Showing posts with label specific heat capacity. Show all posts
Showing posts with label specific heat capacity. Show all posts

Friday, November 10, 2017

Chapter 6.5 - Latent heat of Fusion

In the previous section we saw the principle of method of mixtures. In this section we will see change of state.

• We know that there are three states of matter: Solid, Liquid and Gas. 

• The change from one state to another occurs by either one of the two:
    ♦ the absorption of heat 
    ♦ release of heat. 
• This can be shown in the form of flow charts:
    ♦ SOLID (absorbs heat)  LIQUID (absorbs heat) ⟶ GAS
    ♦ GAS (releases heat)  LIQUID (releases heat) ⟶ SOLID

■ How do a change in state occur when heat is either absorbed or released?
To find the answer, we will do an experiment:
1. Fill half a beaker with ice pieces. Insert a thermometer into it. Fix the thermometer in a stand in such a way that the thermometer does not touch the walls of the beaker. 
2. Record the initial temperature. 
3. Slowly heat the beaker in a water bath. At the same time start a stop watch. 
4. Record the readings in the thermometer every 30 seconds. Also record the changes taking place in the state of the ice pieces. The table 6.3 shown below can be conveniently used for this purpose.
Table 6.3
Time (s)
Temperature
Change in state of ice pieces
5. Using the temperatures draw a time – temperature graph. The graph should be drawn with time in the X axis and temperature in the Y axis. The following table shows the recordings made while conducting this experiment in a lab.

Time (s)
30 60 90 120 150 180 210 240 270 300
Temperature 0 0 0 0 30 60 90 120 150 180
Change in state of ice pieces Ice continues to melt No ice piece left
The graph based on the table is shown below:


1. The scale along X axis is: 1 unit = 30 seconds
The scale along Y axis is: 1 unit = 20 oC
2. The initial temperature (when time = 0 s) is 0 oC.   So the first point in the graph is (0,0)
• We can see that, from the first point itself,  the graph is a straight horizontal line upto 120 seconds
• That means., there is no rise in temperature upto 120 s
3. After 120 s, the temperature increases
• We have to see the details during the first 120 s. 
• At this time the ice is melting. But it takes 120 s for all the ice to melt. And during this melting process, the temperature does not rise. 
4. So where does the heat energy supplied from the water bath go?
Ans: During the 120 seconds, the applied heat energy is used up to break up the bonds between the molecules. 
• When the bonds are broken, the molecules become free to flow, and the 'solid ice' becomes 'liquid water'. 
• During the process of breaking up of bonds, all the heat energy is used up for that purpose. So there is no increase in kinetic energy. And hence no increase in temperature. 
• Thus we get a horizontal line from (0,0) to (120,0). 
5. At (120,0), all the ice have melted. The heat energy received from that point onwards will be used to increase the kinetic energy. So the temperature will rise after (120,0)

■ So 'melting point' is a 'constant temperature' at which a solid changes into it's liquid at normal atmospheric pressure. 
'Normal atmospheric pressure' is mentioned because, if the solid is not under such a pressure, the melting point will be a different temperature.

We can consider the reverse also:
1. If a liquid substance continues to release heat energy, it's temperature will continuously decrease. 
2. But at a certain temperature, it will stop decreasing. Even if it continues to release heat energy, the temperature will not decrease. 
3. This is because, the heat released during this time is the energy which kept the molecules apart. When that energy is lost, the molecules bind together to form a solid. 
■ The constant temperature at which the liquid changes into it's solid form is called freezing point. 
• We can represent the two points as follows:
    ♦ Melting point  SOLID (absorbs heat)  LIQUID
    ♦ Freezing point  LIQUID (releases heat) ⟶ SOLID 
For most substances, melting point and freezing point is the same temperature

