Predicting Equilibrium Position from pKa
Drop sodium hydride into ethanol and it fizzes violently. It spits out hydrogen gas until every last O–H bond is gone. Now drop sodium hydride into a hydrocarbon solvent like hexane instead. Assuming it could dissolve, nothing at all would happen. The difference is not mysterious once you know one number for each species: the p. Acid-base reactions are the most common elementary step in all of organic chemistry. They show up in every mechanism as proton transfers. These proton transfers set up nucleophiles, protonate leaving groups, or generate reactive intermediates. Every single one is quietly governed by a comparison of two p values. This matters because organic chemists almost never memorize equilibrium constants for individual acid-base reactions. Instead they memorize (or look up) a table of maybe thirty p values. This list includes water, ammonia, alcohols, carboxylic acids, ketones, and terminal alkynes. From that short list they can predict the outcome of an acid-base reaction. This works for any two species on the table. It even works for pairs never directly measured against each other. This is the payoff of understanding Defining pKa and the Acidity Constant. p is not just a label for "how acidic." It is a thermodynamic handle that lets you chain comparisons together algebraically. The big picture is a single rule, so simple it looks almost too easy. Proton transfer runs downhill from the stronger acid to the stronger base. The equilibrium constant for the reaction is . Here is the difference between two values. It equals the p of the product acid minus the p of the starting acid. Get the sign right, and you can predict which side an equilibrium favors. You can also predict by how much it is favored. This could be a factor of 10, or , or anything in between. You can know this without ever running the reaction. This article builds that rule from first principles using the definition of . It shows exactly how to combine two acid dissociation equilibria into one proton-transfer equilibrium. Full curved-arrow mechanisms are included. Proton transfer is a real bond-breaking, bond-making event, not just bookkeeping. The rule is then applied to three worked examples of increasing sophistication. These range from a textbook acetic acid/ammonia comparison to a real synthetic decision. That decision involves which base can deprotonate a ketone. It closes with the traps that catch beginners. One trap is forgetting that lower p means stronger acid. Another is confusing thermodynamic favorability with kinetic feasibility. A third is misapplying aqueous p values to reactions run in a very different solvent.
- Every acid-base equilibrium can be predicted from just two p values, one for each conjugate acid in the reaction.
- Lower p = stronger acid = weaker conjugate base; the equilibrium favors formation of the weaker acid and weaker base.
- The equilibrium constant obeys , derived by dividing one expression by another.
- A p gap of just 1 unit means a 10:1 equilibrium preference; a gap of 10 units means :1 — effectively irreversible.
- This lets you predict outcomes for acid-base pairs that were never directly measured, by chaining through a common reference (usually water).
- The rule predicts thermodynamic position only; it says nothing about reaction rate, which is why weak, hindered bases can still be kinetically slow even when thermodynamically favored.
- Key idea: subtract the two p values — the sign and size of tell you the direction and magnitude of the equilibrium in one step.
An acid-base equilibrium always proceeds toward the side with the weaker acid and weaker base (the more stable, lower-energy pair), and the equilibrium constant for going from one conjugate pair to another is exactly , with measured as (p of the acid being formed) minus (p of the acid being consumed).
Where this lives today
Every retrosynthetic decision about "which base do I use to deprotonate this substrate" is a live application of reasoning: choosing LDA versus NaH versus -BuLi versus a milder amine base for a given enolization, as touched on in Example 3, is exactly the calculation medicinal and process chemists run mentally (or on paper) before every alkylation, aldol, or Claisen condensation is planned. The same logic underlies buffer design in biochemistry and pharmaceutical formulation, where the Henderson–Hasselbalch equation — itself a direct rearrangement of the expression — sets the ratio of protonated to deprotonated drug at physiological pH, controlling solubility, membrane permeability, and bioavailability. In peptide and nucleic acid chemistry, the protonation states of histidine (imidazole side chain, p), lysine (p), and phosphate backbones are all predicted from exactly this framework, which is why enzyme active-site mechanisms are routinely drawn with explicit judgments about which residue is protonated at physiological pH 7.4 — a direct comparison against water's effective p of 15.7 (or, more properly, against the local -referenced pH). In materials and battery chemistry, proton-coupled electron transfer steps in fuel cells and metal-air batteries are analyzed with combined p/redox-potential ("square scheme") diagrams that are a direct two-dimensional generalization of the single p-subtraction rule developed here. And in everyday process chemistry, the decision to use aqueous sodium bicarbonate (carbonic acid p 6.35) versus sodium hydroxide (water p 15.7) to quench or wash a reaction mixture containing a carboxylic acid byproduct is, again, nothing more than picking the base whose conjugate acid p guarantees the you need for clean, complete deprotonation without also stripping protons off more sensitive functional groups nearby.
