In thermodynamics, heat is not a
noun. It’s a verb. This is confusing. Why? Because colloquially we think
thermal energy and heat are the same thing, but in thermodynamics they are not.
One is a noun and the other is a verb. Before diving into the weeds, let’s
first acknowledge that nouns and verbs are labels. Keeping things simple: a
noun labels a ‘thing’; a verb labels an ‘action’. Now we’re ready to define the
two.
Thermal energy, from the chemical
perspective, is the energy of molecular motion. The amount of thermal energy in
a chemical system can be quantified by measuring its temperature. Thermal
energy is a noun. This is confusing because its definition contains the word
‘motion’ that sounds verb-ish. Considering the two broad categories of kinetic
energy and potential energy, thermal energy is more closely associated with
kinetic energy, the energy due to motion.
Heat is the transfer of thermal energy. Heat is a verb because it involves the
‘action’ of transferring. This transfer of energy takes place spontaneously
across a temperature gradient if a
suitable pathway for the flow of energy is available. Heat is the flow, not the
thing that flows. The thing that flows is thermal energy. The zeroth law of
thermodynamics is about this flow: When a hot object is placed next to a cold
object, thermal energy is transferred from the hot object to the cold one. The
cold object is heated by the hot one. Simultaneously the hot object is cooled
by the cold one. Heat is more closely associated with potential energy, as are
other gradient-related energies such as gravitational (potential) energy.
But it’s hard to exclusively use
heat as a verb. We easily slip into saying that ‘heat’ is transferred when
something becomes hotter or colder. To repeat, heat is the transfer, not what is being transferred (which is thermal energy).
In our minds, because of how we colloquially use the word ‘heat’, we associate
it with temperature change – and thus conflate it with thermal energy. I tell my
students to link thermal energy with thermometer (its measure). Thus, a change
in thermal energy of an object leads to a change in its temperature. Many
examples of heat-flow do lead to a change in temperature, but not always.
Let’s look at three examples.

In the zeroth law example shown
above, two objects at different temperatures are brought together.
Spontaneously, the direction of heat-flow down the gradient is indicated by the
red arrow. Both objects change temperature during the process. Finally, thermal
equilibrium is reached. Both objects now measure the same temperature. The
temperature gradient has been degraded – it no longer exists. We say that the
two-object system has reached thermal equilibrium.
Chemists want to know about
energy changes in a chemical reaction. In thermodynamics, we define the
‘system’ as the chemical substances. They have some energy content before the
reaction, and after a chemical reaction (where chemical bonds have been made
and broken) they often have a different energy content. We cannot easily
measure the system’s change in energy directly, so we couple the system to what
we call ‘thermal surroundings’ – typically modeled as an insulated water bath.
If a chemical reaction releases energy (and most favorable reactions do), that
energy is transferred to the water and when its temperature rises, we can
calculate the rise in thermal energy of the thermal surroundings. A calorimeter
is our device to measure this energy change. (An insulated water bath works
well as a calorimeter, hence the model used!) This is illustrated below.

