Table of Contents

- 1 Ideal Gas Law
- 2 Equations of State
- 3 Isotherms
- 4 Constant Pressure
- 5 Problem Solving
- 6 Avogador’s Number
- 7 Absolute Temperature
- 8 Isothermal Processes: Definition, Formula & Examples
- 9 What Is an Isothermal Process?
- 10 Isothermal Processes and the First Law of Thermodynamics
- 11 Isothermal Processes in Heat Engines
- 12 Other Expressions for Work Done in Isothermal Processes
- 13 Other Thermodynamic Processes

## Ideal Gas Law

## Equations of State

The ideal gas law is the equation of state of a hypothetical ideal gas (in which there is no molecule to molecule interaction).

### LEARNING OBJECTIVES

Describe how ideal gas law was derived.

### KEY TAKEAWAYS

#### Key Points

- Ideal gas law was derived empirically by combining Boyle’s law and Charles’ law.
- Although the empirical derivation of the equation does not consider microscopic details, the ideal gas law can be derived from first principles in the classical thermodynamics.
- Pressure and volume of a gas can be related to the average velocity of molecues:

#### Key Terms

**mole**: In the International System of Units, the base unit of amount of substance; the amount of substance of a system which contains as many elementary entities as there are atoms in 12 g of carbon-12. Symbol: mol.**ideal gas**: A hypothetical gas whose molecules exhibit no interaction and undergo elastic collision with each other and with the walls of the container.**Avogadro’s number**: the number of constituent particles (usually atoms or molecules) in one mole of a given substance. It has dimensions of reciprocal mol and its value is equal to 6.02214129·1023 mol-1

The ideal gas law is the equation of state of a hypothetical ideal gas (an illustration is offered in ). In an ideal gas, there is no molecule-molecule interaction, and only elastic collisions are allowed. It is a good approximation to the behavior of many gases under many conditions, although it has several limitations. It was first stated by Émile Clapeyron in 1834 as a combination of Boyle’s law and Charles’ law.

### Empirical Derivation

Boyle’s law states that pressure P and volume V of a given mass of confined gas are inversely proportional:

P∝1/V,

while Charles’ law states that volume of a gas is proportional to the absolute temperature T of the gas at constant pressure

V∝T.

By combining the two laws, we get

where C is a constant which is directly proportional to the amount of gas, n (representing the number of moles).

The proportionality factor is the universal gas constant, R, i.e. C = nR.

Hence the ideal gas law

PV=nRT.

Equivalently, it can be written as PV=NkT,

where k is Boltzmann’s constant and N is the number of molecules.

(Since N = nN_{A}, you can see that R=NAk, where N_{A} is Avogadro’s number. )

Note that the empirical derivation does not consider microscopic details. However, the equation can be derived from first principles in the classical thermodynamics (which goes beyond the scope of this Atom ).

### Microscopic version

We have seen in the Atom on “Origin of Pressure” that

where P is the pressure, N is the number of molecules, m is the mass of the molecule, v is the speed of molecules, and V is the volume of the gas. Therefore, we derive a microscopic version of the ideal gas law

## Isotherms

An isothermal process is a change of a system in which the temperature remains constant: ΔT = 0.

### LEARNING OBJECTIVES

Identify conditions at which isothermal processes can occur.

### KEY TAKEAWAYS

#### Key Points

- Isothermal processes typically occur when a system is in contact with an outside thermal reservoir ( heat bath), and the change occurs slowly enough to allow the system to adjust continually to the temperature of the reservoir through heat exchange.
- For an ideal gas, from the ideal gas law PV = NkT, PV remains constant through an isothermal process. A curve in a P-V diagram generated by the equation PV = const is called an isotherm.
- For an isothermal, reversible process, the work done by the gas is equal to the area under the relevant pressure -volume isotherm. It is given as

#### Key Terms

**adiabatic**: Occurring without gain or loss of heat.**internal energy**: The sum of all energy present in the system, including kinetic and potential energy; equivalently, the energy needed to create a system, excluding the energy necessary to displace its surroundings.**ideal gas**: A hypothetical gas whose molecules exhibit no interaction and undergo elastic collision with each other and with the walls of the container.

