In last article, we have studied the concept of temperature. In this article, we shall discuss different thermodynamic or temperature scales.

Temperature can be defined in several ways:

• The temperature may be defined as the degree of hotness or coldness of a body.
• The temperature of a body is an indicator of the average thermal energy (Kinetic energy) of the molecules of the body.
• It is that physical quantity which decides the flow of heat in bodies brought in contact. Heat always flow from the body at higher temperature to the body at the lower temperature.

It is measured in °C (centigrade or Celsius) or K (Kelvin). It is measured by a device called a thermometer. The common thermometer is a mercury thermometer.

The branch of Physics that deals with the measurement of temperature is called Thermometry.

Concept of Thermal Equilibrium:

Two bodies are said to be in thermal equilibrium with each other if no transfer of heat takes place when they are brought in contact, clearly, the two bodies are at the same temperature.

Characteristics of Thermal Equilibrium:

When two or more bodies are kept in contact and they are at the same temperature and there is no transfer of heat taking place between them, then those bodies are said to be in thermal equilibrium with each other. If thermal equilibrium does not exist, then heat flows from a body at a higher temperature to the body at a lower temperature, till thermal equilibrium is established.  Characteristics define thermal equilibrium are as follows:

• Equal Temperatures: In thermal equilibrium, all objects or systems involved have the same temperature. Temperature is a measure of the average kinetic energy of the particles within a substance. When objects are in thermal equilibrium, their average kinetic energies are the same.
• No Net Heat Transfer: In thermal equilibrium, there is no net transfer of heat between the objects or systems. Thus, there is no heat transfer between the bodies due to conduction or convection. This means that while individual particles may still exchange energy through collisions, the overall transfer of thermal energy between the objects results in no net change in their temperatures.
• Stable State: Thermal equilibrium represents a stable state in which the thermal properties of the objects or systems involved remain constant over time. Any initial differences in temperature between the objects or systems will eventually lead to thermal equilibrium as heat is transferred between them.
• Zero Temperature Gradient: A temperature gradient refers to the change in temperature over a distance. In thermal equilibrium, there is no temperature gradient between the objects or systems. This means that the temperature is uniform throughout the system.
• Dynamic Equilibrium: While there is no net transfer of thermal energy in thermal equilibrium, individual particles within the system may still be in motion, exchanging energy through collisions. Thermal equilibrium represents a dynamic balance where the rates of energy transfer between particles are equal.

Understanding thermal equilibrium is crucial in various fields such as thermodynamics, heat transfer, and the study of thermal properties of materials. It helps in analyzing and predicting the behaviour of systems where heat exchange is involved.

Zeroth Law of Thermodynamics:

The Zeroth Law of Thermodynamics is one of the fundamental principles that govern thermodynamic systems. It was formulated after the First and Second Laws of Thermodynamics, but its importance in establishing temperature measurement and the concept of thermal equilibrium led to its designation as the “Zeroth” law. This law introduces the concept of hotness and coldness which leads to the concept of the temperature of a body.

The Zeroth Law states that “If two systems are each in thermal equilibrium with a third system, then they are in thermal equilibrium with each other.”

Thus, if two bodies P and Q are in thermal equilibrium and also P and R in thermal equilibrium then Q and R, are also in thermal equilibrium.

The Zeroth Law essentially establishes the concept of temperature and allows us to define and measure it. It provides a basis for the construction of thermometers and temperature scales. For instance, if two objects are in thermal equilibrium, they have the same temperature.

The importance of the Zeroth Law lies in its role in defining the concept of temperature and establishing the foundation for thermal equilibrium. It allows us to compare temperatures and define scales, which are fundamental for understanding and analyzing the behaviour of thermodynamic systems.

Triple Point of Water:

Phase diagram of water consists of three curves sublimation curve, evaporation curve and melting curve meeting each other at a point called the triple point. Due to these curves, the phase diagram has three regions

The region to the left of the melting curve and above the sublimation curve represents the solid phase of water i.e. ice. The region to the right of the melting curve and above the evaporation curve represents the liquid phase of water i.e. water. The region below the sublimation curve and evaporation curve represent the gaseous phase of water i.e. vapours.

A curve on the phase diagram represents the boundary between two phases of the two substances. Along any curve, the two phases can coexist in equilibrium.

Along the melting curve, ice and water can remain in equilibrium. This curve is called a fusion curve or ice line. This curve indicates that the melting point of ice decreases with an increase in pressure. Along the evaporation curve, water vapours and water can remain in equilibrium. This curve is called the vaporisation curve or steam line. This curve indicates that the boiling point of water increases with an increase in pressure. Along the sublimation curve, ice and water vapours can remain in equilibrium. This curve is called the sublimation line or hoar frost line.

The three curves meet each other at a single point at A. This common point is known as the triple point of water. At the triple point of water can coexist in all the three states in equilibrium. The triple point of water corresponds to a pressure of 0.006023 atmospheres and temperature (0.01 °C) 273.16 K.

Significance of Triple Point of Water:

• Triple point temperature of the water is the temperature at which water can coexist in all the three states viz. Ice (solid), water (liquid), vapours (gas) in equilibrium.
• This triple point temperature of the water is used for defining the absolute temperature scale. In absolute or Kelvin scale 0 K is considered as the lower fixed point while the triple point temperature of the water is taken as the upper fixed point.
• Thus one kelvin temperature corresponds to 1/273.16 of the triple point temperature.

Various Temperature Scales:

There are several temperature scales used around the world, each with its own reference points and units of measurement. Here are the most common temperature scales:

Celsius Scale (° C):

In this scale, the melting point of ice at one-atmosphere pressure and at mean sea level is taken as the lower reference point and consider as 0° C. While boiling point of water at one atmosphere pressure and at mean sea level is taken as an upper reference point and consider as 100° C. The range between the two reference points is divided into 100 equal parts and each part is called 1° C (one degree Celsius). This scale is also called a centigrade scale.

A lower limit of 0° C is considered arbitrary, this scale can be extended to indicate negative temperatures also. A temperature below -273.15° C is not possible.

