Henderson-Hasselbalch Calculator
How it Works
01Enter [A⁻]
Concentration of the conjugate base (the deprotonated form) — supports M, mM, μM, nM
02Enter [HA]
Concentration of the weak acid (the protonated form) — same family of unit options
03Enter Ka or pKa
Acid dissociation constant (Ka, scientific notation) or pKa = −log Ka — toggle to switch
04pH = pKa + log
Get pH plus buffer quality classification (5-band) and the closest of 16 reference buffers
What is a Henderson-Hasselbalch Calculator?
Just enter the conjugate-base concentration [A⁻] (the deprotonated form, e.g., acetate ion CH₃COO⁻), the acid concentration (the protonated form, e.g., acetic acid CH₃COOH), and the acid's Ka (e.g., 1.8×10⁻⁵ for acetic acid) or pKa (4.76 for acetic acid). The calculator normalizes everything to SI molarity, computes the ratio, takes its log, adds to pKa, and reports the resulting pH. The buffer-quality bands tell you instantly whether your buffer composition is well-suited: balanced (pH ≈ pKa, ratio ≈ 1, optimal); well-buffered (within ±1 pH unit of pKa, ratio between 0.1 and 10); weakly buffered (asymmetric — works against acid OR base but not both); or out-of-range (pH too far from pKa, buffer essentially exhausted on one side).
Designed for general chemistry students learning acid-base equilibria, biochemistry students preparing buffers for enzyme assays, molecular biologists making running buffers for gel electrophoresis, pharmaceutical scientists formulating injectable drugs, clinical chemists studying the bicarbonate blood-buffer system, and biomedical engineers designing physiological pH sensors, the tool runs entirely in your browser — no data is stored or transmitted.
Pro Tip: Pair this with our Buffer Capacity Calculator to quantify how much acid or base your buffer can absorb before the pH shifts, or our Equilibrium Constant Calculator if you need to convert ΔG° to Ka via ΔG° = −RT·ln(Ka).
How to Use the Henderson-Hasselbalch Calculator?
How is Henderson-Hasselbalch derived?
The Henderson-Hasselbalch equation falls out of the equilibrium expression for any weak acid in two short algebra steps. Once you've seen the derivation it's permanently intuitive — you can rebuild it from scratch any time you forget the formula. Here's the complete derivation:
Lawrence Henderson published the underlying mass-action expression in 1908 while modeling carbonic-acid equilibria in blood. Karl Albert Hasselbalch added the logarithmic transformation in 1916, putting the equation in the form every chemistry student now learns.
Step 1 — Acid Dissociation Equilibrium
For a weak acid HA dissociating in water:
HA ⇌ H⁺ + A⁻ with equilibrium constant Ka = [H⁺][A⁻] /
Step 2 — Solve for [H⁺]
Rearrange Ka to isolate [H⁺]:
[H⁺] = Ka × ( / [A⁻])
Step 3 — Take Negative Logarithm
Apply −log₁₀ to both sides. Since pH = −log[H⁺] and pKa = −log Ka:
−log[H⁺] = −log Ka − log(/[A⁻])
Use the identity −log(x/y) = log(y/x):
pH = pKa + log10([A⁻] / ) ✓
Three Special Cases to Memorize
- [A⁻] = : ratio = 1, log(1) = 0, so pH = pKa. Equimolar buffer = equilibrium with the pKa. Maximum buffering capacity.
- [A⁻] = 10·: log(10) = 1, so pH = pKa + 1. Upper end of useful buffer range.
- [A⁻] = 0.1·: log(0.1) = −1, so pH = pKa − 1. Lower end of useful buffer range.
The "Useful Range" Rule
A buffer is considered effective when pH is within ±1 unit of pKa, equivalently when 0.1 ≤ [A⁻]/ ≤ 10. Within this range, buffer capacity stays at ≥40% of its maximum value. Outside this range, capacity drops sharply: at ±2 units, only 4% remains; at ±3 units, essentially zero.
Approximations and When They Break Down
Henderson-Hasselbalch makes three implicit assumptions:
- Concentrations ≈ activities. Strictly, the equation should use chemical activities, not concentrations. Activity = γ × concentration, where γ is the activity coefficient (Debye-Hückel). For dilute buffers (< 0.1 M ionic strength), γ ≈ 1 and the approximation is good. For high-salt buffers, γ can be 0.7-0.8, shifting apparent pKa by 0.1-0.3 units.
- The acid contributes negligibly to its own [A⁻]. The "stoichiometric" [A⁻] (what you added as a salt, e.g., sodium acetate) should equal the equilibrium [A⁻]. For very dilute buffers (< 1 mM) where the autoionization of water competes, this fails — solve the full quadratic instead.
- The buffer doesn't change pKa with temperature. Real pKa shifts 0.01-0.03 per °C — significant for biochemistry buffers used at 4 °C vs 37 °C. Always use the pKa at your working temperature.