Students can quantify the heat by
the formula qtherm = mCΔT where m is the mass of water, C
is the specific heat capacity of water, and ΔT is the change in temperature of
the water. All this is for the thermal surroundings. If the temperature goes
up, ΔT
is positive and therefore qtherm
is also positive. But what about the system? Since the thermodynamic universe
containing both the system and the surroundings is ‘isolated’, the energy
gained by the thermal surroundings must have come solely from the chemical
system. Thus, students learn that qsys
= –qtherm and energy is
conserved. But heat is a verb. The noun that is used to represent the energy of
the system is ‘enthalpy’. Textbooks and chemistry instructors often refer to it
as ‘heat energy’ which is historically true (and noun-ish) but semantically
confusing. This is why students have trouble with understanding the concept of
state functions: enthalpy, the noun, is a state function; heat, the verb, is
not.
A brief aside: I have skipped
using the term ‘internal energy’ for the chemical system and ignored PV-work in the model of the
thermodynamic universe, although I did draw the piston and shaft (in black) to
represent it. Leaving PV-work out of
the discussion, as I argue in a previous blog post, keeps this analysis cleaner
and simpler for students.
In the model shown above, we only
measured temperature changes in the thermal surroundings. The temperature of
the system may or may not change. If we consider reactions solely carried out
under ‘standard conditions’ so that we can tabulate standard enthalpies of
formation, then we consider that the chemical reactants and their subsequent products
to be at the same temperature. The system temperature didn’t change! But the
temperature of the thermal surroundings might have. Thus heat-flow in this case
only involves a temperature change in one milieu, not both. It makes sense to
refer to qtherm as ‘heat’
because the thermal surroundings did change temperature, but for historical
reasons, we still call qsys
‘heat’ even though the system many not have changed in temperature. Why is
there still an enthalpy change? The chemical bonds made and broken in the
reaction have different enthalpies. In a typical ‘exothermic’ reaction, one
that ‘releases heat to the surroundings’, weaker bonds are broken and stronger
bonds are formed in the chemical system. Thus the system becomes more stable or
lower in energy and ΔH, the change in enthalpy of the
system, is negative.
Second aside: In some physical
systems, students may be analyzing the opposite situation where the system is
changing temperature, and exchanges energy with a thermal bath (which remains
constant in temperature). For example, you could use a water bath to ‘heat’ a
system as shown below. For that matter, you can consider a heating element in a
reaction to act as such a reservoir of thermal energy.

In my final example, energy can
change between the system and the surroundings without any change in
temperature in either milieu. Consider the picture above where energy is being
supplied by the thermal bath/reservoir to melt ice, the system, at zero
Celcius. The ice receives energy and turns into liquid water at zero Celcius.
Was thermal energy transferred? Hmm… no temperature change was involved.
Historically we’ve come to call this ‘latent heat’. We don’t measure any
temperature change although the word ‘heat’ is still invoked. In class, I avoid
saying latent heat and simply refer to this as “delta-H of fusion” or ΔHfus.
All this seems very clumsy. In
class, I try to avoid using the phrase ‘heat of formation’ and use the more
cumbersome ‘standard enthalpy of formation’. I get better every year but old
habits die hard. I warn the students that they will often hear many of these enthalpies
referred to as the “heat of [something]” even if there are no temperature
changes. From a chemist’s point of view, I emphasize to students that when they
think of ΔH,
they should be thinking about changes in the strengths of chemical bonds (or
interactions that fall under the rubric of “intermolecular forces”) – the old
ones being broken and the new ones being made – in a chemical process. They
shouldn’t think about heat per se.
This becomes doubly important
when students begin learning about entropy. In any chemical reaction, there is
an inherent entropy change. Here’s my brief one-paragraph version. If you’re
utilizing a chemical reaction to do useful functional work (which may be
different from PV-work), you may lose
some of that energy as ‘heat’ to the thermal surroundings that isn’t due to
inefficiencies in your apparatus (which may also be present). Rather, it is
inherent to the chemical reaction. In the picture below, you want to minimize
this ‘heat’ loss (the small double-headed arrow) and maximize the energy
transfer from the system to functional work. In an equation, I would write this
as ΔH
= w’ + TΔS. As the enthalpy changes, the
entropy changes (ΔS), and w’ (w-prime, to distinguish it from PV work) is the maximum useful work you could get out of the
system, under ideal conditions. Students learn w’ as ΔG, the change in free energy of
the system. When we talk about heat as the worst form of energy when it comes
to utilization, we’re primarily referring to issues of entropy, not enthalpy.

I could go on, but this post has
likely passed the TL;DR threshold. If you’re a student reading this, I hope
this helped you. If you’re an instructor reading this, the take-home message is
that when you use the word ‘heat’ in place of enthalpy in the context of
thermodynamics, using it as a noun rather than a verb, you’re essentially using
it as a label – a name – for a more abstract quantity. Your students hearing
the word ‘heat’ might be associating it with temperature changes even if no
such changes occur. Yes, I do want my students to use the phrases ‘endothermic’
and ‘exothermic’ correctly based on the sign of ΔH. But I want to drum into them
that, conceptually, they should primarily associate ΔH in terms of the relative
strengths of chemical bonds and interactions; that’s the system property
chemists want to focus on! In thermodynamics, heat (unless being used as a more
abstract label) is not a noun.