pH & pOH / pKa↔Ka Calculator

pH is a logarithmic measure of hydrogen ion concentration, defined as pH = -log₁₀[H⁺]. While [H⁺] is the actual molar concentration (mol/L) of hydrogen ions—which can span from 10⁰ to 10⁻¹⁴ or smaller—pH transforms these unwieldy numbers into a manageable 0-14 scale. For example, [H⁺] = 1.0 × 10⁻⁷ M becomes pH = 7. The logarithmic scale means each 1-unit pH change represents a 10-fold change in [H⁺]: pH 3 is 10× more acidic than pH 4, and 100× more acidic than pH 5.

At 25°C, pH + pOH = 14, derived from the water ionization constant Kw = [H⁺][OH⁻] = 1.0 × 10⁻¹⁴. However, this relationship is temperature-dependent because Kw increases with temperature (water ionization is endothermic). At 0°C, Kw ≈ 1.1×10⁻¹⁵, so pH + pOH ≈ 14.9. At 100°C, Kw ≈ 5.5×10⁻¹³, so pH + pOH ≈ 12.3. Pure water is always neutral ([H⁺] = [OH⁻]), but neutral pH shifts from 7.0 at 25°C to 6.1 at 100°C.

Convert using pKa = -log₁₀(Ka) and Ka = 10⁻ᵖᴷᵃ. The same formulas apply for pKb and Kb. Use pKa for comparisons and conceptual understanding (lower pKa = stronger acid), and use Ka for equilibrium calculations. For example, acetic acid with Ka = 1.8 × 10⁻⁵ has pKa = 4.75. Textbooks and reference tables prefer pKa because it's easier to compare: pKa 4.75 vs 9.25 instantly shows which acid is stronger, whereas comparing 1.8×10⁻⁵ vs 5.6×10⁻¹⁰ requires more mental effort.

Strong acids (HCl, HNO₃, H₂SO₄) dissociate completely in water, so pH is calculated directly: for 0.1 M HCl, [H⁺] = 0.1 M, pH = 1. No equilibrium calculations needed. Weak acids (CH₃COOH, HF, H₂CO₃) only partially dissociate, establishing equilibrium. Their pH requires Ka and equilibrium expressions: for 0.1 M acetic acid (Ka = 1.8×10⁻⁵), [H⁺] ≈ 1.34×10⁻³ M (from √(Ka×C)), pH ≈ 2.87. You can't assume 0.1 M weak acid gives [H⁺] = 0.1 M—it's typically < 5% ionized.

This approximation is valid when percent ionization < 5%, meaning ([H⁺]/C) × 100% < 5%. It assumes the weak acid concentration doesn't change significantly upon dissociation ([HA] ≈ C). Check validity after calculating: if % ionization > 5%, the approximation breaks down and you must use the exact quadratic formula Ka = x²/(C-x). This typically happens with very dilute solutions (low C) or relatively strong weak acids (higher Ka). The calculator automatically detects this and switches to the exact solution when needed.

The Henderson-Hasselbalch equation is pH = pKa + log₁₀([A⁻]/[HA]), where [A⁻] is the conjugate base concentration and [HA] is the weak acid concentration. Use it to calculate buffer solution pH or to find the ratio [A⁻]/[HA] needed for a target pH. Buffers resist pH changes and work best when pH is within pKa ± 1 (where buffer capacity is highest). When [A⁻] = [HA] (equal concentrations), pH = pKa, providing maximum buffering. This equation is fundamental in biochemistry, analytical chemistry, and pharmaceutical formulation.

Temperature affects pH through changes in Kw (water ionization constant). As temperature increases, Kw increases because water ionization is endothermic. This shifts neutral pH: at 25°C neutral is pH 7.0, at 0°C it's pH 7.5, at 100°C it's pH 6.1. Additionally, pKa values of acids and bases change with temperature through the van't Hoff equation. Most pH calculations assume 25°C unless stated otherwise. In real lab work, pH meters must be temperature-compensated, and solutions should be measured at the temperature specified in the procedure.

Salt hydrolysis occurs when dissolved salt ions react with water to produce H⁺ or OH⁻, changing pH. Salts from weak acids + strong bases (like sodium acetate, NaCH₃COO) produce basic solutions because CH₃COO⁻ accepts H⁺ from water. Salts from strong acids + weak bases (like ammonium chloride, NH₄Cl) produce acidic solutions because NH₄⁺ donates H⁺. Salts from strong acids + strong bases (like NaCl) are neutral. To calculate pH, identify which ion hydrolyzes, find its Ka or Kb (using pKa + pKb = 14 for conjugates), and solve the equilibrium problem.

