Question
Question: At \[1000K\], from the data : \[{N_2}\left( g \right) + 3{H_2}\left( g \right) \to 2N{H_3}\left( g...
At 1000K, from the data :
N2(g)+3H2(g)→2NH3(g); ΔH=−123.77kJmol−1
Substance | N2 | H2 | NH3 |
---|---|---|---|
P/R | 3.5 | 3.5 | 4 |
Calculate the heat of formation of NH3 at 300K.
A.−44.42kJmol−1
B.−88.85kJmol−1
C.+44.42kJmol−1
D.+88.85kJmol−1
Solution
We need to know the effect of Temperature on Heat of Reaction. Chemical or physical processes where heat change takes place, generally depends on the temperature at which the process takes place. This dependence is given by the Kirchhoff equation. This dependence is mathematically expressed in the form of what is known as Kirchhoff equation after G. R. Kirchhoff (1858) who first developed this equation. The equation may easily be derived with the help of the first law of thermodynamics.
Complete answer:
We need to know that the Kirchhoff equation relates the heat of reaction with the definite heats of a structure before and after the reaction.
Consider the process in which the reactants in state A at temperature T1 are converted into products in state B a temperature T2.Then The reactants in state A at temperature T1 are heated to a temperature T2. The heat absorbed is (ΔT)(CP)A. Where, ΔT=T2− T1 , and (CP)A is the heat capacity of the reactants in the state A. The reaction is now allowed to take place at this temperature and the heat change for the process is (HB−HA)2=ΔH2
The total heat change for the process = (ΔT)(CP)A+ΔH2
Also, the reactants in state A at temperature T1 are considered to products in state B at the same temperature. The heat change =(HB−HA)1=ΔH1. The temperature of the products is then raised from T1to T2 and the heat absorbed is (ΔT)(CP)B, where (CP)B-the heat capacity of the products.
The total heat change for the process =(ΔT)(CP)B+ΔH1
According to Hess’s Law of Constant Heat summation, if the reaction takes place in several steps then its Total heat change is the sum of the heat changes of the individual reactions.
Therefore, (ΔT)(CP)A+ΔH2=(ΔT)(CP)B+ΔH1
Or , ΔH2−ΔH1=[(CP)B−(CP)A]x(ΔT)
ΔH2−ΔH1=ΔCP(ΔT)
As given in the question,
ΔH2(1000K)=−123.77kJ/mol
ΔT=1000K−300K
On simplification we get,
⇒ΔT=700K
ΔCP=2CP(NH3)−[CP(N2)+3CP(H2)]
⇒ΔCp=−6×8.314×10−3kJ
ΔH1(300K)=?
From Kirchhoff's equation.
ΔH2(1000K)=ΔH1(300K)+ΔCpΔT
On substituting the known values we get,
⇒−123.77=ΔH1(300K)+(−6×8.314×10−3)×700
On simplification we get,
⇒ΔH1(300K)=−88.85kJ
This value implies for 2 moles of NH3
Therefore, heat of formation of NH3 at 300K=2−88.85
=−44.42kJmol−1
Note:
It must be noted that Heat formation or heat change is also known as standard enthalpy change and is independent of the path between initial state (reactants) and final state (products). The combination of Kirchoff’s Law and Hess’s Law can be used to calculate the formation of heat at different temperatures.