Fahrenheit Scale (° F):

In this scale, the melting point of ice at one-atmosphere pressure and at mean sea level is taken as the lower reference point and consider as 32° F. While boiling point of water at one atmosphere pressure and at mean sea level is taken as the upper reference point and consider as 212° F. The range between the two reference points is divided into 180 equal parts and each part is called 1° F (one degree Fahrenheit). Nowadays, this scale is not in use.

Kelvin Scale (K):

In this scale, the lowest possible temperature -273.15° C  is taken as a lower reference point. This temperature is called absolute zero. The division of 1 K is equal to 1° C. The unit of temperature in the kelvin scale is K (kelvin) and is considered as the fundamental unit in the S.I. system of units.

Reaumer Scale:

In this scale, the melting point of ice at one-atmosphere pressure and at mean sea level is taken as the lower reference point and consider as 0° R. While boiling point of water at one-atmosphere pressure and at mean sea level is taken as an upper reference point and consider as 80° R. The range between the two reference points is divided into 80 equal parts and each part is called 1° R (one-degree Reaumer).

Conversion of Temperature in Different Scales:

Celsius scale to Kelvin scale  ° C  +  273 = K

Kelvin scale to Celsius scale  K  –  273 = ° C

Numerical Problems:

Example 01:

Find the temperature at which the temperature scales in the following pairs give the same reading: (1) Celsius and Fahrenheit and (2) Fahrenheit and Kelvin

(1) Celsius and Fahrenheit

Solution:

Let θ be the required temperature, such that F = C = θ .

We have

∴ (θ – 32)/180 = θ /100

∴ 100θ – 3200 = 180 θ

∴ – 80θ = 3200

∴ θ = – 40^oF = – 40^oC

Ans: Thus at – 40^oC or – 40^oF, the temperature scales in Celsius and Fahrenheit give the same reading.

(2) Fahrenheit and kelvin:

Solution:

Let θ be the required temperature, such that F = K = θ .

We have

∴ (θ – 32)/9 = ( θ – 273)/5

∴ 5θ – 160 = 9 θ – 2457

∴ 4θ = 2297

∴ θ = 574.25^oF = 574.25 K

Ans: Thus at 574.25^oF or 574.25^oK, the temperature scales in Fahrenheit and Kelvin give the same reading.

Example 02:

Determine the temperature on the Fahrenheit scale which is indicated by double the number on the Centigrade scale.

Solution:

Let θ be the required temperature in centigrade scale, such that C = θ and F = 2 θ .

We have

∴ (2 θ – 32)/180 = θ /100

∴ 200 θ – 3200 = 180 θ

∴ 20 θ = 3200

∴ θ = 160^oC

∴ 2 θ = 2 x 160^o = 320 ^oF

Ans: 320 ^oF is the temperature on the Fahrenheit scale which is indicated by double the number on the Centigrade scale (160^oC).

Example 03:

Convert the following temperature in centigrade into Fahrenheit

• -37 ^oC

Given C = -37 ^oC

∴ (F – 32)/180 = (-37)/100

∴ 100F – 3200 = 6660

∴ 100F = 9860

∴ F = 98.6^oF

Ans: Thus equivalent of temperature -37 ^oC is 98.6 ^oF

• 100^oC

Given C = -100 ^oC

∴ (F – 32)/180 = 100/100

∴ (F – 32)/180 = 1

∴ F – 32 = 180

∴ F = 212^oF

Ans: Thus equivalent of temperature 100 ^oF is 212 ^oF

• -192 ^oC

Given C = -192 ^oC

∴ (F – 32)/180 = (-192)/100

∴ 100F – 3200 = – 34560

∴ 100F = – 31360

∴ F = – 313.6^oF

Ans: Thus equivalent of temperature -192 ^oC is – 313.6 ^oF

Example 04:

Convert the following temperature in centigrade into Fahrenheit

• -108

Given F = -108 ^oF

∴ (-108 – 32)/180 = C/100

∴ -140/180 = C/100

∴ C = (7/9) x 100

∴ C = – 77.78 ^oC

Ans: Thus equivalent of temperature -108 ^oF is – 77.78 ^oC

• 176

Given F = 176 ^oF

∴ (176 – 32)/180 = C/100

∴ 144/180 = C/100

∴ C = (4/5) x 100

∴ C = 80 ^oC

Ans: Thus equivalent of temperature 176 ^oF is 80 ^oC

• 140

Given F = 140 ^oF

∴ (140 – 32)/180 = C/100

∴ 108/180 = C/100

∴ C = (3/5) x 100

∴ C = 60 ^oC

Ans: Thus equivalent of temperature 140 ^oF is 60 ^oC

Example 05:

The fundamental interval of a thermometer is arbitrarily divided into 80 divisions. The lower fixed point of the thermometer is marked 10 ^o. Find what reading this thermometer will show when the reading on a centigrade thermometer is 60 ^oC.

Solution:

Scale 1: Number of Divisions = n = 80, the lower Fixed Point = L = 10^o.

Centigrade Scale: Number of divisions = n = 100, the lower fixed point = L = 0^o.

Given C = 60^oC

∴ ( θ – 10)/4 = 60/5

∴ ( θ – 10)/4 = 12

∴ ( θ – 10) = 48

∴ θ = 58^o on the new scale

Ans: Thus equivalent of temperature 60 ^oC is 58^o on the new scale.

Example 06:

The lower fixed point of a thermometer is marked 10^o and the upper fixed point is 130^o, the interval between the fixed points is divided into 120 equal divisions. What should be the reading indicated by this thermometer when a Centigrade thermometer reads 40^o?

Solution:

Scale 1: Number of Divisions = n = 120, the lower Fixed Point = L = 10^o., The upper fixed point = U = 130^o

Centigrade Scale: Number of divisions = n = 100, the lower fixed point = L = 0^o.

Given C = 60^oC

∴ ( θ – 10)/6 = 40/5

∴ ( θ – 10)/6 = 8

∴ ( θ – 10) = 48

∴ θ = 58^o on the new scale

Ans: Thus equivalent of temperature 40 ^oC, is = 58^o on the new scale.

Example 07:

The fundamental interval of a thermometer is divided arbitrarily into 40 equal parts and that of another thermometer 𝑦 into 80 equal parts. If the freezing point is marked 20^o and that of y is marked 10^o, what is the temperature on when y indicates 70^o? What is the temperature in degrees celsius?

