The term
"thermodynamics" originates from two distinct words:
"thermo," referring to heat, and "dynamics," which denotes
movement. Consequently, "thermodynamics" encapsulates the study of
heat flow. In the realm of physical chemistry, this field delves into the
quantitative relationships between heat and other forms of energy, occasionally
referred to as "energetics." At its core, thermodynamics rests upon
four fundamental laws, forming the basis for understanding energy relationships
in both physical and chemical processes. These laws facilitate predictions
regarding:
1) The
likelihood of a chemical reaction occurring upon mixing chemical substances.
2) The
amount of energy theoretically required or released during the reaction.
3) The
equilibrium extent of a chemical reaction, indicating the ratio of products to
reactants.
Chemical
thermodynamics primarily concerns itself with the equilibrium position of a
reaction, although it does not directly forecast the rate of reaction.
These
four laws are:
The Zeroth Law: It establishes the concept of
temperature, asserting that if two systems are each in thermal equilibrium with
a third system, they are in thermal equilibrium with each other.
The First Law: Also known as the principle of
the conservation of energy, it states that energy cannot be created or
destroyed in an isolated system, but can only change forms, maintaining the
total energy of a closed system.
The Second Law: This law dictates that the
total entropy (a measure of disorder or randomness) of an isolated system
always increases over time, with any reversible process accompanied by an
increase in total entropy. It emphasizes the tendency of natural processes to
move towards greater disorder.
The Third Law: It posits that as the temperature
of a system approaches absolute zero, the entropy of the system approaches a
minimum or constant value, making it impossible to reach absolute zero through
a finite number of processes.
These
laws, although not derived from experimental data, have undergone rigorous
mathematical treatments, correlating with various observable properties of matter
across natural phenomena.
Classical
thermodynamics concerns itself with the bulk or macroscopic properties of a
system, independent of its atomic and molecular structure. Conversely,
statistical thermodynamics applies the laws of mechanics to individual
molecules, utilizing statistical averages to derive results. The insights
gained from classical and statistical thermodynamics complement each other.
The zeroth
law introduces the concept of temperature, while the first law emphasizes the
equivalence between different forms of energy without specifying the conditions
under which such equivalence is achieved. The second law imposes restrictions
on the first law and deals with the directions of physico-chemical
transformations and the equilibrium properties of the system. The third law
focuses on evaluating thermodynamic functions.
To
facilitate the study of thermodynamics, it is imperative to grasp certain
terminologies employed in this field:
To study
and understand thermodynamics it is very essential to understand some
terminologies employed in thermodynamics. These terminologies are
1) System: A thermodynamic system is a
part of universe which is studied for our observations.
2) Surrounding: Everything apart from the
system in the rest of the universe is called the surrounding.
3) Boundary or wall: It is a real or
imaginary interface which separates the system and surrounding.
Types of system: There are mainly three different
types of systems are observed in thermodynamics, depending on the interaction
between the system and surroundings. These are:
1) Open systems: A system which can
exchange both matter and energy with the surroundings. Because of these
exchanges is neither matter nor energy remain constant in open systems.
2) Closed systems: These systems in which
exchange of energy with the surroundings is possible while the transfer of matter
with surroundings does not take place. Because of this, in a close system mass
remains constant but energy changes.
3) Isolated systems: In these systems
there are no exchange of matter and energy between the system and the
surroundings. Therefore in this system both mass and energy remain constant.
Systems
can also be categorized in another way
Homogeneous system: A system is said to be
homogeneous if it is uniform throughout. For example, a gas or a mixture of
gases or a pure liquid or a pure solid or a solution of a solid in a liquid are
all homogeneous systems such a system is said to have one face only.
Heterogeneous system: If a system is not uniform
throughout, it is said to be heterogeneous. It then consists of two or more
pages which are separated from each other by definite bounding surfaces. If you
common examples of the heterogeneous systems are (a) a system consisting of a
liquid and its vapour, (b) to or more immiscible liquids, (c) a mixture of two
or more solids.
Macroscopic system: Means a system containing a
large amount of substances. In other words, system is one in which there are
large number of particles i.e. atoms, ions or molecules.
Microscopic property: A property associated with the
collective behaviour of particles in a macroscopic system is called a
microscopic property. If you examples of this properties are pressure volume
temperature surface tension viscosity density refractive index etc.
There
are also several properties of a system. Measurable properties of a system maybe
divided into two classes, viz., extensive and intensive.
1) Extensive property: This property of a system depends upon the
total amount of material in the system. Mass, volume, internal energy, heat
contents, free energy, entropy, heat capacity are some examples of extensive
properties.
