Kp to Kc Converter

Kp to Kc Converter – Equilibrium Constant Calculator

Convert between Kp (equilibrium constant in terms of partial pressure) and Kc (equilibrium constant in terms of concentration) for chemical equilibrium reactions. This calculator uses the relationship Kp = Kc(RT)Δn to perform accurate conversions.

Result:

Quick Conversions

Click on any example below to instantly calculate the conversion:

Haber Process

Kc = 0.0227 at 298 K, Δn = -2

Calculate Kp →

Equal Moles

Kc = 4.5 at 500 K, Δn = 0

Calculate Kp →

Single Mole Increase

Kc = 1.5×10-3 at 373 K, Δn = 1

Calculate Kp →

Two Moles Increase

Kc = 2.8 at 400 K, Δn = 2

Calculate Kp →

Reverse Haber Process

Kp = 3.796×10-5 at 298 K, Δn = -2

Calculate Kc →

Single Mole Decrease

Kc = 0.15 at 298 K, Δn = -1

Calculate Kp →

Conversion Formula

The Relationship Between Kp and Kc:

Kp = Kc × (RT)Δn

Alternatively:

Kc = Kp × (RT)-Δn

Where:

  • Kp = Equilibrium constant in terms of partial pressure
  • Kc = Equilibrium constant in terms of molar concentration
  • R = Universal gas constant (value depends on pressure unit)
  • T = Absolute temperature in Kelvin
  • Δn = Change in number of moles of gas = (moles of gaseous products) – (moles of gaseous reactants)
Important Note: When Δn = 0 (equal number of moles of gaseous products and reactants), then Kp = Kc. Only count gaseous species when calculating Δn; solids and liquids are not included.

Gas Constant Values

The gas constant R varies depending on the pressure unit used in your calculation. Select the appropriate value:

Pressure Unit Gas Constant (R) Value Units
Atmospheres (atm) 0.0820574614 L·atm/(K·mol)
Kilopascals (kPa) 8.314462 L·kPa/(K·mol)
Bars (bar) 0.083144621 L·bar/(K·mol)
Torr 62.36367 L·Torr/(K·mol)
Millimeters of Mercury (mmHg) 62.36367 L·mmHg/(K·mol)

Conversion Examples

Example 1: Converting Kc to Kp (Haber Process)

Reaction: N2(g) + 3H2(g) ⇌ 2NH3(g)

Given: Kc = 2.27 × 10-2 at 298 K

Find: Kp in atmospheres

  1. Calculate Δn: Δn = 2 – (1 + 3) = -2
  2. Identify R: R = 0.0820574614 L·atm/(K·mol) for atmospheres
  3. Apply formula: Kp = Kc × (RT)Δn
  4. Substitute values: Kp = 2.27 × 10-2 × (0.0820574614 × 298)-2
  5. Calculate: Kp = 2.27 × 10-2 × (24.453)-2 = 2.27 × 10-2 × 1.672 × 10-3
  6. Result: Kp ≈ 3.796 × 10-5

Example 2: Converting Kp to Kc

Reaction: H2O(g) + C(s) ⇌ H2(g) + CO(g)

Given: Kp = 0.236 atm at 1000 K

Find: Kc

  1. Calculate Δn: Δn = (1 + 1) – 1 = 1 (carbon is solid, not counted)
  2. Identify R: R = 0.0820574614 L·atm/(K·mol)
  3. Apply formula: Kc = Kp × (RT)-Δn
  4. Substitute values: Kc = 0.236 × (0.0820574614 × 1000)-1
  5. Calculate: Kc = 0.236 × (82.0574614)-1 = 0.236 / 82.0574614
  6. Result: Kc ≈ 2.876 × 10-3

Example 3: When Δn = 0

Reaction: H2(g) + I2(g) ⇌ 2HI(g)

Given: Kc = 54.3 at 700 K

Find: Kp

  1. Calculate Δn: Δn = 2 – (1 + 1) = 0
  2. Apply formula: Kp = Kc × (RT)0 = Kc × 1
  3. Result: Kp = 54.3 (same as Kc)

When the change in moles equals zero, Kp and Kc are numerically equal regardless of temperature or pressure.

