Intuition Why this page exists
The parent note gave you the formula α = K a / C and two clean examples. But real problems come in many flavours : sometimes the shortcut works, sometimes it explodes, sometimes the acid is so weak or so dilute that water itself joins in. This page walks through one worked example per flavour so no exam question can surprise you.
Before we start, let us name the four quantities we will juggle, each with its plain meaning:
C = how many moles of acid you dissolved per litre (the "crowding").
α = the fraction that actually split into ions (a number between 0 and 1 ).
K a = the fixed "eagerness to split" — depends only on temperature, never on how much you dissolved.
[ H + ] = the actual concentration of hydrogen ions floating around, = C α .
Every Ostwald problem lands in one of these cells. The rest of the page fills each cell with a worked example.
Cell
Situation
Which tool?
Danger
A
Normal weak acid, α < 5%
Simple α = K a / C
none
B
Dilution comparison (same acid, two C )
Ratio trick α ∝ 1/ C
thinking pH falls
C
α turns out large (> 5% )
Full quadratic K a = 1 − α C α 2
using shortcut anyway
D
Reverse problem: given α , find K a or C
Rearrange the exact formula
using approximate one
E
Limiting / degenerate: C → 0 , or extremely dilute
Watch α → 1 ; water's own [ H + ] matters
formula predicting α > 1
F
Strong acid mistakenly fed in
Don't use Ostwald; [ H + ] = C
α > 1 nonsense
G
Real-world word problem (vinegar)
Translate words → C , K a
unit slips
H
Exam twist: percent ionisation given, find pH from scratch
chain α → [ H + ] → pH
forgetting C
The figure above plots α against C on a log axis. Notice the cyan curve (the exact answer) hugging the white dashed line (the shortcut) at high C , then peeling away toward α = 1 as we dilute — that peel-off region is exactly cells C and E .
Worked example A · 0.05 M formic acid,
K a = 1.8 × 1 0 − 4
Forecast: guess — will α be above or below 5% ? (Formic is ~10× stronger than acetic.)
Step 1. Apply the shortcut α = K a / C .
α = 0.05 1.8 × 1 0 − 4 = 3.6 × 1 0 − 3 = 0.0600
Why this step? The shortcut is the fastest route when we can trust it — we test that next.
Step 2. Check the 5% rule. α = 6.0% > 5% .
Why this step? The shortcut secretly assumed 1 − α ≈ 1 . At 6% that assumption is already fraying, so we should refine — this actually pushes us into cell C territory. Keep this in mind; we redo it properly in Example C.
Verify: plug α = 0.06 back into the exact law: 1 − α C α 2 = 0.94 0.05 × 0.0036 = 1.91 × 1 0 − 4 , slightly above the true 1.8 × 1 0 − 4 — confirming the shortcut over-estimates α here. Lesson: always run the 5% test.
Worked example A(clean) · 0.2 M acetic acid,
K a = 1.8 × 1 0 − 5
Forecast: more concentrated than the parent's 0.1 M example — so α smaller or larger?
Step 1. α = 0.2 1.8 × 1 0 − 5 = 9 × 1 0 − 5 = 9.49 × 1 0 − 3 .
Why: direct shortcut.
Step 2. 5% test: 0.95% ≪ 5% ✓ — the shortcut is trustworthy.
Why: denominator 1 − α = 0.99 really is ≈ 1 .
Step 3. [ H + ] = C α = 0.2 × 9.49 × 1 0 − 3 = 1.90 × 1 0 − 3 M.
pH = − log ( 1.90 × 1 0 − 3 ) = 2.72
Why this step? pH is what an exam or a pH-meter actually reports; − log [ H + ] turns the raw ion concentration into that familiar acidity scale.
Verify: shortcut [ H + ] = K a C = 1.8 × 1 0 − 5 × 0.2 = 3.6 × 1 0 − 6 = 1.90 × 1 0 − 3 ✓ — matches to 3 s.f.
Worked example B · Take the 0.2 M acetic acid above and dilute 100×
Forecast: α goes UP by roughly which factor? And does pH go up or down?
Step 1. New concentration C = 0.002 M. Ratio trick: since α ∝ 1/ C , diluting 100 × multiplies α by 100 = 10 .
α new = 9.49 × 1 0 − 3 × 10 = 9.49 × 1 0 − 2 = 9.49%
Why this step? We avoid a fresh square root by exploiting the proportionality — but note 9.49% > 5% , so this is now cell C and the answer is an over-estimate.
