Weak Acids, Weak Bases, and pKa
A single amino acid side chain — the imidazole of histidine — can act as an acid or a base. This depends on what surrounds it. This dual identity lets triad histidines in serine proteases pull a proton off water. It happens at exactly the moment catalysis demands it. Understanding why histidine does this, and why aspartate does something else entirely, requires more than memorizing the The pH Scale. It requires the quantitative language of dissociation constants and pKa. Every biological acid-base event is governed by the same equilibrium logic. This includes a proton hopping off carbonic acid in red blood cells, a phosphate group buffering the cytoplasm, and a lysine side chain gripping DNA. pKa is the single number that tells you which side of that equilibrium a molecule sits on. This holds true for any given pH. This matters because life runs on molecules that are only weakly acidic or weakly basic. They are never fully dissociated, never fully protonated. It is precisely this incompleteness that gives biology its buffering capacity. It also gives biology its exquisite pH-dependent switches. Enzyme active sites, ion channels, hemoglobin's oxygen affinity, and the stability of protein folds all depend on this. Each depends on partially ionized groups whose behavior is captured by a single equilibrium constant. Strong acids and strong bases, by contrast, are biologically almost irrelevant inside cells. HCl in the stomach is the one great exception. This is precisely because full dissociation gives no room for regulation. The big picture is that dissociation is Chemical Equilibrium applied to proton transfer. pKa is nothing more than a specially-scaled equilibrium constant, . It is chosen so that biologically relevant acids land on a convenient numerical scale (roughly 0 to 14). This scale lines up directly with the The pH Scale. Once Ka and pKa are properly defined and derived from first principles, the fractional ionization of any weak acid becomes clear. This derivation includes the thermodynamics that connects to . The fractional ionization at any pH becomes a matter of straightforward algebra. This article builds that machinery from scratch. It covers the equilibrium expression for a generic weak acid HA. It also covers the conjugate acid-base pair concept and the free-energy origin of pKa. It explains the physical meaning of "weak" versus "strong." It works three examples in increasing sophistication. These are acetic acid, the biologically central phosphate system, and a multiprotic amino acid. It sets up, without yet deriving, the titration-curve and buffer mathematics. These follow directly from these foundations.
- A weak acid HA dissociates only partially in water; Ka quantifies exactly how partially, via .
- pKa is defined as ; low pKa means strong tendency to donate a proton, high pKa means the opposite.
- Every acid HA has a conjugate base A⁻, and every base B has a conjugate acid BH⁺ — they always differ by exactly one proton.
- pKa is a free-energy quantity in disguise: .
- At pH = pKa, a weak acid is exactly half dissociated — this single fact underlies all buffering and titration behavior.
- Biological acids (carboxylic acids, phosphates, ammonium, imidazolium) span pKa 2–12, giving cells a toolkit of pH-sensitive switches.
- Key idea: pKa is a thermodynamically defined "tipping point" pH at which an acid and its conjugate base are present in equal amounts, and it sets the acid's entire ionization behavior at any other pH.
