WEBVTT

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RAFAEL JARAMILLO: All right,
so let's talk about processes

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and thermodynamics.

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So we talked about thermo
being this weird thing

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that can tell you about starting
state and the final state.

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But it doesn't
really have a clue

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as to the process that takes
you from one to the other.

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That is thermo doesn't
describe real world processes.

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But that doesn't
mean it's useless.

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The concept of state functions,
which are history independent,

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allows us to make predictions.

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So for example, if someone told
you the pressure, temperature,

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and volume of the
system at the beginning

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and then told you the
pressure and temperature

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of the system at the end,
with that information

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you could calculate the
volume without knowing

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the process that took it from
A to B. So that's useful.

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So here's the property
of state functions.

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Any process connecting A
to B will give same results

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for the final state.

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These are the final
state variables,

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because they are
state variables.

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So you want to
calculate something.

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You want to do the easiest
calculation you can,

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conceptualize the simplest
process to calculate it.

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So in the same
way that we choose

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a system, its components,
and its boundaries out

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of convenience depending on the
problem we're trying to solve,

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you calculate the simplest
process to calculate out

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of convenience, not
necessarily the process

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that nature actually takes.

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So the simplest processes
to calculate are reversible.

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So reversible process,
that's a new concept.

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That's a new concept for us.

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And it has a very
deep and important

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thermodynamic meaning.

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It means a process
that does not change

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the entropy of the universe.

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That is a system plus
its surroundings.

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And we'll see that in the
next couple of lectures.

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Reversible processes
have these properties--

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the system plus surroundings
are in equilibrium at all times.

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That's an assumption.

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This violates our day-to-day
notion of an arrow of time.

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It's really inconsistent
with most of our experience.

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In practice, a reversible
process would take forever.

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So we're imagining a process,
which doesn't actually exist.

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But it makes a
calculation easier.

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So in order for a process to
be in equilibrium at all times,

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it has to go arbitrarily slowly.

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In order for our process
to be able to go forwards

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or backwards, we need to be
able to play the movie forwards

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or backwards without being able
to tell which one is forwards

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and which one is backwards.

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That violates our day-to-day
notion of the arrow of time.

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And the requirement to
go arbitrarily slowly

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means that in practice,
a reversible process

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would take forever.

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But it makes
calculations really easy.

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Is that surprising to anybody?

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Or we're comfortable
with the concept

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of a reversible process?

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None of your day-to-day
processes are reversible.

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If you think you can think
of one, just toss it out.

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And we can try to
figure out why it's not.

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Those are kind of fun
thought experiments.

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Let's describe processes.

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In the last lecture,
we described systems.

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Now we're going to
describe processes.

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So things you can
do to a system--

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you can work on it,
you can heat it,

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or you can add or
subtract stuff.

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These are things you can do.

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These are verbs in thermo.

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All of these are
verbs in thermo.

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They're actions that
you do on a system.

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Work, what is work?

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It's a mechanical way
of exchanging energy,

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mechanical exchange of energy.

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So we use w, and what's that?

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Kilogram meter squared
per second squared,

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that's the units of energy.

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Just a little bit of
dimensional analysis--

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you guys separate that
out, it's kilogram meter

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per second squared per meter
equals force times distance.

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That's force, and
that's distance.

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That's fine.

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In thermo, we normally
separate that out a little bit

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differently.

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We grab kilogram per
meter per second squared.

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What do I need?

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What do I need to
multiply this by in order

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to get the same units?

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What do I need?

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STUDENT: Volume, meters.

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RAFAEL JARAMILLO: Volume,
yeah, meters cubed.

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So what's this?

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This is a pressure
times a volume.

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So when you take
Intro Mechanics,

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let's say in a physics
class, you normally

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do force times distance work.

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But when you take
Intro Thermodynamics,

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you normally do
pressure volume work.

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Course C is where I got this at.

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But this is P, PVV
work, we call it.

