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Thermodynamics is a branch of Physics which deals with the equilibrium, energy and its transformation from one form to another. It deals with the relationships between heat and work, and the properties of the system in equilibrium. Historically, Thermodynamics originated as a result of man's endeavor to convert heat into work. The principles of thermodynamics are summarized in the form of four laws that fall within the constraints implied by each which are zeroth law of thermodynamics, first law of thermodynamics, second law of thermodynamics and third law of thermodynamics.
Thermodynamics studies the behavior of Energy. Energy exists in many forms, such as heat, light, electrical energy, chemical energy etc. Energy is the ability to bring about change or to do work. It deals with various macroscopic variables like pressure, temperature, internal energy etc. The results of thermodynamics are useful for other branches and fields of physics and engineering like mechanical, chemical, physical, biomedical, geology, psychrometrics, statistics etc.
Thermodynamics is the study of Heat and Thermal energy.  It is a science which studies various interactions amongst energy, heat, work and temperature, with matter that brings about significant changes in the macroscopic properties of a substance that are measurable. It is basically a phenomenological science based on certain laws of nature which are always obeyed and never seen to be violated.


What is Thermodynamics?

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Thermodynamics is a macroscopic science which studies various interactions amongst energy, notably heat and work transfer, with matter that brings about significant changes in the macroscopic properties of a substance that are measurable. The laws of thermodynamics dictate energy behavior, for example, sweating in a crowded room, taking a bath, melting ice cube etc.
These are the basic laws of thermodynamics :
  1. Zeroth law of thermodynamics
  2. First law of thermodynamics
  3. Second law of thermodynamics
  4. Third law of thermodynamics
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Thermodynamics Equations

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The most fundamental equation of thermodynamics is:

 $P$ = $\frac {W}{t}$

Here, P = power, W = work, t = time
$P$ = $\frac {mgH}{t}$
The fundamental equations of thermodynamics are first and second law of thermodynamics. Both of them are combined to form a common thermodynamic relation.
$dU = TdS – pdv + \sum_{i=1}^{k}u(i)dN(i)$
There are K+2 dimensions for thermodynamics space. U, S, V and N are the extensive quantities. The connections between the state variables are called equation of thermodynamic state. When the system reaches the state of thermal equilibrium then it is described with certain measurable variables that are called state variables. For example for ideal gas we write, $PV = nRT$

Thermodynamics Examples

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  1. The Evaporation of sweat from your body is an example of thermal equilibrium in action.
    Solution A:
    System : The sweat
    Surroundings :Your body + the rest of the universe
    q > 0 so, Heat flows into the system (sweat) from you in order to raise the kinetic energy of the sweat molecules enough to allow them to go from the liquid phase to the gas phase.
    Solution B
    System: You
    Surroundings: The sweat + the rest of the universe
    q < 0 : Heat flows out of the system (you) into the sweat.
    Since heat leaves your body this cools you down. This is the reason for our sweating.                                   
  2. Let us consider two glasses full of water. For one glass, the temperature of water is above the normal room temperature, and for the other glass it is below the normal room temperature. They are left on the table for some time such that they both are not in contact with each other. If you check the glasses after some time, both the glasses reach equilibrium. As observed, both the glasses of water are at the same temperature. The two glasses actually come in contact with the thermal equilibrium with the surroundings. Hence, they are in thermal equilibrium with each other also and they are at the same temperature.
An adiabatic process is a Thermodynamic process in which no heat is gained or lost by the system. If the container of the system in which the process is taking place has thermally-insulated walls or the process completes in a very short time period, so that, there is no opportunity for significant heat exchange then we say an adiabatic process has occurred. Where, Q = 0.Applying the law of Thermodynamics to an adiabatic process we get dQ = 0. Since delta-U is the change in internal energy of the system and W is the work done by the system. Any process that occurs within a system that is a good thermal insulator is also adiabatic.

$dQ = dv + dw = 0, du = -dw$

$U_{2}-U_{1}$=$\Delta U$ = $\Delta - dW$ (Adiabatic process)

When a system expands adiabatically, dW is positive (the system does work on its surroundings), so $\Delta U$ is negative and the internal energy decreases. When a system is compressed adiabatically, dW is negative (work is done on the system by its surroundings) and $\Delta U$ increases. In many (but not all) systems, an increase of internal energy is accompanied by a rise in temperature. The compression stroke in an internal-combustion engine is almost an adiabatic process. The temperature rises as the air-fuel mixture in the cylinder is compressed. The expansion of the burned fuel during the power stroke is also nearly an adiabatic expansion with a drop in temperature.
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An Isothermal Process is a thermodynamic process in which the temperature of the system remains constant.  Where, $\Delta$ T= 0. For a process to be isothermal, any heat flow into or out of the system must occur slowly enough so that thermal equilibrium is maintained. In general, none of the quantities $\Delta$U, Q or dW is zero in an isothermal process. During an isothermal process there is a change in internal energy, work and heat. The heat transfer into or out of the system naturally must happen at such a slow rate that the thermal equilibrium is maintained.Isothermal Process

