Intuition What this page is for
The parent note gave you the formula A r = ∑ i m i f i and three clean examples. But real problems come in flavours: forwards, backwards, three isotopes, percentages that don't sum to 100, a degenerate "one isotope only" case, a word problem, and a sneaky exam twist. This page walks every one of them so you never meet a version you haven't already seen.
Read the scenario matrix first. Then each worked example is tagged with the exact cell it fills.
Every problem this topic can throw at you is one of these cell classes:
Cell
Case class
What is unknown?
The twist
A
Forward, 2 isotopes, % given
A r
none — the baseline
B
Forward, 3+ isotopes
A r
more terms to add
C
Backward, solve for abundance
one f i
one equation, one constraint
D
Percentages don't sum to 100
A r
must divide by the real total
E
Degenerate: single isotope
A r
answer is that isotope's mass
F
Limiting / bounds check
is my answer sane?
must lie between the extremes
G
Word problem (marbles / real sample)
A r or count
translate words → m i , f i
H
Exam twist: mass number vs true mass, or missing isotope
A r or a missing f
don't confuse A with m ; fill the gap
The examples below hit cells A, B, C, D, E, F, G, H in order. Symbols used everywhere:
Definition Symbols on this page (all earned in the parent note)
m i ::: the true measured isotopic mass of isotope i , in atomic mass units u .
f i ::: the fractional abundance (a number between 0 and 1) of isotope i ; all the f i add to 1.
p i ::: the same abundance written as a percentage (p i = 100 f i ).
A r ::: the abundance-weighted average mass, the number on the periodic table.
Worked example Copper (Cell A)
63 Cu: mass = 62.930 u, abundance = 69.15% .
65 Cu: mass = 64.928 u, abundance = 30.85% .
Find A r .
Forecast: Both percentages sum to 100 . 63 Cu is roughly twice as common, so guess an answer nearer 63 than 65 — around 63.5 ?
Step 1 — Multiply each mass by its percentage.
Why this step? A weighted average lets the abundant isotope "vote" more; multiplying by the abundance is the vote.
62.930 × 69.15 = 4351.6 , 64.928 × 30.85 = 2003.0
Step 2 — Add the votes and divide by the total weight (100).
Why this step? The percentages add to 100 , so dividing by 100 turns the total back into a per-atom average (the /100 is the "÷ total weight" from the parent derivation).
A r = 100 4351.6 + 2003.0 = 100 6354.6 = 63.55 u
Verify: 63.55 lies between 62.930 and 64.928 ✔️ and leans toward the lighter, more abundant isotope ✔️. The periodic table lists Cu as 63.55 — match.
Worked example Silicon (Cell B)
28 Si (27.977 u, 92.23%), 29 Si (28.976 u, 4.67%), 30 Si (29.974 u, 3.10%). Find A r .
Forecast: 28 Si is over 92% of the sample. The answer must sit very close to 27.977 , only nudged up a hair by the rare heavier isotopes.
Step 1 — One term per isotope.
Why this step? Mass is additive: the total mass of the bucket is every isotope's contribution added together. Three isotopes → three terms.
27.977 × 92.23 = 2580.4
28.976 × 4.67 = 135.3
29.974 × 3.10 = 92.9
Step 2 — Sum and divide by 100.
Why this step? Same normalisation as Cell A — the percentages total 100 , so divide by 100 .
A r = 100 2580.4 + 135.3 + 92.9 = 100 2808.6 = 28.09 u
Verify: 28.09 sits just above 27.977 , exactly as forecast ✔️. Periodic table: Si = 28.09 — match.
Worked example Gallium — find the percentages (Cell C)
Gallium has 69 Ga (68.926 u) and 71 Ga (70.925 u) and a known A r = 69.723 u. What is the percent abundance of each?
Forecast: 69.723 is closer to 68.926 (the light one). So the light isotope must be the majority — expect 69 Ga above 50%.
Step 1 — Use one variable for both abundances.
Why this step? The two fractions must sum to 1, so if f is the fraction of 69 Ga, then 71 Ga is 1 − f . One constraint kills one unknown.
A r = 68.926 f + 70.925 ( 1 − f )
Step 2 — Expand and collect.