Step 2. [ H + ] = K a C = 1.8 × 1 0 − 5 × 0.002 = 3.6 × 1 0 − 8 = 1.90 × 1 0 − 4 M.
Why: to test the pH trap we need the actual ion count, not the percentage.
Step 3. pH = − log ( 1.90 × 1 0 − 4 ) = 3.72 .
Why this step: compare with the original pH = 2.72 .
The lesson (Mistake-buster): α rose 10 × , yet pH rose from 2.72 to 3.72 — the solution became less acidic. Percent-ionised went up; total ions per litre went down.
Verify: Δ pH = 3.72 − 2.72 = 1.00 . Since [ H + ] ∝ C and C fell 100 × , [ H + ] falls 10 × , so pH rises by exactly log 10 = 1.00 ✓.
Worked example C · 0.001 M HF,
K a = 6.8 × 1 0 − 4 (the parent's Example 3, done exactly)
Forecast: the shortcut screams α = 0.68 = 0.825 . Do you trust 82.5% ?
Step 1. Reject the shortcut. α = 0.825 > 5% badly, and 1 − α = 0.175 is nowhere near 1 .
Why this step? Using the shortcut here would double-count ions that no longer exist as HA.
Step 2. Write the exact law and clear the fraction:
K a = 1 − α C α 2 ⇒ C α 2 + K a α − K a = 0.
Plug numbers: 0.001 α 2 + 6.8 × 1 0 − 4 α − 6.8 × 1 0 − 4 = 0 .
Why: a quadratic in α keeps the depletion of HA honest.
Step 3. Quadratic formula, taking the positive root (a fraction can't be negative):
α = 2 ( 0.001 ) − 6.8 × 1 0 − 4 + ( 6.8 × 1 0 − 4 ) 2 + 4 ( 0.001 ) ( 6.8 × 1 0 − 4 ) = 0.552
Why the positive root? α lives in [ 0 , 1 ] ; the negative root is physically meaningless.
Verify: put α = 0.552 back: 1 − 0.552 0.001 × 0.55 2 2 = 0.448 3.05 × 1 0 − 4 = 6.80 × 1 0 − 4 = K a ✓. The true α is ≈ 55% , far below the fake 82.5% .
Worked example D · A 0.10 M weak acid is measured to be
3.0% ionised. Find K a .
Forecast: will you use the simple or the exact formula? (3% < 5% …)
Step 1. α = 0.030 , C = 0.10 . Since α < 5% , the simple K a = C α 2 is safe.
Why this step? We were given α directly, so no square root is needed — just multiply.
K a = C α 2 = 0.10 × ( 0.030 ) 2 = 0.10 × 9 × 1 0 − 4 = 9.0 × 1 0 − 5
Step 2 (rigor check). Compute with the exact formula for comparison:
K a exact = 1 − α C α 2 = 0.97 9 × 1 0 − 5 = 9.28 × 1 0 − 5
Why: to show the 3% error the approximation introduces — small, as promised.
Verify: the two K a values differ by ( 9.28 − 9.0 ) /9.28 = 3.0% — exactly the α value, since the fractional error of the shortcut is ≈ α . Neat sanity check ✓.
Worked example E · Push acetic acid toward infinite dilution
Forecast: the formula says α = K a / C → ∞ as C → 0 . But α can't exceed 1 . What actually happens?
Step 1. Find the C at which the shortcut would (falsely) reach α = 1 :
set K a / C = 1 ⇒ C = K a = 1.8 × 1 0 − 5 M.
Why this step? This marks where the shortcut breaks down completely — below it the shortcut is nonsense.
Step 2. For C ≪ K a the acid is essentially fully ionised : α → 1 , so [ H + ] → C .
Why: physically, with so few acid molecules and so much water, every molecule finds room to split.
Step 3 (the real degeneracy). Take C = 1 0 − 8 M. Even fully ionised that gives only 1 0 − 8 M of H + from the acid — less than water's own 1 0 − 7 M. So the pH is set by water , not the acid: pH ≈ 7 (slightly below), NOT 8 .
Why: Ostwald's law ignores water's autoionisation; at extreme dilution you must add it back.
Verify: a full water-inclusive calc for 1 0 − 8 M strong-ish acid gives [ H + ] ≈ 1.05 × 1 0 − 7 , pH ≈ 6.98 — acidic, never basic ✓. The naive pH = 2 1 ( p K a − log C ) would give a wrong pH > 7 .
Worked example F · Someone writes "
α = K a / C for 0.1 M HCl."
Forecast: HCl's K a ≈ 1 0 6 . What does the formula spit out?