2) Intensive property: This property on
the other hand is defined as a property which is independent of the amount of
material in the system. Density, molar properties, i.e., molar volume, molar
energy, molar entropy, molar heat capacity etc., surface tension, viscosity,
specific heat, thermal conductivity, refractive index, pressure, temperature,
boiling and freezing points, vapour pressure of a liquid, etc., are some
intensive properties.
State of a system: A thermodynamic system is said
to be in a definite state when the properties have definite values various
measurable properties of a system which completely define the state of a system
are pressure, volume, temperature and concentration. These are known as the state
variables or thermodynamic variables. Any change in the property due to a
change in the state of a system depends only on the initial and final state.
These variables are directly measurable from experiments and do not require any
assumption regarding the structure of matter and related to one another by an
equation called equation of state.
For an
ideal gas the equation of state for n moles is PV= nRT while for a van der
waals gas, the equation of state is (P+an2/V2)(V-nb) =
nRT.
The
thermodynamic state of a system in such cases can be defined completely by
specifying any two of the three variables any change in the value of these
variables will change in the state of the system which will attend a new state.
If it is desired to bring the system back to its initial state the variables
will have their original values.
Change in the state: Change in the state of a system
is completely defined when the initial and final states are specified.
Path: It is the sequence of
intermediate States or stages arranged in order, followed by the system in
going from its initial to the final state.
Thermodynamic equilibrium: A system is said to be in a
state of thermodynamic equilibrium if none of the observable properties of the
system appears to change with time. The term Thermodynamic Equilibrium assumes
the existence of three types of equilibria in the system. They are
1) Thermal equilibrium: This equilibrium
demands that there should be no flow of heat from one portion of the system to
another. This can happen if the temperature of the system remains constant.
2) Mechanical equilibrium: This
equilibrium implies that no work should be done by one part of the system over
another i.e. No microscopic movement of matter should occur within the system
or of the system with respect to its surroundings. This is possible if the
pressure of the system remains constant.
3) Chemical equilibrium: This equilibrium
demands that no change in composition should take place in any part of the
system with passage of time.
An
equilibrium may be stable, metastable or unstable. If after displacement to a
new state and release of the constant causing displacement, it goes back to its
original state, the system is said to be in a state of stable equilibrium. In
metastable equilibrium, the system is stable for smaller displacements and
unstable for larger displacements.
Process: A thermodynamic process is
defined as the method of operation with the help of which a change in the state
of a system is affected. There are various kinds of process and these are:
Cyclic process: If a system after undergoing
through a series of changes in its state comes back to its initial state, then
the process is turned as cyclic process and the path followed is known as the
cyclic path.
Isothermal process: When a process is carried out in
such a manner that the temperature remains constant throughout the process, it
is called and isothermal process. During this process can flow from the system
to the surroundings and vice versa in order to keep the temperature of the
system constant.
Adiabatic process: When a process is carried out in
such a manner that no heat can flow from the system to the surroundings or vice
versa, i.e., the system is completely insulated from the surroundings, it is
called and adiabatic process.
Isochoric process: It is a process during which the
volume of the system remains constant.
Isobaric process: It is a process during which the
pressure of the system remains constant.
Reversible process: A reversible process is when a
process is carried out infinitesimally slowly
so that all changes occurring in the direct process can be exactly reversed and
the system remains almost in a state of equilibrium at all times. In other
words, a reversible process may be defined as a process which is conducted in
such a manner that at every stage, driving force is only infinitesimally
greater than the opposite force and which can be reversed by increasing the
opposing force by infinitesimal amount. Reversible process is, therefore, always
in a state of equilibrium at each of the small stages. As an example of a
reversible process, consider a case in which a system absorbs heat from the
surroundings. Reversibility in the case implies that the temperature of the
surroundings should be infinitesimally higher than that of the system. If heat
is to flow from the system to the surroundings, the temperature of the latter
must be only infinitesimally lower than that of the system. Similarly, the
expansion of a gas at constant temperature in closed in a cylinder fitted with
a weightless and frictionless piston will be reversible only if the pressure on
the gas during expansion is reduced by an infinitesimal amount. During
compression, the pressure on the gas at each stage is increased by a very small
amount.
A truly
reversible process has to be carried out in an infinite number of states or
stages and would thus require infinite time for its completion. In actual
practice, the small changes in a process have definite magnitudes and are only
approximately closer to strictly reversible process. Strictly speaking, a
reversible process is almost impossible to achieve.