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That's work.

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What about heat?

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Well, it's kind difficult
to define, actually.

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Heat is a process that exchanges
energy without mechanical work

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or mass exchanges.

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So heat is defined
by what it's not.

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It's kind of a weird thing.

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And for heat, we're
going to use q.

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So work is w, heat is q.

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They both have units
of energy, joules.

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So we have described
state variables,

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which are history-independent.

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But we also have
process variables

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that are process-dependent.

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So infinitesimal increments,
infinitesimal of process

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variables are denoted as--

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I'm going to put this in
quotes, "inexact differentials."

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That is dq/d work.

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Using d, not D.

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This is annoying.

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Don't blame, don't
shoot the messenger.

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This is one really key
area where thermo deviates

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from multivariable calculus.

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So try not to get confused
because it is confusing.

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There's a mini
lecture I recorded.

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It's up on the website
called, the Three

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d's of Thermodynamics,
because it gets kind of hairy.

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We use a lot of d's
to denote differences.

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So hopefully, that's
useful at some point,

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if not now, then maybe in
a week or two in the class.

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In thermodynamics this Greek
dx means path dependent.

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That's what it means.

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So what is a process variable?

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If you have a state
A and a state B,

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a process variable
is a variable,

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which depends on the process
it takes to get from A to B.

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So you might have path 1
with work 1 and heat 1,

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and path 2 with
work 2 and heat 2.

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And those are different because
they're not state variables.

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They're process variables.

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If we were on campus,
the nice analogy to use

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is the amount of
work you need to get

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from the second
floor of building 1

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to the fifth floor
of building 32,

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or just pick a pair like that.

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There is myriad ways of
connecting those two.

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Because the campus is connected.

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You can go upstairs
and downstairs,

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you can take
elevators, you could

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get between those two points
in a very large number

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of different combinations.

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And the amount of mechanical
work you need to do

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will vary with combination.

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But the change in your
gravitational potential energy

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between the starting and final
point, that's a fixed change.

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That's an example
of process variables

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versus state variables.

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But we're not on campus.

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That's so sad.

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You're just going
to have to imagine

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all the work you'd
have to do to get

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from building 1 to building 32.

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So this is infinitesimal
increments and process

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variables.

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Infinitesimal-- I think
I need new markers.

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And state variables are
denoted as exact differentials.

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So for example, dT,
dP, dV, and so on,

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using regular lowercase d
as in a total differentiable

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in calculus.

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So all I can do is tell you
that understanding that can only

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come through practice, for sure
at the beginning of the class.

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So all I can do is tell you--

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I'm going to try to switch
the purple so things show up

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a little better.

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So let's talk about how
we classify processes.

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So an isothermal process is a
process at fixed temperature.

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What about an adiabatic process?

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Anybody know?

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STUDENT: It's like very fast.

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STUDENT: Does it permeate
through a boundary?

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STUDENT: Heat is 0.

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RAFAEL JARAMILLO: I
heard a couple of things

00:16:39.860 --> 00:16:41.152 align:middle line:90%
which are equivalent, actually.

00:16:41.152 --> 00:16:42.890 align:middle line:90%
Somebody said very fast.

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Somebody else said, no heat
flow across the boundary.

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So the strict definition is no
heating across the boundary.

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In reality, heat will always
flow from a hot object

00:17:07.540 --> 00:17:10.420 align:middle line:90%
through a cold object.

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But if you've
insulated your system,

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whether it's your house
or a beaker in the lab,

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then that heat flow
could be slowed down.

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So one way of approximating
an adiabatic process

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is to run it quickly.

00:17:30.310 --> 00:17:33.270 align:middle line:84%
If you run a process
very quickly,

00:17:33.270 --> 00:17:36.570 align:middle line:84%
the entire process can run
before an appreciable amount

00:17:36.570 --> 00:17:40.170 align:middle line:84%
of heat flows
across the boundary.