Where this lives today
The pKa concept is the quantitative backbone of drug design: pharmaceutical chemists routinely tune a candidate molecule's pKa to control its ionization state at physiological pH (7.4) versus stomach pH (~1.5–3.5), because only the neutral (un-ionized) form of most small-molecule drugs crosses lipid membranes efficiently — a principle formalized in the pH-partition hypothesis and central to predicting oral bioavailability. Aspirin (acetylsalicylic acid, pKa ≈ 3.5) is absorbed efficiently in the acidic stomach where it remains largely neutral, while morphine's tertiary amine (pKa ≈ 8) is protonated and charged at physiological pH, affecting its distribution and blood-brain-barrier penetration. In enzymology, catalytic residues are chosen by evolution precisely because their pKa values can be tuned by the local protein environment to sit near the operating pH of the reaction. The catalytic triad of chymotrypsin (Ser195–His57–Asp102) works because the local electrostatic environment lowers the effective pKa of the serine hydroxyl (via the histidine acting as a general base) enough for it to act as a nucleophile at physiological pH — a mechanism whose full kinetic analysis depends on exactly the equilibrium framework built here. Aspartate and glutamate side chains (free pKa ≈ 3.9 and 4.1) are sometimes shifted upward by 3–4 units when buried in a hydrophobic active site, allowing them to act as general acids at neutral pH where they would otherwise be fully deprotonated in bulk solution — this is the essence of pKa perturbation in enzyme catalysis. Hemoglobin's Bohr effect — the pH-dependence of oxygen binding that lets red blood cells release more O₂ in metabolically active, CO₂-rich (and hence more acidic) tissue — arises because specific histidine residues (notably His146 of the β-chain) change pKa upon the protein's conformational shift between oxy and deoxy states, altering how many protons the protein binds as it changes shape. Buffer systems throughout physiology — bicarbonate/carbonic acid in blood plasma (pKa ≈ 6.1, effective near pH 7.4 because of the open CO₂ reservoir), phosphate in cytoplasm (pKa₂ = 7.21), and histidine imidazole groups in proteins (pKa ≈ 6.0) — are all selected because their pKa values sit usefully close to the pH ranges they must stabilize, a direct, load-bearing application of everything derived above, and the immediate conceptual bridge to The Henderson-Hasselbalch Equation and quantitative Titration Curves.
Ask the tutor: How does burying a histidine side chain in a hydrophobic active-site pocket shift its pKa, and why does that shift matter for catalysis?
The physical picture — thorough prose
Consider dropping acetic acid, CH₃COOH, into water. Some molecules give up a proton to a nearby water molecule; most do not. The reaction
reaches equilibrium almost instantly — proton transfers are among the fastest reactions known, occurring on picosecond-to-nanosecond timescales because they require no bond-making to heavy atoms, only the shuttling of a proton along a hydrogen-bonded network. What distinguishes a weak acid from a strong one is not the speed of the reaction but its position at equilibrium. Strong acids like HCl transfer essentially all their protons to water; weak acids like acetic acid transfer only a small, well-defined fraction, leaving the bulk of the acid in its protonated (neutral) form. The equilibrium constant for this reaction, written with water's concentration folded into the constant (since [H₂O] ≈ 55.5 M is essentially unchanged by the reaction — a compositional invariant, not a "coincidence"), is called the acid dissociation constant Ka:
Here [H⁺] is shorthand for [H₃O⁺], the hydronium ion. A large Ka means the equilibrium lies far to the right — lots of dissociation, a "stronger" weak acid. A small Ka means the equilibrium favors the intact HA — a "weaker" weak acid still. Because Ka values for biological acids span more than twelve orders of magnitude (from Ka ≈ 10⁻² for phosphoric acid's first proton to Ka ≈ 10⁻¹³ for some very weakly acidic protons), chemists compress this range logarithmically, exactly as is done for [H⁺] itself:
This is the same logarithmic trick that turns [H⁺] into pH, and it is why pKa values conveniently fall in the 0–14 range that overlaps directly with physiological pH. A low pKa (e.g., 2) means a large Ka — a comparatively strong (readily dissociating) acid. A high pKa (e.g., 10) means a tiny Ka — a very weak acid that mostly stays protonated even in neutral water. Every acid HA is paired with a conjugate base A⁻: the species that remains after the proton leaves. Conversely, every base B (like ammonia, NH₃) has a conjugate acid BH⁺ (ammonium, NH₄⁺). A conjugate acid-base pair always differs by exactly one proton and share the same equilibrium — writing the base reaction
with equilibrium constant Kb, one finds Ka(for BH⁺) and Kb(for B) are linked through water's autoionization constant Kw:
This means every base's strength can be re-expressed as the pKa of its conjugate acid — biochemists almost universally do this, so that ammonia's basicity is reported as "pKa(NH₄⁺) = 9.25" rather than as a separate Kb. This single-scale convention is what lets a table of pKa values describe both acids and bases with one consistent number.
The next figure shows why pKa is the "tipping point" pH: it is precisely the pH at which [HA] = [A⁻], so that the log term in the ionization ratio vanishes.
