Activity: Heat and Temperature of Water Vapor

In this introduction to heat capacity, students determine a derivative that indicates how much the internal energy changes as the temperature changes when volume is held constant.
What students learn
  • Heat capacity at constant volume relates to changes in internal energy, i.e. \({\mathit{\unicode{273}}} Q = dU\).
  • A conceptual definition of heat capacity at constant volume is the derivative of internal energy with respect to temperature without changing the volume.
  • Not all derivatives are slopes but they are all ratios of small changes.
  • Heat capacity at constant volume depends on the value of the volume. optional: Heat capacity at constant pressure is NOT \(\left(dU/dT\right)_p\) - you have to account for work done.
  • Media
    • activity_media/heat_capacity_tpu_sv_horizlabels_axis.pdf
    • activity_media/heat_capacity_tpu_sv_horizlabels_axis.png

A pressure cooker is an enclosed pot that expels air and traps water vapor, which increases the internal pressure. This in turn raises the boiling point of water and allows food to cook at high temperatures.


Imagine you have a large industrial pressure cooker that holds 1 kg of water vapor. You would like to know how responsive the system is to changes in temperature. To do this, you need to determine a characteristic rate: the ratio of the amount of heat needed to change the temperature a small amount and the change in temperature (i.e., the amount of heat transferred per change in temperature).


The graph provided by your instructor shows internal energy and volume contours plotted on temperature and pressure axes.



  1. Estimate the Temperature-Responsiveness: Use the graph to determine this temperature-responsiveness when the volume is held fixed. The initial state of the system corresponds to the black square. Describe your process.

    Student Ideas: Students might need help in recognizing that for a pressure cooker, you can control the pressure and temperature but the volume of water vapor is constant.

    Answer: We want the ratio of change in internal energy and the change in temperature along the path of constant volume. It is the ratio of small changes, not a slope on this graph.

    Discussion: Which derivative? We haven't yet told students what derivative to estimate. Have a whole class discussion about this after most groups have struggled for a few minutes and have had some insights. It's nice to have done the Quantifying Change activity before this one. Some correct answers might look like: \({\mathit{\unicode{273}}} Q/dT\), \(\left(dU/dT\right)_V\), \(Q/\Delta T\), \(\left(\Delta U/\Delta T\right)_V\).

    Student Ideas: Students try to use equipartition theorem or other equations, rather than directly measuring the rate on the graph. Students might not always realize that work done is zero, or how this would relate U and Q.

    Follow-Up: For what graph would the slope be the rate you're looking for? How is that graph related to the surface?


  2. Reflect on Your Process: Why do you think it matters that you held volume constant in the above estimate?

    Answer: Two reasons: (1) you need to specify a path in order to take the derivative, and (2) holding the volume constant means the work done is zero, so the heat added is equal to the change in internal energy.


  3. Explore Dependencies on State Variables: Does the value of your estimate depend on the value of the volume? the temperature?

    Any answer is productive here. For an ideal gas, the answer is no. Water vapor is nearly an ideal gas (but not quite). The heat capacity at constant volume is not the directional derivative.

    Optional Extensions:
    • How would you estimate the heat capacity at constant PRESSURE?

      Answer: The most straightforward way is to account for the work done along the constant pressure path and subtract that from the change in internal energy.)

      Which value is bigger: \(C_V\) or \(C_p\)? Why do you think that is?

    • What procedure would you use to you estimate \(C_v\) from the purple surface?


SUMMARY PAGE

Goals

  • Heat capacity at constant volume relates to changes in internal energy, i.e. \({\mathit{\unicode{273}}} Q = dU\).
  • A conceptual definition of heat capacity at constant volume is the derivative of internal energy with respect to temperature without changing the volume.
  • Not all derivatives are slopes but they are all ratios of small changes.
  • Heat capacity at constant volume depends on the value of the volume.
  • Optional: Heat capacity at constant pressure is NOT \(\left(dU/dT\right)_p\) -- you have to account for work done.

Equipment Needed:

  • Heat Capacity contour map
  • Student worksheet for each student
  • A personal or shared writing space for each student to write/draw/sketch.
  • Optional: Blue \(U(T,p)\) plastic surface for each group

Introduction

  • Students should have seen 1st Law of Thermodynamics and the Thermodynamic Identity
  • Students should know how to compute work as \(p\;dV\)

Whole Class Discussion:

  • Students need to figure out what derivative they're trying to estimate. Having an early WCD about this would be useful.
  • The derivative they are trying to estimate is tantalizingly close to a slope, especially for the blue dot and the green triangle. Not all partial derivatives are slopes but they are all ratios of small changes.
  • For an ideal gas, the heat capacities are constant. Water vapor is not an ideal gas but it is pretty close. In general, the heat capacity is a state variable.

