Specific heat capacity
Take two beakers and name them as A
and B. Fill the two beakers with some water. Let us assume that the mass
of water in both the beakers be 1 kg.
Here “Q” represents heat and “t” represents temperature.
We repeat the same activity for the second time
But in this case we take different masses. And the same change in temperature.
So let us assume that water in beaker B is 1 kg and mass of water in beaker A is 2 kg. And let us assume that the temperature of water in both the beakers has to be raised to 500 centigrade each for a given constant time.
So in this case definitely more heat energy should be supplied to beaker B, as it has more mass when compared to water in Beaker A. Even though change in temperature is same.
So heat energy required is directly proportional to mass of the body to change its temperature.
From the above two proportions, we have
To convert proportion to
an equation we multiply with a constant say “S”
Therefore we get
From the above equation, we can also writeCGS unit of specific heat is cal / g 0c
SI unit of specific heat is J / kg-k (DIMENTIONAL FORMULA IS M0 L2 T-2 K-1 )
- Where M = Mass
- K = Temperature
- L = Length
- T = Time
The specific heat value varies from
body to body depending upon its nature.
i.e, these materials has more ability
to restrict the sudden changes in their temperatures.
They neither get heated up faster nor
cooled down faster.
Daily
life applications of specific heat
We have a lot of examples where we can observe the concept of specific heat in our daily life. The best example is sea breeze and land breeze.
1)
During daytime when
sun raises up, Land gets heated up fast when compared to seawater, as
water has a high specific heat value.
So as a result water remains cool even though land becomes hot.
So air present on the land will be warm(less density) when compared to the air present on the water (much density). So it forms high pressure area on sea water and low pressure area on land due to difference in the densities.
As a result The Gentle Wind blows from sea to the land. This is what we are calling as sea breeze.
And at the time of sunset the land gets cold faster when compared to the seawater.
So it forms high pressure area on the land and low pressure area on the seawater.
As a result a Gentle Wind blows from land to water. This is what we are calling as land breeze.
2) We can take watermelon as a best example to understand the concept of specific heat.
When a watermelon kept in a Refrigerator is
taken out, we can observe the difference in the coolness of the outer
peel of the watermelon and the pulp inside the watermelon because of difference
in their specific heat values
As the pulp of watermelon contains 90% of water, it has more specific heat when compared to the outer surface.
3) Also we use water as coolant to cool down the heated up engines of vehicles.
Like this we can observe number of
examples of specific heat in our daily life where we make use of this concept
but actually without knowing the reason.
Heat capacity or thermal capacity
Heat capacity can be defined as it is
the amount of heat energy required to raise the temperature of entire mass of a substance by
1 degree centigrade.
it is denoted with a symbol “H”.
And the formula is
CGS unit of thermal capacity is cal/0c
SI unit of thermal capacity is J/K
DIMENSIONAL FORMULA IS M L2T−2 K−1
Relation between the specific heat capacity and thermal capacity
We know, S=Q/m∆t and H=Q/∆t
From the above two equations we have
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