An isothermal process is a change of a system in which the temperature remains constant: ΔT = 0. Typically this occurs when a system is in contact with an outside thermal reservoir (heat bath), and the change occurs slowly enough to allow the system to adjust continually to the temperature of the reservoir through heat exchange. In contrast, an adiabatic process occurs when a system exchanges no heat with its surroundings (Q = 0). In other words, in an isothermal process, the value ΔT = 0 but Q ≠ 0, while in an adiabatic process, ΔT ≠ 0 but Q = 0.

For an ideal gas, the product PV (P: pressure, V: volume) is a constant if the gas is kept at isothermal conditions (Boyle’s law). According to the ideal gas law, the value of the constant is NkT, where N is the number of molecules of gas and k is Boltzmann’s constant.

The family of curves generated by this equation is shown in the graph presented in. Each curve is called an isotherm. Such graphs are termed indicator diagrams—first used by James Watt and others to monitor the efficiency of engines. The temperature corresponding to each curve in the figure increases from the lower left to the upper right.

### Calculation of Work

In thermodynamics, the work involved when a gas changes from state A to state B is simply:

(This equation is derived in our Atom on “Constant Pressure” under kinetic theory. Note that P = F/A. This definition is consistent with our definition of work being force times distance. )

For an isothermal, reversible process, this integral equals the area under the relevant pressure-volume isotherm, and is indicated in blue in for an ideal gas. Again, P = nRT / V applies and with T being constant (as this is an isothermal process), we have:

By convention, work is defined as the work the system does on its environment. If, for example, the system expands by a piston moving in the direction of force applied by the internal pressure of a gas, then the work is counted as positive. As this work is done by using internal energy of the system, the result is that the internal energy decreases. Conversely, if the environment does work on the system so that its internal energy increases, the work is counted as negative (for details on internal energy, check our Atom on “Internal Energy of an Ideal Gas”).

## Constant Pressure

Isobaric processis a thermodynamic process in which the pressure stays constant (at constant pressure, work done by a gas is PΔV).

### LEARNING OBJECTIVES

Describe behavior of monatomic gas during isobaric processes.

### KEY TAKEAWAYS

#### Key Points

- Gases can expand or contract under a certain constraint. Depending on the constraint, the final state of the gas may change.
- The heat transferred to the system does work but also changes the internal energy of the system. In an isobaric process for a monatomic gas, heat and the temperature change satisfy the following equation:

- For a monatomic ideal gas, specific heat at constant pressure is
^{5}/_{2}R.

#### Key Terms

**the first law of thermodynamics**: A version of the law of energy conservation: the change in the internal energy of a closed system is equal to the amount of heat supplied to the system, minus the amount of work done by the system on its surroundings.**specific heat**: The ratio of the amount of heat needed to raise the temperature of a unit mass of substance by a unit degree to the amount of heat needed to raise that of the same mass of water by the same amount.

Under a certain constraint (e.g., pressure), gases can expand or contract; depending on the type of constraint, the final state of the gas may change. For example, an ideal gas that expands while its temperature is kept constant (called isothermal process) will exist in a different state than a gas that expands while pressure stays constant (called isobaric process). This Atom addresses isobaric process and correlated terms. We will discuss isothermal process in a subsequent Atom.

### Isobaric Process

An isobaric process is a thermodynamic process in which pressure stays constant: ΔP = 0. For an ideal gas, this means the volume of a gas is proportional to its temperature (historically, this is called Charles’ law ). Let’s consider a case in which a gas does work on a piston at constant pressure P, referring to Fig 1 as illustration. Since the pressure is constant, the force exerted is constant and the work done is given as W=Fd, where F (=PA) is the force on the piston applied by the pressure and d is the displacement of the piston. Therefore, the work done by the gas (W) is:

W=PAd.

