General Chemistry · Aqueous Equilibria · BUFFER ACTION

Buffer action — same NaOH, different pH change

Add 5.0 mL of 4.0 M NaOH to 1 L of pure water and to 1 L of an acetic acid buffer solution, side by side. The pH of both beakers is calculated by solving the charge-balance equation exactly. Dilute the buffer components or add more base, and find for yourself the moment when the buffer capacity breaks down.

Learning objectives After this activity you can …
explain, from the reactions of the components, the difference in pH change when the same OH⁻ is added to a buffer and to water.
calculate the pH of a buffer after adding a strong base in two steps: stoichiometry → equilibrium.
show by experiment how the amount of buffer components relates to the buffer capacity.

Estimated time 15–20 min · Prerequisites: pH and pOH, Ka of a weak acid, amounts in neutralization reactions (limiting reactant)

Progress 0% · Predict → Observe → Check → Complete

Two beakers compared

Buffer pH —
ΔpH —
Pure water pH —
ΔpH —

Amounts of components (bars)

Stoichiometry step (mol after reaction)—

pH vs volume added (solid: buffer · dashed: water)

Point where a buffer component is used up (vertical dotted line)—
Entry check Before you start — prerequisites and key terms

What happens when OH⁻ from a strong base meets the weak acid CH₃COOH?

They react almost completely to form CH₃COO⁻ and H₂O It is a weak acid, so they do not react Only half reacts, then it stops at equilibrium
Key terms

Buffer solution: a solution that contains a weak acid and its conjugate base (or a weak base and its conjugate acid) in similar amounts, so its pH changes little when a small amount of strong acid or strong base is added. · Conjugate acid–base pair: HA/A⁻, which differ by one H⁺ (here CH₃COOH/CH₃COO⁻). · Henderson–Hasselbalch equation: pH = pKa + log([A⁻]/[HA]). · Buffer capacity: the amount of strong acid or strong base a buffer can take up before its pH changes greatly. · Charge balance: total positive charge = total negative charge in the solution.

Predict Think first, before you observe

You add 5.0 mL of 4.0 M NaOH to 1 L of pure water (pH 7.00) and to 1 L of a 0.300 M CH₃COOH/0.300 M CH₃COO⁻ buffer (pH 4.74). How large is the rise in pH?

Both rise by a similar, large amount The buffer rises much less The buffer rises more The pH of the buffer does not change at all
ConfidenceMedium
The explanation opens after you lock in a prediction
0 mL100 mL
strong base NaOHstrong acid HCl
0.005 M (dilute)0.500 M (concentrated)

Explanation notes (open after prediction)

The two-step calculation (stoichiometry → equilibrium) and the explanation of the pH changes in water and in the buffer open after you submit your prediction. For now, think about what the added OH⁻ meets in each beaker.

Two-step calculation

① Stoichiometry: OH⁻ reacts completely with HA (K = 1/Kb ≈ 10⁹, practically complete). 0.020 mol OH⁻ → HA 0.300→0.280 mol, A⁻ 0.300→0.320 mol. ② Equilibrium: use the remaining HA/A⁻ to find the pH. The volume (1.005 L) cancels in the ratio.

pH = 4.74 + log(0.320 / 0.280) = 4.80

Why water changes so much · buffer breakdown

Water has no HA to take up the OH⁻, so [OH⁻] = 0.020/1.005 = 0.0199 M → pOH 1.70 → pH 12.30. A buffer also jumps in pH once its HA is completely used up: the leftover OH⁻ then sets the pH (buffer capacity exceeded). Soils resist pH change in a similar way: a soil with a larger buffer capacity needs more lime to change its pH.

[Na⁺] + [H⁺] = [A⁻] + [OH⁻] (+ [Cl⁻])
Limits of this model — activity coefficients ignored (ideal solution), 25 °C · Kw = 1.0×10⁻¹⁴, Ka(CH₃COOH) = 1.8×10⁻⁵, volumes are additive, CO₂ uptake from air ignored. The starting pH 7.00 of "pure water" is an ideal value; real distilled water is about 5.6 because of CO₂. The pH on screen is a numerical solution of the charge balance, without approximation (x is not neglected).
Check Formative check — pass all items to complete
Q1What mainly happens to the OH⁻ added to the buffer?
It reacts with CH₃COO⁻ and disappears It reacts with CH₃COOH to form CH₃COO⁻ and H₂O It does not react and stays in the solution It combines with Na⁺ and precipitates
Hint

OH⁻ is a base. A base reacts with something that can give it an H⁺.

