

Sometimes the relative atomic mass is known and the isotope abundances are unknown. The model is still the weighted mean, but one abundance becomes the unknown.

Worked example: two isotopes

Element Y has two isotopes, X10X2210Y\ce{^{10}Y} and X11X2211Y\ce{^{11}Y}. Its relative atomic mass is 10.81. Calculate the percentage abundance of each isotope.

Let the percentage abundance of X10X2210Y\ce{^{10}Y} be xx.

Then the percentage abundance of X11X2211Y\ce{^{11}Y} is 100−x100 - x.

Use the weighted mean:

10.81=[10x+11(100−x)]/10010.81 = [10x + 11(100 - x)] / 100

Multiply by 100:

1081=10x+1100−11x1081 = 10x + 1100 - 11x

1081=1100−x1081 = 1100 - x

x=19x = 19

So:

X10X2210Y\ce{^{10}Y} = 19%

X11X2211Y\ce{^{11}Y} = 81%

This is chemically sensible because the relative atomic mass, 10.81, is much closer to 11 than to 10, so the isotope with mass 11 must be more abundant.

Common-error contrast

Tempting but wrong: "10.81 is 81% of the way from 10 to 11, so X10X2210Y\ce{^{10}Y} is 81%."

Correct: being 81% of the way towards mass 11 means the heavier isotope is 81% abundant. The average moves towards the isotope that is more common.

Predicting Diatomic Molecule Spectra

Diatomic molecules create a new layer of reasoning because each molecule contains two atoms. The mass peak for the molecule depends on the isotope combination inside that molecule.

The chlorine pattern

Chlorine has two main isotopes, approximately in a 3:13 : 1 abundance ratio:

X35X2235Cl\ce{^{35}Cl} : X37X2237Cl\ce{^{37}Cl} = 3 : 1

So the probabilities are:

P(X35X2235Cl\ce{^{35}Cl}) = 3/4

P(X37X2237Cl\ce{^{37}Cl}) = 1/4

For chlorine molecules, there are three possible masses:

Molecule ionm/z for singly charged ionProbability routeRelative peak height
X35X2235Cl\ce{^{35}Cl}-X35X2235Cl\ce{^{35}Cl}70(3/4)×(3/4)(3/4)\times (3/4)9
X35X2235Cl\ce{^{35}Cl}-X37X2237Cl\ce{^{37}Cl} or X37X2237Cl\ce{^{37}Cl}-X35X2235Cl\ce{^{35}Cl}722×(3/4)×(1/4)2\times (3/4)\times (1/4)6
X37X2237Cl\ce{^{37}Cl}-X37X2237Cl\ce{^{37}Cl}74(1/4)×(1/4)(1/4)\times (1/4)1

The middle peak is doubled because there are two ways to make a mixed molecule: the lighter isotope can be first or second. The instrument does not care about order, so both mixed combinations contribute to the same m/z=72m/z = 72 peak.

Therefore the predicted molecular-ion peak pattern for ClX2\ce{Cl2} is:

m/z 70 : 72 : 74 = 9 : 6 : 1

Worked comparison: equal isotope abundances

Element E has two isotopes, X79X2279E\ce{^{79}E} and X81X2281E\ce{^{81}E}, in a 1:11 : 1 ratio. The three molecular-ion peaks for EX2\ce{E2} follow from the pair probabilities below.

Masses:

79+79=15879 + 79 = 158

79+81=16079 + 81 = 160

81+81=16281 + 81 = 162

Probabilities:

P(79-79) = 1/2 × 1/2 = 1/4

P(79-81 or 81-79) = 2 × 1/2 × 1/2 = 1/2

P(81-81) = 1/2 × 1/2 = 1/4

So the peak-height ratio is:

m/z 158 : 160 : 162 = 1 : 2 : 1

Common error: atomic and molecular peaks

The ClX2\ce{Cl2} peak at m/z=72m/z = 72 is not evidence for a chlorine isotope with mass 36.

A strong explanation says that m/z=72m/z = 72 comes from one X35X2235Cl\ce{^{35}Cl} atom plus one X37X2237Cl\ce{^{37}Cl} atom in the same molecule. The peak belongs to a molecule ion, not to a single chlorine atom.

[DIAGRAM: asset_name: Chlorine Molecule Mass Spectrum; asset_slug: edexcel_a_level_chemistry_l003_chlorine_molecule_mass_spectrum; recommended_method: matplotlib; description: Predicted mass spectrum for chlorine molecules, showing m/z 70, 72 and 74 peaks with relative peak heights 9, 6 and 1.]
Diagram

Using The Molecular Ion Peak

Mass spectrometry can also give the relative molecular mass of a molecule. In this part of the specification, the allowed reasoning is deliberately narrow: use the m/zm/z value for the molecular ion, MX+\ce{M+}, to find MrM_r.

What MX+\ce{M+} means

Molecular ion, M+

The ion formed when a whole molecule loses one electron without breaking apart.

It forms like this:

M(g)→MX+(g)+eX−\ce{M(g) -> M+(g) + e-}

For a singly charged molecular ion:

m/z of MX+\ce{M+} = relative molecular mass

So if the molecular ion peak is at m/z=46m/z = 46, the molecule has:

Mr=46M_r = 46

This does not by itself prove the full structure of the molecule. Many different molecules can have the same relative molecular mass. Fragment patterns and high-resolution mass spectrometry are later analytical tools; here the focus is the molecular ion peak giving relative molecular mass.

Worked example: do not confuse MX+\ce{M+} with the base peak

A mass spectrum has major peaks at:

m/zRelative intensity
1540
29100
4628

The peak at m/z=29m/z = 29 is the base peak because it is the tallest. The molecular ion peak is stated or identified as MX+\ce{M+} at m/z=46m/z = 46.

Therefore:

Mr=46M_r = 46

The base peak is useful in later organic mass spectrometry because it tells chemists about a stable fragment. For this lesson, the key statement is simply that the MX+\ce{M+} peak gives the relative molecular mass.

Recap

The reasoning chain for mass-spectrometry calculations is compact but very assessable:

  • To calculate ArA_r, use a weighted mean: isotope mass multiplied by relative abundance, divided by total abundance.
  • To find abundance from ArA_r, set up the same weighted mean with one abundance as the unknown.
  • To predict a diatomic molecule spectrum, add isotope masses and use probability to get relative peak heights.
  • To find MrM_r from mass spectrometry for singly charged ions, use the m/zm/z value of the molecular ion, MX+\ce{M+}.

Command words call for a visible route. For calculate, show the weighted mean and denominator. For predict, show both the possible masses and the relative peak-height logic. For determine, identify the molecular ion peak before giving MrM_r.