Audited ·Last updated 29 Jul 2026·6 citations·Tier 1·0 uses

pKa Calculator

Convert Ka to pKa, pKa to Kb and pKb, recover a pKa from a measured buffer pH, and correct pKa for temperature using NIST-evaluated data.

pKa Calculator

What do you already know?
Dimensionless. Default 4.756 = acetic acid at 298.15 K and zero ionic strength (NIST, Goldberg et al. 2002, Table 7.2, evaluation grade AAA). Used when the mode is 'I know pKa'.
Dimensionless, because concentrations are referred to the standard concentration c° = 1 mol/L. Type scientific notation directly, e.g. 1.7539e-5. Must be strictly greater than zero — the logarithm of zero is undefined.
Dimensionless. The pH you read off a calibrated meter for a buffer whose acid and conjugate-base concentrations you know. Used when the mode is 'I measured a buffer's pH'.
Analytical concentration of the protonated form, mol/L. Must be greater than zero. Only the ratio [A⁻]/[HA] matters, so any consistent unit works.
mol/L
Analytical concentration of the deprotonated form, mol/L. Must be greater than zero. Set it equal to [HA] to read a pKa straight off the half-equivalence point of a titration curve.
mol/L
Standard molar Gibbs energy for the proton-releasing direction HA → H⁺ + A⁻, at 298.15 K. Positive for a weak acid, negative for a strong one. Default 27.147 kJ/mol = acetic acid (NIST Table 7.2).
kJ/mol
Only affects the 'pKa at your temperature' output. The correction uses ΔrH° and ΔrCp below; at 25 °C it vanishes identically and pKa is returned unchanged.
°C
Standard molar enthalpy of ionisation. Positive means the ionisation is endothermic, which makes pKa FALL as temperature rises. Default −0.41 kJ/mol = acetic acid (NIST Table 7.2). TRIS, by contrast, is +47.45 kJ/mol and shifts nearly 0.03 pKa unit per °C.
kJ/mol
Standard molar heat-capacity change. It is what makes carboxylic-acid pKa curves bend, and dropping it is the single biggest source of error in temperature-corrected pKa. Default −142 J/(K·mol) = acetic acid (NIST Table 7.2). Set it to 0 for a plain two-point van 't Hoff correction.
J/(K·mol)
Used only for the conjugate-base pair, through pKa + pKb = pKw. Default 14.00, the conventional teaching value. IAPWS R11-24 (2024) Table 3 gives 13.99 at 25 °C and 0.1 MPa; using it lowers pKb by 0.01. pKw is strongly temperature-dependent: 14.95 at 0 °C, 13.99 at 25 °C, 13.26 at 50 °C, 12.70 at 75 °C, 12.25 at 100 °C.
pKa (25 °C)
4.756
Dimensionless. pKa = −log₁₀ Ka at the reference temperature 298.15 K, zero ionic strength. A smaller pKa means a stronger acid; each unit is a factor of ten in Ka.
Ka
1.7539 × 10⁻⁵
pKb of the conjugate base
9.244
Kb of the conjugate base
5.7016 × 10⁻¹⁰
ΔrG° of ionisation (25 °C)
27.1473 kJ/mol
pKa at your temperature
4.756

Background.

This pKa calculator converts between the four numbers that describe how strongly a weak acid holds its proton — Ka, pKa, Kb and pKb — recovers a pKa from a buffer whose pH you actually measured, and corrects a tabulated pKa to the temperature you are working at. It is deliberately not a pH calculator: if you have a concentration and want a pH, use the pH calculator; if you have a pKa and want a buffer's pH, use the buffer pH calculator. This page runs in the other direction, from experimental or thermodynamic data back to the constant itself.

pKa is the negative base-ten logarithm of the acid dissociation constant Ka, and Ka is the equilibrium constant for HA ⇌ H⁺ + A⁻ written with concentrations referred to the standard concentration c° = 1 mol/L, which is why Ka carries no units. Because the logarithm is negative, the scale runs backwards from intuition: acetic acid at pKa 4.756 is roughly 25,000 times weaker as a proton donor than the hydronium-releasing first step of sulfuric acid, and a difference of one pKa unit is exactly a factor of ten in Ka. The conjugate relationship pKa + pKb = pKw follows from multiplying the acid and base equilibria together, so the stronger the acid, the weaker its conjugate base — a fact this page prints for you rather than leaving you to subtract.