The core ideas — governing equations
The central equilibrium expression for any monoprotic weak acid HA is
where: is the equilibrium hydrogen-ion (hydronium) concentration in mol/L, and are the equilibrium concentrations of conjugate base and undissociated acid, and has units of concentration (mol/L), though it is conventionally treated as dimensionless once referenced to the standard 1 M state.
Reading: Ka is just the equilibrium constant of a proton-transfer reaction, no more mysterious than the equilibrium constant for any other reversible reaction. It tells you the ratio of products to reactant concentrations that the system settles into, not how fast it gets there. The logarithmic form:
Reading: This is a purely notational compression, identical in spirit to pH = −log₁₀[H⁺]. A one-unit change in pKa corresponds to a tenfold change in Ka. Rearranging the Ka expression gives the ionization ratio directly as a function of pH — the seed of the Henderson–Hasselbalch relation developed elsewhere:
Reading: When pH = pKa, the exponent is zero, so — equal concentrations. When pH exceeds pKa by one unit, A⁻ outnumbers HA tenfold; when pH is one unit below pKa, HA outnumbers A⁻ tenfold. This single relation is the mechanistic seed of both Titration Curves and The Henderson-Hasselbalch Equation, though their full development belongs elsewhere. The thermodynamic origin of pKa, connecting equilibrium to free energy:
where: , is absolute temperature (K), and is the standard free-energy change for the dissociation reaction HA → H⁺ + A⁻ in dilute aqueous solution.
Reading: pKa is not an arbitrary empirical number — it is a disguised free energy. A high pKa (weak acid) corresponds to a large positive ΔG° (dissociation is thermodynamically unfavorable); a low pKa (strong acid) corresponds to a small or negative ΔG° (dissociation is favorable). At 25°C (298 K), each pKa unit corresponds to 2.303RT ≈ 5.7 kJ/mol of standard free energy.
Goal. Show explicitly how the empirically measurable Ka for a weak acid connects to (1) the logarithmic pKa scale and (2) the standard Gibbs free energy of dissociation, and verify the connection numerically for a concrete, non-round acid.
Step 1 — Write the equilibrium and its constant. For a weak acid HA in water,
At equilibrium, by the law of mass action,
Water does not appear because its concentration (55.5 M) is essentially constant and is absorbed into Ka's definition — this is a standard convention, not an approximation that introduces meaningful error, since even removing 10 mM of water via dissociation changes [H₂O] by under 0.02%.
Step 2 — Take the negative logarithm to define pKa. Applying to both sides,
Define and recall . Then
Rearranged, this is exactly the ionization-ratio relation used above; it is algebraically identical to the Henderson–Hasselbalch form, though its full buffering interpretation is developed separately.
Step 3 — Connect Ka to standard free energy via the van't Hoff relation for equilibrium constants. For any reaction at equilibrium, thermodynamics gives
This follows because at equilibrium the reaction quotient Q equals Keq, and the general relation must equal zero at equilibrium (no further net driving force), forcing . Applying this to acid dissociation with :
Step 4 — Convert natural log to base-10 log to expose pKa explicitly. Using ,
since by definition.
Step 5 — Numerical check with an asymmetric, real example: propionic acid (Ka = 1.34 × 10⁻⁵). First compute pKa:
(Check: , so pKa = 4.873, matching the literature value of 4.87 for propionic acid.) Now compute ΔG° at T = 298 K:
Compute stepwise: ; then ; then .
Limiting case check. As Ka → 1 (pKa → 0, a "moderately strong" acid at the boundary of the weak-acid regime), ΔG° → 0, meaning dissociation becomes thermodynamically neutral — exactly as expected, since Ka = 1 means products and reactants are equally favored at standard state. This confirms the sign and scaling of the formula: positive ΔG° for pKa > 0 (unfavorable dissociation, the acid mostly stays intact), consistent with weak acids being, by definition, only partially dissociated.
Go deeper · Derivation B · 1 minRelating Ka and Kb of a conjugate pair through Kw
Goal. Derive the relationship for a conjugate acid-base pair, and use it to find the pKa of an ammonium ion given the pKb of ammonia — an asymmetric, real numerical case.