A hypothetical setup for studying the behavior of gases

The pressure p, volume V, temperature T and number of moles of a gas can be controlled and measured using this setup.  → Read More
Like pressure, volume, temperature and internal energy, we have another thermodynamic variable of a system, named Entropy. The energy that is not available for work is determined by using entropy. According to the second law of thermodynamics, the entropy of the isolated system is constant and never decreases they evolve towards thermodynamic equilibrium. In a given state of equilibrium, the system has a definite value of entropy. For example, a block of ice placed on a hot stove surely melts, while the stove grows cooler. If the system has a temperature T (in absolute scale) and a small amount of heat $\Delta Q is given to it, we define the change in the entropy of the system as $\Delta S$ = $\frac {\Delta Q}{T}$

In general, the temperature of the system may change during a process. If the process is reversible, the change in entropy is defined as

$S_{f} -S_{i}$ = $\int_{i}^{f} \frac {\Delta Q}{T}$

In an adiabatic reversible process, no heat is given out to the system. The entropy of the system remains constant in such a process. Entropy is related to the disorder in the system. Thus, if all the molecules in a given sample of a gas are made to move in the same direction with the same velocity, the entropy will be smaller than that in the actual situation in which the molecules move randomly in all directions.

An interesting fact about entropy is that, it is not a conserved quantity. More interesting is the fact that entropy can be created but cannot be destroyed. The second law of thermodynamics may be stated in terms of entropy as "It is not possible to have a process in which the entropy of an isolated system decreases."

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The total energy of a thermodynamic system can be measured by using enthalpy. This includes the internal energy (the energy required to create a system), and the amount of energy required to make room for it by displacing its environment and establishing its volume and pressure.
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According to the kinetic theory of gases, a gas has a large number of small particles viz atoms or molecules all of which are in constant, random motion. These moving particles collide with each other and with the walls of the container on a constant basis. The kinetic theory explains the macroscopic properties of gases, such as pressure, temperature, or volume is explained by considering their molecular composition and motion.
→ Read More Brownian motion also called the Brownian movement is any physical phenomena in which some quantity is constantly undergoing small, random fluctuations. It is the random motion of particles suspended in a fluid resulting from their collision with the quick atoms or molecules in the gas or liquid. To describe this pre assumed movement we use the concept of Brownian movement. The Jittery motion of particles present in the liquid or gas is called Brownian motion which is also called as Pedesis. This is presumed because there is no relative motion if solids are considered. → Read More

Thermodynamics Table

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The table describing various thermodynamic properties of the compounds is called thermodynamics table. An example is shown below:
Thermodynamics Table

Thermodynamics Problems

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Question 1: Assume a man standing on top of a tower, which is 200m tall and is holding a small, heavy ball that weighs 5kg. What would be the velocity of the ball when it hits the ground assuming it was dropped on the ground with zero initial velocity? What would be the velocity of the ball when it hits the ground assuming it was dropped on the ground with 20m/s?

Question 3: Why does the air pressure of the tire rise while driving?

Question 4: Why should the coolant used in nuclear plants have more specific heat?

Solved Examples

Question 1: A 0.2 m3 container holds oxygen at 70°C and 25 bars. Calculate the amount of oxygen in the container if the atmospheric pressure is 1 bar.
$\bar{R}$-Universal gas constant, M-Molecular weight
We have $PV = nRT$
P = Pressure = 25 + 1 = 26 bars
V = Volume = 0.2 m3
$R$ = $\frac{\bar{R}}{M}$
= $\frac{(8314.3 J/kg.mol-K)}{(32 kg/kg.mol)}$
= 259.8 J/kg-K
T = 273 + 70 = 343K

$m$ = $\frac{PV}{RT}$
= $\frac{26 \times 10^{-5}(N/m^{2})\times0.2 m^{3})}{(259.8 \times343 K}$
= 4.6337928 kg

Question 2: Given the mass of the substance is 12 grams. 3 joules of heat energy is required to raise it temperature by 6 °C. Find the specific heat capacity of the substance? [Hint:S = $\frac{1}{m}\frac{\Delta Q}{\Delta T}$]
Given m = 12g = 0.012 kg
$\Delta Q$ = 3 joules
$\Delta T$ = 6 °C
S = $\frac{1}{m}\frac{\Delta Q}{\Delta T}$
= $\frac{1}{.012}\frac{3}{279}$
= 41.6666 J/kg K

Practice Problems

Question 1: Suppose a man standing on top of a tower, 200m tall. He is holding a small, heavy ball that weighs 5kg. What would be the velocity of the ball be when it hits the ground assuming it was dropped on the ground with zero initial velocity? What would be the velocity of the ball be when it hits the ground assuming it was dropped on the ground with 20m/s?
Question 2: Water is flowing at the rate of 2 litres per minute from a tap and a geyser is heating it such that the temperature rises from 23 to 77 degree centigrade. If the geyser is supplied and aided with a burner than find the rate of combustion of the fuel given the heat of combustion is 2 $\times$ 100000 J/g.
Question 3: Why does the air pressure of the tire rises during driving?
Question 4: Why the coolant used in nuclear plants should have more specific heat?
More topics in Thermodynamics
Phase Change Laws of Thermodynamics
Adiabatic Process Isothermal Process
Entropy Enthalpy
Brownian Motion Kinetic Theory
Gas Laws Ideal Gases
Classical Thermodynamics Phase Transitions
Related Topics
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