• It may be noted that, the time 120 s is not constant. 
    ♦ If we take a larger quantity of ice, it may take more than 120 s for all the ice to become water
    ♦ If we take a smaller quantity of ice, it may take less than 120 s for all the ice to become water
• Also, if we supply a larger quantity of heat, within a short span of time, by say using a larger burner, all the ice will become water in a short span of time.
• So the 'time required to break all the bonds' is not constant. 
• But the 'quantity of energy required by 1 kg' of the substance to break all the bonds will be a constant. This quantity is called the Latent heat of fusion. ('fusion' is another term for 'melting'). So we can write the definition:
Latent heat of fusion (Lf) of a solid is the quantity of heat absorbed by 1 kg of that solid to change into it's liquid state at it's melting point, without change in temperature 
• Since it is the energy per 1 kg, it's unit is Jkg. That is., J kg-1.
The following table 6.4 shows the Lf values of some common substances
Table 6.4
Substance Melting point (oC) Lf (J kg-1)
Ice 0 335 × 103
Silver 962 88 × 103
Copper 1083 180 × 103
Let us analyse the values in the above table:
A. Ice:
1. Consider some ice kept in a vessel. Let it's temperature be -10 oC. 
2. Let this ice be heated. Once we begin heating, the temperature will begin to rise. 
• That is., it will become -9, -8, -7, . . . so on. The graph indicating this rise in temperature will be a rising line.  
    ♦ During this rise in temperature, the ice do not melt 
3. But once it reaches 0 oC, the temperature will not rise. 
• Also, the ice do not completely melt just when it becomes 0 oC
• The heat supplied just after reaching 0 oC, will be used to break the strong bonds between the water molecules in the ice. 
• Each 1 kg of ice in that vessel will require 335×103 joules of heat energy to break all the bonds in it. 
4. If we supply the required energy with in a short span of time, like by using a large burner, then the bonds will break within that short span of time. We will find that the ice began to melt sooner. 
• For our present discussion, the time in which 335×10J kg-1 is supplied is not important. 
• What is important is that, 335×10J kg-1 is required to break all the bonds. 
5. While this energy is being absorbed, the ice begins to melt. 
• But the temperature of the newly formed water will remain at 0 oC
• This is because, all the energy being received is used up for breaking more and more bonds. There is no energy available to increase the kinetic energy of the newly formed water. 
• So the temperature do not rise above 0 oC during this process. The graph indicating this constant temperature will be a horizontal line. 
• When all the bonds are broken, we will get 'all water' (at 0 oC) and 'no ice'. 
6. Further energy supply will be used to increase the temperature from 0 oC up wards. So the graph will again be a rising line.

B. Silver:
1. Consider some silver kept at room temperature say 30 oC. 
2. Let this silver be heated. Once we begin heating, the temperature will begin to rise. 
• That is., it will become 31, 32, 33, . . . so on. The graph indicating this rise in temperature will be a rising line. 
    ♦ During this rise in temperature, the silver do not melt 
3. But once it reaches 962 oC, the temperature will not rise. 
• Also, the silver do not completely melt just when it becomes 962. 
• The heat supplied just after reaching 962 oC, will be used to break the strong bonds between the molecules in the silver
• Each 1 kg of solid silver will require 88×103 joules of heat energy to break all the bonds it it. 
4. If we supply the required energy with in a short span of time, like by using a large burner, then the bonds will break within that short span of time. We will find that the silver began to melt sooner. 
• For our present discussion, the time in which 88×10J kg-1 is supplied is not important. 
• What is important is that, 88×10J kg-1 is required to break all the bonds. 
5. While this energy is being absorbed, the silver begins to melt. 
• But the temperature of the newly formed liquid silver will remain at 962 oC
• This is because, all the energy being received is used up for breaking more and more bonds. There is no energy available to increase the kinetic energy of the newly formed liquid silver. 
• So the temperature do not rise above 962 oC during this process. The graph indicating this constant temperature will be a horizontal line. 
• When all the bonds are broken, we will get 'all liquid silver' (at 962 oC) and 'no solid silver'. 
6. Further energy supply will be used to increase the temperature from 962 oC up wards. So the graph will again be a rising line

C. Copper:
The reader may write the steps for copper in the same way


Now we can explain some common phenomenon that we see around us:
1. Large glaciers do not melt all of a sudden:
• Glaciers are large masses of ice. 
• During winter seasons, the temperature of the surroundings will most probably be below zero. So there is no chance for them to melt. 
• But when summer approaches, the temperature may become zero or above. Then the ice should melt. 
• But the glaciers do not melt all of a sudden. This is because, latent heat of fusion of ice is large even for 1 kg. 
• So very large heat will be required for huge masses of ice. 
• But the phenomenon of Global warming is supplying this required quantity at an alarming rate.