Ask the tutor: If I only have aqueous p values but my reaction is run in DMSO, how do I adapt this comparison safely?
The physical picture
Every acid-base reaction you will ever draw in organic chemistry has the same skeleton: an acid HA hands off a proton to a base B, generating a new acid HB⁺ (or HB) and a new base A⁻ (or A). Mechanistically this is a single concerted step — a lone pair on B attacks the proton on HA while the H–A bond breaks heterolytically, both electrons going to A. There is no intermediate; it is one curved arrow into the proton, one curved arrow breaking the bond behind it.
The question "which side does this sit on?" is really the question "is HB⁺ a stronger or weaker acid than HA?" If HB⁺ is the weaker acid (higher p), it holds onto its proton more tightly than HA did, so the system prefers to sit as B–H⁺ and A⁻ — equilibrium lies to the right. If HB⁺ is the stronger acid, it would rather give the proton back to A⁻, so equilibrium sits to the left, mostly as B and HA. This is fundamentally a statement about thermodynamic stability of conjugate bases. A⁻ is more stable than B (lower in energy, better able to bear negative charge) whenever HA is the stronger acid. The reaction moves toward whichever configuration puts the negative charge (or the proton) on the more accommodating partner — exactly analogous to the way a ball rolls toward the lower of two energy wells. The size of the p gap is a direct read of the height of that energy difference, since p is a logarithmic transform of a free energy: .
Notice the axis: this is not literally an energy diagram with a transition state drawn (proton transfers are fast, low-barrier processes), but a schematic of relative thermodynamic depth. The product well (acetate + ammonium) is deeper because ammonium (p 9.25) is a much weaker acid than acetic acid (p 4.76) — so the equilibrium sits overwhelmingly to the right, with . The mechanistic bookkeeping generalizes to any pair of acids, and the key trick for organic chemists is that you rarely need a table of cross reactions — you only need each species' p relative to the same reference reaction (dissociation in water, or DMSO, depending on the table), because subtracting two such values cancels the common reference and gives you the reaction you actually care about.
The important qualitative habit to build: scan a p table, find the acid on each side of the arrow, and ask which one is lower. The lower p species is the stronger acid, and the reaction runs so that the stronger acid ends up as its (weaker) conjugate base while the weaker acid stays protonated. No memorized "product favored/reactant favored" rule of thumb is needed once you can do this comparison in five seconds.
The core ideas
The acidity constant of a generic acid HA is defined (for a dilute aqueous or common reference solvent) as
where: , , are equilibrium concentrations (activities, strictly) of the proton, conjugate base, and acid. For a proton-transfer reaction between acid HA and base B, forming A⁻ and the conjugate acid HB⁺,
the equilibrium constant is
where: the numerator holds the product concentrations, the denominator the reactant concentrations, exactly as any is written from the balanced equation. The central relationship of this whole topic is
where: is the acidity constant of the acid you start with, and is the acidity constant of the acid you end up with (the conjugate acid of the base B). Taking of both sides converts this into the form every chemist actually uses at the bench:
where: , so that
Reading this equation: if the acid being formed (HB⁺) has a higher p than the acid you started with (HA), the exponent is positive, , and equilibrium favors products. If HB⁺ has a lower p than HA, the exponent is negative, , and equilibrium favors reactants. The rule of thumb "equilibrium favors the weaker acid and weaker base side" is just this equation in words.
Goal. Show rigorously that the equilibrium constant for a proton transfer between any two acid-base pairs is the ratio of their individual values, so that only tabulated p data (never a direct measurement of the cross-reaction) is needed.
Step 1 — Write the two reference half-reactions. Both HA and HB⁺ have their own, independently measurable dissociation equilibria in the same reference solvent (say, water):
Mechanistically each of these is water (or another solvent molecule) acting as the base that removes the proton; we are simply using the same solvent as a common reference point for both acids, which is exactly why tabulated p's (all referenced to the same solvent) can be combined.
Step 2 — Add the two half-reactions (Hess's-law-style combination). Reverse the second equilibrium (so B picks up a proton to become HB⁺) and add it to the first:
Adding these two equilibria cancels the free H⁺ on both sides — mechanistically, the proton that leaves HA never has to become a genuinely free, solvent-separated H⁺; it is transferred directly from HA's O–H (or N–H, C–H) bond into B's lone pair in one concerted step, but the thermodynamics of adding two equilibria are identical whether or not a real free-proton intermediate ever exists, because is a state function.
