Sign up
|
Login
Home
|
Math
|
Physics
|
Chemistry
|
Biology
|
Other
|
Tools
Submit New Formulas/Articles
Recently Added Physical Formulas
·
Heat Capacity
·
Thermodynamics - Introduction
·
Van der Waals' Equation
·
Clausius–Clapeyron Relation
·
Gibbs Free Energy
Additional Formulas
·
Thermodynamics - Introduction
·
First Law of Thermodynamics
·
Ideal Gas Law
·
Van der Waals' Equation
·
Clausius–Clapeyron Relation
·
Density
·
Molar Mass
·
Molar Volume
·
Helmholtz Free Energy
·
Internal Energy
Current Location
>
Physics Formulas
>
Thermodynamics
> Heat Capacity
Heat Capacity
Short Summary:
The heat capacity is defined as:
d
T
: temperature change
d'
Q
: heat added to the system
Heat capacity (Constant Volume )
For constant volume, the heat capacity is defined as:
C
v
= d
U
/ d
T
Heat capacity (Constant Pressure )
For constant pressure, the heat capacity is defined as:
C
p
= d'
Q
/ d
T
More about heat capacity:
The heat capacity of a body is the quantity of energy needed to cause its temperature to change by 1
o
C. The heat capacity, C, of a system is the ratio of the heat added to the system, or withdrawn from the system, to the resultant change in the temperature:
C = q/
Δ
T =
δ
q/dT [J/deg]
The heat capacity of a body depends on what substance (s) it is made of and the masses of the different substances in the body. The specific heat capacity of a substance is the quantity of energy needed to change the temperature of 1 kg of substance by 1
o
C.
This definition is only valid in the absence of phase transitions.
Units of specific heat capacity are joule
kg
-1 o
C
-1
.
New state of the system is not defined by T only, need to specify or constrain the second variable:
:
heat capacity at constant volume
:
heat capacity at constant pressure
The fact that
δ
q
is not a state function and depends on the path is reflected in the dependence of the heat capacity on the path, cp ≠ cv
(Note that small c is used for the derived intensive quantity, per mass, per volume, or per mole, versus capital C for the extensive quantity. For a system containing n moles
C
p
= nc
p
and
C
v
= nc
v
where
c
v
and
c
p
are molar values).
c
v
and
c
p
can be measured experimentally
isobaric process: dH = δq =
c
p
dT
isochoric process: dU = δq =
c
v
dT
H and U can be calculated from
c
p
and
c
v
c
v
VS c
p
If a material is allowed to expand during heating, how does this affect its heat capacity?
Since U= U(V,T)
Differentiation with respect to T at constant P gives:
: work of expansion at constant P due to the temperature increase by dT
: work of expansion against internal cohesive forces due to the temperature increase by dT
Calculation of enthalpy from heat capacity
For P = constant and dH =
c
p
dT , the integration gives:
Example (1)
Let us find enthalpy for copper at 500K.
c
p
≈ 24.4 Jmol
-1
K
-1
for copper at 1atm.
From the first law we can only calculate the difference ΔH – need a reference enthalpy at 1atm and 298 K is called
enthalpy of formation
, H298. For pure elements in their equilibrium states H
298
= 0.
Enthalpy of substances other than pure elements can also be calculated.
The enthalpy of a compound at 298 K =
standard heat of formation
of the substance from the elements.
Example (2)
For oxidation of copper at 25
o
C:
Cu
solid
+ 1/2C
2
gas = CuO
solid
The reaction is
exothermic
– heat and/or work are produced.
Example (3)
What is the specific heat capacity of water?
Ans: The specific heat capacity of water is S
water
= 4200 joule
kg
-1 o
C
-1
(approximately)
Example (4)
what are the two principle specific (or molar) heat capacities of gases?
Ans: Two principle specific (or molar) heat capacities of gases are:
The specific (or molar) heat capacity at constant volume,
C
v
The specific (or molar) heat capacity at constant pressure,
C
p
Web-Formulas.com ©
2024
|
Contact us
|
Terms of Use
|
Privacy Policy
|