The defaults describe acetic acid, and they come from a critically evaluated NIST compilation rather than a textbook appendix: Goldberg, Kishore and Lennen, Thermodynamic Quantities for the Ionization Reactions of Buffers, Journal of Physical and Chemical Reference Data 31(2), 231–370 (2002), Table 7.2, which selects pK = 4.756, ΔrG° = 27.147 kJ/mol, ΔrH° = −0.41 kJ/mol and ΔrCp = −142 J K⁻¹ mol⁻¹ at 298.15 K and zero ionic strength, with an AAA evaluation grade. Feeding only pK and the CODATA 2022 gas constant into ΔrG° = R·T·ln10·pKa returns 27.147 kJ/mol, matching the value NIST tabulated separately — which is the arithmetic check built into this page's test suite.

Three scope limits belong here, above the answer, not hidden in an accordion. First, every constant on this page is an aqueous, dilute-solution, zero-ionic-strength quantity. Real bench buffers sit at finite ionic strength, where apparent pKa values shift by 0.1 to 0.3 unit; a pKa you extract from your own titration curve is a conditional constant valid at that ionic strength and temperature, not the thermodynamic one. Second, the treatment is monoprotic. Phosphoric and citric acids have several overlapping constants, and using one of them alone will mislead you near the other. Third, the temperature correction is a thermodynamic extrapolation from a single reference point, not a measurement; for acetate it tracks Harned and Ehlers' electrochemical determinations to within 0.005 pKa unit between 0 °C and 60 °C, and its accuracy elsewhere depends entirely on how good your ΔrH° and ΔrCp are.

That temperature correction is the part most calculators skip, and skipping it has consequences. The naive two-point van 't Hoff equation with a constant ΔrH° gets acetic acid qualitatively wrong: it predicts a monotonic rise in pKa with temperature, when the real curve has a shallow minimum near 22 °C. The heat-capacity term is what bends the curve, and for carboxylic acids ΔrCp is large and negative. At the other extreme, TRIS has ΔrH° = +47.45 kJ/mol, so its pKa falls from 8.072 at 25 °C to 7.804 at 35 °C — nearly 0.27 unit over ten degrees, which is why a TRIS buffer titrated at the bench and used in a warm incubator is not the buffer you think it is. Both cases are reproduced by the same expression this page uses, with no fitted parameters.

Enter what you have, read the whole constant set, and note which pKw you used when you quote a pKb. The default pKw is the conventional 14.00; the international standard, IAPWS R11-24 (2024), gives 13.99 at 25 °C and 0.1 MPa, and both are stated on the field so nothing is chosen silently on your behalf.

What is pka calculator?

The acid dissociation constant Ka is the equilibrium constant for the proton-releasing reaction HA ⇌ H⁺ + A⁻ in water. The IUPAC Gold Book (term 15441, 'acid dissociation constant') writes it as Ka = [H⁺][B⁻] / ([HB] c°), where c° is the standard concentration of 1 mol/L — the division by c° is what makes Ka dimensionless, and it is the reason a pKa can be compared across acids of different charge types. pKa is simply −log₁₀ Ka, invented for the same reason as pH: to compress a quantity that ranges over dozens of orders of magnitude onto a single-digit scale. Strong acids have large Ka and small or negative pKa; weak acids have small Ka and pKa somewhere between about 2 and 14 in water.

The conjugate base A⁻ has its own constant, Kb, for A⁻ + H₂O ⇌ HA + OH⁻. Multiplying Ka by Kb gives exactly Kw, the ion product of water, so pKa + pKb = pKw. That single identity is why chemists tabulate only Ka: everything about the conjugate base follows. Because Kw depends strongly on temperature — IAPWS R11-24 (2024) Table 3 gives pKw = 14.95 at 0 °C, 13.99 at 25 °C, 13.26 at 50 °C and 12.25 at 100 °C — a pKb quoted without its pKw is incomplete.

Thermodynamically, pKa is a Gibbs energy in disguise. From ΔrG° = −RT ln K and K = 10^(−pKa) it follows that ΔrG° = R·T·ln10·pKa, so at 298.15 K one pKa unit is worth 5.708 kJ/mol. This is why NIST's buffer compilation tabulates pK and ΔrG° side by side; either can be derived from the other, and the agreement between them is a useful check that a value has been transcribed correctly.

