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Henderson–Hasselbalch Equation

The Henderson-Hasselbalch equation is a logarithmic chemical equilibrium relationship that relates the pH of an aqueous solution to the acid dissociation constant (pKa) and the concentration ratio of conjugate base to weak acid.

The Henderson–Hasselbalch equation is a fundamental logarithmic equation in analytical chemistry, biochemistry, and human physiology that relates the pH of an aqueous solution to the negative logarithm of the acid dissociation constant (p*K*a) of a weak acid and the base-10 logarithm of the concentration ratio of its deprotonated conjugate base ([A−]) to its protonated weak acid ([HA]):

`` pH = pKₐ + log₁₀( [A⁻] / [HA] ) ``

First formulated in non-logarithmic mass-action form in 1908 by the American physiologist Lawrence Joseph Henderson to describe how carbonic acid and bicarbonate salts stabilize blood neutrality, the relation was recast into logarithmic pH notation in 1916 by the Danish physician and chemist Karl Albert Hasselbalch (following Søren Sørensen's 1909 introduction of the pH scale). Grounded in Brønsted–Lowry acid–base theory, the Henderson–Hasselbalch equation provides the quantitative framework for designing laboratory buffer solutions, predicting the ionization charge state of amino-acid side chains in proteins and enzymes, modeling drug transmembrane diffusion across lipid bilayers, and diagnosing clinical respiratory and metabolic acid–base disorders.

Thermodynamic Derivation and Activity Corrections

Derivation from the Equilibrium Dissociation Constant

Consider a weak Brønsted–Lowry monoprotic acid HA (such as acetic acid, CH3COOH, or an ammonium ion, R–NH3+) undergoing reversible proton transfer in water:

`` HA (aq) + H₂O (l) ⇌ H₃O⁺ (aq) + A⁻ (aq) ``

At thermodynamic equilibrium, the apparent molar acid dissociation constant (Ka) is defined by the law of mass action (incorporating the constant activity of bulk liquid water into Ka and writing H3O+ simply as H+):

`` Kₐ = ( [H⁺] · [A⁻] ) / [HA] ``

Solving this algebraic expression for the hydronium ion concentration yields [H+] = Ka · ([HA] / [A−]). Taking the negative base-10 logarithm (−log10) of both sides gives:

`` -log₁₀[H⁺] = -log₁₀(Kₐ) - log₁₀( [HA] / [A⁻] ) ``

Substituting the definitions pH = −log10[H+] and p*K*a = −log10(Ka)—and inverting the numerator and denominator inside the logarithm to flip its sign—produces the canonical Henderson–Hasselbalch equation:

`` pH = pKₐ + log₁₀( [Conjugate Base] / [Weak Acid] ) = pKₐ + log₁₀( [A⁻] / [HA] ) ``

From the relationship between standard Gibbs free energy and the equilibrium constant (Δ*G*° = −*RT* ln Ka = 2.303 RT p*K*a), every 1.0 unit increase in p*K*a corresponds to a +5.71 kJ/mol (+1.36 kcal/mol at 25 °C) increase in the free energy required for deprotonation.

Ionic Strength and Debye–Hückel Activity Coefficients

In rigorous chemical thermodynamics, equilibrium constants are defined in terms of dimensionless chemical activities (ai = γi[i]/c°) rather than raw molar concentrations, where γi is the activity coefficient:

`` pH = pKₐ° + log₁₀( [A⁻] / [HA] ) + log₁₀( γ_A⁻ / γ_HA ) ``

In dilute solutions with ionic strength I > 0.01 M (such as intracellular fluid or blood plasma, where I ≈ 0.15 M), the extended Debye–Hückel equation shows that charged ions experience electrostatic shielding from the surrounding ionic atmosphere (γi < 1), which lowers the apparent operational p*K*a' relative to the infinite-dilution thermodynamic p*K*a° (for example, shifting the second dissociation constant of phosphoric acid from p*K*a2° = 7.20 at zero ionic strength to an apparent p*K*a2' = 6.80–6.86 at physiological ionic strength and 37 °C).

Buffer Capacity, Titration Curves, and Polyprotic Systems

The Van Slyke Buffer Capacity Equation

When a strong acid (HCl) or strong base (NaOH) is added to an equimolar mixture of a weak acid HA and its conjugate base A−, the added H+ ions are consumed by A− to form HA, and added OH− ions react with HA to form A− + H2O. Consequently, the ratio [A−]/[HA] changes gradually, resisting large shifts in pH. At the midpoint of a titration curve where [A−] = [HA], log10(1) = 0 and pH = p*K*a. A 10-fold ratio in either direction ([A−]/[HA] = 10:1 or 1:10) shifts the pH by ±1.0 unit (log10(10) = +1; log10(0.1) = −1), defining the effective buffering range of any monoprotic buffer as pH = p*K*a ± 1.0 (spanning 9.1% to 90.9% ionization).