Part I:

Solution:

Scale of thermometer x: Number of Divisions = n = 40, the lower Fixed Point = L = 20^o,

Scale of thermometer y: Number of divisions = n = 80, the lower fixed point = L = 0^o.

Given Y = 70^oC

∴ (X – 20)/40 = 70/80

∴ X – 20 = 35

∴ X = 55^o on the scale of thermometer X.

Ans: Thus equivalent of temperature 70 ^o on scale of thermometer y, is = 55^o on the scale of thermometer x.

Part II:

Solution:

Scale on thermometer y: Number of Divisions = n = 80, the lower Fixed Point = L = 0^o.

Centigrade Scale: Number of divisions = n = 100, the lower fixed point = L = 0^o.

Given Y = 70^oC

∴ 70/4 = C/5

∴ C = (70/4) x 5 = 87.5^oC

Ans: Thus equivalent of temperature 70 ^o on the scale of thermometer y, is = 87.5^oC on the centigrade scale.

Example 08:

Two arbitrary scales A and B have triple points of water defined on 200 A and 350 B. What is the relation between T_A and T_B?

Solution:

The triple point of water is 373 K

For Scale A, 273 K = 200 A i.e. 1 K = (273/200) T_A …………… (1)

For Scale B, 273 K = 350 B i.e. 1 K = (273/350) T_B …………… (2)

From relations (1) and (2) we have

(273/200) T_A = (273/350) T_B

∴ 350 T_A = 200 T_B

∴ T_A / T_B = 200/350

∴ T_A / T_B = 4/7

Ans: T_A / T_B = 4/7

Example 09:

A Centigrade thermometer has its lower and upper fixed points marked – 0.5 ^oC and 100.5 ^oC. What is the true temperature when this thermometer reads30^oC? The bore of the thermometer is uniform.

Solution:

Scale 1: The lower Fixed Point = L = – 0.5 ^oC., the upper fixed point = U = 100.5 ^oC

Centigrade scale: Number of divisions = n = 100, the lower fixed point = L = 0^o.

Given S = 30^oC

∴ (30 + 0.5)/101= C/100

∴ C = (30.5/101) x 100

∴ C = 30.198^oC

Ans: Thus true temperature reading is 30.198^oC

Example 10:

A thermometer is fixed points marked as 5 and 95. What is the correct temperature in Celsius when the thermometer reads 59?

Solution:

Scale 1: The lower Fixed Point = L = 5, the upper fixed point = U = 95

Centigrade scale: Number of divisions = n = 100, the lower fixed point = L = 0^o.

Given S = 59

∴ (59 – 5)/90= C/100

∴ C = (54/90) x 100

∴ C = 60^oC

Ans: Thus correct temperature reading is 60^oC

Example 11:

In an arbitrary scale of temperature, water boils a 40 ^oC and boils at 290 ^oC. Find the boiling point of water in this scale if it boils at 62 ^oC.

Solution:

Scale 1: The lower Fixed Point = L = 40 ^oC, the upper fixed point = U = 290 ^oC

Centigrade scale: Number of divisions = n = 100, the lower fixed point = L = 0^o.

Given C = 62^oC

∴ (S – 40)/250 = 62/100

∴ S – 40 = 0.62 x 250

∴ S – 40 = 155

∴ S = 195 ^oC

Ans: Thus the boiling point of water, in the new scale is 195^oC

Example 12:

The distance between the upper and lower fixed point is 80 cm. Find the temperature on the Celsius scale if the mercury level rises to a height 10.4 cm above the lower fixed point.

Scale 1: The lower Fixed Point = L = 0 cm, the upper fixed point = U = 80 cm

Centigrade scale: Number of divisions = n = 100, the lower fixed point = L = 0^o.

Given S = 10.4 cm

∴ 10.4/80 = C/100

∴ 80C = 1040

∴ C = 1040/80 = 13 ^oC

Ans: Thus the temperature on the Celsius scale is 13 ^oC

Example 13:

The temperature of the two bodies differs by 1oC. How much do they differ on the Fahrenheit scale?

Solution:

Differentiating both sides w.r.t. temperature T

Ans: Thus the difference of 1^oC in Celsius scale corresponds to the difference of 1.8oF on the Fahrenheit scale.

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In last article we have discussed concept of heat. In this article, we shall study the concept of temperature, different temperature scales, and convert temperature in different temperature scales.

Defining Temperature:

Temperature can be defined in several ways:

• The temperature may be defined as the degree of hotness or coldness of a body.
• It is an indicator of the average thermal energy (Kinetic energy) of the molecules of the body.
• It is that physical quantity which decides the flow of heat in bodies brought in contact. Heat always flow from the body at higher temperature to the body at the lower temperature.

It is measured in °C (centigrade or Celsius) or K (Kelvin). It is measured by a device called a thermometer.

Kinetic Interpretation of Temperature:

Temperature reflects the average kinetic energy of particles in a substance. The kinetic energy of a particle is the energy associated with its motion. According to the kinetic theory:

• Temperature and Kinetic Energy: As the temperature of a substance increases, the average kinetic energy of its particles also increases. This means that at higher temperatures, the particles move faster on average.
• Temperature and Particle Speed: Temperature is directly related to the average speed of the particles in a substance. Higher temperatures correspond to higher average speeds, while lower temperatures correspond to lower average speeds.
• Collisions and Pressure: The kinetic theory also explains pressure in terms of particle motion. When particles collide with the walls of their container, they exert a force, resulting in pressure. The force of the collisions depends on the speed of the particles, which in turn is related to temperature.
• Absolute Zero: According to the kinetic theory, at absolute zero (0 Kelvin), particles would have minimal kinetic energy, meaning they would completely cease their motion. This is the lowest possible temperature and represents the point at which particles have minimal energy.

Thus, the kinetic interpretation of temperature provides a fundamental understanding of how the motion of particles at the microscopic level influences the macroscopic properties of a substance, such as its temperature, pressure, and volume.

Various Temperature Scales:

There are several temperature scales used around the world, each with its own reference points and units of measurement. Here are the most common temperature scales:

Celsius Scale (° C):

In this scale, the melting point of ice at one-atmosphere pressure and at mean sea level is taken as the lower reference point and consider as 0° C. While boiling point of water at one atmosphere pressure and at mean sea level is taken as an upper reference point and consider as 100° C. The range between the two reference points is divided into 100 equal parts and each part is called 1° C (one degree Celsius). This scale is also called a centigrade scale.