Why this step? We want f alone, so gather the f terms.
69.723 = 70.925 − 1.999 f
Step 3 — Solve for f .
Why this step? Basic algebra: isolate f .
1.999 f = 70.925 − 69.723 = 1.202 ⇒ f = 1.999 1.202 = 0.601
So 69 Ga ≈ 60.1% and 71 Ga ≈ 39.9% .
Verify: plug back — 68.926 ( 0.601 ) + 70.925 ( 0.399 ) = 69.72 ✔️, and the light isotope is indeed the majority as forecast ✔️.
Worked example A trace-contaminated reading (Cell D)
A mass-spectrometry readout gives isotope X-63 (62.930 u, 68.50%) and X-65 (64.928 u, 30.50%). These sum to only 99.00% (the missing 1% was unreadable noise). Estimate A r from the two clean peaks.
Forecast: If we lazily divide by 100 we'd get an answer that's slightly too small , because we'd be treating the missing 1% as if it had zero mass. Dividing by the true total (99) fixes this.
Step 1 — Compute the weighted sum.
Why this step? Same numerator as always: mass × its weight, summed.
62.930 × 68.50 = 4310.7 , 64.928 × 30.50 = 1980.3
sum = 6291.0
Step 2 — Divide by the actual total weight, not 100.
Why this step? A proper average divides by the sum of the weights you actually used. Here that sum is 99.00 , not 100 . This is the A r = ∑ p i ∑ m i p i form.
A r = 99.00 6291.0 = 63.55 u
Verify: if we'd wrongly divided by 100 we'd get 62.91 — too low, and outside the range near the light isotope. Dividing by 99 gives 63.55 , safely between 62.930 and 64.928 ✔️.
Common mistake The dangerous shortcut in Cell D
Dividing by 100 when your data only sums to 99 silently pretends the missing atoms weigh nothing. Always divide by ∑ p i .
Worked example Fluorine — a single stable isotope (Cell E)
Fluorine in nature is essentially 100% 19 F (18.998 u). What is A r ?
Forecast: With one isotope there is nothing to average against — the answer must be that isotope's own mass.
Step 1 — Apply the formula with f = 1 .
Why this step? The general formula still works; the single fraction is 1 .
A r = 18.998 × 1 = 18.998 u
Verify: the "average" of a single number is itself ✔️. This is the boundary case that shows a weighted average never breaks — even with one term it gives the sensible answer.
Intuition Why this degenerate case matters
It's the sanity anchor for the "answer lies between the extremes" rule (Cell F): when there's only one extreme, the average is that extreme.
The weighted average is a slider. As the light isotope's fraction f runs from 0 to 1 , A r slides from the heavy mass all the way down to the light mass. The picture below shows this straight-line slide for chlorine (35 Cl at 34.969 u, 37 Cl at 36.966 u).
Worked example Reading the limits off the line (Cell F)
Using A r ( f ) = 34.969 f + 36.966 ( 1 − f ) for chlorine, evaluate the three landmark points f = 0 , f = 0.5 , f = 0.7577 .
Forecast: at f = 0 (no light atoms) the answer must be the heavy mass 36.966 ; at f = 1 the light mass 34.969 ; at f = 0.5 the plain midpoint.
Step 1 — f = 0 (all heavy).
Why this step? It tests the top of the slider.
A r = 34.969 ( 0 ) + 36.966 ( 1 ) = 36.966 u
Step 2 — f = 0.5 (equal mix).
Why this step? Equal abundances is the only case where the naive midpoint is correct.
A r = 34.969 ( 0.5 ) + 36.966 ( 0.5 ) = 35.968 u
Step 3 — f = 0.7577 (natural chlorine).
Why this step? The real-world value — it must sit low, near 35 .
A r = 34.969 ( 0.7577 ) + 36.966 ( 0.2423 ) = 35.453 u
Verify: all three lie in [ 34.969 , 36.966 ] ✔️, and they decrease as f (fraction of light isotope) increases ✔️ — exactly the downward line in the figure.
