Integration Of The Heat Capacity - The Kitchin Research Group

Table of Contents

  • 1. Integrate the heat capacity
    • 1.1. solution   solution
  • 2. Verify via Δ H
    • 2.1. solution   solution

From thermodynamics, the heat capacity is defined as \(C_p = \left(\frac{dH}{dT}\right)_P\). That means we can calculate the heat required to change the temperature of some material from the following integral:

\(H_2 - H_1 = Q = \int_{T_1}^{T_2} C_p(T) dT\)

In the range of 298-1200K, the heat capacity of CO2 is given by a Shomate polynomial:

\(C_p(t) = A + B t + C t^2 + D t^3 + E/t^2\) with units of J/mol/K.

where \(t = T / 1000\), and \(T\) is the temperature in K. The constants in the equation are

  value
A 24.99735
B 55.18696
C -33.69137
D 7.948387
E -0.136638
F -403.6075
G 228.2431
H -393.5224

1 Integrate the heat capacity

Use this information to compute the energy (Q in kJ/mol) required to raise the temperature of CO2 from 300K to 600K. You should use scipy.integrate.quad to perform the integration.

1.1 solution   solution

A = 24.99735 B = 55.18696 C = -33.69137 D = 7.948387 E = -0.136638 F = -403.6075 G = 228.2431 H = -393.5224 def Cp(T): t = T / 1000 return A + B*t + C*t**2 + D*t**3 + E / t**2 from scipy.integrate import quad dH, _ = quad(Cp, 300, 600) print(f'The change in enthalpy is {dH / 1000:1.3f} kJ/mol') The change in enthalpy is 12.841 kJ/mol

2 Verify via Δ H

The change in enthalpy (in kJ / mol) from standard state is

\(dH − dH_{298.15}= A t + B t^2/2 + C t^3/3 + D t^4/4 − E/t + F − H\)

again, \(t = T / 1000\).

Use this equation to compute the change in enthalpy when you increase the temperature from 300 K to 600 K.

2.1 solution   solution

def dH(T): t = T / 1000 return A * t + B*t**2 / 2 + C * t**3 / 3 + D * t**4 / 4 - E/t + F - H print(f'The change in enthalpy is {dH(600) - dH(300):1.3f} kJ/mol') The change in enthalpy is 12.841 kJ/mol

Copyright (C) 2018 by John Kitchin. See the License for information about copying.

org-mode source

Org-mode version = 9.1.13

Từ khóa » H=cpdt