00:17:40.170 --> 00:17:43.660 align:middle line:84%
So that's why a fast
process can be equivalent,

00:17:43.660 --> 00:17:46.200 align:middle line:90%
so I like both of those answers.

00:17:46.200 --> 00:17:59.850 align:middle line:84%
Isobaric-- isobaric process is
that fixed P. And isochoric, we

00:17:59.850 --> 00:18:15.230 align:middle line:84%
don't use as much,
it's fixed V. And we'll

00:18:15.230 --> 00:18:18.020 align:middle line:84%
see that means that there can
be no work done on the system

00:18:18.020 --> 00:18:21.050 align:middle line:90%
if the volume is fixed.

00:18:21.050 --> 00:18:26.410 align:middle line:84%
And then there is
classifying boundaries.

00:18:26.410 --> 00:18:30.080 align:middle line:90%


00:18:30.080 --> 00:18:32.320 align:middle line:84%
We've seen this a
little bit so far.

00:18:32.320 --> 00:18:39.230 align:middle line:84%
But as a practical matter, the
way that we set up processes

00:18:39.230 --> 00:18:42.000 align:middle line:90%
are by defining boundaries.

00:18:42.000 --> 00:18:48.930 align:middle line:84%
So for example, an
insulating boundary,

00:18:48.930 --> 00:18:51.900 align:middle line:90%
and no or say, slow heat flow.

00:18:51.900 --> 00:18:57.630 align:middle line:90%


00:18:57.630 --> 00:19:08.085 align:middle line:84%
Diathermal-- heat
but no mass transfer.

00:19:08.085 --> 00:19:16.980 align:middle line:90%


00:19:16.980 --> 00:19:31.970 align:middle line:84%
Open or closed, is mass the
transfer allowed or disallowed?

00:19:31.970 --> 00:19:35.910 align:middle line:90%


00:19:35.910 --> 00:19:40.890 align:middle line:90%
And rigid, fixed volume.

00:19:40.890 --> 00:19:46.060 align:middle line:90%


00:19:46.060 --> 00:19:50.370 align:middle line:84%
So when we run processes,
we can somewhat

00:19:50.370 --> 00:19:52.170 align:middle line:84%
determine what kind
of process we're

00:19:52.170 --> 00:19:56.140 align:middle line:84%
going to run by setting up
the boundary conditions.

00:19:56.140 --> 00:19:57.390 align:middle line:90%
And this is a practical thing.

00:19:57.390 --> 00:19:58.515 align:middle line:90%
This is a practical matter.

00:19:58.515 --> 00:20:01.650 align:middle line:84%
And all of us who run
labs, we do this every day

00:20:01.650 --> 00:20:02.550 align:middle line:90%
in various ways.

00:20:02.550 --> 00:20:07.140 align:middle line:90%


00:20:07.140 --> 00:20:10.620 align:middle line:84%
So classifying processes,
classifying boundaries,

00:20:10.620 --> 00:20:11.970 align:middle line:90%
and so forth--

00:20:11.970 --> 00:20:15.660 align:middle line:84%
let's talk about other things
associated with processes.

00:20:15.660 --> 00:20:18.810 align:middle line:90%
What about heat capacity?

00:20:18.810 --> 00:20:21.860 align:middle line:84%
Most folks have encountered
heat capacity before.

00:20:21.860 --> 00:20:24.380 align:middle line:84%
Heat capacity, we're
going to use C.

00:20:24.380 --> 00:20:34.700 align:middle line:84%
And it is the change in heat,
an incremental amount of heat

00:20:34.700 --> 00:20:46.510 align:middle line:84%
for an incremental change of
temperature, heat increment,

00:20:46.510 --> 00:20:47.530 align:middle line:90%
temp increment.

00:20:47.530 --> 00:20:56.560 align:middle line:90%


00:20:56.560 --> 00:21:02.470 align:middle line:84%
Is heat capacity a state
variable or a process variable?