Irreversible process: A process that occurs rapidly or
spontaneously such that it does not remain in equilibrium during the transformation
is called an irreversible process search process do not involve a succession of
equilibrium states of the system. After undergoing a change such processes do
not return themselves to their initial state but can be reverse only with the
help of external agencies. Expansion of gas against zero applied pressure,
dissolution of solute in a solvent, mixing of gases, flow of liquid from higher
to lower levels etc. are examples of irreversible process.
Complete differentials
Thermodynamic
functions like pressure, volume, temperature, energy, entropy, etc. are state
functions. The change in the values of these quantities does not depend on how
the change is carried out but depends only on the initial and final states of
the system. If Z is any thermodynamic property of a homogeneous system of
constant composition then its value is completely determined by the three
thermodynamic variables pressure, volume, and temperature. They are related to
one another by an equation of state. Any two of these three variables are
sufficient to define any thermodynamic property. Therefore we can write,
Z =
f(P,T)
Here Z
may be energy, volume, enthalpy content or any other property to be considered
in details at a later stage. Any change in Z resulting from changes in the
values of P and T is given by
ΔZ = Zfinal-Zinitial
Utilizing
the principle of calculus, we may write for an infinitesimal change dZ in the
property Z
ΔZ =
(dZ/dP)TdP +(dZ/dT)PdT
Where
the partial derivatives (dZ/dP)T represents the rate of change of Z
with pressure at constant temperature and (dZ/dT)P denotes the rate
of change of Z with temperature at constant pressure. Therefore, the first term
on the right hand side denotes the contribution of change in pressure and the
second term indicates the contribution for changes in temperature. The
differential dZ of a function Z as defined by this expression is called a
complete or exact differential. If we put (dZ/dP)T = L (P,T) and
(dZ/dT)P = M(P, T), then we get
dZ = L(P,T)dP
+ M (P,T)dT
On
differentiating L(P, T) [=(dZ/dP)T] with respect to T keeping P
constant and M(P, T) [=(dZ/dT)P] with respect to P maintaining T
constant, we get
(dL/dT)P
= d2Z/dTdP
(dM/dP)T
= d2Z/dPdT
d2Z/dTdP
= d2Z/dPdT
(dL/dT)P
= (dM/dP)T
Hence,
if Z is any thermodynamic function, dZ is an exact differential then the cross
derivatives, (dL/dT)P and (dM/dP)T must be equal. This is
known as Euler’s theorem of exactness. Another characteristic of an exact
differential is that its value for a value for a cyclic transformation is zero,
i.e.,
∮dZ = 0
Here, ∮ denotes the cyclic integral.
We can therefore conclude that dZ will be an exact differential when:
(i) Z is a single-valued function depending entirely on the values of
temperature and pressure,
(ii) dZ between two specified states is independent of the path of the
transformation,
(iii) for a cyclic process ∮dZ = 0
(iv) d2Z/dTdP = d2Z/dPdT
As an example, suppose we have a system containing an ideal gas. The
pressure for a given quantity, say one mole, of the gas is a function of
temperature and volume of the gas, i.e.,
P = f (T, V)
For dP to be an exact differential, we have
dP = (dP/dT)VdT + (dP/dV)TdV
d2P/dTdV = d2P/dVdT
These equations can be evaluated using the ideal gas equation PV = RT. Thus
(dP/dT)V = R/V and d2P/ dVdT = -R/V2
(dP/dV)T = -RT/V and d2P/ dTdV = -R/V2
From these equations we can see that
d2P/ dVdT = d2P/ dTdV
Hence dP is an exact differential.
There are other thermodynamic functions which depend only on the state of
the state of the system and are therefore state functions.
Cyclic rule: Considering any thermodynamic function of volume V and
temperature T, we can write
Z = f (V, T)
Since Z is a state function dZ is given by
dZ = (dZ/dV)T dV + (dZ/dT)V dT
dZ = 0
(dZ/dV)T dV = - (dZ/dT)V dT
(dZ/dV)T (dV/dT)Z = - (dZ/dT)V
Therefore from rearrangement we get
(dZ/dV)T (dV/dT)Z (dT/dZ)V = -1
This expression represents the cyclic rule. Similar types of expressions
can be deduced for any other thermodynamic quantity. For example, if Z is the
pressure of a gas, this expression can be written as
(dP/dV)T (dV/dT)P (dT/dP)V = -1
These expressions represents the basic terminology which is very much required to understand thermodynamics as a subject.
1) Peter Atkins, Julio de Paula, Atkins’ physical chemistry book, eighth edition.
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