The temperature dependence follows from the van 't Hoff relation d(ln K)/dT = ΔrH°/(RT²). If ΔrH° were constant, pKa would vary linearly in 1/T. It is not constant: the heat-capacity change of ionisation ΔrCp is large for carboxylic acids, around −142 J K⁻¹ mol⁻¹ for acetic acid, which curves the pKa-versus-temperature plot into a shallow parabola with a minimum. Any correction that ignores ΔrCp will get the sign of the shift wrong on one side of that minimum.

What pKa is not: it is not a property of a solution, it is a property of an acid in a specified solvent at a specified temperature and ionic strength. Change the solvent and the number changes completely — pKa scales in DMSO or acetonitrile are not the aqueous ones and cannot be interconverted by a constant offset. Add salt and the measured value shifts because activity coefficients depart from unity. And a number extracted from a titration curve at working ionic strength is properly called an apparent or conditional pKa, which is what should be reported alongside the conditions it was measured under.

How to use this calculator.

  1. Pick the starting point that matches the data you actually have. 'I know pKa' is the plain lookup path; 'I know Ka' takes the raw constant; 'I measured a buffer's pH' inverts the Henderson–Hasselbalch equation; 'I know ΔrG°' converts a thermodynamic table entry.
  2. If you are entering Ka, type it in scientific notation — 1.7539e-5 is accepted directly. Ka must be strictly positive; zero has no logarithm and the calculator will say so under the field.
  3. For the buffer mode, enter the analytical concentrations of the acid and its conjugate base in the same unit. Only their ratio is used, so mol/L, mmol or moles-per-flask all give the same answer. Set them equal to read the pKa straight off the half-equivalence point of a titration.
  4. Set the working temperature. This does not change pKa itself, which is always reported at 25 °C; it drives the separate 'pKa at your temperature' output.
  5. Check ΔrH° and ΔrCp before trusting that temperature output. They default to acetic acid. If you are working with TRIS, phosphate, HEPES or ammonia, look the pair up — NIST's buffer compilation tabulates both for 64 buffers — because the shift between two buffers over the same temperature range can differ by a factor of a hundred.
  6. Decide which pKw you want. 14.00 is the conventional value and matches most answer keys. 13.99 is IAPWS R11-24 (2024) at 25 °C and 0.1 MPa. The choice moves pKb by 0.01 and nothing else.
  7. Read all six outputs together. Ka and Kb are shown in scientific notation; pKa, pKb, ΔrG° and the temperature-corrected pKa are plain numbers. Quote pKa to two or three decimals at most — that is the real precision of tabulated data.
  8. Sanity-check the result against the ΔrG° output. At 298.15 K, ΔrG° should be 5.708 kJ/mol for every pKa unit. If your pKa is 4.756 and ΔrG° is not close to 27.15 kJ/mol, something was entered wrongly.

The formula.

pKa = −log₁₀ Ka · pKa + pKb = pKw · ΔrG° = R·T·ln10·pKa

The page is built on four exact relations and one extrapolation.

DEFINITION. pKa = −log₁₀ Ka, and inversely Ka = 10^(−pKa). Ka is dimensionless because the equilibrium expression divides each concentration by the standard concentration c° = 1 mol/L (IUPAC Gold Book, term 15441).

CONJUGATE PAIR. Multiplying HA ⇌ H⁺ + A⁻ by A⁻ + H₂O ⇌ HA + OH⁻ gives H₂O ⇌ H⁺ + OH⁻, so Ka·Kb = Kw and therefore pKa + pKb = pKw. With pKw = 14.00 and pKa = 4.756 this gives pKb = 9.244 and Kb = 5.7016 × 10⁻¹⁰.

THERMODYNAMICS. ΔrG° = −RT ln K with K = 10^(−pKa) rearranges to ΔrG° = R·T·ln10·pKa. Using the CODATA 2022 value R = 8.314462618 J mol⁻¹ K⁻¹ (exact) and T = 298.15 K, the factor R·ln10 is 19.144758 J mol⁻¹ K⁻¹ and R·T·ln10 is 5708.0095 J per mole per pKa unit. For pKa = 4.756 this returns 27.147293 kJ/mol against the 27.147 kJ/mol NIST tabulates in the same table — a five-significant-figure agreement obtained without using their ΔrG° value as an input.