2. It feels much colder when an ice piece at 0 oC is placed in the mouth than when drinking water which is at 0 oC:
• When we place ice in our mouth we feel cold because heat flows from the mouth into the ice. The mouth loses heat and we feel cold
    ♦ When we place cold water also, the same thing happens: Heat flows from the mouth into the water. The mouth loses heat and we feel cold
• But the ice takes up more heat from the mouth. This is because, the ice first has to become water at 0 oC, by taking up the latent heat of fusion. Once it becomes water at 0 oC, it takes additional heat to increase it's temperature from 0 oC upwards.
• So in the case of ice, there is an additional latent heat, being taken from the mouth. So we feel much colder

Solved example 6.8
(a) A 1.5 kg sample of copper is at 1083 oC and is continuously heated to melt it into it's liquid state. How much heat will be required to make the sample completely melt into liquid copper at 1083 oC?
(b) A 1.0 kg sample of ice is at 0 oC and is continuously heated to melt it into it's liquid state. How much heat will be required to make the sample completely melt into water at 0 oC?
Solution:
(a) • The melting point of copper is 1083 oCThe given sample is at this temperature. 
• If we give more heat at this point, the temperature will not increase. That heat will be used to break the bonds between the molecules. When all the bonds are broken we will get liquid copper at 1083 oC
• We are asked to find the heat energy to be supplied between the following two points:
    ♦ Point A at which the temperature of 1.5 kg of the solid copper is 1083 oC
    ♦ Point B at which all the solid is melted into 1.5 kg of liquid copper which is at 1083 oC
• Beyond point B, the heat energy will be used to increase the temperature of the liquid. We need the energy between A and B only
• We can use the following steps:
1. Energy required to melt 1 kg of solid copper at 1083 oC to 1 kg of liquid copper at 1083 oC = Lf of copper = 180 × 10J kg-1 
2. So Energy required for 1.5 kg = 1.5 × 180 × 10= 270 × 10J

(b) • The melting point of ice is 0 oCThe given sample is at this temperature. 
• If we give more heat at this point, the temperature will not increase. That heat will be used to break the bonds between the molecules. When all the bonds are broken we will get liquid water at 0 oC
• We are asked to find the heat energy to be supplied between the following two points:
    ♦ Point A at which the temperature of 1.0 kg of the ice is 0 oC
    ♦ Point B at which all the ice is melted into 1.0 kg of water which is at 0 oC
• Beyond point B, the heat energy will be used to increase the temperature of the water. We need the energy between A and B only
• We can use the following steps:
1. Energy required to melt 1 kg of ice at 0 oC to 1 kg of water at 0 oC = Lf of ice = 335 × 10J kg-1 
• This is the required value because, the given sample is also of 1 kg.
■ We can see that, though the given ice has less mass than the given copper, that ice requires more energy

Solved example 6.9
Calculate the quantity of heat required to convert 5 kg of ice at 0 oC into water at the same temperature
Solution:
The melting point of ice is 0 oCThe given sample is at this temperature. 
• If we give more heat at this point, the temperature will not increase. That heat will be used to break the bonds between the molecules. When all the bonds are broken we will get liquid water at 0 oC
• We are asked to find the heat energy to be supplied between the following two points:
    ♦ Point A at which the temperature of 5.0 kg of the ice is 0 oC
    ♦ Point B at which all the ice is melted into 5.0 kg of water which is at 0 oC
• Beyond point B, the heat energy will be used to increase the temperature of the water. We need the energy between A and B only
• We can use the following steps:
1. Energy required to melt 1 kg of ice at 0 oC to 1 kg of water at 0 oC = Lf of ice = 335 × 10J kg-1 
2. So Energy required for 5 kg = 5 × 335 × 10= 1675 × 10J

Solved example 6.10
A solid is at an initial temperature of 0 oC. It is continuously heated. The graph showing the change in temperature according to the heat energy absorbed is given below:

Based on the graph, calculate the following:
(a) Mass of the solid
(b) Latent heat of fusion (Lf) of the substance
Given: Specific heat capacity of the substance = 500 J kg-1 K-1
Solution:
Part (a):
1. Let 'm' be the mass of the solid
2. Consider the first sloping line in the graph. The end point of this sloping line is (1000, 80). From this, we get two information:
• The total energy absorbed by the substance upto that point is 1000 J
• This 1000 J causes an increase in temperature from 0 oC to 80 oC
So we can write:
• Q = 1000 J
• rise in temperature (θ) = (θ2 - θ1) = (80 - 0) = 80
3. We have: Q = mcθ.
substituting the known values, we get:
1000 = m×500×80 1000 = m×40000 ⟹ m = 0.025 kg
Part (b):
1. From the graph we can see that, the end points of the horizontal line are: (1000,80) and (2000,80). From this we get two information:
• When the temperature becomes 80 oC, it becomes constant. That means, it has reached the melting point. 
• It continues to melt at the constant temperature of 80 oC until it's whole mass becomes liquid.
• The total energy absorbed until the beginning of the melting process is 1000 J 
• The total energy absorbed until the end of the melting process is 2000 J 
• So the total energy absorbed during the melting process is (2000 - 1000) = 1000 J 
• Once it completely becomes liquid, the temperature will begin to rise again
2. So 0.025 kg of that substance requires 1000 J to completely melt into liquid state
• So energy required by 1 kg = 10000.025  = 40000 J
3. The energy required by 1 kg is the latent heat of fusion. So we can write:
• Lof the substance = 40000 J kg-1

In the next section, we will see the Latent heat of Vaporisation.

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Tuesday, November 7, 2017

Chapter 6.4 - Principle of method of mixtures

In the previous section we saw the details about the specific heat capacity. In this section we will see Principle of method of mixtures.

Let us do an experiment:
1. Take 0.2 kg of cold water in a beaker. Measure it's initial temperature . It is found to be 303 K. It is recorded in the table 6.2 below.
2. Take the same quantity (0.2 kg) of hot water in another beaker. Measure it's temperature. It is found to be 323 K. It is also recorded in the table 6.2 below.
3. Pour cold water into the hot water and stir. Measure the resultant temperature. It is found to be 313 K. It is also recorded in the table 6.2:
Table 6.2
Water
Initial temperature (θ1)
Resultant temperature (θ2)
Difference in temperature (θθ1)
Heat gained/Heat lost
Cold
303 K
313 K
10 K
8400 J
Hot
323 K
323 K
10 K
8400 J
Based on the recordings, we can do some calculations:
4. The 0.2 kg of water which was initially cold, is present in the resultant mixture. That mass of water has gained some heat. Let us calculate the heat energy that it has gained:
(i) We have : Q = mcθ.
(ii) θ = (θθ1) = (313 - 303) = 10 K 
(iii) Substituting the known values we get: Q = 0.2×4200×10 = 8400 J
5. The 0.2 kg of water which was hot, is present in the resultant mixture. That mass of water has lost some heat. Let us calculate the heat energy that it has lost:
(i) We have : Q = mcθ.
(ii) θ = (θθ1) = (313 - 323) = -10 K
• The negative sign indicates that, heat energy is given out 
(iii) Substituting the known values we get: Q = 0.2×4200×-10 = -8400 J
6. With the calculated values, we can fill up the table. The completed table is shown below:
Water Initial temperature (θ1) Resultant temperature (θ2) Difference in temperature (θθ1) Heat gained/Heat lost
Cold 303 K 313 K 10 K 8400 J
Hot 323 K 323 K 10 K 8400 J
■ From the table, we can see that:
Heat energy lost = heat energy gained
■ When a hot body is in contact with a cold body, heat flows from the hot body to the cold body, till both the bodies attain the same temperature. The heat lost by the hot body = heat gained by the cold body. This is the principle of method of mixtures

Solved example 6.8
4 kg of hot water at 343 K is added to 6 kg of water at 293 K. The resultant temperature is 313 K. Calculate the heat lost by the hot water and the heat gained by the cold water. Assume that there is no heat loss to the surroundings
Solution:
1. 4 kg of hot water:
(i) We have : Q = mcθ.
(ii) θ = (θθ1) = (313 - 343) = -30 K
• The negative sign indicates that, heat energy is given out 
(iii) Substituting the known values we get: Q = 4×4200×-30 = -504000 J
2. 6 kg of water:
(i) We have : Q = mcθ.
(ii) θ = (θθ1) = (313 - 293) = 20 K 

(iii) Substituting the known values we get: Q = 6×4200×20 = 504000 J
3. So we can write:
Heat energy lost by the hot water = heat energy gained by the cold water