Step 1 — Write both equilibria explicitly. For a base B (e.g. ammonia) reacting with water:
For its conjugate acid BH⁺ dissociating in water:
Step 2 — Multiply the two equilibrium expressions.
The terms cancel (one in numerator, one in denominator) and the terms cancel likewise:
Step 3 — Recognize the water autoionization constant. By definition, at 25°C (this itself is the equilibrium constant for ). Therefore
Taking of both sides gives the additive form used throughout biochemistry:
Step 4 — Apply to ammonia, using its measured Kb. Ammonia has , so
Then the pKa of its conjugate acid, ammonium (NH₄⁺), is
This matches the well-known literature value pKa(NH₄⁺) ≈ 9.25, confirming the derivation.
Limiting case check. If a base were so strong that Kb → 1 (pKb → 0), its conjugate acid would have pKa → 14 — an extraordinarily weak acid, essentially never donating a proton in water. This is the correct extreme: a very strong base (like O²⁻, which reacts completely with water to form OH⁻) has a conjugate acid (OH⁻ itself) that is indeed a very poor proton donor, consistent with pKa(H₂O) ≈ 15.7 for water acting as an acid.
Worked examples
Example 1 — Foundational: fractional ionization of acetic acid at gastric-adjacent pH. Acetic acid has pKa = 4.76. Find the ratio [A⁻]/[HA] and the percent ionized at pH 3.20 (a mildly acidic environment, distinctly asymmetric from pKa — not the trivial pH = pKa case). Using :
Evaluate: . So at pH 3.20, only about 2.75 A⁻ ions exist for every 100 HA molecules. Converting to percent ionized: if , then from the ratio ,
So acetic acid is only 2.68% ionized at pH 3.20 — it is overwhelmingly present as neutral CH₃COOH. This illustrates the general principle: when pH is well below pKa, a weak acid stays predominantly protonated. Limiting case check: at pH = pKa = 4.76 exactly, the ratio becomes , giving exactly 50% ionization — the defining tipping point, consistent with the derivation above.
Example 2 — Applied: the second dissociation of phosphoric acid in cytoplasmic buffering. Inorganic phosphate is one of the cell's dominant buffers, and its physiologically important equilibrium is the second dissociation,
Find the ratio at intracellular pH 7.05 (a physiologically realistic, slightly acidic-of-neutral value, chosen deliberately off pKa2 and off pH 7.00 to avoid masking errors with round numbers).
Evaluate: . So at pH 7.05, there are about 0.692 mol of HPO₄²⁻ for every mole of H₂PO₄⁻ — the two forms are present in comparable amounts (roughly 41% HPO₄²⁻, 59% H₂PO₄⁻), which is exactly why phosphate is such an effective physiological buffer: its pKa2 sits close to intracellular pH, so both the proton-donating and proton-accepting forms are abundant simultaneously and can respond to acid or base loads in either direction. Compute the percent as HPO₄²⁻ explicitly: with ,
So 40.9% of phosphate is in the HPO₄²⁻ form at pH 7.05, and 59.1% is H₂PO₄⁻ — confirming the near-even split expected when pH is close to pKa.
Example 3 — Exam/competition level: multiprotic amino acid, finding the pH at which a specific microspecies dominates. Histidine has three ionizable groups: the α-carboxyl (pKa₁ = 1.82), the imidazole side chain (pKa₂ = 6.00), and the α-amino group (pKa₃ = 9.17). At what pH is the ratio of the fully protonated cationic species (COOH, imidazolium⁺, NH₃⁺; net charge +2) to the next species (COO⁻, imidazolium⁺, NH₃⁺; net charge +1) equal to exactly 3:1, and which ionization event does this correspond to? The transition between the +2 species and the +1 species is governed entirely by loss of the α-carboxyl proton, since that is the only group differentiating the two species (both retain protonated imidazole and protonated amino group). This is governed by pKa₁ = 1.82:
We want the protonated (+2) form to exceed the deprotonated (+1) form by 3:1, i.e., :
Take of both sides:
So at pH 1.34, the fully protonated (+2) form of histidine outnumbers the (+1) form three to one — a pH found in the stomach, where free histidine (from protein digestion) would indeed exist predominantly in its doubly protonated cationic form. Notice this calculation used only pKa₁, correctly ignoring pKa₂ and pKa₃ since at pH 1.34 those groups are essentially fully protonated regardless (pH is more than four units below both), so their ionization states do not change appreciably across this narrow pH window — a check worth stating explicitly: at pH 1.34, , so , confirming imidazole is >99.998% protonated and can be treated as a spectator group in this calculation.