Step 3 — Multiply (not divide!) the corresponding equilibrium constants. Adding two reaction steps multiplies their equilibrium constants. The constant for the reversed step is , so:
Step 4 — Convert to p language. Take of both sides:
Since , substitute and likewise for HB⁺:
Exponentiating both sides gives the working formula:
Step 5 — Sanity limiting case. If HA and HB⁺ happen to have identical p (an acid reacting with the conjugate base of an identical acid, a "self-exchange"), and — equal amounts of both sides at equilibrium, exactly as required by symmetry.
Go deeper · Derivation B · 2 minCurved-arrow mechanism for a real proton transfer, with orbital reasoning
Goal. Show the actual bond-making/bond-breaking event for a specific case — hydroxide deprotonating acetic acid — and connect the orbital picture to why the equilibrium constant works out the way Step 4 above predicts.
Step 1 — Identify the acidic proton and the incoming lone pair. Acetic acid's O–H bond is highly polarized: the acidic hydrogen sits on an oxygen that is also doubly bonded to a second, resonance-stabilizing oxygen. Hydroxide brings a filled sp³-like lone pair on oxygen, which is the HOMO of the nucleophile/base.
Step 2 — Draw the two curved arrows. One arrow starts at a lone pair on hydroxide's oxygen and points to the acidic proton of acetic acid (new O–H σ bond forming, using the base's HOMO overlapping the σ\*(O–H) antibonding orbital of the acid — this is the orbital interaction that makes proton transfer favorable in the first place). A second arrow starts at the breaking O–H bond and points onto the acid's carbonyl oxygen, becoming a lone pair there:
Step 3 — Track charge and note the resonance stabilization of the product. The negative charge that lands on the carboxylate oxygen is not localized: it delocalizes over both oxygens of the carboxylate group by resonance, because the C–O π system and the newly formed lone pair are coplanar and can conjugate. This resonance delocalization is why acetic acid's O–H bond is so much weaker (p 4.76) than, say, ethanol's O–H bond (p ~16) — the conjugate base is dramatically stabilized. This is the molecular-orbital reason the p values differ at all; the p table is really a table of relative conjugate-base (or, for cationic acids, relative lone-pair basicity) stabilities.
Step 4 — Plug into the Keq formula and check the direction makes chemical sense. Here HA = acetic acid (p 4.76) and the acid formed, HB⁺, is water (p 15.7, i.e., of water acting as an acid losing a proton to become hydroxide). So:
Essentially complete, irreversible proton transfer — exactly consistent with the everyday observation that aqueous NaOH instantly and completely deprotonates acetic acid. The mechanism (a fast, essentially barrierless proton transfer along a hydrogen bond) and the huge thermodynamic driving force () are two views of the same underlying orbital/energetic reality.
Worked examples
Example 1 — Foundational: acetic acid + ammonia. Predict the position of, and for,
Identify the acid on each side: on the left it is acetic acid, p; on the right, the acid formed is ammonium, p. Apply the formula, with "acid formed" = NH₄⁺ and "acid consumed" = CH₃COOH:
Direction check: ammonium (p 9.25) is a much weaker acid than acetic acid (p 4.76), so the reaction moves toward the side with ammonium and acetate — decisively to the right, as the large positive exponent confirms. As a limiting-case sanity check, if instead you asked about acetic acid reacting with its own conjugate base acting as a base towards another acetic acid molecule (), you would correctly recover , i.e. no net preference — this is the identity-reaction check built into the formula.
Example 2 — Applied: can DBU deprotonate a malonate ester enough to run a Knoevenagel condensation? DBU (1,8-diazabicyclo[5.4.0]undec-7-ene) is a common non-nucleophilic amidine base with a conjugate-acid p (in water, protonated-DBU-H⁺) of about 12.0. Diethyl malonate's acidic C–H (flanked by two ester carbonyls) has p in water (or ~16.4 in DMSO — pick one solvent scale consistently; we use the aqueous scale here to match DBU's aqueous p). We want:
The mechanism: DBU's basic imine nitrogen lone pair attacks the malonate C–H proton; the C–H σ bond breaks heterolytically, both electrons flowing onto carbon, where they are immediately delocalized by resonance into both flanking ester carbonyls (the true reason malonate C–H protons are as acidic as p ~13, comparable to phenols, despite being on carbon). Identify acids: acid consumed = malonate ester (p 13.3), acid formed = DBU-H⁺ (p 12.0).