00:21:02.470 --> 00:21:03.442 align:middle line:90%
STUDENT: Process.

00:21:03.442 --> 00:21:04.900 align:middle line:84%
RAFAEL JARAMILLO:
Process is right.

00:21:04.900 --> 00:21:07.480 align:middle line:90%
Why is it a process very well?

00:21:07.480 --> 00:21:11.800 align:middle line:84%
STUDENT: Because the
dq is path-dependent.

00:21:11.800 --> 00:21:13.150 align:middle line:90%
RAFAEL JARAMILLO: Yeah, exactly.

00:21:13.150 --> 00:21:14.740 align:middle line:84%
It's a process
variable because it

00:21:14.740 --> 00:21:17.840 align:middle line:90%
depends on a process variable.

00:21:17.840 --> 00:21:20.690 align:middle line:84%
One corollary of the
postulate that there

00:21:20.690 --> 00:21:24.020 align:middle line:84%
exists state functions, is that
state functions can only depend

00:21:24.020 --> 00:21:26.280 align:middle line:90%
on other state functions.

00:21:26.280 --> 00:21:28.610 align:middle line:84%
So if something depends
on a process variable,

00:21:28.610 --> 00:21:32.330 align:middle line:84%
it itself, is a
process variable.

00:21:32.330 --> 00:21:35.120 align:middle line:90%
C is path dependent.

00:21:35.120 --> 00:21:43.250 align:middle line:90%


00:21:43.250 --> 00:21:53.440 align:middle line:90%
Dq is a process variable.

00:21:53.440 --> 00:22:05.150 align:middle line:84%
So it's useful to
define common processes.

00:22:05.150 --> 00:22:09.820 align:middle line:90%


00:22:09.820 --> 00:22:12.670 align:middle line:84%
I should say define
for common processes.

00:22:12.670 --> 00:22:14.860 align:middle line:84%
And the ones that we
encounter in this class

00:22:14.860 --> 00:22:33.590 align:middle line:84%
are CV equals dq/dt at
fixed volume and CP, which

00:22:33.590 --> 00:22:39.035 align:middle line:90%
is dq/dt at fixed pressure.

00:22:39.035 --> 00:22:45.548 align:middle line:90%


00:22:45.548 --> 00:22:47.340 align:middle line:84%
And the reason these
are what you encounter

00:22:47.340 --> 00:22:50.438 align:middle line:84%
is because these
are the most useful.

00:22:50.438 --> 00:22:52.230 align:middle line:84%
How do you keep a system
at fixed pressure?

00:22:52.230 --> 00:22:54.840 align:middle line:84%
Let's say, you want to keep a
system at atmospheric pressure.

00:22:54.840 --> 00:22:56.257 align:middle line:84%
What's the easiest
way to do that?

00:22:56.257 --> 00:22:58.780 align:middle line:90%


00:22:58.780 --> 00:23:01.160 align:middle line:90%
STUDENT: Use it like a piston.

00:23:01.160 --> 00:23:03.660 align:middle line:84%
RAFAEL JARAMILLO: It's actually,
I would think the opposite.

00:23:03.660 --> 00:23:07.710 align:middle line:84%
Expose it to the atmosphere,
remove the piston.

00:23:07.710 --> 00:23:10.500 align:middle line:84%
Because if a system is
exposed to the atmosphere,

00:23:10.500 --> 00:23:12.660 align:middle line:84%
it can exchange volume
with the atmosphere.

00:23:12.660 --> 00:23:14.490 align:middle line:84%
It can get bigger
or get smaller.

00:23:14.490 --> 00:23:16.410 align:middle line:84%
If it's higher
pressure in atmosphere,

00:23:16.410 --> 00:23:18.390 align:middle line:84%
it'll push against
the atmosphere

00:23:18.390 --> 00:23:20.380 align:middle line:84%
and return back to
atmospheric pressure.