Step 1. α = 1 0 6 /0.1 = 1 0 7 ≈ 3160 .
Why this step? To expose the absurdity: a fraction came out as 3160 .
Step 2. Since α ≤ 1 always, the formula is invalid here. Strong acids have α ≈ 1 by definition.
Why: Ostwald's derivation assumed α ≪ 1 (that's how 1 − α ≈ 1 entered). Strong acids violate the premise from line one.
Step 3. Correct treatment: [ H + ] = C = 0.1 M, so pH = − log ( 0.1 ) = 1.00 .
Why this step? With α = 1 every acid molecule donates one H + , so [ H + ] simply equals C ; taking − log converts that to the reported pH.
Verify: pH of 0.1 M strong acid is exactly 1.00 ✓. Rule: if K a / C > 0.05 , stop and reconsider.
Worked example G · Household vinegar is
5.0% acetic acid by mass; density ≈ 1.0 g/mL. Find its pH. (K a = 1.8 × 1 0 − 5 , molar mass 60 g/mol.)
Forecast: vinegar tastes sharply sour — guess pH between 2 and 3 .
Step 1. Convert "5% by mass" to molarity. In 1 L = 1000 g solution, mass of acid = 50 g.
Why this step? Ostwald needs C in mol/L; the label gives mass.
C = 60 g/mol 50 g ÷ 1 L = 0.833 M
Step 2. α = K a / C = 1.8 × 1 0 − 5 /0.833 = 2.16 × 1 0 − 5 = 4.65 × 1 0 − 3 .
Why: 0.47% ≪ 5% , shortcut valid.
Step 3. [ H + ] = K a C = 1.8 × 1 0 − 5 × 0.833 = 1.50 × 1 0 − 5 = 3.87 × 1 0 − 3 M.
pH = − log ( 3.87 × 1 0 − 3 ) = 2.41
Why this step? The question asked for pH, the everyday measure of sourness; − log [ H + ] is the bridge from ion concentration to that number.
Verify: [ H + ] = C α = 0.833 × 4.65 × 1 0 − 3 = 3.87 × 1 0 − 3 ✓, and the pH 2.41 sits in the forecast band 2 –3 ✓. Real vinegar measures pH ≈ 2.4 –2.9 — spot on.
0.25 M weak acid is 2.0% ionised. Find pH and p K a .
Forecast: you're handed α — no square root needed. Chain straight to [ H + ] .
Step 1. α = 0.020 . [ H + ] = C α = 0.25 × 0.020 = 5.0 × 1 0 − 3 M.
Why this step? pH depends on the ion count, which is C α regardless of how α was found.
Step 2. pH = − log ( 5.0 × 1 0 − 3 ) = 2.30 .
Why this step? The exam asks for pH; applying − log to the [ H + ] from Step 1 converts the ion concentration into the acidity scale it wants.
Step 3. K a = C α 2 = 0.25 × ( 0.020 ) 2 = 0.25 × 4 × 1 0 − 4 = 1.0 × 1 0 − 4 , so p K a = − log ( 1 0 − 4 ) = 4.00 .
Why: the twist rewards you for knowing both α and C pin down K a .
Verify: cross-check via pH = 2 1 ( p K a − log C ) = 2 1 ( 4.00 − log 0.25 ) = 2 1 ( 4.00 + 0.602 ) = 2.30 ✓ — the two independent routes agree.
Recall What triggers the quadratic instead of the shortcut?
When α = K a / C exceeds 0.05 (i.e. K a / C > 2.5 × 1 0 − 3 ). Then use C α 2 + K a α − K a = 0 .
When you dilute a weak acid 100 × , by what factor does α rise? Vinegar 5% by mass, density 1 g/mL — what is its molarity? 50 g /60 g mol − 1 = 0.833 M.
Why does the Ostwald formula give α > 1 for strong acids? Its derivation assumed α ≪ 1 so that 1 − α ≈ 1 ; strong acids break that premise, so the result is meaningless — use [ H + ] = C .
At C = 1 0 − 8 M, why isn't the pH above 7? The acid contributes fewer H + than water's own 1 0 − 7 M, so water sets the pH near (just below) 7 — the acid can never make it basic.
Connections:
Common Ion Effect : cell D/H reverse-solve if [ A − ] is spiked.
pH Calculation Methods : cells C and E are exactly where the shortcut is replaced by full methods.
Le Chatelier's Principle : cell B's dilution shift explained.
Buffer Capacity and Henderson-Hasselbalch Equation : what happens once α nears 0.5 .