Limiting cases, scope & common traps
| Regime | Behavior | Why |
|---|---|---|
| pH ≪ pKa | Acid almost entirely protonated (HA form) | |
| pH ≫ pKa | Acid almost entirely deprotonated (A⁻ form) | |
| pH = pKa | Exactly 50% HA, 50% A⁻ | exponent is zero |
| Ka ≫ 1 (pKa < 0) | "Strong acid" regime; dissociation essentially complete in water | ΔG° strongly negative |
| Ka ≪ 1 (pKa > 14) | Essentially non-acidic in water; deprotonation not observable | ΔG° strongly positive, exceeds accessible range |
| Multiprotic acid | Treat each dissociation step with its own Ka, valid when pKa's differ by ≥ 3 units | Overlapping equilibria otherwise couple non-trivially |
The chemist behind it
Ka and pKa as we use them today are inseparable from the broader Brønsted–Lowry framework for acids and bases, developed independently and almost simultaneously in 1923 by Johannes Nicolaus Brønsted in Denmark and Thomas Martin Lowry in England. Before their work, acids and bases were understood mainly through the more restrictive Arrhenius definition (acids produce H⁺ in water; bases produce OH⁻), which could not naturally accommodate species like ammonia or the amino acid side chains central to biochemistry. Brønsted's insight — that an acid is simply a proton donor and a base is a proton acceptor, defined always in relation to a conjugate partner — is exactly the conceptual scaffold used throughout this article: every HA has its A⁻, every B has its BH⁺, and "acid" or "base" is a role a molecule plays relative to a specific proton-transfer partner, not an immutable label. Brønsted, a physical chemist working at the University of Copenhagen, was deeply interested in reaction kinetics and catalysis, and his acid-base theory grew out of his attempts to systematize how general acid and general base catalysis worked in organic reactions — a concern that turns out to be exactly the concern of enzymologists studying how histidine, aspartate, and lysine side chains catalyze biological reactions today. The logarithmic pKa notation itself traces to Søren Sørensen's 1909 introduction of pH at the Carlsberg Laboratory, extended naturally by later chemists to dissociation constants once Brønsted's generalized framework made "acid strength" a quantity worth tabulating systematically across both classical mineral acids and the growing catalogue of biologically relevant weak acids and bases.
Origins · 1 minJohannes Nicolaus Brønsted and how this was discovered
Brønsted trained originally as a chemical engineer before turning to physical chemistry, where his major contributions spanned acid-base theory, catalysis, and the thermodynamics of ion activities (the Brønsted–Bjerrum equation for reaction rates in electrolyte solutions bears his name alongside Niels Bjerrum). His 1923 paper "Einige Bemerkungen über den Begriff der Säuren und Basen" ("Some Remarks on the Concept of Acids and Bases") proposed the proton-donor/proton-acceptor definition that unified what had been a scattered set of acid-base phenomena — including, crucially, non-aqueous acid-base chemistry that the Arrhenius picture could not touch. Brønsted was also politically active, serving briefly as a member of the Danish parliament, and was nominated for the Nobel Prize in Chemistry several times, though he died in 1947 without receiving it, the same year Thomas Lowry (who proposed the equivalent theory independently in England) had died six years earlier in 1936.
What exactly does "weak" mean if it isn't about concentration?
"Weak" describes the extent of ionization at equilibrium, a property fixed by the molecule's pKa (equivalently, by ΔG° for the dissociation reaction), not by how much of the substance is dissolved. A weak acid never fully ionizes in water no matter how dilute you make it — some finite equilibrium fraction always remains as HA — whereas a strong acid ionizes essentially completely across an enormous concentration range. Practically, "weak" acids have Ka roughly between 10⁻¹⁴ and 10⁻² (pKa between about 2 and 14), while classic strong acids (HCl, H₂SO₄'s first proton, HNO₃) have Ka values so large that essentially no undissociated HA is left at equilibrium under normal conditions, making their pKa values negative or close to it.