A lower limit of 0° C is considered arbitrary, this scale can be extended to indicate negative temperatures also. A temperature below -273.15° C is not possible.

Fahrenheit Scale (° F):

In this scale, the melting point of ice at one-atmosphere pressure and at mean sea level is taken as the lower reference point and consider as 32° F. While boiling point of water at one atmosphere pressure and at mean sea level is taken as the upper reference point and consider as 212° F. The range between the two reference points is divided into 180 equal parts and each part is called 1° F (one degree Fahrenheit). Nowadays, this scale is not in use.

Kelvin Scale (K):

In this scale, the lowest possible temperature -273.15° C  is taken as a lower reference point. This temperature is called absolute zero. The division of 1 K is equal to 1° C. The unit of temperature in the kelvin scale is K (kelvin) and is considered as the fundamental unit in the S.I. system of units.

Reaumer Scale:

In this scale, the melting point of ice at one-atmosphere pressure and at mean sea level is taken as the lower reference point and consider as 0° R. While boiling point of water at one-atmosphere pressure and at mean sea level is taken as an upper reference point and consider as 80° R. The range between the two reference points is divided into 80 equal parts and each part is called 1° R (one-degree Reaumer).

Difference between Heat and Temperature:

Heat and temperature are related concepts in thermodynamics, but they represent different aspects of thermal energy.

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Mathematical relationships between volume, pressure, and temperature of a given mass of gas are referred to as Gas laws. In this article. we shall study Charle’s Law.

Charle’s Law:

The relationship between the volume of a gas and temperature was observed by Jacques Charles in 1787.

Statement:

At constant pressure the volume of a given mass of a gas increases or decreases by 1/273 of its volume at 0^oC for every degree rise or fall in temperature.

Explanation:

Let V_o be the volume of a gas at 0 °C, Let this gas be heated through t °C, Let V_t be the volume of the gas at t °C. then,

Thus V ∝ T

Alternate Statement of Charle’s Law:

Thus at constant pressure, the volume of the certain mass of enclosed gas is directly proportional to the absolute temperature of the gas.

In general

This relation is called the mathematical statement of Charle’s law.

Graphical Representation:

A graph is drawn by taking the absolute temperature on the x-axis and volume on the y-axis. The graph is as follows. This graph is also known as a V-T  diagram.

Each line of the graph represents different constant pressure. The lines are called isobar lines.

Charle’s Law and Kinetic Theory of Gases:

According to the kinetic theory of gases, gas consists of a large number of minute particles which are always in constant random motion. During this process, they collide with each other and with the walls of the container containing it. When molecules collide with the walls of the container, there is a change in the momentum of the colliding molecules. This is the cause of the pressure of the gas. According to the kinetic theory of gases, the kinetic energy of molecules is directly proportional to the absolute temperature of the gas.

Thus when gas is heated, the kinetic energy of molecules increases. Due to which the velocity of molecules increases, which results in more collision of the molecules with the walls of the container. But pressure is kept constant, hence the volume of the gas increases proportionally. Hence at constant pressure, the volume of a given mass of a gas is directly proportional to temperature.

Significance of Charle’s Law:

• Charle’s law is significant because it explains how gases behaviour at constant pressure and the relation between the absolute temperature and the volume of the gas. According to Charle’s law, at constant pressure, the volume and absolute temperature of a gas are directly proportional to each other.
• At constant pressure, the density of a gas is inversely proportional to its pressure.
• Using this concept hot air is used to fill the ballons used for meteorological purposes.

Numerical Problems:

Example – 01:

At 300 K a certain mass of a gas occupies  1 x 10^-4 dm³ by volume. Calculate the volume of the gas at 450 K at the same pressure.

Given: Initial temperature = T₁ = 300 K, Initial volume = V₁ = 1 x 10^-4 dm³ , Final temperature = T₂ = 450 K

To Find: Final volume = V₂ = ?

Solution:

By Charle’s Law

∴  V₂ =(T₂/T₁) x V₁

∴  V₂ =(450/300) x 1 x 10^-4 dm³ = (1.5) x 1 x 10^-4 dm³ = 1.5 x 10^-4 dm³

Ans: The volume of the gas at 450 K is 1.5 x 10^-4 dm³

Example – 02:

The volume of a given mass of a gas at 0 °c is 2 dm³. Calculate the new volume of the gas at the constant pressure where (i) the temperature is increased by 10 °C (ii) the temperature is decreased by 10 °C.

Solution:

Part – I: the temperature is increased by 10 °C

Given: Initial temperature = T₁ = 0 °C= 0 + 273.15 = 273.15 K, Initial volume = V₁ = 2 dm³ , Final temperature = T₂ = 0 °C + 10 °C = 10 °C = 10 + 273.15 = 283.15 K

To Find: Final volume = V₂ = ?

By Charle’s Law

∴  V₂ =(T₂/T₁) x V₁

∴  V₂ =(283.15/273.15) x 2 dm³ = 2.07 dm³

Part – II: the temperature is decreased by 10 °C

Given: Initial temperature = T₁ = 0 °C= 0 + 273.15 = 273.15 K, Initial volume = V₁ = 2 dm³ , Final temperature = T₂ = 0 °C – 10 °C = – 10 °C = – 10 + 273.15 = 263.15 K

To Find: Final volume = V₂ = ?

By Charle’s Law

∴  V₂ =(T₂/T₁) x V₁

∴  V₂ =(263.15/273.15) x 2 dm³ = 1.93 dm³

Ans: When the temperature is increased by 10 °C, the new volume of gas is 2.07 dm³. When the temperature is decreased by 10 °C, the new volume of gas is 1.93 dm³

Example – 03:

A certain mass of a gas occupies a volume of 0.2 dm³ at 273 K. Calculate the volume of the gas if the absolute temperature is doubled at the same pressure.

Given: Initial temperature = T₁ = 273 K, Initial volume = V₁ = 0.2 dm³ , Final temperature = T₂ = 2 x 273 = 546 K

To Find: Final volume = V₂ = ?