The equilibrium actually lies mostly on the starting-material side — only about 5% of the malonate is deprotonated at equilibrium, since DBU-H⁺ (p 12.0) is a slightly stronger acid than the malonate ester (p 13.3), meaning DBU is a slightly weaker base than the malonate anion. This is chemically realistic and important: DBU works in Knoevenagel-type condensations not because it fully deprotonates the substrate, but because even a small equilibrium concentration of enolate is enough to feed a fast, essentially irreversible subsequent step (aldol-type addition), continually pulling the pre-equilibrium forward by Le Chatelier's principle — a subtlety that a purely qualitative "DBU deprotonates malonates" statement would miss, but the quantitative calculation reveals immediately.
Example 3 — Exam/competition level: choosing between LDA and NaOEt for a mono-deprotonation, with a numeric selectivity target. A chemist needs to generate the enolate of cyclohexanone (p in DMSO, using a self-consistent DMSO p scale since we also need an alkoxide value on the same scale) essentially quantitatively (define "essentially quantitatively" as , i.e., forward-favored by at least a million-fold) before adding an electrophile. Two candidate bases are proposed: sodium ethoxide (conjugate acid ethanol, p in DMSO) and LDA (lithium diisopropylamide, conjugate acid diisopropylamine, p in DMSO). Test NaOEt first:
acid consumed = cyclohexanone (p 26); acid formed = EtOH (p 29).
sounds large, but check against the stated target: it is well short of . At equilibrium with excess ethoxide the ketone is mostly, but not overwhelmingly, deprotonated — with 1000:1 favoring enolate at exactly stoichiometric base, a small but real equilibrium population of un-deprotonated ketone remains, which matters for reactions demanding kinetic control of enolate geometry or clean mono-alkylation without competing aldol side reactions. Now test LDA:
acid consumed = cyclohexanone (p 26); acid formed = diisopropylamine (p 36).
comfortably clears the bar — deprotonation with LDA is, for practical purposes, complete and irreversible, which is exactly why LDA (not ethoxide) is the standard reagent for generating a specific, kinetically controlled enolate cleanly at low temperature, with no equilibrium ketone left to scramble the enolate geometry through reversible reprotonation. The mechanistic reason LDA is so much more basic than ethoxide, despite both bearing a full negative charge, is that nitrogen is less electronegative than oxygen and stabilizes negative charge far less well — the amide lone pair is higher in energy (a poorer HOMO match for a weak acid, but exactly the deep, low-affinity-for-H⁺-relative-partner needed here) and correspondingly a stronger base, consistent with diisopropylamine's very high conjugate-acid p of 36.
Limiting cases, scope & common traps
| Situation | What the rule predicts | Why / caveat |
|---|---|---|
| (identical acids) | , statistical 50:50 (per molecule) | Symmetry — no thermodynamic preference either way |
| (e.g. > 5) | Reaction essentially irreversible, product side | ; treat as going to completion for stoichiometric purposes |
| (e.g. < −5) | Negligible product formed | Only trace equilibrium concentration of product; may still be synthetically useful if product is consumed downstream (Example 2) |
| Comparing p's measured in different solvents | Formula does not directly apply | p scales in water, DMSO, and MeCN are not interconvertible by a simple additive constant across all functional-group classes; always use one internally consistent scale |
| Very fast, low-barrier proton transfers | Equilibrium position reached almost instantly | Rule predicts position, not rate — but for simple proton transfers, rate is rarely rate-limiting |
| Steric hindrance at the base (e.g. LDA vs a smaller amide) | Rule still predicts thermodynamics correctly | Kinetics of approach to the acidic proton is a separate question from the thermodynamic |
The chemist behind it
The modern p framework rests on the acid-base theory formalized independently by Johannes Nicolaus Brønsted and Thomas Martin Lowry in 1923, which defined acids and bases purely in terms of proton donation and acceptance — a huge simplification over the older, more restrictive Arrhenius picture that required acids and bases to be defined only in aqueous solution in terms of H⁺ and OH⁻ ions specifically. Brønsted, a Danish physical chemist working in Copenhagen, was deeply interested in the quantitative relationship between acid strength and catalytic ability (what is now called the Brønsted catalysis law, relating rate constants of acid/base-catalyzed reactions to the p of the catalyst) — precisely the kind of thermodynamics-meets-kinetics thinking that underlies the modern practice of scanning a p table to choose a base for a synthetic step.