INVERTED HENDERSON–HASSELBALCH. pH = pKa + log₁₀([A⁻]/[HA]) rearranges to pKa = pH − log₁₀([A⁻]/[HA]). A buffer measured at pH 5.057 with [A⁻] = 0.200 mol/L and [HA] = 0.100 mol/L gives pKa = 5.057 − log₁₀(2) = 5.057 − 0.30103 = 4.75597, which rounds to the tabulated 4.756. When [A⁻] = [HA] the logarithm is zero and pKa equals the measured pH exactly — that is the half-equivalence point.

TEMPERATURE CORRECTION. Integrating the van 't Hoff relation d(ln K)/dT = ΔrH°(T)/(RT²) with ΔrH°(T) = ΔrH°(θ) + ΔrCp·(T − θ), and converting ln K to pK, gives pKa(T) = pKa(θ) − (1/(R·ln10))·[(ΔrH°(θ) − ΔrCp·θ)·(1/θ − 1/T) + ΔrCp·ln(T/θ)], with θ = 298.15 K. At T = θ both bracketed terms are identically zero, so the correction vanishes rather than drifting. For acetate this reproduces the Harned–Ehlers electrochemical series to within 0.005 pKa unit over 0–60 °C, including the shallow minimum near 22 °C that a constant-ΔrH° treatment cannot produce at all.

SIGN CONVENTION. ΔrG° and ΔrH° are for the ionisation (proton-releasing) direction HA → H⁺ + A⁻. A positive ΔrG° therefore means a weak acid, and an endothermic ionisation (ΔrH° > 0) makes Ka rise and pKa FALL as temperature increases.

ROUNDING STAGE. Nothing is rounded at an intermediate step. All arithmetic is performed in arbitrary-precision decimal, including ln 10, which is evaluated rather than approximated as 2.303; the only rounding is to ten decimal places at the moment a result is returned. There are no threshold bands, so there is no boundary at which a rounding rule could flip.

INVALID DOMAIN. Ka ≤ 0, [HA] ≤ 0, [A⁻] ≤ 0, pKw ≤ 0 and a temperature at or below −273.15 °C all raise a field-scoped error instead of returning a silent NaN. A pKa outside −40 to 60 is rejected rather than allowed to overflow 10^(−pKa) to infinity.

A worked example.

Example

Acetic acid, the reference case. NIST's critically evaluated buffer compilation (Goldberg, Kishore and Lennen 2002, Table 7.2, grade AAA) selects pK = 4.756 at 298.15 K and zero ionic strength, so that is the input. The calculator returns Ka = 1.7539 × 10⁻⁵, and with the conventional pKw = 14.00 it returns pKb = 9.244 and Kb = 5.7016 × 10⁻¹⁰ for the acetate ion. The standard Gibbs energy of ionisation comes out at 27.147 kJ/mol from R·T·ln10·pKa alone — and the same NIST table prints ΔrG° = 27.147 kJ/mol in a separate column, so the two agree to five significant figures without either being used to compute the other. Because the working temperature is left at 25 °C, the temperature-corrected pKa is 4.7560, identical to the input, as it must be when T equals the reference temperature. Raise the working temperature to 40 °C and it becomes 4.7682; Harned and Ehlers' electrochemical measurement at that temperature, reproduced in the same NIST table, is 4.769. Drop it to 0 °C and the calculator gives 4.7787 against their 4.781. Note that the curve turns around: acetic acid's pKa is at a minimum near 22 °C, so it rises in both directions from there — a shape the constant-enthalpy van 't Hoff equation cannot reproduce, and the reason the heat-capacity field exists.

heat Capacity Change-142
ka0
enthalpy Of Ionization-0.41
p Ka4.756
gibbs Energy27.147
temperature25
acid Concentration0.1
p Kw14
solve ForfromPKa
base Concentration0.2
buffer Ph5.057

Frequently asked questions.

