Welcome, aspiring chemists! Today, we're going to dive deep into one of the most fundamental and frequently tested concepts in chemical equilibrium: the
Relationship between Kp and Kc. You might have heard these terms before – Kp and Kc – as equilibrium constants. But why do we have two, and how are they connected? Let's unravel this mystery step-by-step, building a strong conceptual foundation that will serve you well in both board exams and competitive tests like JEE.
---
### Understanding the Equilibrium Constants: Kp and Kc
Before we connect them, let's briefly recap what Kp and Kc represent individually.
#### 1. Kc: The Equilibrium Constant in terms of Molar Concentrations
The equilibrium constant,
Kc, expresses the ratio of product concentrations to reactant concentrations at equilibrium, with each concentration raised to the power of its stoichiometric coefficient. It is primarily used for reactions occurring in
aqueous solutions or when the concentrations of gaseous reactants/products are directly given.
For a general reversible reaction:
aA + bB ⇌ cC + dD
Where a, b, c, d are the stoichiometric coefficients, and A, B, C, D are the chemical species.
The expression for Kc is:
Kc = ([C]c [D]d) / ([A]a [B]b)
Here,
[ ] denotes the
molar concentration (moles/liter or Molarity) of the respective species at equilibrium. Kc is temperature-dependent and has units that vary depending on the stoichiometry of the reaction, though it's often treated as dimensionless in advanced discussions.
#### 2. Kp: The Equilibrium Constant in terms of Partial Pressures
When we deal with
gaseous reactions, it's often more convenient or direct to measure the partial pressures of the reactants and products rather than their molar concentrations. This is where
Kp comes into play. Kp is the equilibrium constant expressed in terms of the
partial pressures of the gaseous reactants and products.
For the same general gaseous reaction:
aA(g) + bB(g) ⇌ cC(g) + dD(g)
The expression for Kp is:
Kp = (PCc PDd) / (PAa PBb)
Here,
P denotes the
partial pressure of the respective gaseous species at equilibrium, usually in atmospheres (atm) or bar. Like Kc, Kp is also temperature-dependent, and its units depend on the reaction stoichiometry.
### The Need for a Relationship: Bridging the Gap
Imagine you have experimental data from a gaseous reaction. Sometimes you measure concentrations, other times you measure partial pressures. Or perhaps you have a value for Kc and need to calculate Kp for a specific application. This is why a relationship between these two constants is absolutely essential. It allows us to
convert between concentration and pressure terms for gaseous species, ensuring consistency and flexibility in our calculations.
### Derivation of the Relationship between Kp and Kc
Let's derive the connection using the Ideal Gas Law. This is a crucial derivation for your understanding and will solidify the concept.
Consider a general reversible gaseous reaction:
aA(g) + bB(g) ⇌ cC(g) + dD(g)
We know the expression for Kp is:
Kp = (PCc PDd) / (PAa PBb) ---(1)
And the expression for Kc is:
Kc = ([C]c [D]d) / ([A]a [B]b) ---(2)
Now, let's bring in the
Ideal Gas Law:
PV = nRT
Where:
* P = Pressure
* V = Volume
* n = Number of moles
* R = Ideal gas constant
* T = Absolute temperature (in Kelvin)
From the Ideal Gas Law, we can express pressure in terms of concentration:
P = (n/V)RT
We know that
molar concentration (C or [ ]) = n/V.
So, for any gaseous species 'X', its partial pressure P
X can be written as:
PX = [X]RT
Now, let's substitute this relationship for each partial pressure in the Kp expression (Equation 1):
* P
A = [A]RT
* P
B = [B]RT
* P
C = [C]RT
* P
D = [D]RT
Substituting these into the Kp expression:
Kp = (([C]RT)c ([D]RT)d) / (([A]RT)a ([B]RT)b)
Let's rearrange the terms:
Kp = ([C]c (RT)c [D]d (RT)d) / ([A]a (RT)a [B]b (RT)b)
Group the concentration terms and the (RT) terms:
Kp = ([C]c [D]d) / ([A]a [B]b) * ((RT)c (RT)d) / ((RT)a (RT)b)
Notice that the first part of this expression is simply
Kc (from Equation 2).
So, we can write:
Kp = Kc * ((RT)c+d) / ((RT)a+b)
Using the rule of exponents (x
m / x
n = x
m-n), we get:
Kp = Kc * (RT)(c+d) - (a+b)
Let's define
Δn_g (delta n gas) as the change in the number of moles of gaseous species during the reaction.