Because the change in volume of a cylinder is its cross-sectional area A times the displacement d, we see that Ad=ΔV, the change in volume. Thus,

W=PΔV

(as seen in Fig 2—isobaric process ). Note: if ΔV is positive, then W is positive, meaning that work is done by the gas on the outside world. Using the ideal gas law PV=NkT (P=const),

W=NkΔT

(Eq. 1) for an ideal gas undergoing an isobaric process.

### Monatomic Gas

According to the first law of thermodynamics,

Q=ΔU+W

(Eq. 2), where W is work done by the system, U is internal energy, and Q is heat. The law says that the heat transferred to the system does work but also changes the internal energy of the system. Since,

U=^{3}/_{2}NkT for a monatomic gas, we get ΔU=^{3}/_{2}NkΔT

(Eq. 3; for the details on internal energy, see our Atom on “Internal Energy of an Ideal Gas”). By using the Equations 1 and 3, Eq. 2 can be written as:

Q=^{5}/_{2}NkΔT for monatomic gas in an isobaric process.

### Specific Heat

Specific heat at constant pressure is defined by the following equation:

Q=ncPΔT.

Here n is the amount of particles in a gas represented in moles. By noting that N=N_{A}n and R = kN_{A }(N_{A}: Avogadro’s number, R: universal gas constant), we derive:

cP=^{5}/_{2}kNA= ^{5}/_{2}R for a monatomic gas.

## Problem Solving

With the ideal gas law we can figure pressure, volume or temperature, and the number of moles of gases under ideal thermodynamic conditions.

### LEARNING OBJECTIVES

Identify steps used to solve the ideal gas equation.

### KEY TAKEAWAYS

#### Key Points

- Write down all the information that you know about the gas and convert the known values to SI units if necessary.
- Choose a relevant gas law equation that will allow you to calculate the unknown variable, and substitute the known values into the equation. Then calculate the unknown variable.
- The general gas equation only applies if the molar quantity of the gas is fixed.

#### Key Terms

**ideal gas**: A hypothetical gas whose molecules exhibit no interaction and undergo elastic collision with each other and with the walls of the container.**SI units**: International System of Units (abbreviated SI from French: Le Système international d’unités). It is the modern form of the metric system.

The Ideal Gas Law is the equation of state of a hypothetical ideal gas. It is a good approximation to the behavior of many gases under many conditions, although it has several limitations. It is most accurate for monatomic gases at high temperatures and low pressures.

The ideal gas law has the form:

PV=nRT,

where R is the universal gas constant, and with it we can find values of the pressure P, volume V, temperature T, or number of moles n under a certain ideal thermodynamic condition*.* Typically, you are given enough parameters to calculate the unknown. Variations of the ideal gas equation may help solving the problem easily. Here are some general tips.

The ideal gas law can also come in the form:

PV=NkT,

where N is the number of particles in the gas and k is the Boltzmann constant.

To solve the ideal gas equation:

- Write down all the information that you know about the gas.
- If necessary, convert the known values to SI units.
- Choose a relevant gas law equation that will allow you to calculate the unknown variable.
- Substitute the known values into the equation. Calculate the unknown variable.

Remember that the general gas equation only applies if the molar quantity of the gas is fixed. For example, if a gas is mixed with another gas, you may have to apply the equation separately for individual gases.

### Example

Let’s imagine that at the beginning of a journey a truck tire has a volume of 30,000 cm^{3} and an internal pressure of 170 kPa. The temperature of the tire is 16^{∘}C. By the end of the trip, the volume of the tire has increased to 32,000 cm^{3} and the temperature of the air inside the tire is 40^{∘}C. What is the tire pressure at the end of the journey?

Solution:

Step 1. Write down all the information that you know about the gas: P_{1} = 170 kPa and P_{2} is unknown. V_{1} = 30,000 cm^{3} and V_{2} = 32,000 cm^{3}. T_{1} = 16^{∘}C and T_{2} = 40^{∘}C.