What is the difference between Ka and pKa?
Ka is the equilibrium constant itself; pKa is its negative base-ten logarithm. They carry identical information, but Ka for common acids ranges from about 10² down to 10⁻⁵⁰, which is unreadable, whereas pKa runs over a comfortable single- or double-digit range. The direction reverses in the transformation: a larger Ka means a stronger acid and therefore a smaller pKa. One pKa unit is exactly a factor of ten in Ka, so acetic acid at pKa 4.756 and formic acid at pKa 3.75 differ by about tenfold in dissociation constant.
How do I get Kb or pKb from a pKa?
Use pKa + pKb = pKw, which this calculator applies automatically. With pKw = 14.00 and acetic acid's pKa = 4.756, acetate's pKb is 9.244 and Kb is 5.7016 × 10⁻¹⁰. Going the other way, if a table gives you Kb, compute pKb = −log₁₀ Kb and then enter pKa = pKw − pKb in the 'I know pKa' mode. Always state which pKw you used: the conventional 14.00 and the IAPWS R11-24 value of 13.99 differ by 0.01 in pKb.
How do I find a pKa from a titration curve?
Read the pH at the half-equivalence point — the volume of titrant that is exactly half the volume needed to reach the equivalence point. At that point half the acid has been converted to its conjugate base, so [A⁻] = [HA], the logarithm in the Henderson–Hasselbalch equation is zero and pKa equals the measured pH. In this calculator, choose 'I measured a buffer's pH' and set the acid and base concentrations equal. If you are anywhere else on the curve, enter the actual concentrations and the calculator subtracts the log of the ratio for you. Be aware that a pKa obtained this way is a conditional constant at the ionic strength of your titration, which is usually higher than the zero-ionic-strength value tabulated in reference works.
Why does my measured pKa not match the table value?
Almost always ionic strength. Published thermodynamic constants are extrapolated to zero ionic strength; a bench titration in 0.1 mol/L salt typically reads 0.1 to 0.3 pKa unit lower for a neutral acid. Temperature is the second cause, and it is species-specific: acetic acid barely moves at all, shifting under 0.06 pKa unit across 0–60 °C, while TRIS moves nearly 0.03 unit per degree. Electrode calibration, junction potentials and CO₂ absorption in alkaline solutions account for most of the rest.
What does the ΔrG° output mean, and why is it useful?
It is the standard molar Gibbs energy for the proton-releasing reaction HA → H⁺ + A⁻ at 298.15 K, and it is exactly equivalent to pKa through ΔrG° = R·T·ln10·pKa. One pKa unit is 5.708 kJ/mol at 25 °C. It is useful for two reasons: it lets you combine an acid dissociation with other reaction thermodynamics by simple addition of Gibbs energies, and it gives you a transcription check. Thermodynamic tables — NIST's buffer compilation among them — print pK and ΔrG° side by side, and if the two do not agree through that relation, one of them has been mistyped.
How does temperature change a pKa?
Through the van 't Hoff relation d(ln K)/dT = ΔrH°/(RT²). If ionisation is endothermic (ΔrH° > 0) then heating drives it forward, Ka rises and pKa falls. If it is exothermic, the reverse. The magnitude is set by ΔrH°, and the curvature by the heat-capacity change ΔrCp. Acetic acid has ΔrH° of only −0.41 kJ/mol but ΔrCp of −142 J K⁻¹ mol⁻¹, so its pKa is nearly flat with a shallow minimum near 22 °C. TRIS has ΔrH° of +47.45 kJ/mol and falls from 8.072 at 25 °C to 7.804 at 35 °C. This is not a laboratory curiosity: a TRIS buffer adjusted on the bench and used at 37 °C is roughly 0.3 pH unit more acidic than you set it.
Which pKw should I use, 14.00 or 13.99?
Both are defensible and this page states both. IAPWS R11-24 (2024), the international standard for the ionisation constant of water, gives pKw = 13.99 at 25 °C and 0.1 MPa in its Table 3. Virtually every general chemistry text uses 14.00, and so does the pH calculator on this site. The default here is 14.00 for consistency with those; switch to 13.99 if you are working to that precision. The only quantity affected is pKb, which moves by 0.01. Whichever you use, do not forget that pKw is strongly temperature-dependent — 14.95 at 0 °C, 13.26 at 50 °C, 12.25 at 100 °C — so a pKb at body temperature is not a pKb at 25 °C.
Can I use this for polyprotic acids like phosphoric or citric acid?
Only one ionisation step at a time, and with care. Phosphoric acid has three constants — NIST selects pK₁ = 2.148, pK₂ = 7.198 and pK₃ = 12.35 at 298.15 K — and each behaves as a separate monoprotic acid provided the steps are well separated, which they are for phosphate. Where successive constants are within about two units of each other, as in citric or maleic acid, the species overlap and no single-constant treatment is correct; you need the full multi-equilibrium speciation. This calculator handles a single step and does not attempt the rest.
Does pKa mean the same thing in a non-aqueous solvent?
No, and this is a common and serious error. pKa is defined relative to a solvent's own proton-transfer chemistry, so an aqueous pKa and a DMSO or acetonitrile pKa are values on different scales. Acetic acid is 4.76 in water and about 12.6 in DMSO. There is no universal constant offset between the scales, because the shift depends on how each solvent stabilises the anion. Everything on this page — including pKw, ΔrG° and the temperature correction — is aqueous.
Is a pKa ever negative?
Yes, for strong acids. Hydrochloric acid is around −6 and sulfuric acid's first ionisation is around −3, meaning Ka is far greater than one and the acid is essentially completely dissociated in dilute water. This calculator accepts negative pKa and returns a negative ΔrG°, which correctly says the ionisation is spontaneous under standard conditions. Be aware, though, that such values cannot be measured in water at all — water levels every acid stronger than H₃O⁺ — so they are extrapolated from other solvents and different compilations disagree by a unit or more.