In 1922, Donald Van Slyke quantified the resistance of a buffer solution of total molar concentration Cbuf = [HA] + [A−] to pH changes via the differential buffer capacity (β = dCb / *d*pH = −*dC*a / *d*pH, the moles of strong base or acid per liter required to change pH by 1.0 unit):

`` β = 2.303 · ( (K_w / [H⁺]) + [H⁺] + ( C_buf · Kₐ · [H⁺] ) / ( Kₐ + [H⁺] )² ) ``

Differentiating with respect to [H+] proves that for a given total buffer concentration Cbuf, maximum buffer capacity occurs when [H+] = Ka (pH = p*K*a), where the buffer term simplifies to βmax = 0.576 · Cbuf.

Buffer System / Ionizable GroupConjugate Acid / Base Pairp*K*a' (25–37 °C)Effective Range (p*K*a ± 1)Primary Physiological or Biochemical Role
Acetic Acid / AcetateCH3COOH / CH3COO−4.763.76 – 5.76Biochemical buffer for acidic organelle and enzyme assays
Histidine Imidazole Side ChainImidazolium (His-H+) / Imidazole (His)6.00 – 7.005.00 – 8.00Principal protein buffer in hemoglobin and cytosol; enzyme general acid–base catalysis
Bicarbonate / Carbonic AcidCO2(d) + H2O (H2CO3*) / HCO3−6.10 (at 37 °C)Open respiratory systemPrimary extracellular blood plasma buffer (24 mM HCO3− / 40 mmHg P(CO2))
Inorganic Phosphate (Ka2)H2PO4− / HPO42−6.86 (at I = 0.15 M)5.86 – 7.86Major intracellular fluid buffer and renal tubular urinary buffer
Tris (THAM) Buffer(HOCH2)3CNH3+ / (HOCH2)3CNH28.06 (at 25 °C)7.06 – 9.06Standard molecular biology buffer for DNA electrophoresis and protein purification

Physiological Blood Buffering and Clinical Acid–Base Balance

The Open Bicarbonate–Carbon Dioxide Buffer System

Human arterial blood plasma is maintained within a narrow pH window of 7.35 to 7.45 (average pH 7.40, corresponding to [H+] = 40 nmol/L), primarily through the synergistic action of the extracellular bicarbonate buffer system and intracellular hemoglobin/protein histidine residues. Dissolved carbon dioxide (CO2(d)) undergoes reversible hydration—accelerated >106-fold in erythrocytes and renal tubules by the Zn2+ metalloenzyme carbonic anhydrase—to form carbonic acid (H2CO3), which rapidly dissociates into bicarbonate (HCO3−) and H+:

`` CO₂ (g) ⇌ CO₂ (d) + H₂O ⇌ H₂CO₃ ⇌ H⁺ + HCO₃⁻ ``

Because true undissociated H2CO3 exists at <0.3% of dissolved CO2 concentration, clinical physiology combines [CO2(d)] + [H2CO3] into an effective carbonic acid pool whose concentration is given by Henry's Law: [CO2(d)] = α · P(CO2), where α = 0.0301 mmol·L−1·mmHg−1 is the solubility coefficient of CO2 in plasma at 37 °C and P(CO2) is the arterial partial pressure of carbon dioxide (in mmHg). With an apparent combined p*K*a' = 6.10 at 37 °C, the physiological Henderson–Hasselbalch equation for arterial blood is:

`` pH = 6.10 + log₁₀( [HCO₃⁻] / (0.03 × P_CO₂) ) ``

At normal arterial values of [HCO3−] = 24 mmol/L and P(CO2) = 40 mmHg (so that 0.03 × 40 = 1.2 mmol/L dissolved CO2), the base-to-acid ratio is 24 / 1.2 = 20 : 1. Because log10(20) = 1.30, arterial blood pH equals 6.10 + 1.30 = 7.40.