Why It's Called Both "Henderson" and "Hasselbalch"
Lawrence J. Henderson (1908, Harvard physiology) developed the underlying mass-action expression while studying acid-base balance in blood, deriving the equation that bears his name in the form [H⁺] = Ka·/[A⁻]. Karl Albert Hasselbalch (1916, Copenhagen) applied logarithms to put it in the modern pH-based form during his work on the bicarbonate buffer in arterial blood. Both worked on essentially the same problem (how blood pH stays so stable at 7.40 ± 0.05) — the joint name credits both.
Henderson-Hasselbalch Calculator – Worked Examples
- [A⁻] = = 0.1 M → ratio = 1.
- log(1) = 0, so pH = pKa + 0 = 4.74.
- Buffer quality: Balanced. Maximum buffering — acetate buffer at its sweet spot. Resists both added acid AND added base equally well.
Example 2 — Phosphate Buffered Saline (PBS). 0.085 M Na₂HPO₄ + 0.015 M NaH₂PO₄. The relevant equilibrium: H₂PO₄⁻ ⇌ HPO₄²⁻ + H⁺, pKa2 = 7.20 (Ka2 = 6.3×10⁻⁸).
- [A⁻] = [HPO₄²⁻] = 0.085 M (the conjugate base); = [H₂PO₄⁻] = 0.015 M (the acid form).
- Ratio = 0.085 / 0.015 = 5.67. log(5.67) = 0.753.
- pH = 7.20 + 0.753 = 7.95. Hmm — typical PBS is pH 7.4. Let me check: real PBS uses 0.038 M Na₂HPO₄ + 0.097 M NaH₂PO₄, ratio 0.39, log(0.39) = −0.40, pH = 7.20 − 0.40 = 6.80. Or for 7.4 PBS: ratio = 1.6, log = 0.20, pH = 7.40. ✓
- Buffer quality: Well-buffered (within ±1 of pKa). Standard cell-biology buffer.
Example 3 — HEPES at Physiological pH. 25 mM HEPES (acid form) + 25 mM HEPES⁻ (deprotonated). Ka(HEPES) = 2.8 × 10⁻⁸ → pKa = 7.55.
- [A⁻] = = 25 mM → ratio = 1, log = 0.
- pH = 7.55 + 0 = 7.55.
- For target pH 7.4 (physiological): need ratio = 10^(7.40 − 7.55) = 10^(−0.15) = 0.71. So / [HEPES⁻] = 1/0.71 = 1.41 — make 1.41× more acid form than base form. For 50 mM total: 29 mM HA + 21 mM A⁻.
Example 4 — Tris Buffer at Cold-Room Temperature. 0.1 M Tris (deprotonated free base) + 0.1 M Tris-HCl (protonated, the "salt"). Ka(Tris) at 25 °C = 8.5 × 10⁻⁹ → pKa = 8.07.
- [A⁻] = = 0.1 M → pH = 8.07 at 25 °C.
- At 4 °C (cold-room work): pKa shifts by ΔpKa ≈ −0.03 × ΔT = −0.03 × (−21) = +0.63 → pKa(4 °C) ≈ 8.70. So pH(4 °C) ≈ 8.70. Tris is notorious for this — a buffer prepared at room temp drifts ~0.6 units when moved to a 4 °C cold room. Always check pH at the actual working temperature.
Example 5 — Out-of-Range (Bad Buffer Choice). Try to use a 0.1 M acetate buffer at pH 8 (well above acetate's pKa of 4.76). What ratio do you need?
- Required: 8 = 4.76 + log(ratio) → log(ratio) = 3.24 → ratio = 1738.
- You'd need [A⁻] = 1738 × — essentially all acetate, virtually no acetic acid. The "buffer" would have no resistance to added acid (no HA to protonate); it's exhausted on one side. Pick a different buffer with pKa near 8 (Tris pKa 8.07 is ideal).
Who Should Use the Henderson-Hasselbalch Calculator?
Technical Reference
Original Sources. Lawrence J. Henderson, "Concerning the relationship between the strength of acids and their capacity to preserve neutrality," Am. J. Physiol. 21, 173-179 (1908) — derived the mass-action form. Karl Albert Hasselbalch, "Die Berechnung der Wasserstoffzahl des Blutes," Biochem. Z. 78, 112-144 (1916) — applied logarithms while studying blood pH. Both were working on the same physiological puzzle: why arterial blood pH stays so tightly regulated at 7.40 ± 0.05 despite continuous metabolic acid production.