Solution:

By Charle’s Law

∴  V₂ =(T₂/T₁) x V₁

∴  V₂ =(546/273) x 0.2 dm³ = 0.4 dm³

Ans: When the temperature is doubled, the new volume of gas is 0.4 dm³

Example – 04:

When a ship is sailing in pacific ocean where the temperature is 23.4 °C, a balloon filled with 2.0 L of air. What will be the volume of the balloon when the ship reaches the Indian ocean, where the temperature is 26.1 °C.

Given: Initial temperature = T₁ = 23.4 °C = 23.4 + 273 = 296.4 K, Initial volume = V₁ =2.0 L, Final temperature = T₂ = 26.1 °C = 26.1 + 273 = 299.1 K

To Find: Final volume = V₂ = ?

Solution:

By Charle’s Law

∴  V₂ =(T₂/T₁) x V₁

∴  V₂ =(299.1/296.4) x 2.0 L =  2.018 L

Ans: The volume of the balloon in the Indian ocean is 2.018 L.

Example – 05:

A sample of a gas occupies 10 dm³ at 127 °C and 1 bar pressure. The gas is cooled to – 73 °C at the same pressure. What will be the volume of the gas?

Given: Initial temperature = T₁ = 127 °C = 127 + 273 = 400 K, Initial volume = V₁ =10 dm³, Final temperature = T₂ = – 73 °C = – 73 + 273 = 200 K

To Find: Final volume = V₂ = ?

Solution:

By Charle’s Law

∴  V₂ =(T₂/T₁) x V₁

∴  V₂ =(200/400) x 10 dm³ =  5 dm³

Ans: The new volume of the gas is 5 dm³

Example – 06:

A sample of gas is found to occupy a volume of 900 cm³ at 27 °C. Calculate the temperature at which it will occupy a volume of 300 cm³, provided the pressure is kept constant.

Given: Initial temperature = T₁ = 27 °C = 27 + 273 = 300 K, Initial volume = V₁ = 900 cm³ , Final volume = V₂ =300 cm³

To Find: Final temperature = T₂ = ?

Solution:

By Charle’s Law

∴  T₂ =(V₂/V₁) x T₁

∴  T₂ =(300 cm³/900 cm³) x 300 K  = 100 K

∴  T₂ = 100 – 273 = -173 °C

Ans: At temperature  -173 °C the volume is 300 cm³

Example – 07:

A gas occupies 100.0 mL at 50  °C and 1 atm pressure. The gas is cooled at constant pressure so that its volume is reduced to 50 mL. What is the final temperature?

Given: Initial temperature = T₁ = 50 °C = 50 + 273 = 323 K, Initial volume = V₁ = 100.0 mL , Final volume = V₂ = 50.0 mL

To Find: Final temperature = T₂ = ?

Solution:

By Charle’s Law

∴  T₂ =(V₂/V₁) x T₁

∴  T₂ =(50.0 mL/100.0 mL) x 323 K  = 161.5 K

∴  T₂ = 150 – 273 = -111.5 °C

Ans: At temperature  – 115.5 °C the volume is 50 mL.

Example – 08:

A gas occupies 100.0 mL at 50  °C and 1 atm pressure. The gas is cooled at constant pressure so that its volume is reduced to 50 mL. What is the final temperature?

Given: Initial temperature = T₁ = 50 °C = 50 + 273 = 323 K, Initial volume = V₁ = 100.0 mL , Final volume = V₂ = 50.0 mL

To Find: Final temperature = T₂ = ?

Solution:

By Charle’s Law

∴  T₂ =(V₂/V₁) x T₁

∴  T₂ =(50.0 mL/100.0 mL) x 323 K  = 161.5 K

∴  T₂ = 150 – 273 = -111.5 °C

Ans: At temperature  – 115.5 °C the volume is 50 mL.

Example – 09:

A vessel of capacity 400 cm³ contains hydrogen gas at 1 atm pressure and 7°C. In order to expel 28.57 cm³ of the gas the same pressure to what temperature the vessel should be heated?

Given: Initial temperature = T₁ = 7 °C = 7 + 273 = 280 K, Initial volume = V₁ = 400 cm³, Final volume = V₂ = 400 cm³ + 28.57 cm³ = 428.57cm³.

To Find: Final temperature = T₂ = ?

Solution:

By Charle’s Law

∴  T₂ =(V₂/V₁) x T₁

∴  T₂ =(428.57 cm³/400.0 cm³) x 280 K  = 300 K

∴  T₂ = 300 – 273 = 27 °C

Ans: At temperature  27 °C, 28.57 cm³ of the gas expels.

Example – 10:

1 L of air weighs 1.293 g at 0 °C and 1 atm pressure. At what temperature 1 L of air at 1 atm pressure will weigh 1 g.

Given: Initial temperature = T₁ = 0 °C = 0 + 273 = 273 K, Initial density = ρ₁ = 1.293 g/L, Final density = ρ₂ = 1 g/L.

To Find: Final temperature = T₂ = ?

Solution:

By Charle’s Law

∴  T₂ =(V₂/V₁) x T₁

∴  T₂ =((m/ρ₂)/(m/ρ₁)) x T₁

∴  T₂ =(ρ₁/ρ₂) x T₁

∴  T₂ =(1.293/1) x 273 = 353 K

∴  T₂ = 353 – 273 = 27 °C

Ans: At temperature  80 °C, 1 L of air weighs 1 g

Science > Chemistry > States of Matter > Charle’s Law

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Mathematical relationships between volume, pressure, and temperature of a given mass of gas are referred to as Gas laws. In this article. we shall study Boyle’s Law.

Boyle’s Law:

In 1662, Robert Boyle, on the basis of his experiments put forward the law. It is the relation between the volume and the pressure of enclosed gas at constant temperature.

Statement:

At constant temperature, the volume of a certain mass of enclosed gas varies inversely with its pressure.

Explanation:

Let P be the pressure and V be the volume of a certain mass of enclosed gas, then at the constant temperature

P   ∝  1/V

Thus PV = Constant.

Thus, for a given amount of the gas, the product of pressure and volume is constant at constant temperature.

If V₁ and V₂ are the volumes of a gas at pressures P₁ and P₂ respectively at a constant temperature.