Worked example The marble bag made real (Cell G)
A tray holds 5000 atoms of element Z. Analysis shows 3800 are 85 Z (84.912 u) and the rest are 87 Z (86.909 u). Find A r without first converting to percentages.
Forecast: most atoms (3800/5000 = 76% ) are the light one, so A r leans toward 84.9 .
Step 1 — Turn counts into fractions.
Why this step? Fraction = count ÷ total. This is the "fraction × total = count" step from the parent derivation, run backwards.
f 85 = 5000 3800 = 0.760 , f 87 = 5000 5000 − 3800 = 5000 1200 = 0.240
Step 2 — Weighted sum with fractions (no /100 needed).
Why this step? Fractions already sum to 1 , so we do not divide by anything — that's the beauty of the fraction form.
A r = 84.912 ( 0.760 ) + 86.909 ( 0.240 )
= 64.533 + 20.858 = 85.39 u
Verify: answer sits between 84.912 and 86.909 and near the light end ✔️. (This element is rubidium; true A r ≈ 85.47 — our tray's proportions are close to nature.)
Mnemonic Fractions vs percentages
Fractions already sum to 1 → just multiply and add . Percentages sum to 100 → multiply, add, then ÷ 100 (or ÷ ∑ p ).
Worked example Three isotopes, one abundance hidden (Cell H)
Element M has three isotopes with true masses 23.985 , 24.986 , 25.983 u. You are told the first is 79.00% and the second is 10.00% , and that A r = 24.31 u. Find the percentage of the third isotope — and note why you must not just use mass numbers 24 , 25 , 26 .
Forecast: the three abundances must sum to 100 , so the third is 100 − 79 − 10 = 11% . But the question wants us to derive it from A r to confirm consistency.
Step 1 — Name the unknown.
Why this step? Let p 3 be the missing percentage. The constraint ∑ p i = 100 is available, but let's confirm it via A r instead.
Step 2 — Write the A r equation with the unknown.
Why this step? A r ties all three isotopes together.
24.31 = 100 23.985 ( 79.00 ) + 24.986 ( 10.00 ) + 25.983 p 3
Step 3 — Isolate p 3 .
Why this step? Standard algebra. First the known part of the numerator:
23.985 ( 79.00 ) = 1894.8 , 24.986 ( 10.00 ) = 249.86
2431 = 1894.8 + 249.86 + 25.983 p 3
25.983 p 3 = 2431 − 2144.66 = 286.34 ⇒ p 3 = 25.983 286.34 = 11.02
So the third isotope is ≈ 11% ✔️ (matches 100 − 79 − 10 ).
The mass-number trap: if you had used 24 , 25 , 26 (mass numbers) instead of the true masses, the sum 100 24 ( 79 ) + 25 ( 10 ) + 26 ( 11 ) = 24.32 would come out slightly wrong . Mass number A is a whole-number count of nucleons; the true isotopic mass is a hair smaller because of nuclear binding-energy mass defect . Use the true masses when given.
Verify: with p 3 = 11.02 , A r = 100 1894.8 + 249.86 + 25.983 ( 11.02 ) = 24.31 ✔️, and 79 + 10 + 11.02 = 100.02 ≈ 100 ✔️.
Recall Which cell is each of these?
a) "Element has isotopes at 20% and 80%, find atomic mass." ::: Cell A (forward, 2 isotopes).
b) "Given A r , find how much of each isotope." ::: Cell C (backward).
c) "Peaks sum to 98%." ::: Cell D (divide by ∑ p , not 100).
d) "Element has one stable isotope." ::: Cell E (degenerate; A r = that mass).
Recall Blitz answers
Copper A r ? ::: 63.55 u
Silicon A r ? ::: 28.09 u
Gallium 69 Ga fraction? ::: ≈ 0.601 (60.1% )
Element Z (word problem) A r ? ::: 85.39 u
← Back to the topic note
Weighted Average (mathematics) — the slider behind Cell F.
Mass Spectrometry — where the noisy Cell D percentages come from.
Isotopes and Mass Number — the mass-number trap in Cell H.
Nuclear Binding Energy and Mass Defect — why true mass < mass number.
Atomic Mass Unit (u) and the Carbon-12 standard — the unit on every answer.