00:23:20.380 --> 00:23:21.960 align:middle line:84%
If it's at lower
pressure, it will

00:23:21.960 --> 00:23:24.390 align:middle line:84%
get compressed by the
atmosphere and return back

00:23:24.390 --> 00:23:25.870 align:middle line:90%
to atmospheric pressure.

00:23:25.870 --> 00:23:30.910 align:middle line:84%
So the existence of a free
surface regulates the pressure.

00:23:30.910 --> 00:23:33.700 align:middle line:84%
Cost in volume, that would be
a case like a piston, where

00:23:33.700 --> 00:23:36.850 align:middle line:84%
you have something rigid,
a really rigid container.

00:23:36.850 --> 00:23:39.618 align:middle line:84%
You can fix the volume
and then run the process.

00:23:39.618 --> 00:23:41.035 align:middle line:84%
The volume is not
going to change.

00:23:41.035 --> 00:23:43.650 align:middle line:90%


00:23:43.650 --> 00:23:45.792 align:middle line:90%
Which one of these is bigger?

00:23:45.792 --> 00:23:47.292 align:middle line:84%
That requires a
little more thought.

00:23:47.292 --> 00:23:49.292 align:middle line:84%
We're going to increase
the energy of the system

00:23:49.292 --> 00:23:49.930 align:middle line:90%
by heating it.

00:23:49.930 --> 00:23:53.120 align:middle line:90%


00:23:53.120 --> 00:23:56.920 align:middle line:84%
We're going to increase
the energy by heating it.

00:23:56.920 --> 00:24:00.060 align:middle line:84%
For a given increase
in temperature,

00:24:00.060 --> 00:24:02.310 align:middle line:84%
do I need to hear it more
of a fixed volume or a fixed

00:24:02.310 --> 00:24:03.572 align:middle line:90%
pressure?

00:24:03.572 --> 00:24:05.030 align:middle line:84%
We haven't really
gotten there yet.

00:24:05.030 --> 00:24:08.360 align:middle line:84%
But I'm wondering if
somebody wants to venture

00:24:08.360 --> 00:24:09.800 align:middle line:90%
a guess with an explanation.

00:24:09.800 --> 00:24:16.360 align:middle line:90%


00:24:16.360 --> 00:24:19.656 align:middle line:84%
STUDENT: Maybe for
fixed pressure.

00:24:19.656 --> 00:24:22.660 align:middle line:84%
RAFAEL JARAMILLO: Fixed
pressure, how do you figure?

00:24:22.660 --> 00:24:25.420 align:middle line:84%
STUDENT: I mean, I think if
the system is like half fixed

00:24:25.420 --> 00:24:31.090 align:middle line:84%
volume, it wouldn't be able
to use the heat as work.

00:24:31.090 --> 00:24:33.790 align:middle line:84%
But with fixed
pressure, it can expand.

00:24:33.790 --> 00:24:35.860 align:middle line:90%
RAFAEL JARAMILLO: Yeah.

00:24:35.860 --> 00:24:38.290 align:middle line:84%
So your reasoning is right,
but your answer is wrong.

00:24:38.290 --> 00:24:40.000 align:middle line:84%
So I'm glad-- the
reason there is

00:24:40.000 --> 00:24:42.160 align:middle line:84%
when you have a system
that's at fixed volume,

00:24:42.160 --> 00:24:44.620 align:middle line:84%
it can't do any work
on the surroundings.

00:24:44.620 --> 00:24:46.270 align:middle line:90%
It's hemmed in.

00:24:46.270 --> 00:24:48.580 align:middle line:84%
So all of these thermal
energy you put in

00:24:48.580 --> 00:24:51.520 align:middle line:84%
will go into a change in the
internal energy of the system,

00:24:51.520 --> 00:24:53.710 align:middle line:90%
increase in temperature.