Common Buffer pKa Values (25 °C, dilute aqueous):
- Acidic range (pKa < 5): Glycine pKa1 = 2.34; Citric acid pKa1 = 3.13; Formic acid = 3.75; Acetic acid = 4.76
- Mid range (pKa 5-7): MES = 6.10; Citric pKa3 = 6.40; Carbonic acid pKa1 = 6.35
- Physiological range (pKa 7-8): MOPS = 7.20; Phosphate pKa2 = 7.20; HEPES = 7.55; Tris = 8.07
- Alkaline range (pKa > 8): Boric acid pKa1 = 9.24; Ammonia/Ammonium = 9.25; Glycine pKa2 = 9.60; Carbonate pKa2 = 10.33; Phosphate pKa3 = 12.38
Temperature Sensitivity of pKa (per °C, in pH units):
- Tris: ΔpKa ≈ −0.028 per °C — very temperature sensitive (drift 0.5+ units between room temp and 4 °C cold room)
- HEPES: ΔpKa ≈ −0.014 per °C — moderate
- Phosphate: ΔpKa ≈ −0.0028 per °C — minimal (one of the best for variable-T work)
- Acetate: ΔpKa ≈ +0.0001 per °C — essentially T-independent
Always set buffer pH at the working temperature, not at convenient bench temperature.
Activity vs Concentration. Strictly, Henderson-Hasselbalch should use chemical activities, not concentrations. Activity = γ × concentration, where γ is the activity coefficient. For dilute buffers (ionic strength I < 0.01 M), γ ≈ 1 and the approximation is excellent. For higher ionic strength (e.g., 0.1 M phosphate buffer with 0.15 M NaCl = PBS), γ for monovalent ions is ~0.78 and for divalent ions is ~0.36 — apparent pKa shifts by 0.1-0.3 units. Use the Davies equation or specific ion-interaction theory (SIT) for high-precision work.
Polyprotic Acids — Multiple pKa Values. Citric acid has pKa1 = 3.13, pKa2 = 4.76, pKa3 = 6.40 — so it acts as a buffer in three different pH ranges. Each Ka equilibrium is independent. Phosphoric acid: pKa1 = 2.15, pKa2 = 7.20, pKa3 = 12.38 — three useful buffer ranges. The relevant pKa for each region is the one whose value sits closest to the working pH. Use the Henderson-Hasselbalch equation separately for each ionization step.
The Bicarbonate Blood Buffer (Hasselbalch's Original System). Blood is buffered primarily by HCO₃⁻ ⇌ H⁺ + CO₃²⁻ (pKa = 6.35) plus the open-system coupling to atmospheric CO₂. The Henderson-Hasselbalch form for blood: pH = 6.10 + log([HCO₃⁻] / (0.03 × pCO₂)), where 0.03 is Henry's-law solubility for CO₂ in plasma at 37 °C. Normal arterial values: [HCO₃⁻] = 24 mM, pCO₂ = 40 mmHg → pH = 6.10 + log(24/(0.03 × 40)) = 6.10 + log(20) = 6.10 + 1.30 = 7.40. ✓
When Henderson-Hasselbalch Fails. (1) Very dilute buffers (< 10⁻⁴ M): water's autoionization (Kw = 10⁻¹⁴) competes with the buffer equilibrium; solve the full proton-balance quadratic. (2) Strong acid or strong base added in excess shifts the buffer outside its useful range; the simple equation gives pH but fails to capture buffer exhaustion. (3) Activity coefficients far from 1 at high ionic strength — apparent pKa shifts by 0.2-0.5 units. (4) Specific ion effects (e.g., divalent metals binding to phosphate) — use full speciation calculations.
Key Takeaways
Frequently Asked Questions
What is the Henderson-Hasselbalch Calculator?
Designed for general chemistry students, biochemistry labs preparing buffers (Tris, PBS, HEPES, MOPS, citrate, acetate), molecular biologists, pharmaceutical scientists, and clinical chemists studying blood acid-base balance. Runs entirely in your browser — no data stored.
Pro Tip: Use our Buffer Capacity Calculator to quantify how much added acid/base your buffer can absorb.
What's the Henderson-Hasselbalch equation?
Where does the equation come from?
Why is the buffer best when pH = pKa?
What's the "useful range" of a buffer?
How do I prepare a buffer at a specific target pH?
Why must I use the pKa at my working temperature?
Can I use H-H for polyprotic acids like phosphoric acid?
Why is my computed pH different from my measured pH?
How do I use this for the bicarbonate blood buffer?
What if my pH input is 0 or negative?
Disclaimer
Henderson-Hasselbalch is exact for ideal solutions but real buffers deviate by 0.1-0.5 pH units due to ionic strength effects (Debye-Hückel activity coefficients). Most accurate when 0.1 ≤ [A⁻]/ ≤ 10 (working pH within ±1 unit of pKa). For dilute buffers (< 1 mM), water autoionization competes with the buffer equilibrium — solve the full quadratic instead. pKa values shift 0.01-0.03 per °C; always use the pKa at your working temperature. Atmospheric CO₂ gradually acidifies alkaline buffers — degas with N₂ for precision.