Δn_g = (Sum of stoichiometric coefficients of gaseous products) - (Sum of stoichiometric coefficients of gaseous reactants)
In our general reaction:
Δn_g = (c + d) - (a + b)
Substituting Δn_g into our derived equation, we finally get the highly important relationship:
Kp = Kc (RT)Δn_g
This is the fundamental equation you need to remember and understand!
### Decoding Δn_g: The Change in Moles of Gaseous Species
The term
Δn_g is absolutely critical. Remember these key points:
1.
Only Gaseous Species: When calculating Δn_g, you
must only consider the moles of gaseous reactants and products. Solids and liquids are excluded because their concentrations (and hence partial pressures) do not change significantly and are typically incorporated into the value of K.
2.
Product Moles - Reactant Moles: It's always (moles of gaseous products) minus (moles of gaseous reactants).
Let's look at how Δn_g affects the relationship:
#### Case 1: Δn_g = 0
If the sum of the stoichiometric coefficients of gaseous products equals the sum of the stoichiometric coefficients of gaseous reactants, then Δn_g = 0.
In this case, (RT)
0 = 1.
So, the relationship simplifies to:
Kp = Kc
Example:
H2(g) + I2(g) ⇌ 2HI(g)
* Moles of gaseous products = 2 (for HI)
* Moles of gaseous reactants = 1 (for H
2) + 1 (for I
2) = 2
* Δn_g = 2 - 2 = 0
Therefore, for this reaction,
Kp = Kc.
#### Case 2: Δn_g > 0
If the sum of the stoichiometric coefficients of gaseous products is greater than that of gaseous reactants, then Δn_g is positive.
In this case, Kp will be greater than Kc (assuming RT > 1, which is typically true at normal temperatures).
Kp = Kc (RT)+Δn_g => Kp > Kc
Example:
PCl5(g) ⇌ PCl3(g) + Cl2(g)
* Moles of gaseous products = 1 (for PCl
3) + 1 (for Cl
2) = 2
* Moles of gaseous reactants = 1 (for PCl
5)
* Δn_g = 2 - 1 = +1
Therefore, for this reaction,
Kp = Kc(RT)1 or
Kp = KcRT.
#### Case 3: Δn_g < 0
If the sum of the stoichiometric coefficients of gaseous products is less than that of gaseous reactants, then Δn_g is negative.
In this case, Kp will be less than Kc (assuming RT > 1).
Kp = Kc (RT)-Δn_g => Kp < Kc
Example:
N2(g) + 3H2(g) ⇌ 2NH3(g) (Haber Process)
* Moles of gaseous products = 2 (for NH
3)
* Moles of gaseous reactants = 1 (for N
2) + 3 (for H
2) = 4
* Δn_g = 2 - 4 = -2
Therefore, for this reaction,
Kp = Kc(RT)-2 or
Kp = Kc / (RT)2.
### The Gas Constant (R) and Temperature (T)
The values of R and T are crucial in using the Kp-Kc relationship:
*
T: Must always be in
Kelvin (K). If given in Celsius, convert it: T(K) = T(°C) + 273.15.
*
R: The choice of R depends on the units of pressure used in Kp.
* If partial pressures are in
atmospheres (atm), use
R = 0.0821 L atm mol⁻¹ K⁻¹. This is the most common R value in Kp-Kc calculations for JEE.
* If partial pressures are in
Pascals (Pa), use R = 8.314 J mol⁻¹ K⁻¹ (which is also 8.314 Pa m³ mol⁻¹ K⁻¹).
* If partial pressures are in
bar, use R = 0.08314 L bar mol⁻¹ K⁻¹.
JEE FOCUS: Always double-check the units of pressure given in the problem and choose the appropriate value of R. Mismatched units are a common source of errors!
### Advanced Considerations and JEE Insights
1.
Heterogeneous Equilibria: When solids or liquids are involved in the equilibrium, they do not appear in the Kp or Kc expressions, and therefore, they do not contribute to Δn_g.
Example:
CaCO3(s) ⇌ CaO(s) + CO2(g)
Here, Kp = P
CO2 and Kc = [CO
2].
* Moles of gaseous products = 1 (for CO
2)
* Moles of gaseous reactants = 0 (CaCO
3 is solid)
* Δn_g = 1 - 0 = +1
So,
Kp = Kc(RT)1 or
Kp = KcRT. This holds true as P
CO2 = [CO
2]RT.
