Thermodynamics on a Midwinter Morning
Problem Statement
Thermodynamics on a Midwinter Morning
Problem Statement
On a very cold midwinter morning, the room’s window was open, causing the indoor temperature to drop to below freezing. We close the window and trap a mass of air ma inside a completely insulated, sealed container (which models this room). The initial temperature of the air at this point was T1.
To serve as a substitute for heating, a mass mw of hot water at an initial temperature of T2 was gently placed inside the container, which was then resealed.
After a sufficient amount of time had elapsed, the air inside the room and the hot water reached thermal equilibrium, and the overall temperature became T3. In this process, we assume the following conditions:
- We consider only heat transfer from the hot water to the air; heat exchange with the outside and the heat capacity of the container can be neglected.
- Changes in the volume of the air can be neglected, so we treat the process as a constant-volume process. Let the specific heat at constant volume of the air be cv.
- Let the specific heat of water be cw.
- Let the melting point of water be T0. Assume that the water remains entirely in the liquid state without freezing and does not evaporate.
Derive the temperature T3 at thermal equilibrium using an algebraic expression, then substitute the given values of the constraints to find the value of T3.
Constraints
- Mass of air: ma=35kg
- Specific heat capacity of air at constant volume: cv=720J/(kg⋅K)
- Initial temperature of air: T1=266K
- Mass of hot water: mw=0.8kg
- Initial temperature of hot water: T2=368K
- Specific heat of water: cw=4200J/(kg⋅K)
- Melting point of water: T0=273K
Input Format
Enter the value of the temperature T3 at thermal equilibrium as a natural number.
Solution
Explanation
Application of Physical Laws
Since this phenomenon occurs within an insulated, sealed container with no heat exchange with the outside, the total energy of the system is conserved. In other words, the “heat gained by the air, Qgain,” and the “heat lost by the hot water (water), Qloss,” are equal.
Qgain=Qloss
Deriving the Heat Changes for Each Substance
Let T3 be the overall temperature at thermal equilibrium.
-
Heat gained by the air Qgain The air is heated from temperature T1 to T3 in a constant-volume process. Qgain=macv(T3−T1)
-
Heat lost by the hot water Qloss The hot water is cooled from temperature T2 to T3. Qloss=mwcw(T2−T3)
Deriving T3 Using the Law of Conservation of Heat
Substitute each term into the equation for the conservation of heat.
macv(T3−T1)=mwcw(T2−T3)
Rearrange this equation for T3.
(macv+mwcw)T3=macvT1+mwcwT2
T3=macv+mwcwmacvT1+mwcwT2
Substituting Values and Calculating
Substitute the given constraint values.
- macv=35×720=25200 J/K
- mwcw=0.8×4200=3360 J/K
The denominator is as follows. macv+mwcw=25200+3360=28560 J/K
The numerator is as follows. macvT1+mwcwT2=25200×266+3360×368 =6,703,200+1,236,480=7,939,680 J
Therefore, T3 is calculated as follows: T3=28,5607,939,680=278 K
Converted to Celsius, this temperature is 278−273=5 ∘C. Since this exceeds the melting point of water, T0=273 K, it satisfies the problem’s assumption that “water does not freeze and remains in a liquid state.” It divides evenly into an integer without any rounding or approximation.
The natural number to enter is 278.