P₁V₁ = P₂V₂

This relation is called the mathematical statement of Boyle’s Law.

Graphical Representation:

Graph of Pressure (P) Versus Volume (V):

A graph is drawn by taking volume on the x-axis and pressure on the y-axis. The graph is as follows. This graph is also known as PV diagram.

Each curve is rectangular hyperbola and corresponds to a different constant temperature and is known as an isotherm (constant temperature plot). Higher curves correspond to higher temperatures. It should be noted that volume of the gas doubles if pressure is halved.

Graph of Pressure (P) Versus Reciprocal of Volume (1 / V):

The straight lines obtained in the graph confirms that P ∝ 1/V.

Graph of Product of Pressure and Volume (PV) Versus Pressure (P):

The graph parallel to x-axis confirms that at a particular temperature of the gas, the product of its volume and corresponding pressure is always constant.

Graphs in terms of Logarithmic Variations:

By Boyle’s law, we have PV = k = constant

Taking log of both sides

Log P + Log V = log K

∴  LogP = – LogV + log K

∴  LogP = log (1/V) + log k

Relation Between Density and Pressure:

Thus the density of the certain mass of an enclosed gas is directly proportional to its pressure.

Boyle’s Law and Kinetic Theory of Gases:

According to the kinetic theory of gases, gas consists of a large number of minute particles which are always in constant random motion. During this process, they collide with each other and with the walls of the container containing it. When molecules collide with the walls of the container, there is a change in the momentum of the colliding molecules. This is the cause of the pressure of the gas. According to the kinetic theory of gases, the kinetic energy of molecules is directly proportional to the absolute temperature of the gas. In Boyle’s law temperature is constant. Hence the kinetic energy of the molecules is a constant.

For enclosed gas, the number of molecules of a gas is constant. When the volume of a gas is reduced, the molecules are forced more closer together. Thus the density of gas increased and they collide more frequently. Hence at less volume, there are more collisions and hence more pressure. When the volume of a gas is increased, the molecules are away from each other and they collide less frequently. Hence at larger volumes, there are fewer collisions and hence less pressure. So at a constant temperature, the volume and pressure of a gas are inversely proportional.

Significance of Boyle’s Law:

• Boyle’s law is significant because it explains how gases behaviour at constant temperature and the relation between the pressure and the volume of the gas. According to Boyle’s law, at a constant temperature, the pressure and volume of a gas are inversely proportional to each other.
• At constant temperature, the density of a gas is directly proportional to its pressure.
• Atmospheric pressure is low at high altitudes, so air is less dense. Hence, a lesser quantity of oxygen is available for breathing. This is the reason why mountaineers have to carry oxygen cylinders with them.

Numerical Problems:

Example – 01:

5 dm³ volume of a gas exerts a pressure of 2.02 × 10⁵ kPa. This gas is completely pumped into another tank where it exerts a pressure of 1.01 × 10⁵ kPa at the same temperature, calculate the volume of the tank

Given: Initial volume = V₁ = 5 dm³, Initial pressure = P₁ = 2.02 × 10⁵ kPa, Final pressure P₂ = 1.01 ₁ kPa, Temperature constant

To Find: Final volume = V₂ =?

Solution:

At constant temperature by Boyle’s law

P₁V₁ = P₂V₂

∴ V₂ = P₁V₁ /P₂

∴  V₂ = 2.02 × 10⁵ kPa × 5 dm³ / 1.01 × 10⁵ kPa

∴ V₂ = 10 dm³

Hence the volume of the tank is 10 dm³.

Example – 02:

Given the mass of a gas occupies a volume of 2.5 dm³ at NTP. Calculate the change in volume of gas at same temperature if the pressure of the gas is changed to 1.04 × 10⁵ Nm^-2.

Given: Initial volume = V₁ = 2.5 dm3, Initial pressure = P₁ = 1.013 × 10⁵ Nm^-2 (Normal pressure), Final pressure P₂ = 1.04 × 10⁵ Nm^-2, Temperature constant

To Find: Final volume = V₂ =?

Solution:

At constant temperature by Boyle’s law

P₁V₁ = P₂V₂

∴ V₂ = P₁V₁ /P₂

∴  V₂ = 1.013 × 10⁵ Nm^-2 × 2.5 dm³ / 1.04 × 10⁵ Nm^-2

∴   V₂ = 2.435 dm³

∴  Change in volume = V₁ – V₂ = 2.5 dm³ – 2.435 dm³ = 0.065 dm³

Hence the change in volume of the gas is 0.065 dm³.

Example – 03:

A balloon is inflated with helium gas at room temperature of 25 ^oC and at 1 bar pressure when its initial volume is 2.27 L and allowed to rise in the air. As it rises the external pressure decreases and volume of the gas increases till finally, it bursts when external pressure is 0.3 bar. What is the limit to which volume of the balloon can be inflated?

Given: Initial volume = V₁ = 2.27 L, Initial pressure = P₁ = 1 bar, Final pressure P₂ = 0.3 bar, Temperature constant

To Find: Final volume = V₂ =?

Solution:

At constant temperature by Boyle’s law

P₁V₁ = P₂V₂

∴ V₂ = P₁V₁ /P₂

∴  V₂ = 1 bar × 2.27 L/ 0.3 bar

∴ V₂ = 7.567 L

Thus balloon can be inflated to the maximum volume of 7.567 L.

Example – 04:

The volume of given mass of a gas is 0.6 dm³ at a pressure of 101.325 kPa. Calculate the volume of the gas if its pressure is ballooned to 142.860 kPa at the same temperature.

Given: Initial volume = V₁ = 0.6 dm³, Initial pressure = P₁ = 101.325 kPa, Final pressure P₂ = 142.860 kPa, Temperature constant

To Find: Final volume = V₂ =?

Solution:

At constant temperature by Boyle’s law

P₁V₁ = P₂V₂

∴ V₂ = P₁V₁ /P₂

∴  V₂ = 101.325 kPa × 0.6 dm³ / 142.860 kPa

∴ V₂ = 0.426 dm³

Thus final volume of the gas is 0.426 dm³.