Respiratory and Metabolic Acid–Base Disturbances

Although a closed buffer with p*K*a = 6.10 would exhibit poor buffer capacity at pH 7.40 (where the ratio is 20:1 rather than 1:1), the physiological bicarbonate buffer operates as an open thermodynamic system coupled to two organs: the lungs regulate the denominator (P(CO2)) within minutes via alveolar ventilation, while the kidneys regulate the numerator ([HCO3−]) over hours to days via proximal tubule HCO3− reabsorption and distal H+/NH4+ excretion:

  • Respiratory Acidosis (↑ P(CO2) > 45 mmHg due to hypoventilation or COPD) lowers pH; kidneys compensate by retaining and generating HCO3−.
  • Respiratory Alkalosis (↓ P(CO2) < 35 mmHg due to hyperventilation or high altitude) raises pH; kidneys compensate by excreting HCO3−.
  • Metabolic Acidosis (↓ [HCO3−] < 22 mM due to diabetic ketoacidosis, lactic acidosis, or renal failure) lowers pH; carotid and central chemoreceptors trigger compensatory hyperventilation (Kussmaul breathing) to blow off CO2 and lower P(CO2).
  • Metabolic Alkalosis (↑ [HCO3−] > 26 mM due to gastric HCl vomiting or loop diuretics) raises pH; respiratory centers modestly decrease ventilation to raise P(CO2).

Frequently Asked Questions

Why is the bicarbonate buffer so effective at blood pH 7.40 even though its pKa is 6.10?

In a sealed test tube (a closed system), a buffer with p*K*a = 6.10 loses most of its buffering capacity at pH 7.40 because adding strong acid converts HCO3− into dissolved CO2, rapidly lowering the [HCO3−]/[CO2] ratio. In the human body (an open system), any excess dissolved CO2 formed when HCO3− neutralizes metabolic H+ is immediately exhaled by the lungs, holding arterial P(CO2) fixed near 40 mmHg (1.2 mM). This physiological clamping of the denominator multiplies the effective buffer capacity of the bicarbonate system several-fold at pH 7.40.

How does the Henderson–Hasselbalch equation predict drug absorption and ion trapping across cell membranes?

Most pharmaceutical drugs are weak organic acids (HA ⇌ H+ + A−, such as aspirin with p*K*a ≈ 3.5) or weak organic bases (BH+ ⇌ H+ + B, such as morphine with p*K*a ≈ 8.0). Because only the uncharged species (HA or B) readily permeates hydrophobic lipid bilayers via simple diffusion, the Henderson–Hasselbalch equation determines the uncharged fraction in each compartment. In the acidic stomach lumen (pH ≈ 1.5), aspirin exists almost exclusively in its protonated, neutral HA form ([HA]/[A−] = 103.5−1.5 = 100:1) and diffuses rapidly into mucosal cells (pH 7.4), where it deprotonates to charged A− ([A−]/[HA] ≈ 7,900:1) and becomes "ion-trapped."

When does the Henderson–Hasselbalch approximation fail in analytical chemistry?

In deriving the standard laboratory form of the Henderson–Hasselbalch equation, one assumes that the initial analytical concentrations placed into solution (CHA and CA−) remain unchanged at equilibrium ([HA] ≈ CHA and [A−] ≈ CA−). This approximation breaks down when (1) the acid is very strong or moderately strong (Ka > 10−2, p*K*a < 2) or very weak (p*K*a > 12), or (2) the total buffer concentration is highly dilute (Cbuf < 10−4 M or comparable to [H+] and [OH−]), requiring exact solution of the cubic charge-balance and water-autoionization (Kw) equations.

References

  1. Henderson, L. J. (1908). "Concerning the relationship between the strength of acids and their capacity to preserve neutrality." American Journal of Physiology, 21(2), 173–179. https://doi.org/10.1152/ajplegacy.1908.21.2.173
  2. Hasselbalch, K. A. (1916). "Die Berechnung der Wasserstoffzahl des Blutes aus der freien und gebundenen Kohlensäure desselben, und die Sauerstoffbindung des Blutes als Funktion der Wasserstoffzahl." Biochemische Zeitschrift, 78, 112–144. https://doi.org/10.1152/physrev.1924.4.3.347
  3. Van Slyke, D. D. (1922). "On the measurement of buffer values and on the relationship of buffer value to the dissociation constant of the buffer and the concentration and reaction of the buffer solution." Journal of Biological Chemistry, 52(2), 525–570. https://doi.org/10.1016/S0021-9258(18)85842-285842-2)
  4. Po, H. N., & Senozan, N. M. (2001). "The Henderson–Hasselbalch equation: Its history and limitations." Journal of Chemical Education, 78(11), 1499–1503. https://doi.org/10.1021/ed078p1499
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