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    1. Solve for the heat capacity of a vacuum, given the above, and assuming that photons represent all the energy present in vacuum.
    2. Compare the heat capacity of vacuum at room temperature with the heat capacity of an equal volume of water.
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    Potential energy Heat capacity Thermal and Statistical Physics 2020 Consider a column of atoms each of mass \(M\) at temperature \(T\) in a uniform gravitational field \(g\). Find the thermal average potential energy per atom. The thermal average kinetic energy is independent of height. Find the total heat capacity per atom. The total heat capacity is the sum of contributions from the kinetic energy and from the potential energy. Take the zero of the gravitational energy at the bottom \(h=0\) of the column. Integrate from \(h=0\) to \(h=\infty\). You may assume the gas is ideal.
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    1. Compute the entropy.

    2. Work out the heat capacity at constant pressure \(C_p\).

    3. Find the connection among \(V\), \(p\), \(N\), and \(T\), which is called the equation of state (Hint: find the volume as a partial derivative of the Gibbs free energy).

    4. Compute the internal energy \(U\).

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    assignment Homework

    Ice calorimetry lab questions
    This question is about the lab we did in class: Ice Calorimetry Lab.
    1. Plot your data I Plot the temperature versus total energy added to the system (which you can call \(Q\)). To do this, you will need to integrate the power. Discuss this curve and any interesting features you notice on it.
    2. Plot your data II Plot the heat capacity versus temperature. This will be a bit trickier. You can find the heat capacity from the previous plot by looking at the slope. \begin{align} C_p &= \left(\frac{\partial Q}{\partial T}\right)_p \end{align} This is what is called the heat capacity, which is the amount of energy needed to change the temperature by a given amount. The \(p\) subscript means that your measurement was made at constant pressure. This heat capacity is actually the total heat capacity of everything you put in the calorimeter, which includes the resistor and thermometer.
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    5. Entropy of fusion The change in entropy is easy to measure for a reversible isothermal process (such as the slow melting of ice), it is just \begin{align} \Delta S &= \frac{Q}{T} \end{align} where \(Q\) is the energy thermally added to the system and \(T\) is the temperature in Kelvin. What is was change in the entropy of the ice you melted? What was the change in entropy per molecule? What was the change in entropy per molecule divided by Boltzmann's constant?
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    It has been proposed to use the thermal gradient of the ocean to drive a heat engine. Suppose that at a certain location the water temperature is \(22^\circ\)C at the ocean surface and \(4^{o}\)C at the ocean floor.

    1. What is the maximum possible efficiency of an engine operating between these two temperatures?

    2. If the engine is to produce 1 GW of electrical power, what minimum volume of water must be processed every second? Note that the specific heat capacity of water \(c_p = 4.2\) Jg\(^{-1}\)K\(^{-1}\) and the density of water is 1 g cm\(^{-3}\), and both are roughly constant over this temperature range.

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    The isothermal compressibility is defined as \begin{equation} K_{T}=-\frac{1}{V} \left(\frac{\partial V}{\partial p}\right)_{T} \end{equation} \(K_T\) is be found by measuring the fractional change in volume when the the pressure is slightly changed with the temperature held constant. In contrast, the adiabatic compressibility is defined as \begin{equation} K_{S}=-\frac{1}{V} \left(\frac{\partial V}{\partial p}\right)_{S} \end{equation} and is measured by making a slight change in pressure without allowing for any heat transfer. This is the compressibility, for instance, that would directly affect the speed of sound. Show that \begin{equation} \frac{K_{T}}{K_{S}} = \frac{C_{p}}{C_{V}} \end{equation} Where the heat capacities at constant pressure and volume are given by \begin{align} C_{p} &= T \left(\frac{\partial S}{\partial T}\right)_{p} \\ C_{V} &= T \left(\frac{\partial S}{\partial T}\right)_{V} \end{align}

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    Consider the bottle in a bottle problem in a previous problem set, summarized here.

    A small bottle of helium is placed inside a large bottle, which otherwise contains vacuum. The inner bottle contains a slow leak, so that the helium leaks into the outer bottle. The inner bottle contains one tenth the volume of the outer bottle, which is insulated.

    The volume of the small bottle is 0.001 m23 and the volume of the big bottle is 0.01 m3. The initial state of the gas in the small bottle was \(p=106\) Pa and its temperature \(T=300\) K. Approximate the helium gas as an ideal gas of equations of state \(pV=Nk_BT\) and \(U=\frac32 Nk_BT\).

    1. How many molecules of gas does the large bottle contain? What is the final temperature of the gas?

    2. Compute the integral \(\int \frac{{\mathit{\unicode{273}}} Q}{T}\) and the change of entropy \(\Delta S\) between the initial state (gas in the small bottle) and the final state (gas leaked in the big bottle).

    3. Discuss your results.


Learning Outcomes