Example – 05:

In a J tube partially filled with mercury, the volume of the air column is 4.2 mL and the mercury level in the two limbs is the same. Some mercury is now added to the tube so that the volume of air enclosed in the shorter limb is now 2.8 mL. What is the difference in the level of mercury in this case? Atmospheric pressure is 1 bar.

Given: Initial volume = V₁ = 4.2 mL, Initial pressure = P₁ = 1 bar, Final volume V₂ = 2.8 mL Temperature constant

To Find: Difference in mercury levels =?

Solution:

At constant temperature by Boyle’s law

P₁V₁ = P₂V₂

∴ P₂ = P₁V₁ /V₂

∴  P₂ = 1 bar × 4.2 mL / 2.8 mL

∴ P₂ = 1.5 bar

Difference in pressure = P2 – P1 = 1.5 bar – 1 bar = 0.5 bar

Now 1 bar corresponds to 750.12 mm of mercury

Hence 0.5 bar corresponds to 750.12 x 0.5 =375.06 mm of mercury

Hence the difference in mercury levels is 375.06 mm or 37.51 cm

Example – 06:

A thin glass bulb of 100 mL capacity is evacuated and kept in 2.0 L container at 27 °C and 800 mm pressure. If the bulb implodes isothermally, calculate the new pressure in the container in kPa.

Given: Initial Volume = 2000 mL – 100 mL = 1900 mL

To Find: Final pressure =?

Solution:

At constant temperature by Boyle’s law

P₁V₁ = P₂V₂

∴ P₂ = P₁V₁ /V₂

∴  P₂ = 800 mm × 1900 L / 2000 mL

∴  P₂ = 76o mm = 760 mm/760 mm = 1 atm = 101.325 kPa

Hence the new pressure is 101.325 kPa

Example – 07:

Certain bulb A containing gas at 1.5 bar pressure was put into communication with an evacuated vessel of 1.0 dm³ capacity through the stop cock. The final pressure of the system dropped to 920 mbar, at the same temperature. What is the volume of container A.

Given: Initial pressure P1 = 1.5 bar, Final Pressure = 920 mbar = 0.920 bar. Let V dm³ be the volume of the container A. Initial Volume = V1 = V dm³, Final Volume = (1.0 + V) dm³

To Find: Volume of container A = V =?

Solution:

At constant temperature by Boyle’s law

P₁V₁ = P₂V₂

∴ 1.5 bar × V dm³ = 0.920 bar × (100 – V) dm³

∴ 1.5 V = 92  – 0.920V

∴ 1.5 V + 0.920V = 92

∴ 2.42 V = 92

∴ V = 92 / 2.42 = 39.02

Hence the volume of container A is 38.02 dm³.

Example – 08:

What will be the minimum pressure required to compress 500 dm³ of air at 1 bar to 200 dm³ at 30 °C

Given: Initial volume = V₁ = 500 dm³, Initial pressure = P₁ = 1 bar, Final volume V₂ = 200 dm³ Temperature constant

To Find: Final Pressure = P₂ =?

At constant temperature by Boyle’s law

P₁V₁ = P₂V₂

∴ P₂ = P₁V₁ /V₂

∴ P₂ = 1 bar × 500 dm³ / 200 dm³

∴ P₂ = 2.5 bar

Hence minimum pressure required = 2.5 bar

Example – 09:

A vessel of 120 mL capacity contains a certain amount of gas at 35 °C and 1.2 bar pressure. The gas is transferred to another vessel of volume 180 mL at 35 °C. What would be the pressure?

Given: Initial volume = V₁ = 120 mL, Initial pressure = P₁ = 1.2 bar, Final volume V₂ = 180 mL, Temperature constant

To Find: Final Pressure = P₂ =?

At constant temperature by Boyle’s law

P₁V₁ = P₂V₂

∴ P₂ = P₁V₁ /V₂

∴ P₂ = 1.2 bar × 120 dm³ / 180 dm³

∴ P₂ = 0.8 bar

Hence minimum pressure required = 0.8 bar

Science > Chemistry > States of Matter > Boyle’s Law

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In this article, we shall study the general characteristics of the gaseous state and the measurable properties of gases.

General Characteristics of Gaseous State:

• A gas has neither a definite shape nor a definite volume. They acquire the volume and shape of the container in which they are kept.
• A gas is capable of expanding to any limit and is capable of occupying whole available space.
• Gas is highly compressible. As the pressure on the gas is increased its volume decreases.
• Gases have comparatively less density w.r.t. solids and liquids.
• Gases have two specific heats viz. specific heat at constant pressure and specific heat at constant volume.
• In the gaseous state, the intermolecular forces of attraction are very weak i.e. almost zero.
• The molecules of a gas are in continuous random motion.
• Gases have the capacity to diffuse with each other irrespective of the difference in their densities.
• Gases have low viscosity.
• A gas exerts pressure on the walls of the container in which it is kept.
• All the gases obey certain laws known as gas laws. These relat5ions or laws are based on experimental results.

Note: Eleven out of all known elements exist in the gaseous state under normal atmospheric conditions of temperature (25° C) and pressure (1 bar) are as shown below.

Measurable Properties of a Gases:

The measurable properties used to describe the physical state of a gas are (a) mass, (b) volume (c) pressure and (d) temperature.

Mass:

It is given directly or in terms of moles of gas. It is measured in grams or kilograms. Generally, the mass of a gas is expressed in terms of moles.

Number of moles of a gas = Given mass of the gas/Molecular mass of the gas = m/M

Molecular masses of some gases are hydrogen (2), oxygen (32), nitrogen (28), carbon dioxide (44), ammonia (17), methane (16), and chlorine (71)

Measurement of Mass of a Gas:

The mass of the container with enclosed gas is measured. Then the container is completely emptied and the mass of the empty container is measured. The difference between the two masses gives the mass of the gas in the container.

Conversions:

Volume:

It means space occupied by the gas. It is measured in cubic centimeters, millilitres (mL), litres (L), dm³, m³. In the case of gas, the volume of the gas is equal to the volume of the container containing it.

Measurement of Volume of a gas:

The gas acquires volume and shape of the container in which they are kept. Hence the volume of the container is taken as the volume of the gas.

Conversions:

Temperature:

The temperature of a gas is a measure of the quantity of energy possessed by the gas molecules.  It is measured in °C (centigrade or celsius) or K (Kelvin).