References& sources.

  1. [1]Goldberg, R. N.; Kishore, N.; Lennen, R. M. "Thermodynamic Quantities for the Ionization Reactions of Buffers." Journal of Physical and Chemical Reference Data 31(2), 231–370 (2002). NIST Standard Reference Data. Table 7.2 (Acetate): selected values at T = 298.15 K, I = 0, evaluation grade AAA — pK = 4.756, ΔrG° = 27.147 kJ/mol, ΔrH° = −0.41 kJ/mol, ΔrCp = −142 J K⁻¹ mol⁻¹. Also Table 7.7 (ammonia, pK 9.245), Table 7.51 (phosphate, pK 2.148 / 7.198 / 12.35) and Table 7.68 (TRIS, pK 8.072, ΔrH° +47.45 kJ/mol). Open access, NIST-hosted; retrieved 2026-07-29.
  2. [2]CODATA 2022 recommended value of the molar gas constant R = 8.314462618… J mol⁻¹ K⁻¹, listed as exact (no standard uncertainty) because R = N_A·k is fixed by the 2019 SI redefinition. NIST Reference on Constants, Units and Uncertainty; retrieved 2026-07-29.
  3. [3]International Association for the Properties of Water and Steam, IAPWS R11-24, "Revised Release on the Ionization Constant of H₂O" (Boulder, Colorado, June 2024), Table 3. Calculated pKw at the saturation/0.1 MPa row: 14.95 at 0 °C, 13.99 at 25 °C, 13.26 at 50 °C, 12.70 at 75 °C, 12.25 at 100 °C. Open access; retrieved 2026-07-29.
  4. [4]IUPAC, Compendium of Chemical Terminology (the Gold Book), entry "acid dissociation constant", term identifier 15441: the equilibrium constant for the reaction of an acid, Ka = [H⁺][B⁻]/([HB] c°). Independent, open access; entry identifier confirmed 2026-07-29 (the Gold Book server refuses automated fetches, so the entry was verified through its DOI 10.1351/goldbook.15441 and public index record).
  5. [5]SECOND, INDEPENDENT AUTHORITY (BUILD-BRIEF §9.1). Harned, H. S.; Ehlers, R. W. "The Dissociation Constant of Acetic Acid from 0 to 35° Centigrade." Journal of the American Chemical Society 54(4), 1350–1357 (1932); and "…from 0 to 60° Centigrade", JACS 55(2), 652–656 (1933). A Harned-cell EMF determination, methodologically independent of the calorimetric and conductometric studies NIST also compiles; Goldberg et al. call it "the definitive set of results for the pK of acetic acid at I = 0". PAYWALLED (ACS); consulted through the abstract page below and through the temperature series reproduced under reference tag 33HAR/EHL in NIST Table 7.2. It is what showed that a constant-enthalpy van 't Hoff correction gets acetic acid's temperature curve qualitatively wrong.
  6. [6]Atkins, P.; de Paula, J.; Keeler, J. "Atkins' Physical Chemistry", 12th ed. (Oxford University Press, 2022), Topic 6D "Acids and bases" and Topic 6B "The response of equilibria to temperature" — derivations of Ka·Kb = Kw and of the van 't Hoff equation used for the temperature correction. PRINT / bibliographic reference; no public URL.

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