Solved example 6.9
In a bucket, there is 8 kg of water at 298 K. To this, 2 kg of water at 353 K is added. Calculate the resultant temperature assuming that the bucket and the surroundings do not receive any heat.
Solution:
1. 8 kg of water:
(i) We have : Q = mcθ.
(ii) θ = (θθ1) = (θ2 - 298)
• θis the resultant temperature. It is the unknown quantity. 
(iii) Substituting the known values we get: Q = 8×4200×(θ2 - 298)
2. 2 kg of water:
(i) We have : Q = mcθ.
(ii) θ = (θθ2) = (353 - θ2)
• θis subtracted from 353 because we know that the 2 kg water will lose heat, and so θwill be lesser than 353
(iii) Substituting the known values we get: Q = 2×4200×(353-θ2)
3. Heat energy lost by the hot water = heat energy gained by the cold water
So we can write:
8×4200×(θ2 - 298) = 2×4200×(353- θ2)
⟹ 8×(θ2 - 298) = 2×(353- θ2⟹ 4×(θ2 - 298) = (353- θ2)  
⟹ 4×θ2 - 4×298 = 353- θ⟹ × θ2  = 1192 +353 = 1545 ⟹ θ15455 = 309 K

Solved example 6.10
How much water at 370 K is required to raise the temperature of 5 kg water at 300 K to 350 K 
Solution:
• 5 kg water at 300 K is placed in a vessel
 To that, 'm' kg water at 370 K is to be added.
• The resultant temperature must be 350 K. So θ= 350 K
 We have to find 'm'   
1. 5 kg of water:
(i) We have : Q = mcθ.
(ii) θ = (θθ1) = (350 - 300) = 50  
(iii) Substituting the known values we get: Q = 5×4200×50
2. 'm' kg of water:
(i) We have : Q = mcθ.
(ii) θ = (θθ1) = (370 - 350) = 20  

(iii) Substituting the known values we get: Q = m×4200×20
3. Heat energy lost by the hot water = heat energy gained by the cold water

So we can write:
5×4200×50 = m×4200×20 
⟹ 250 = 20m ⟹ m = 25020  = 12.5 kg

In the next section, we will see Change of state.

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Monday, November 6, 2017

Chapter 6.3 - Specific heat capacity

In the previous section we saw the details about the Kelvin scale to measure temperatures. In this section we will see Specific heat capacity.

Some experiments related to heat was conducted on various substances like Coconut oil, Copper, Lead etc., The observations can be written as follows:

Experiment 1:
• 10 kg of coconut oil was taken. 
• It's initial temperature in K was noted down. 
• Then it was heated until the temperature increased by 20 K. (For example, if the initial temperature was 301 K, the heating was stopped when the temperature became 321 K) 
• The amount of heat energy required to bring about this increase in temperature was found to be 420000 joules
Experiment 2:
• 10 kg of copper was taken. 
• It's initial temperature in K was noted down. 
• Then it was heated until the temperature increased by 20 K.
• The amount of heat energy required to bring about this increase in temperature was found to be 77000 joules
Experiment 3:
• 10 kg of water was taken. 
• It's initial temperature in K was noted down. 
• Then it was heated until the temperature increased by 20 K.
• The amount of heat energy required to bring about this increase in temperature was found to be 837200 joules
Experiment 4:
• 10 kg of lead was taken. 
• It's initial temperature in K was noted down. 
• Then it was heated until the temperature increased by 20 K.
• The amount of heat energy required to bring about this increase in temperature was found to be 24000 joules

Now we can do some calculations:
CALCULATION A:
In experiment 1:
1. The heat energy required to bring about a rise of 20 K is 420000 J
2. So the heat energy required to bring about a rise of 1 K = 42000020 = 210000 J
In experiment 2:
1. The heat energy required to bring about a rise of 20 K is 77000 J
2. So the heat energy required to bring about a rise of 1 K = 7700020 = 3850 J
In experiment 3:
1. The heat energy required to bring about a rise of 20 K is 1260000 J
2. So the heat energy required to bring about a rise of 1 K = 83720020 = 41860 J
In experiment 4:
1. The heat energy required to bring about a rise of 20 K is 24000 J
2. So the heat energy required to bring about a rise of 1 K = 2400020 = 1200 J

