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Solution

  1. Use the equation for heat transfer Q = m c Δ T to express the heat lost by the aluminum pan in terms of the mass of the pan, the specific heat of aluminum, the initial temperature of the pan, and the final temperature:
    Q hot = m A1 c A1 ( T f 150 ° C ) .
  2. Express the heat gained by the water in terms of the mass of the water, the specific heat of water, the initial temperature of the water, and the final temperature:
    Q cold = m w c w ( T f 20.0 ° C ) .
  3. Note that Q hot < 0 and Q cold > 0 and that as stated above, they must sum to zero:
    Q cold + Q hot = 0 Q cold = Q hot m w c w ( T f 20.0 ° C ) = m A1 c A1 ( T f 150 ° C ) .
  4. This a linear equation for the unknown final temperature, T f . Solving for T f ,
    T f = m A1 c A1 ( 150 ° C ) + m w c w ( 20.0 ° C ) m A1 c A1 + m w c w ,

    and insert the numerical values:
    T f = ( 0.500 kg ) ( 900 J/kg ° C ) ( 150 ° C ) + ( 0.250 kg ) ( 4186 J/kg ° C ) ( 20.0 ° C ) ( 0.500 kg ) ( 900 J/kg ° C ) + ( 0.250 kg ) ( 4186 J/kg ° C ) = 59.1 ° C .

Significance

Why is the final temperature so much closer to 20.0 ° C than to 150 ° C ? The reason is that water has a greater specific heat than most common substances and thus undergoes a smaller temperature change for a given heat transfer. A large body of water, such as a lake, requires a large amount of heat to increase its temperature appreciably. This explains why the temperature of a lake stays relatively constant during the day even when the temperature change of the air is large. However, the water temperature does change over longer times (e.g., summer to winter).

Check Your Understanding If 25 kJ is necessary to raise the temperature of a rock from 25 °C to 30 ° C, how much heat is necessary to heat the rock from 45 °C to 50 ° C ?

To a good approximation, the heat transfer depends only on the temperature difference. Since the temperature differences are the same in both cases, the same 25 kJ is necessary in the second case. (As we will see in the next section, the answer would have been different if the object had been made of some substance that changes phase anywhere between 30 ° C and 50 ° C .)

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Temperature-dependent heat capacity

At low temperatures, the specific heats of solids are typically proportional to T 3 . The first understanding of this behavior was due to the Dutch physicist Peter Debye , who in 1912, treated atomic oscillations with the quantum theory that Max Planck had recently used for radiation. For instance, a good approximation for the specific heat of salt, NaCl, is c = 3.33 × 10 4 J kg · k ( T 321 K ) 3 . The constant 321 K is called the Debye temperature of NaCl, Θ D , and the formula works well when T < 0.04 Θ D . Using this formula, how much heat is required to raise the temperature of 24.0 g of NaCl from 5 K to 15 K?

Solution

Because the heat capacity depends on the temperature, we need to use the equation

c = 1 m d Q d T .

We solve this equation for Q by integrating both sides: Q = m T 1 T 2 c d T .

Then we substitute the given values in and evaluate the integral:

Q = ( 0.024 kg ) T 1 T 2 333 × 10 4 J kg · K ( T 321 K ) 3 d T = ( 6.04 × 10 −4 J K 4 ) T 4 | 5 K 15 K = 30.2 J .

Significance

If we had used the equation Q = m c Δ T and the room-temperature specific heat of salt, 880 J/kg · K, we would have gotten a very different value.

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Summary

  • Heat and work are the two distinct methods of energy transfer.
  • Heat transfer to an object when its temperature changes is often approximated well by Q = m c Δ T , where m is the object’s mass and c is the specific heat of the substance.
Practice Key Terms 7

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Source:  OpenStax, University physics volume 2. OpenStax CNX. Oct 06, 2016 Download for free at http://cnx.org/content/col12074/1.3
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