00:24:53.710 --> 00:24:57.550 align:middle line:84%
Whereas if you have a system
that's fixed pressure,

00:24:57.550 --> 00:24:58.360 align:middle line:90%
it can do work.

00:24:58.360 --> 00:25:01.160 align:middle line:84%
It can expand against
its surroundings.

00:25:01.160 --> 00:25:04.210 align:middle line:84%
So as you pour energy
in the form of heat,

00:25:04.210 --> 00:25:07.010 align:middle line:84%
it can lose energy in
the form of doing work.

00:25:07.010 --> 00:25:08.820 align:middle line:84%
So it's like filling
up a leaky cup.

00:25:08.820 --> 00:25:11.320 align:middle line:84%
You have to pour more water in
because there's stuff leaking

00:25:11.320 --> 00:25:12.528 align:middle line:90%
out at the bottom of the cup.

00:25:12.528 --> 00:25:14.560 align:middle line:84%
In this case, the
stuff leaking out

00:25:14.560 --> 00:25:18.160 align:middle line:84%
is energy in the form of
work on the surroundings.

00:25:18.160 --> 00:25:20.355 align:middle line:90%
So CV is smaller.

00:25:20.355 --> 00:25:21.280 align:middle line:90%
CP is larger.

00:25:21.280 --> 00:25:24.520 align:middle line:84%
But your thinking
about work was correct.

00:25:24.520 --> 00:25:27.880 align:middle line:90%


00:25:27.880 --> 00:25:41.190 align:middle line:84%
C is an empirical observable
recorded in devices.

00:25:41.190 --> 00:25:48.850 align:middle line:90%


00:25:48.850 --> 00:25:50.540 align:middle line:90%
That's really important.

00:25:50.540 --> 00:25:52.570 align:middle line:84%
Maybe you know that,
maybe you don't.

00:25:52.570 --> 00:25:55.990 align:middle line:84%
But the heat
capacity of a system

00:25:55.990 --> 00:25:59.335 align:middle line:84%
tells you so much
about that system.

00:25:59.335 --> 00:26:01.210 align:middle line:84%
But most of those things,
you can't calculate

00:26:01.210 --> 00:26:03.280 align:middle line:90%
from first principles.

00:26:03.280 --> 00:26:06.410 align:middle line:84%
They need to be measured
and then reported.

00:26:06.410 --> 00:26:08.545 align:middle line:84%
So for example,
what has larger--

00:26:08.545 --> 00:26:16.220 align:middle line:90%


00:26:16.220 --> 00:26:29.710 align:middle line:84%
here's some,
here's-- entry level,

00:26:29.710 --> 00:26:32.540 align:middle line:84%
what has a bigger capacity, a
big pot of water or a small pot

00:26:32.540 --> 00:26:33.040 align:middle line:90%
of water?

00:26:33.040 --> 00:26:36.421 align:middle line:90%


00:26:36.421 --> 00:26:37.932 align:middle line:90%
STUDENT: They have the same.

00:26:37.932 --> 00:26:39.640 align:middle line:84%
RAFAEL JARAMILLO:
Well, yeah, it depends.

00:26:39.640 --> 00:26:43.260 align:middle line:84%
Heat capacity could be
extensive or intensive.

00:26:43.260 --> 00:26:46.030 align:middle line:84%
So I think I know what you're
saying, water is water.

00:26:46.030 --> 00:26:49.110 align:middle line:84%
But when we want to regulate
the temperature of something,

00:26:49.110 --> 00:26:51.360 align:middle line:84%
we want to prevent a
temperature change,

00:26:51.360 --> 00:26:57.630 align:middle line:84%
it helps to have a large
heat capacity object nearby,

00:26:57.630 --> 00:27:00.217 align:middle line:90%
a large thermal reservoir.

00:27:00.217 --> 00:27:01.800 align:middle line:84%
That's one reason
why the temperatures

00:27:01.800 --> 00:27:05.400 align:middle line:84%
are more moderate on the coasts
of continents than inland.