So we can write:
• A sample of 10 kg coconut oil will require a heat energy of 210000 for increasing it's temperature by 1 K
• A sample of 10 kg copper  will require a heat energy of 3850 J for increasing it's temperature by 1 K
• A sample of 10 kg water will require a heat energy of 63000 J for increasing it's temperature by 1 K
• A sample of 10 kg lead will require a heat energy of 1200 J for increasing it's temperature by 1 K

■ The heat energy required to raise the temperature of a sample of a substance by 1 K is called the heat capacity of that sample. It's unit is J/K or J K -1
• So we can write: 
• Heat capacity of a sample of 10 Kg of coconut oil is 210000 J K -1
• Heat capacity of a sample of 10 Kg of copper is 3850 J K -1
• Heat capacity of a sample of 10 Kg of water is 41860 J K -1
• Heat capacity of a sample of 10 Kg of lead is 1200 J K -1


Note the use of the word 'sample' in the above steps. A sample can have any mass: 10 kg, 12 kg, 12.5 kg . . . So, to standardise, we will take unit mass. That is., 1 kg.
CALCULATION B:
1. We have: Heat capacity of a sample of 10 Kg of coconut oil is 210000 J K -1 
• So heat capacity of 1 kg of coconut oil = 21000010 = 21000 J 
2. We have: Heat capacity of a sample of 10 Kg of copper is 3850 J K -1 
• So heat capacity of 1 kg of copper = 385010 = 385 J 
3. We have: Heat capacity of a sample of 10 Kg of water is 63000 J K -1 
• So heat capacity of 1 kg of water = 4186010 = 4186 J 
4. We have: Heat capacity of a sample of 10 Kg of lead is 1200 J K -1 
• So heat capacity of 1 kg of lead = 120010 = 120 J

■ The heat capacity of 1 kg of a substance is called the Specific heat capacity of that substance
In the above calculations, we calculated the specific heat capacity of some common substances: Coconut oil, copper, water and lead. We can now write the general procedure to find the specific heat capacity of any given substance.
1. Take a sample of the given substance. Let the mass of the sample be 'm' kg
2. Note down the initial temperature θ1 in K
3. Heat the sample for some time. Note down the final temperature. Let this be θ2.
• Then the rise in temperature = (θθ1). Let this be 'θ' K
4. Note down the heat energy required to bring about the rise in temperature of 'θ' K. Let this energy be 'Q' joules 
5. Then we get: 
• Heat capacity of the sample 
The heat energy required to raise the temperature of a sample of a substance by 1 K 
Qθ
• Specific heat capacity of the substance in the sample 
The heat capacity of 1 kg of a substance 
Qθ×m
6. The 'specific heat capacity' is denoted by the symbol 'c'. So we can write:
Eq.6.6:
c = Qθ×m  .
7. Now we must write the units of 'c':
• In Eq.6.6 above, we have:
    ♦ Energy (whose unit is joules) in the numerator
    ♦ Product of temperature (whose unit is K) and mass (whose unit is kg) in the denominator
• So the unit of 'c' is: JK×kg = J kg-1 K-1. (joules per kilo grams per kelvin)
■ So we can write the definition for Specific heat capacity:
Specific heat capacity of a substance is the heat energy required to raise the temperature of 1 kg of that substance through 1 K

Specific heat capacity (c) is a constant for a substance. That is., every substance has it's own unique value for 'c'. The following table 6.1 shows the c values of some common substances:
Table 6.1
Substance Specific heat capacity (J kg-1 K-1)
Water 4186
Ice 2130
Steam 460
Sea water 3900
Glass 500
Iron 460
Copper 385
Silver 234
Lead 120
From the table, we can see that water has a high specific heat capacity than others It's value is 4186 J kg-1 K-1. For use in numerical problems, it is assumed as 4200 J kg-1 K-1.