Q2 · TaskKeep NaOH at 5.0 mL (±0.5) and lower only the buffer concentration until the buffer ΔpH is 1.0 or more. Then press [Check]. (buffer capacity breakdown)
Current buffer ΔpH: — · concentration 0.300 M
Q3 · Calculate—
Hint

① mol of OH⁻ added = 4.0 × V(L). ② HA decreases by that amount and A⁻ increases. ③ pH = 4.74 + log(nA⁻/nHA).

Q4 · Fill in the blankFill in the blank: the largest amount of strong acid or strong base that a buffer can take up without a large pH change is called the buffer [__].
Hint

The word means "how much a container can hold".

Q5 · Apply (advanced, not required for completion)For 1.000 L of the 0.300 M/0.300 M acetic acid buffer, what is the smallest volume (mL) of 4.0 M NaOH needed to use up all the CH₃COOH?
Reflect Reflect — metacognition · completion

My prediction result: Not predicted yet

In one sentence: why does the buffer change its pH much less than water, with the same NaOH?

Apply Use the idea in a new context (not required for completion)

Transfer task: blood keeps its pH at about 7.4 with the H₂CO₃/HCO₃⁻ buffer system. During hard exercise, lactic acid (H⁺) floods in. Which component takes up the H⁺, and what happens when HCO₃⁻ runs out (acidosis)? Explain, linking it to the strong acid HCl mode of this simulation.

Next up: acid–base titrations — the buffer region and pH = pKa at the half-equivalence point, then solubility equilibria (Ksp).

COMPLETE · Completed — all checks passed.

Worksheet — Buffer action: same NaOH, different pH change

Name ________ Class ________ Date ________

(a) buffer 1.000 L pH 4.74 → [ ] (b) pure water 1.000 L pH 7.00 → [ ] 4.0 M NaOH 5.0 mL (to each) before after adding OH⁻ open bar = HAhatched = A⁻

1. Predict — Which beaker has the smaller rise in pH? Why?

2. Stoichiometry — Reaction: CH₃COOH + OH⁻ → CH₃COO⁻ + H₂O. After the reaction, n(HA) = mol, n(A⁻) = mol

3. Equilibrium — buffer pH = 4.74 + log( / ) = · water pH =

4. Fill in the blank — When a strong base is added, the [] component of the buffer uses up the OH⁻. The limit of what it can take up is called the buffer [].

5. Conclusion — If the buffer concentration is lowered to 0.020 M, what happens with the same NaOH?

Answer key (end of teacher printout) — 1. the buffer (HA uses up the OH⁻) · 2. 0.280 / 0.320 · 3. 0.320/0.280 → 4.80, water 12.30 · 4. weak acid (HA) / capacity · 5. all 0.020 mol of HA is used up, and the pH jumps to about 8.7 (buffer breakdown).

Teacher notes — open the lesson plan

Lesson plan · 5E phase and time

  • Explore and Explain, 15–20 min. Whole-class demonstration (?mode=teacher) or individual work.

Demonstration in 3 steps

  • ① Standard condition (0.300 M, NaOH 5.0 mL): buffer ΔpH 0.06 vs water ΔpH 5.30.
  • ② In the bar chart, HA↓ and A⁻↑ — "Where did the OH⁻ go?"
  • ③ Lower the concentration to 0.020 M, or add 75 mL of NaOH or more, to show the buffer breakdown.

Three key questions

  • "The amount of OH⁻ is the same. Why does only one beaker reach pH 12?"
  • "Why did the buffer pH change at all, even by 0.06?"
  • "Can a buffer be used forever? What sets the limit?"

Common misconceptions

  • MC-buf-01: "it rises as much as water" → use the bars to show that OH⁻ is used up by HA.
  • MC-buf-02: "it does not change at all" → the ratio 0.320/0.280 is not 1, so the pH rises by 0.06.
  • MC-buf-03: "capacity is unlimited" → HA 0.300 mol = NaOH 75 mL is the limit.

Answer key (teacher only)

  • —

Basis and sources

  • Buffer 4.74→4.80, water 7.00→12.30.
  • Ka(CH₃COOH) = 1.8×10⁻⁵ (common reference value). The Henderson–Hasselbalch approximation (pKa 4.74) and the exact charge-balance solution of this simulation agree to two decimal places (4.745→4.803).
  • Verification: multi-point comparison with an external Python charge-balance solver (scipy brentq) — error < 0.001 pH.

Prerequisites

  • pH and pOH, Ka, limiting-reactant calculations, the common-ion effect.
University general chemistry · buffer solutionsEngine E2 equation-driven (exact charge balance)Verified: checked against an external solver (2026-10-01)
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