Common Chemical Equilibrium Conversions

Reaction Type Typical Δn Temperature Range Notes
Synthesis reactions (A + B → C) Negative Varies Kp < Kc when Δn < 0
Decomposition reactions (C → A + B) Positive Varies Kp > Kc when Δn > 0
Isomerization reactions Zero Varies Kp = Kc
Haber process (N₂ + 3H₂ ⇌ 2NH₃) -2 400-500°C Industrial ammonia production
Water gas shift (CO + H₂O ⇌ CO₂ + H₂) 0 800-1000 K Important for hydrogen production
PCl₅ decomposition (PCl₅ ⇌ PCl₃ + Cl₂) +1 200-300°C Kp > Kc at all temperatures

Frequently Asked Questions

What is the difference between Kp and Kc?

Kp is the equilibrium constant expressed in terms of partial pressures of gases, while Kc is expressed in terms of molar concentrations. Both describe the same equilibrium state but use different units. Kp is used when working with gas pressures, while Kc is used when working with solution concentrations.

When are Kp and Kc equal?

Kp equals Kc when the change in the number of moles of gas (Δn) is zero. This occurs when the number of moles of gaseous products equals the number of moles of gaseous reactants in the balanced chemical equation.

Why do we only count gaseous species when calculating Δn?

Only gaseous species are counted because the ideal gas law (PV = nRT) applies only to gases. Solids and liquids have negligible vapor pressures under standard conditions and do not contribute significantly to the pressure-based equilibrium constant. Their activities are taken as unity (1) in equilibrium expressions.

Which gas constant value should I use?

The gas constant R value you use must match the pressure units in your Kp value. For atmospheres, use R = 0.08206 L·atm/(K·mol). For kilopascals, use R = 8.314 L·kPa/(K·mol). Always verify that your R value matches your pressure unit to avoid calculation errors.

Can I use Celsius instead of Kelvin for temperature?

No, you must use absolute temperature in Kelvin for the formula Kp = Kc(RT)Δn. The ideal gas law requires absolute temperature. To convert Celsius to Kelvin, add 273.15 to the Celsius temperature: K = °C + 273.15.

What if Δn is negative?

If Δn is negative (more gaseous reactants than products), Kp will be smaller than Kc at the same temperature. This is because (RT)Δn becomes a fraction when Δn is negative. The more negative Δn is, the smaller Kp will be relative to Kc.

Do Kp and Kc have units?

Technically, both Kp and Kc should have units based on their definitions, but by convention, they are often reported as dimensionless numbers. This is because concentrations and pressures are typically expressed relative to standard states. When converting between them, however, you must be careful with the units of R to get correct numerical values.

How does temperature affect the relationship between Kp and Kc?

Temperature directly affects the conversion factor (RT)Δn. As temperature increases, if Δn is positive, Kp increases relative to Kc. If Δn is negative, Kp decreases relative to Kc. However, both Kp and Kc themselves change with temperature according to the van ‘t Hoff equation, which is independent of this conversion relationship.

Related Equilibrium Constants

Besides Kp and Kc, there are other equilibrium constants used in chemistry:

Ka (Acid Dissociation Constant)

Measures the strength of an acid in solution. It represents the equilibrium constant for the dissociation of an acid into its conjugate base and a proton. Larger Ka values indicate stronger acids.

Kb (Base Dissociation Constant)

Measures the strength of a base in solution. It represents the equilibrium constant for the reaction of a base with water to form its conjugate acid and hydroxide ion. Larger Kb values indicate stronger bases.

Ksp (Solubility Product Constant)

Describes the equilibrium between a solid and its ions in a saturated solution. It is used to calculate the solubility of sparingly soluble salts. Lower Ksp values indicate lower solubility.

Kw (Water Dissociation Constant)

The equilibrium constant for the self-ionization of water: H₂O ⇌ H⁺ + OH⁻. At 25°C, Kw = 1.0 × 10-14. It relates to pH calculations and acid-base chemistry.

References

Purdue University, Department of Chemistry. “Converting Between Kc and Kp.” General Chemistry Help. https://www.chem.purdue.edu/gchelp/howtosolveit/Equilibrium/Converting_Kc_to_Kp.htm
Atkins, P., & de Paula, J. (2010). Atkins’ Physical Chemistry (9th ed.). Oxford University Press.
Levine, I. N. (2009). Physical Chemistry (6th ed.). McGraw-Hill.
Silberberg, M. S., & Amateis, P. (2018). Chemistry: The Molecular Nature of Matter and Change (8th ed.). McGraw-Hill Education.
IUPAC. “Quantities, Units and Symbols in Physical Chemistry” (Green Book), 3rd Edition, 2007. Royal Society of Chemistry.