• The high specific heat capacity of water implies that, lot of heat energy is required to make 'even small increases' in the temperature of water.  
• Now we will see some situations in our day to day life, where this high 'c' value of water have much significance:
1. Water in the rivers and ponds do not get heated even if the temperature of the surrounding environment increases on a hot sunny day. This makes aquatic life possible
2. Body of plants and animals are about 80% water. So the body temperature do not increase rapidly even if the temperature of the surrounding environment increases on a hot sunny day.
3. In motor vehicles, large quantities of heat are produced by the engines continuously. This heat is transmitted to water which is used as a coolant. Because of the high 'c' value, water can absorb large quantities of heat with out itself getting much hot.
4. We know that large quantities of heat are absorbed by water (for a small increase in temperature) when it is heated by an external source
• The reverse happens when it is cooled. That is., even for a small decrease in temperature, large quantities of heat will have to be released. 
• If there is no external cooling device, this fall in temperature will happen only slowly. 
• So water, once heated, will remain hot for a long time. This property makes it useful in 'hot water bags', which are used in the treatments of some illness.
5. Land breeze and Sea breeze
• The 'c' value of sand is only 1/5 of water. So it is easier to heat up the land. 
• During day time, the land quickly gets hotter than sea. So the air above land will be hotter than the air above sea. 
• The hot air will rise up creating a void space near the surface of the land. The cold air above sea will then blows towards this void. This is sea breeze.
• During night, the reverse happens. The land will quickly become cold. 
• But  sea will become cold only slowly. So the air above sea will be hotter than the air above land.
• The hot air will rise up creating a void space near the surface of the sea. The cold air above land will then blows towards this void. This is land breeze.


Now we will see a practical application of specific heat capacity
1. Consider a sample of a substance. 
2. Let the specific heat capacity of the substance be 'c'
• Then the heat energy required to raise the temperature of 1 kg of that substance through 1 K = c joules 
3. Let the mass of the sample be m kg
• Then the heat energy required to raise the temperature of that whole sample through 1 K = mc joules 
• Then the heat energy required to raise the temperature of that whole sample through θ K = mcθ joules
■ So we can write:
If Q is the total heat energy required to raise the temperature of 'm' kg of a substance (whose specific heat capacity is 'c') through theta K, Then
Eq.6.7
Q = mcθ joules

Let us see some solved examples:
Solved example 6.4
(a) c of copper is 385 kg-1 K-1. How much heat energy is required to raise the temperature of 1 kg of copper by 10 K
(b) c of iron is 460 kg-1 K-1. How much heat energy is required to raise the temperature of 1 kg of copper by 20 K
(c) c of water is 4200 kg-1 K-1. How much in K will the temperature of 2 kg water rise, if it receives 42000 J of heat energy

(d) When 1 kg of lead received 1200 J of heat energy, it's temperature was raised by 10 K. What is the 'c' of lead?
Solution:
Part (a):
1. We have : Q = mcθ
2. Substituting the known values we get: Q = 1×385×10 = 3850 J
Part (b):
1. We have : Q = mcθ
2. Substituting the known values we get: Q = 1×460×20 = 9200 J
Part (c):
1. We have : Q = mcθ
2. Substituting the known values we get: 42000 = 2×4200×θ  10 = 2×θ  θ = 5 K
Part (d):
1. We have : Q = mcθ
2. Substituting the known values we get: 1200 = 1×c×10  1200 = 10c  c = 120 kg-1 K-1

Solved example 6.5
Calculate the quantity of heat required to raise the temperature of 5 kg of iron from 303 K to 343 K. Specific heat capacity of iron is 460 kg-1 K-1
Solution:
1. We have : Q = mcθ.
2. θ = (θθ1) = (343 - 303) = 40 K 
3. Substituting the known values we get: Q = 5×460×40 = 92000 J

Solved example 6.6

The temperature of 0.5 kg of water is 303 K. It is cooled to 278 K by keeping it in a refrigerator. What is the time taken by the water to reach 278 K, if 87.5 J of heat is given out in each second? Specific heat capacity of water is 4200.
Solution:
1. We have : Q = mcθ.
2. θ = (θθ1) = (278 - 303) = -25 K
• The negative sign indicates that, heat energy is given out 
3. Substituting the known values we get: Q = 0.5×4200×-25 = -52500 J
4. Energy given out per second = -87.5 J
5. So time taken = -52500-87.5 = 600 seconds = 10 minutes

Solved example 6.7

Heat required to increase the temperature of 10 kg of water by 1 K is 42000 J. Then how much heat will be required to increase the temperature of 1 kg of water by 1 K?
Solution:
1. We have : Q = mcθ.
2. Substituting the known values we get: 42000 = 10×c×1  42000 = 10c  c = 4200 kg-1 K-1
3. In part 2, we have: m = 1 kg, c = 4200 kg-1 K-1 (calculated in (2) above), θ= 1 K
4. Substituting in (1) we get: Q = 1×4200×1 = 4200 J

In the next section, we will see the Principle of method of mixtures.

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