00:27:05.400 --> 00:27:07.890 align:middle line:84%
Our temperature in Boston
doesn't swing nearly

00:27:07.890 --> 00:27:11.030 align:middle line:90%
as much as it does in Iowa.

00:27:11.030 --> 00:27:14.090 align:middle line:84%
You could say the same about any
inland versus coastal community

00:27:14.090 --> 00:27:14.880 align:middle line:90%
in the world.

00:27:14.880 --> 00:27:16.490 align:middle line:84%
And the reason is
that the oceans

00:27:16.490 --> 00:27:18.080 align:middle line:90%
are a big thermal reservoir.

00:27:18.080 --> 00:27:21.830 align:middle line:84%
They have a larger heat capacity
than the Great Lakes do.

00:27:21.830 --> 00:27:23.750 align:middle line:84%
So our temperature
swings are less.

00:27:23.750 --> 00:27:26.590 align:middle line:90%
What about bread or cheese?

00:27:26.590 --> 00:27:29.500 align:middle line:90%


00:27:29.500 --> 00:27:33.113 align:middle line:84%
Same quantity, now, same
mass, bread or cheese?

00:27:33.113 --> 00:27:36.360 align:middle line:90%


00:27:36.360 --> 00:27:38.410 align:middle line:90%
STUDENT: Bread?

00:27:38.410 --> 00:27:39.730 align:middle line:90%
STUDENT: Cheese, maybe.

00:27:39.730 --> 00:27:40.450 align:middle line:84%
RAFAEL JARAMILLO: I
think it's cheese.

00:27:40.450 --> 00:27:42.040 align:middle line:84%
When you eat pizza,
the bread is not

00:27:42.040 --> 00:27:43.520 align:middle line:84%
the one that burns
the top of your mouth.

00:27:43.520 --> 00:27:44.187 align:middle line:90%
It's the cheese.

00:27:44.187 --> 00:27:46.410 align:middle line:90%
It has a larger capacity.

00:27:46.410 --> 00:27:47.808 align:middle line:90%
Cheese has a larger capacity.

00:27:47.808 --> 00:27:49.725 align:middle line:84%
That has to do with, of
course, the chemistry.

00:27:49.725 --> 00:27:51.930 align:middle line:84%
A big pot of water has
a larger heat capacity.

00:27:51.930 --> 00:27:55.155 align:middle line:84%
What about aluminum
foil or a potato?

00:27:55.155 --> 00:28:01.350 align:middle line:90%


00:28:01.350 --> 00:28:03.470 align:middle line:84%
STUDENT: Isn't a larger
heat capacity and ability

00:28:03.470 --> 00:28:06.800 align:middle line:84%
to absorb more thermal energy
without changing temperature,

00:28:06.800 --> 00:28:07.460 align:middle line:90%
though?

00:28:07.460 --> 00:28:09.860 align:middle line:90%
RAFAEL JARAMILLO: Yes, exactly.

00:28:09.860 --> 00:28:14.120 align:middle line:84%
STUDENT: So isn't the cheese
changing more in temperature

00:28:14.120 --> 00:28:15.075 align:middle line:90%
than the bread?

00:28:15.075 --> 00:28:15.950 align:middle line:90%
RAFAEL JARAMILLO: No.

00:28:15.950 --> 00:28:17.750 align:middle line:84%
What it means is
that you have to put

00:28:17.750 --> 00:28:20.030 align:middle line:84%
in more energy from
your mouth to cool down

00:28:20.030 --> 00:28:23.105 align:middle line:84%
the cheese than you do
to cool down the bread.

00:28:23.105 --> 00:28:24.980 align:middle line:84%
So here's another example,
which should help.

00:28:24.980 --> 00:28:26.528 align:middle line:84%
Aluminum foil
versus potato-- you

00:28:26.528 --> 00:28:28.070 align:middle line:84%
bake a potato that's
wrapped in foil.