Step 2. Convert the known values to SI units if necessary: Here, temperature must be converted into Kelvin. Therefore, T_{1} = 16 + 273 = 289 K, T_{2} = 40 + 273 = 313 K

Step 3. Choose a relevant gas law equation that will allow you to calculate the unknown variable: We can use the general gas equation to solve this problem:

The pressure of the tire at the end of the journey is 173 kPa.

Note that in Step 2 we did not bother to convert the volume values to m^{3}. In Step 4, pressure appears both in the numerator and denominator. In this case the conversion was not necessary.

## Avogador’s Number

The number of molecules in a mole is called Avogadro’s number (N_{A})—defined as 6.02x 10^{23} mol^{-1}.

### LEARNING OBJECTIVES

Explain relationship between Avogadro’s number and mole.

### KEY TAKEAWAYS

#### Key Points

- Avogadro hypothesized that equal volumes of gas, at the same pressure and temperature, contain equal numbers of molecules, regardless of the type of gas.
- Avogadro’s constant is a scaling factor between macroscopic and microscopic (atomic scale) observations of nature. It provides the relation between other physical constants and properties.
- Albert Einstein proposed that Avogadro’s number could be determined based on the quantities observable in Brownian motion. NA was measured for the first time by Jean Baptiste Perrin in 1908.

#### Key Terms

**gas constant**: A universal constant, R, that appears in the ideal gas law, (PV = nRT), derived from two fundamental constants, the Boltzman constant and Avogadro’s number, (R = NAk).**Faraday constant**: The magnitude of electric charge per mole of electrons.**Brownian motion**: Random motion of particles suspended in a fluid, arising from those particles being struck by individual molecules of the fluid.

When measuring the amount of substance, it is sometimes easier to work with a unit other than the number of molecules. A mole (abbreviated mol) is a base unit in the International System of Units (SI). It is defined as any substance containing as many atoms or molecules as there are in exactly 12 grams (0.012 kg) of carbon-12. The actual number of atoms or molecules in one mole is called *Avogadro’s constant (N _{A})*, in recognition of Italian scientist Amedeo Avogadro.

*Avogadro’s number (N)* refers to the number of molecules in one gram-molecule of oxygen. This indicates an amount of substance as opposed to an independent dimension of measurement. In 1811 Amedeo Avogadro first proposed that the volume of a gas (at a given pressure and temperature) is proportional to the number of atoms or molecules, regardless of the nature of the gas (i.e., this number is universal and independent of the type of gas). In 1926, Jean Perrin won the Nobel Prize in Physics, largely for his work in determining the Avogadro constant (by several different methods). The value of Avogadro’s constant, N_{A }, has been found to equal 6.02×10^{23 }mol^{−1}.

### Role in Science

Avogadro’s constant is a scaling factor between macroscopic and microscopic (atomic scale) observations of nature. As such, it provides the relation between other physical constants and properties. For example, it establishes a relationship between the gas constant R and the Boltzmann constant k,

R=kNA=8.314472(15) Jmol−1K−1;

and the Faraday constant F and the elementary charge e,

F=NAe=96485.3383(83) Cmol−1.

### Measuring N_{A}

The determination of N_{A }is crucial to the calculation of an atom’s mass, since the latter is obtained by dividing the mass of a mole of the gas by Avogadro’s constant. In his study on Brownian motion in 1905, Albert Einstein proposed that this constant could be determined based on the quantities observable in Brownian motion. Subsequently, Einstein’s idea was verified, leading to the first determination of N_{A} in 1908 through the experimental work of Jean Baptiste Perrin.

## Absolute Temperature

Absolute temperature is the most commoly used thermodyanmic temperature unit and is the standard unit of temperature.

### LEARNING OBJECTIVES

Describe relationship between absolute temperature and kinetic energy.