Why do biochemists prefer pKa over Ka for everyday use?
Because Ka values for biologically relevant acids span roughly twelve orders of magnitude — from about 10⁻² for the first phosphate dissociation to below 10⁻¹³ for some very weak protons — while their pKa values fall neatly between 2 and 13. This mirrors exactly why chemists use pH instead of raw [H⁺]: logarithms turn a sprawling multiplicative range into a compact, additive, easily comparable scale. It also means pKa differences translate directly into free-energy differences via ΔG° = 2.303RT·pKa, so a table of pKa values is simultaneously a table of relative thermodynamic stabilities for the dissociated versus undissociated forms.
Can the same molecule act as both an acid and a base?
Yes — this is called amphoterism, and it is extremely common among biological molecules. Water itself is the textbook example (it can donate a proton to become OH⁻'s conjugate acid partner or accept one to become H₃O⁺). Amino acids are amphoteric because they carry both a carboxyl group (acidic, low pKa) and an amino group (basic, i.e., its conjugate acid has a high pKa); histidine's imidazole ring can act as either proton donor or acceptor depending on pH, which is exactly what makes it so useful catalytically — it can shuttle protons in either direction depending on the immediate chemical step required.
How is pKa actually measured in the laboratory?
The most common method is potentiometric titration: a known amount of acid is titrated with standardized base while continuously monitoring pH with a glass electrode, and the pKa is read as the pH at the half-equivalence point (where exactly half the acid has been converted to its conjugate base) — a fact whose justification follows directly from the pH = pKa when [A⁻] = [HA] relation derived above. Spectrophotometric methods work when protonation changes a molecule's UV-visible absorbance (common for aromatic or conjugated acids); NMR titration tracks how chemical shifts of specific atoms change with pH, which is especially powerful for measuring the pKa of individual side chains buried within a folded protein, since it can resolve one ionizable group from another even when their titrations overlap.
Why do side-chain pKa values in folded proteins differ from those of the free amino acids?
The pKa values tabulated for free amino acids (aspartate 3.9, histidine 6.0, lysine 10.5, etc.) describe the ionizable group in bulk water, fully solvated and far from other charges. Inside a folded protein, a side chain may be buried in a nonpolar pocket (destabilizing the charged form, raising the pKa of an acid or lowering it for a base relative to solution) or positioned near another charged group (stabilizing or destabilizing the ionized state through direct electrostatic interaction, hydrogen bonding, or dipole effects). These perturbations, sometimes shifting pKa by 3–4 units or more, are not exceptions to the theory — they are the same ΔG°=2.303RT·pKa relation applied with a different, protein-specific ΔG° for dissociation, reflecting the altered local environment.
Is there a maximum or minimum possible pKa?
In aqueous solution, pKa values are bounded in practice by the properties of water itself. Below about pKa = −1.7 (the pKa of H₃O⁺ acting as an acid), an acid is so strong it is "leveled" by water — essentially all such acids appear equally strong in water because they fully protonate water to H₃O⁺, which is itself the strongest acid that can exist stably in aqueous solution (the leveling effect). Above about pKa = 15.7 (the pKa of water acting as an acid, i.e., water donating a proton to become OH⁻), a base is so strong that hydroxide, its conjugate acid analog, cannot meaningfully compare it. Outside this roughly −1.7 to 15.7 window, water can't distinguish relative acid or base strength, and other solvents or gas-phase measurements are needed.
How does pKa connect to the material on titration curves and buffers that follows?
The relation derived here is algebraically identical to the buffer equation used in The Henderson-Hasselbalch Equation — that article simply rearranges it into and interprets it as a recipe for buffer preparation. Similarly, a titration curve — pH plotted against equivalents of base added — is nothing more than this same ionization-ratio relation traced out experimentally, with its inflection point (of maximum buffering, minimum slope) occurring exactly at pH = pKa, which is why titration curves are, in practice, the standard method for measuring pKa in the first place.