Origins · 1 minJohannes Nicolaus Brønsted and how this was discovered
Brønsted trained as a chemical engineer before turning to physical chemistry, and spent his career at the University of Copenhagen investigating the thermodynamics of ionic solutions, acid-base catalysis, and (later) isotope separation. His 1923 paper "Einige Bemerkungen über den Begriff der Säuren und Basen" ("Some remarks on the concept of acids and bases") proposed the general proton-donor/proton-acceptor definition that unified what had previously seemed like unrelated acid-base phenomena in water, ammonia, and other solvents — the definition every organic chemist implicitly uses when comparing p values across different functional groups today.
Why does a lower pKa mean a stronger acid, when intuitively "lower number" sounds weaker?
The p scale is a negative logarithm of , specifically . A strong acid dissociates extensively, giving a large (much more product than starting acid at equilibrium). Taking the negative log of a large number gives a small (or even negative) p. So mathematically, strong acid → large → small p. The scale was chosen this way purely for notational convenience (to avoid writing tiny decimal values like for acetic acid), the same motivation behind the pH scale itself. Always keep the definition in mind if the direction ever feels ambiguous — the ordering it implies is arithmetic, not a memorized convention.
Does the ΔpKa rule work for reactions that aren't simple proton transfers, like SN2 or addition reactions?
No — the rule as derived here applies strictly to elementary or overall acid-base (proton-transfer) equilibria, because the derivation relied on combining two dissociation equilibria that both release/accept exactly one proton. Substitution and addition reactions involve different bond reorganizations (C–X bond breaking with backside attack, or π-bond addition) and are governed by different thermodynamic and kinetic factors (leaving-group ability, nucleophilicity, strain, orbital overlap) that are not captured by any single p comparison, though p of a leaving group's conjugate acid is often a useful proxy for how good a leaving group is, since better leaving groups are typically the conjugate bases of stronger acids.
Can I mix p values measured in water with ones measured in DMSO?
Not directly, and this is one of the most common practical errors. Aqueous and DMSO p scales diverge substantially, especially for charged acids and highly delocalized anions, because water solvates small, localized anions (like acetate) far better than DMSO does, while DMSO cannot hydrogen-bond as effectively to stabilize compact anions. As a rough rule, neutral O–H and N–H acids typically show much larger (higher) p values in DMSO than in water, but the shift is not a single additive constant across all functional groups — so always pull both p values from the same solvent-consistent table before subtracting them.
If Keq is astronomically large, does that mean the reaction happens instantly?
Not necessarily — thermodynamic favorability (a large ) and kinetic feasibility (a fast rate) are logically independent, even though for simple, unhindered proton transfers between heteroatoms they are often correlated in practice because such barriers tend to be low. A large tells you where the system will end up if given enough time to equilibrate; it says nothing about how long "enough time" is. Sterically hindered bases, or deprotonations requiring significant geometric reorganization (breaking aromaticity temporarily, for instance), can be thermodynamically overwhelming yet still comparatively slow.
Why do textbooks often list pKa values for the conjugate acid of a base, like ammonium's pKa, rather than a "pKb" for ammonia directly?
Using conjugate-acid p values for every species — acids and bases alike — lets you compare everything on one single, unified numerical scale and directly apply the formula without needing a second, separate p table or any conversion step. Historically p was also used, related by in water at 25 °C, but modern organic practice strongly prefers the single unified conjugate-acid p convention because it is exactly what the derivation here is built around.
What happens right at ΔpKa = 0 — is that ever actually observed?
Yes, whenever an acid reacts with the conjugate base of an acid of (nearly) identical strength, and you get a genuinely mixed, roughly 50:50 (statistically corrected) equilibrium population of both acid-base pairs. This is deliberately exploited in NMR titration experiments and in choosing "matched" buffer systems, where you want partial, tunable protonation rather than an all-or-nothing outcome — for instance, buffers are specifically chosen so that the buffering acid's p is close to the desired pH, which is precisely the regime.
How does this relate to choosing a base for a specific deprotonation in synthesis?
This is exactly the next practical question the framework answers: given a substrate's p, you scan a base table for a conjugate acid p several units higher (for clean, essentially irreversible deprotonation) without being so much higher, or so sterically demanding, that side reactions or slow kinetics become a problem. That systematic base-selection workflow — sometimes needing careful attention to chemoselectivity between multiple acidic sites of different p in the same molecule — is the natural next skill built directly on top of the comparison developed here.