2.
Units of Kp and Kc (Revisited): While Kp and Kc are often quoted as dimensionless, their true units depend on Δn_g.
* If Δn_g = 0, Kp and Kc are dimensionless.
* If Δn_g = +1, Kp has units of (atm) and Kc has units of (mol/L). The (RT) term (L atm mol⁻¹ K⁻¹ * K = L atm mol⁻¹) makes them consistent.
* The relationship
Kp = Kc(RT)Δn_g inherently balances the units.
3.
Temperature Dependence: Both Kp and Kc are constants for a given reaction at a specific temperature. The (RT)
Δn_g term in the relationship explicitly shows that the ratio Kp/Kc is also temperature-dependent.
### Worked Examples
Let's solidify our understanding with some practical applications.
#### Example 1: Calculate Kp from Kc
For the reaction:
2SO2(g) + O2(g) ⇌ 2SO3(g)
Given Kc = 2.8 x 10
2 at 1000 K. Calculate Kp. (R = 0.0821 L atm mol⁻¹ K⁻¹)
Step-by-step Solution:
1.
Identify gaseous species and their stoichiometric coefficients:
* Products: SO
3 (2 moles, gas)
* Reactants: SO
2 (2 moles, gas), O
2 (1 mole, gas)
2.
Calculate Δn_g:
Δn_g = (Moles of gaseous products) - (Moles of gaseous reactants)
Δn_g = (2) - (2 + 1) = 2 - 3 = -1
3.
Apply the Kp-Kc relationship:
Kp = Kc (RT)
Δn_g
Kp = (2.8 x 10
2) * (0.0821 * 1000)
-1
4.
Calculate the (RT) term:
RT = 0.0821 L atm mol⁻¹ K⁻¹ * 1000 K = 82.1 L atm mol⁻¹
5.
Substitute and solve for Kp:
Kp = (2.8 x 10
2) * (82.1)
-1
Kp = 280 / 82.1
Kp ≈ 3.41
#### Example 2: Calculate Kc from Kp (Heterogeneous Equilibrium)
For the reaction:
C(s) + H2O(g) ⇌ CO(g) + H2(g)
Given Kp = 3.25 atm at 1200 K. Calculate Kc. (R = 0.0821 L atm mol⁻¹ K⁻¹)
Step-by-step Solution:
1.
Identify gaseous species and their stoichiometric coefficients:
* Products: CO (1 mole, gas), H
2 (1 mole, gas)
* Reactants: H
2O (1 mole, gas), C (solid -
DO NOT INCLUDE in Δn_g)
2.
Calculate Δn_g:
Δn_g = (Moles of gaseous products) - (Moles of gaseous reactants)
Δn_g = (1 + 1) - (1) = 2 - 1 = +1
3.
Apply the Kp-Kc relationship:
Kp = Kc (RT)
Δn_g
3.25 = Kc * (0.0821 * 1200)
+1
4.
Calculate the (RT) term:
RT = 0.0821 L atm mol⁻¹ K⁻¹ * 1200 K = 98.52 L atm mol⁻¹
5.
Substitute and solve for Kc:
3.25 = Kc * 98.52
Kc = 3.25 / 98.52
Kc ≈ 0.0330
#### Example 3: When Δn_g = 0
For the reaction:
H2(g) + I2(g) ⇌ 2HI(g)
If Kc = 54.3 at 700 K, what is Kp?
Step-by-step Solution:
1.
Identify gaseous species and their stoichiometric coefficients:
* Products: HI (2 moles, gas)
* Reactants: H
2 (1 mole, gas), I
2 (1 mole, gas)
2.
Calculate Δn_g:
Δn_g = (2) - (1 + 1) = 2 - 2 = 0
3.
Apply the Kp-Kc relationship:
Kp = Kc (RT)
Δn_g
Kp = Kc (RT)
0
Kp = Kc * 1
Kp = Kc = 54.3
This shows that when Δn_g is zero, the values of Kp and Kc are identical, regardless of temperature or the value of R.
### Conclusion
The relationship
Kp = Kc (RT)Δn_g is a cornerstone of chemical equilibrium calculations for gaseous systems. It's not just a formula to memorize, but a derived consequence of the Ideal Gas Law connecting concentration and pressure. Mastering its application, especially the correct calculation of Δn_g and the selection of R and T units, is vital for success in your chemistry studies and competitive exams. Remember, careful unit handling and understanding the underlying principles will always lead you to the correct answer!