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For a given value of  T,  the quantity of the heat absorbed also depends upon the mass
            m of the body. The greater is the mass, the greater the quantity of heat absorbed. For
            example,  if  we  heat  50  grams  of  water  through  10C,  and  100  grams  of  water  also
            through 10C, then the quantity of heat absorbed by 100 gms of water will be twice the
            quantity of heat absorbed by 50 gms of water.   In other words, the quantity of heat
            absorbed is directly  proportional to mass. Thus,  we have the relation:

                                                                        Q  = f(m)                                                       (1.31)

                  Combining two relations,  we get :

                                                           Q = f(T, m) or  Q = C m T,                                      (1.32)
                 where C is a constant,  which depends upon the material of the body.

                   C - called the specific heat of the body. If   m     1 kg ;  T   1 K , then   Q   C  by the
            equation  (1.32).
                  Thus  the  specific  heat  of  a  substance  is  the  amount  of  heat  required  to  change
            temperature of one unit quantity of substance through 1K.
                  Neither the heat capacity of a body nor the specific heat of a material is constant but
            depends on the location of the temperature interval.   At ordinary temperatures and over
            ordinary  temperature  intervals,  however,    specific  heats  can  be  considered  to  be

            constants.   For example, the specific heat of water varied less then   1% from its value
            of 4.19   kJoule  over the temperature range from 0C to 100C.   If we calculate specific
                      kg   K
            heat in some temperature interval we get average specific heat :


                                                        t 2  q x
                                                                    C xm    .                                                       (1.33)
                                                        t
                                                         1     t 

                      For the very small interval of the temperature we get true specific heat:

                                                        q     dqx
                                                            C  lim  x    .                                                    (1.34)
                                                x
                                                         T    dt

                 What we gained by this specific heat also depends on character of thermodynamic
            process. When a gas is heated at constant volume,  the quantity of heat required  to raise

            the temperature of unit mass of the gas through 1C is called its specific heat at constant
            volume,  and is denoted by C . When a gas is heated at constant pressure, the quantity of
                                             v
            heat required to raise the temperature of unit mass of the gas through 1°C is called its
            specific heat at constant pressure, and is denoted by C p.
                It can be shown that C p > C v. When a gas is heated at constant volume, no work is
            done by the gas against any external resistance. In this case, the heat supplied to the gas
            is used only in raising the temperature of the gas. But when we heat a gas at constant
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