Article — Buffer Capacity Calculator
Buffer Capacity Calculator: Van Slyke Equation for β at Any pH
Buffer capacity β equals 2.303 × C × (Ka × [H⁺]) / (Ka + [H⁺])² for the buffer term, plus a tiny water term that only matters below pH 3 or above pH 11. β is the moles of strong acid or strong base per litre needed to shift the pH by one unit. Maximum buffer capacity occurs at pH = pKa, where [HA] = [A⁻] and the value reaches βmax ≈ 0.576 × C. A 100 mM phosphate buffer at pH 7.20 (its pKa2) has β ≈ 0.058 mol/(L·pH), meaning you need 58 mmol of HCl per litre to drop the pH from 7.20 to 6.20. Buffers stay effective within pKa ± 1; outside that window the capacity falls below one third of peak.
The calculator includes presets for acetate (pKa 4.76), MES (6.15), carbonate (6.35), phosphate (7.20), HEPES (7.50), Tris (8.06), and ammonium (9.25). Enter your concentration and working pH, and the calculator returns β, the [A⁻]/[HA] ratio, and a tag flagging whether you are inside the effective range.
What is buffer capacity
Buffer capacity is the resistance of a buffer to pH change. The formal definition is β = dn / d(pH) per litre — moles of strong acid or base required to shift pH by one unit. A higher β means a more stubborn buffer. Capacity has units of mol per L per pH unit. Most lab buffers run in the 0.01 to 0.2 range; physiological systems like bicarbonate sit around 0.03 to 0.05 in plasma.
Capacity matters whenever you add a strong acid or base — whether titrating a sample, running an enzyme reaction that produces protons, or buffering CO₂ in cell culture. A weak buffer will swing in pH unpredictably; a strong buffer holds steady.
Human blood plasma has a buffer capacity of about 0.03 mol/(L·pH) at physiological pH 7.4. It is far from impressive in absolute terms — a lab phosphate buffer at 100 mM has nearly twice as much. The reason blood pH stays so steady is not raw β but the open carbonate system: the lungs continuously vent CO₂ and the kidneys excrete bicarbonate, giving an effective capacity orders of magnitude larger than the static β.
Buffer capacity formula (Van Slyke)
The buffer capacity formula from Van Slyke (1922) is β = 2.303·C·Ka[H⁺]/(Ka+[H⁺])² + 2.303·([H⁺] + [OH⁻]). The first term covers the buffer; the second is water self-ionisation. The buffer term peaks at pH = pKa and falls off symmetrically. The water term is negligible between pH 3 and pH 11 but dominates at the extremes — pure water at pH 1 has β ≈ 0.23, comparable to a 0.4 M acetate buffer at its pKa.
The factor 2.303 is ln(10), the conversion between natural log (used in the underlying derivation) and base-10 log (used in pH). C is the total buffer concentration in mol/L; Ka is the dissociation constant of the weak acid.
βmax = 0.576·C at pH = pKaRange = pKa ± 1 useful0.1 M buffer βmax ~0.058Water at pH 1 β ~0.23Maximum buffer capacity and pKa
The maximum buffer capacity occurs at pH equal to pKa, where the acid and conjugate base are present in equal amounts. At that ratio the buffer can absorb either a strong acid (consumed by the A⁻ form) or a strong base (consumed by the HA form) with equal facility. The peak value works out to 2.303 × C / 4 = 0.576 × C.
For a 100 mM buffer that peaks at βmax ≈ 0.058 mol/(L·pH). At pH = pKa ± 0.5 the capacity drops to about 90% of peak. At pH = pKa ± 1 it falls to about 33% of peak. Beyond ±1 it drops sharply.
Buffer capacity of common systems
The buffer capacity of common laboratory systems depends on the choice of weak acid/conjugate base pair and total concentration. Phosphate (pKa2 = 7.20) is the standard for physiological pH around 7.4. HEPES (pKa = 7.50) is preferred in cell culture because phosphate precipitates with calcium and inhibits some enzymes. Tris (pKa = 8.06) is used in molecular biology buffers like TBE and TAE — but Tris is unusually temperature-sensitive, shifting pH by ~0.03 per °C.
How concentration affects buffer capacity
Buffer capacity scales linearly with total concentration. Doubling C doubles β. A 50 mM buffer has half the capacity of a 100 mM buffer at the same pH. The choice of concentration is a trade-off: too low and the buffer fails when you add a few mmol of acid; too high and ionic strength upsets enzymes, membrane transport, or chromatography. Typical laboratory ranges are 10 to 200 mM, with 50 to 100 mM as a default for cell culture and 25 to 50 mM for electrophoresis.
Buffer capacity at the pH extremes
At the pH extremes — below 3 or above 11 — the water self-ionisation term dominates buffer capacity. Strong acid alone (no buffer) at pH 1 has β = 0.23 because adding extra protons barely changes the already-high [H⁺] concentration. Similarly, strongly basic solutions resist pH changes through high [OH⁻]. This is why buffers are unnecessary at the extremes — the solvent provides its own resistance.
For pH 1 to 3, just use a strong acid (HCl, H₂SO₄) at appropriate concentration. For pH 11 to 13, use NaOH or KOH. Adding a weak buffer in these ranges does almost nothing because the protonation state of the buffer is fully shifted to one side.
Choosing a buffer for your experiment
To choose a buffer for your experiment, pick a weak acid whose pKa is within ±1 of your target pH. For pH 7.4 (physiological), phosphate (7.20) and HEPES (7.50) are both excellent — pick HEPES if Ca²⁺ is present. For pH 8.0, use Tris (8.06). For pH 5.0, acetate (4.76) is the classic choice. Concentration should match the expected acid/base load: enzyme assays generating protons need higher β than static binding studies.
Common buffer capacity mistakes
The most common buffer capacity mistake is buffering far from the pKa. A Tris buffer (pKa 8.06) at pH 6.0 has almost no capacity — the [A⁻]/[HA] ratio is 1/100, so adding acid simply shifts the small base reserve out of the way. Second mistake: ignoring temperature. Tris pKa shifts by 0.03 per °C, so a buffer made at room temperature drifts noticeably at 4 °C or 37 °C. Third mistake: ignoring dilution — diluting a 200 mM stock 10× also drops β by 10×.
Some buffer-buffer combinations interact badly. Phosphate precipitates with calcium and magnesium (forming CaHPO₄ at neutral pH). Tris reacts with copper, nickel, and some primary aldehydes. Carbonate buffers absorb atmospheric CO₂ and drift in open containers. Always check that your buffer is compatible with the rest of your reagents and atmosphere.