### KEY TAKEAWAYS

#### Key Points

- Temperature arises from the kinetic energy of the random motions of matter ‘s particle constituents such as molecules or atoms. Therefore, it is reasonable to choose absolute zero, where all classical motion ceases, as the reference point.
- By international agreement, the unit kelvin and its scale are defined by two points: absolute zero and the triple point of the standardized water.
- At absolute zero, the particle constituents of matter have minimal motion and cannot become any colder. They retain minimal, quantum mechanical motion.

#### Key Terms

**absolute zero**: The coldest possible temperature: zero on the Kelvin scale and approximately -273.15°C and -459.67°F. The total absence of heat; the temperature at which motion of all molecules would cease.**International System of Units**: (SI): The standard set of basic units of measurement used in scientific literature worldwide.**Vienna Standard Mean Ocean Water**: A standard defining a standardized isotopic composition of water.

Thermodynamic temperature is the absolute measure of temperature. It is one of the principal parameters of thermodynamics and kinetic theory of gases. Thermodynamic temperature is an “absolute” scale because it is the measure of the fundamental property underlying temperature: its null or zero point (“absolute zero”) is the temperature at which the particle constituents of matter have minimal motion and cannot become any colder. That is, they have minimal motion, retaining only quantum mechanical motion, as diagramed in.

At its simplest, “temperature” arises from the kinetic energy of the random motions of matter’s particle constituents such as molecules or atoms, as seen in. Therefore, it is reasonable to choose absolute zero, where all classical motion ceases, as the reference point (T=0) of our temperature system. By using the absolute temperature scale (Kelvin system), which is the most commonly used thermodynamic temperature, we have shown that the average translational kinetic energy (KE) of a particle in a gas has a simple relationship to the temperature:

Note that this equation would not look this elegant if the Fahrenheit scale were used instead.

### The Kelvin scale

The kelvin (or “absolute temperature”) is the standard thermodyanmic temperature unit. It is one of the seven base units in the International System of Units (SI) and is assigned the unit symbol K. By international agreement, the unit kelvin and its scale are defined by two points: absolute zero and the triple point of Vienna Standard Mean Ocean Water (water with a specified blend of hydrogen and oxygen isotopes). Absolute zero, the lowest possible temperature, is defined precisely as 0 K and −273.15 °C. The triple point of water is defined precisely as 273.16 K and 0.01 °C.

## Isothermal Processes: Definition, Formula & Examples

Understanding what different thermodynamic processes are and how you use the first law of thermodynamics with each one is crucial when you start to consider heat engines and Carnot cycles.

Many of the processes are idealized, so while they don’t accurately reflect how things occur in the real world, they’re useful approximations that simplify calculations and make it easier to draw conclusions. These idealized processes describe how the states of an ideal gas can undergo change.

The isothermal process is just one example, and the fact that it occurs at a single temperature by definition drastically simplifies working with the first law of thermodynamics when you’re calculating things like heat-engine processes.

## What Is an Isothermal Process?

An isothermal process is a thermodynamic process that occurs at a constant temperature. The benefit of working at a constant temperature and with an ideal gas is that you can use Boyle’s law and the ideal gas law to relate pressure and volume. Both of these expressions (as Boyle’s law is one of the several laws that were incorporated into the ideal gas law) show an inverse relationship between pressure and volume. Boyle’s law implies that:

*P*1*V*1=*P*2*V*2

Where the subscripts denote the pressure (*P*) and volume (*V*) at time 1 and the pressure and volume at time 2. The equation shows that if the volume doubles, for instance, the pressure has to reduce by half in order to keep the equation balanced, and vice versa. The full ideal gas law is

PV=nRT

where *n* is the number of moles of the gas, *R* is the universal gas constant and *T* is the temperature. With a fixed amount of gas and a fixed temperature, *PV* must take a constant value, which leads to the previous result.

On a pressure-volume (PV) diagram, which is a plot of pressure vs. volume often used for thermodynamic processes, an isothermal process looks like the graph of *y* = 1/*x*, curving downwards towards its minimum value.