Measurement of Temperature of a gas:

The temperature may be defined as the degree of hotness. It is measured by a device called thermometer. The common thermometer is a mercury thermometer.

Various Temperature Scales:

Celsius Scale (° C):

In this scale, the melting point of ice at one-atmosphere pressure and at mean sea level is taken as the lower reference point and consider as 0° C. While boiling point of water at one-atmosphere pressure and at mean sea level is taken as an upper reference point and consider as 100° C. The range between the two reference points is divided into 100 equal parts and each part is called 1° C (one-degree celsius). This scale is also called a centigrade scale.

A lower limit 0° C is considered arbitrary, this scale can be extended to indicate negative temperatures also. The temperature below -273.15° C is not possible.

Farenheit Scale (° F):

In this scale, the melting point of ice at one-atmosphere pressure and at mean sea level is taken as the lower reference point and consider as 32° F. While boiling point of water at one-atmosphere pressure and at mean sea level is taken as the upper reference point and consider as 212° F. The range between the two reference points is divided into 180 equal parts and each part is called 1° F (one-degree farenheit). Nowadays, this scale is not in use.

Kelvin Scale (K):

In this scale, the lowest possible temperature -273.15° C  is taken as a lower reference point. This temperature is called absolute zero. The division of 1 K is equal to 1° C. The unit of temperature in the kelvin scale is K (kelvin) and is considered as the fundamental unit in S.I. system of units.

Conversion of Temperature in Different Scales:

Celsius scale to Kelvin scale  ° C  +  273 = K

Kelvin scale to celsius scale  K  –  273 = ° C

Pressure:

It means the total force exerted by the gas molecules per unit area of the container walls due to their collision on the same walls.  It is measured In terms of the height of the mercury column in centimetres or milimetres or Nm^-2 or Pa (pascal).

The gas molecules are in random motion. During random motion, they collide with each other and with the walls of the container. During the collision with walls of the container, they exert outward force on the walls of the container. The outward force per unit area of the walls is called the pressure of the gas.

The S.I. unit of pressure is Nm^-2 (newton per square metre). It is called Pa (pascal). Other units of pressure used are atm (atmosphere), bar, and in terms of the height of the mercury column.

Atmospheric Pressure:

A thick blanket of air around the earth is called atmosphere. Molecules of various gases present in the atmosphere are under constant pull of gravitational force of the earth. Thus the weight of air column exerts pressure on the surface of the earth. The force experienced by any area of the earth exposed to the atmosphere is equal to the height of the column of air above it. This force per unit area of the earth is called the atmospheric pressure. The value of atmospheric pressure is not constant over the place. It varies with location, temperature and weather conditions. The atmospheric pressure is very large, but living beings are not getting crushed under it because the pressure inside the body of living beings is equal to that of atmospheric pressure.

Atmospheric pressure is measured by a simple device called barometer. It consists of a glass tube of about 1 m long, closed at one end filled with mercury and inverted in an open vessel. The level of mercury adjusts itself in the tube to balance the atmospheric pressure. At sea level, the height of the mercury column is approximately 76 cm above the mercury level in the open vessel.

A standard atmospheric pressure (1 atm) is the pressure exerted by exactly 76 cm of mercury column at 0° C (273.15 K) measured at sea level where standard gravity is 9.806 ms^-2, with the density of mercury being 13.596 g cm^-3. mm of Hg unit is also called torr. The empty space (vacuum) above the mercury column in the tube is called Torricelli’s space.

Measurement of Pressure of a Gas:

The pressure of a gas is measured using a simple apparatus called mercury manometer or pre-calibrated pressure gauges. Open end manometers are suited for measuring pressure equal to or greater than the atmospheric pressure. While closed end manometer are suited for measure pressure below the atmospheric pressure. In closed end manometer, the difference in the levels of mercury in the two limbs gives the pressure of the gas.

In open end manometer, the difference in the levels of mercury in the two limbs gives gauge pressure of the gas.

There are three possibilities in the measurement

• Levels of Hg is same in both the limbs

Gas Pressure = P_atm

• Level of Hg in open limb is more than that connected to the gas container

Gas Pressure = P_atm + Gauge Pressure

• Level of Hg in open limb is lower than that connected to the gas container

Gas Pressure = P_atm – Gauge Pressure.

Conversions:

Numerical Problems:

Example – 01:

A manometer is connected to a gas containing bulb. The open arm reads 43.7 cm whereas the arm connected to the bulb reads 15.6 cm. If barometric pressure is 743 mm Hg. What is the pressure of the gas in the bulb in bar.

Solution:

Difference in mercury level of two arms = 43.7 cm – 15.6 cm = 28. 1 cm

Hence gauge pressure = 28. 1 cm of Hg = 281 mm of Hg

Absolute Pressure = Gauge pressure + Atmospheric pressure = 743 mm + 281 mm = 1024 mm

= 1024 mm/ 760 mm = 1.347 atm = 1.347 × 1.013 = 1.365 bar

Example – 02:

The side arm of an open-end mercury manometer is attached to a gaseous system. The level of mercury in the arm attached to the system is 125 mm lower than the open end arm. Is it higher than the atmospheric pressure or lower? What is the pressure of the system if the atmospheric pressure is 760 mm of Hg?

Solution:

The level of mercury attached to the system is lower than the level in the open arm. Hence pressure of the gas is more than the atmospheric pressure.

Gauge Pressure = 125 mm of Hg

Pressure of system = Gauge Pressure + Atmospheric Pressure  = 125 mm   + 760 mm = 885 mm of Hg

Example – 03:

Reading in mercury manometer closed end arm is 100 mm and in the arm attached to the system is 70 mm. What is the pressure of the system?

Solution:

System Pressure = Gauge Pressure = Difference in mercury level = 100 mm – 70 mm = 30 mm of Hg

Standard Temperature and Pressure (STP) and Normal Temperature and Pressure (NTP):

The volume of a given mass of a gas depends on its pressure and temperature. Hence we have to specify the pressure and temperature of the gas when specifying its volume. When solving problems on the gaseous state, the condition of STP and NTP means

 P = 1 atm = 1.013 × 10⁵ Pa, T = 273.15 K

Science > Chemistry > States of Matter > Gaseous State

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