Polyprotic acids donate multiple protons sequentially: H₂SO₄ is diprotic (2 protons), H₃PO₄ is triprotic (3 protons). Each dissociation has its own Ka (Ka₁, Ka₂, Ka₃), with Ka₁ > Ka₂ > Ka₃ because removing each successive proton becomes harder. For pH calculations, the first dissociation usually dominates if Ka₁ >> Ka₂ (at least 1000×). For phosphoric acid (pKa₁=2.15, pKa₂=7.20, pKa₃=12.35), treat as monoprotic using Ka₁ since the pKa values are well-separated. Only when pKa values are close do you need to consider multiple equilibria simultaneously.

The approximation [H⁺] = √(Ka × C) assumes < 5% ionization. It fails when: (1) solution is very dilute (C < 10⁻⁶ M), making water's auto-ionization significant, (2) Ka is relatively large (Ka > 10⁻³), causing >5% dissociation, or (3) you're near the boundaries of weak acid behavior. When approximation fails, use the exact quadratic solution: Ka = x²/(C-x), solve for x = [H⁺]. This calculator automatically checks validity and switches methods. Red flag: if calculated % ionization > 5%, redo with quadratic.

No. This calculator is designed for educational, homework, and conceptual understanding purposes only. It helps you learn acid-base equilibria, practice pH calculations, and build chemical intuition. Real-world applications (lab work, clinical chemistry, industrial processes, water treatment, food science) require proper instrumentation (calibrated pH meters), safety protocols, quality controls, and professional expertise. Never use this tool to prepare solutions for consumption, medical use, or any safety-critical application. Use it to understand the theory—consult qualified professionals for practical implementation.

Yes! The calculator typically includes a buffer mode where you input the weak acid pKa, the concentrations of weak acid [HA] and conjugate base [A⁻], and it calculates pH using Henderson-Hasselbalch: pH = pKa + log₁₀([A⁻]/[HA]). It also helps you determine the ratio needed for a desired pH. Buffers work best within pH = pKa ± 1. The calculator may also calculate buffer capacity and warn if your ratio is outside the effective buffering range (e.g., if [A⁻]/[HA] > 10 or < 0.1).

For a conjugate acid-base pair at 25°C, pKa + pKb = 14 (derived from Ka × Kb = Kw = 10⁻¹⁴). This instantly connects an acid's strength to its conjugate base's strength. If acetic acid has pKa = 4.75, its conjugate base (acetate) has pKb = 14 - 4.75 = 9.25. Use this when: (1) given pKa of an acid but need pKb of its conjugate base for a base equilibrium calculation, (2) comparing relative strengths of conjugate pairs, or (3) converting between acid and base dissociation constants. This relationship only holds at 25°C; at other temperatures, use Ka × Kb = Kw(T).

For pH, the number of decimal places should match the number of significant figures in [H⁺]. If [H⁺] = 3.5 × 10⁻⁴ M (2 sig figs), report pH = 3.46 (2 decimals). The integer part of pH (3) corresponds to the exponent (-4 becomes +4 after negative log), while the decimal part (0.46) comes from log₁₀(3.5). Rule of thumb: sig figs in [H⁺] = decimal places in pH. For [H⁺] = 1.0 × 10⁻⁷ (2 sig figs), pH = 7.00 (2 decimals). Don't report pH = 7.000000 if your [H⁺] only has 2 sig figs—that implies false precision.

Strong bases (NaOH, KOH) dissociate completely: [OH⁻] = concentration. Calculate pOH = -log₁₀[OH⁻], then pH = 14 - pOH (at 25°C). For 0.1 M NaOH: [OH⁻] = 0.1, pOH = 1, pH = 13. Weak bases (NH₃, CH₃NH₂) partially dissociate via B + H₂O ⇌ BH⁺ + OH⁻. Use Kb equilibrium: [OH⁻] = √(Kb × C) (if < 5% ionization), then calculate pOH and pH. For 0.1 M NH₃ (Kb = 1.8×10⁻⁵): [OH⁻] ≈ 1.34×10⁻³, pOH ≈ 2.87, pH ≈ 11.13. Weak bases require equilibrium calculations; strong bases are direct.