One point that often confuses people is the distinction between *isothermal* vs. *adiabatic*, but breaking down the word into its two parts can help you remember this. “Iso” means equal and “thermal” refers to something’s heat (i.e., its temperature), so “isothermal” literally means “at an equal temperature.” Adiabatic processes don’t involve heat *transfer*, but the temperature of the system often changes during them.

## Isothermal Processes and the First Law of Thermodynamics

The first law of thermodynamics states that the change in internal energy (*∆U*) for a system is equal to the heat added to the system (*Q*) minus the work done by the system (*W*), or in symbols:

∆U= Q – W

When you’re dealing with an isothermal process, you can use the fact that internal energy is directly proportional to temperature alongside this law to draw a useful conclusion. The internal energy of an ideal gas is:

U = ^{3}/_{2}*nRT*

This means that for a constant temperature, you have a constant internal energy. So with *∆U*= 0, the first law of thermodynamics can easily be re-arranged to:

Q=W

Or, in words, the heat added to the system is equal to the work done by the system, meaning that the heat added is used to do the work. For example, in isothermal expansion, heat is added to the system, which causes it to expand, doing work on the environment without losing internal energy. In an isothermal compression, the environment does work on the system, and causes the system to lose this energy as heat.

## Isothermal Processes in Heat Engines

Heat engines use a complete cycle of thermodynamic processes to convert heat energy into mechanical energy, usually by moving a piston as the gas in the heat engine expands. Isothermal processes are a key part of this cycle, with the added heat energy being completely converted into work without any loss.

However, this is a highly idealized process, because in practice there will always be some energy lost when the heat energy is converted into work. For it to work in reality, it would need to take an infinite amount of time so that the system could remain in thermal equilibrium with its surroundings at all times.

Isothermal processes are considered reversible processes, because if you’ve completed a process (for example, an isothermal expansion) you could run the same process in reverse (an isothermal compression) and return the system to its original state. In essence, you can run the same process forwards or backwards in time without breaking any laws of physics.

However, if you attempted this in real life, the second law of thermodynamics would mean there was an increase in entropy during the “forwards” process, so the “backwards” one wouldn’t completely return the system to its original state.

If you plot an isothermal process on a PV diagram, the work done during the process is equal to the area under the curve. While you can calculate the work done isothermally in this way, it’s often easier to just use the first law of thermodynamics and the fact that the work done is equal to the heat added to the system.

## Other Expressions for Work Done in Isothermal Processes

If you’re doing calculations for an isothermal process, there are a couple of other equations you can use to find the work done. The first of these is:

Where *V*_{f} is the final volume and *V*_{i} is the initial volume. Using the ideal gas law, you can substitute the initial pressure and volume (*P*_{i} and *V*_{i}) for the *nRT* in this equation to get:

It may be easier in most cases to the work through the heat added, but if you only have information about the pressure, volume or temperature, one of these equations could simplify the problem. Since work is a form of energy, its unit is the joule (J).

## Other Thermodynamic Processes

There are many other thermodynamic processes, and many of these can be classified in a similar way to isothermal processes, except that quantities other than temperature are constant throughout. An isobaric process is one that occurs at a constant pressure, and because of this, the force exerted on the walls of the container is constant, and the work done is given by *W* = *P∆V*.

For gas undergoing isobaric expansion, there needs to be heat transfer in order to keep the pressure constant, and this heat changes the internal energy of the system as well as doing work.

An isochoric process takes place at a constant volume. This allows you to make a simplification in the first law of thermodynamics, because if the volume is constant, the system can’t do work on the environment. As a result, the change in internal energy of the system is entirely due to the heat transferred.

An adiabatic process is one that occurs without heat exchange between the system and the environment. This doesn’t mean that there is no change in temperature in the system, though, because the process could lead to an increase or a decrease in temperature without direct heat transfer. However, with no heat transfer, the first law shows that any change in internal energy must be due to work done on the system or by the system, since it sets *Q* = 0 in the equation.

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