00:28:28.070 --> 00:28:30.980 align:middle line:90%


00:28:30.980 --> 00:28:32.210 align:middle line:90%
STUDENT: Potato.

00:28:32.210 --> 00:28:34.127 align:middle line:84%
RAFAEL JARAMILLO: You
take it out of the oven.

00:28:34.127 --> 00:28:37.180 align:middle line:90%


00:28:37.180 --> 00:28:38.110 align:middle line:90%
Someone said potato.

00:28:38.110 --> 00:28:39.460 align:middle line:84%
The answer is going
to be the foil.

00:28:39.460 --> 00:28:42.043 align:middle line:84%
When you take something out of
the oven, it's wrapped in foil.

00:28:42.043 --> 00:28:43.630 align:middle line:90%
You can often open the foil.

00:28:43.630 --> 00:28:45.460 align:middle line:84%
Even if the oven
was at 400 degrees,

00:28:45.460 --> 00:28:48.100 align:middle line:84%
you can open the foil
without burning your fingers.

00:28:48.100 --> 00:28:49.660 align:middle line:90%
You have to avoid the steam.

00:28:49.660 --> 00:28:53.770 align:middle line:84%
But you could grab that foil
and very quickly bring that foil

00:28:53.770 --> 00:28:58.440 align:middle line:84%
down to room temperature
without burning your fingers.

00:28:58.440 --> 00:29:00.170 align:middle line:84%
But if you grab
the potato, you're

00:29:00.170 --> 00:29:02.230 align:middle line:90%
going to burn your hands.

00:29:02.230 --> 00:29:05.140 align:middle line:84%
Because it takes more energy
out of you, in this case,

00:29:05.140 --> 00:29:07.900 align:middle line:84%
to cool the potato than
it does to cool the foil.

00:29:07.900 --> 00:29:09.970 align:middle line:84%
STUDENT: Doesn't that mean
the potato is actually

00:29:09.970 --> 00:29:12.550 align:middle line:90%
the one with a high C?

00:29:12.550 --> 00:29:15.160 align:middle line:84%
RAFAEL JARAMILLO: Larger
C, yeah, sorry, sorry.

00:29:15.160 --> 00:29:18.280 align:middle line:90%
Everything I said, but reverse.

00:29:18.280 --> 00:29:21.310 align:middle line:84%
Exactly, it's easier
to bring down.

00:29:21.310 --> 00:29:22.720 align:middle line:84%
And this is lots
of examples here

00:29:22.720 --> 00:29:25.060 align:middle line:84%
that are every day, why
certain surfaces outside

00:29:25.060 --> 00:29:28.270 align:middle line:84%
feel colder or hotter than other
surfaces on a very cold or very

00:29:28.270 --> 00:29:31.840 align:middle line:84%
hot day, lots of
examples like this.

00:29:31.840 --> 00:29:37.510 align:middle line:90%
So what do I mean to say here?

00:29:37.510 --> 00:29:41.650 align:middle line:90%


00:29:41.650 --> 00:29:52.510 align:middle line:84%
C can be calculated for
simple, we call toy problems.

00:29:52.510 --> 00:29:56.150 align:middle line:90%


00:29:56.150 --> 00:30:01.930 align:middle line:84%
But in most cases,
especially in cases

00:30:01.930 --> 00:30:07.360 align:middle line:84%
that we rely on as engineers,
measurements are necessary.

00:30:07.360 --> 00:30:14.937 align:middle line:90%


00:30:14.937 --> 00:30:16.770 align:middle line:84%
And I actually did
record some numbers here.

00:30:16.770 --> 00:30:22.340 align:middle line:84%
So heat capacity in
joules per gram Kelvin--

00:30:22.340 --> 00:30:24.570 align:middle line:90%
let's see, water.

00:30:24.570 --> 00:30:26.615 align:middle line:90%
Water has a large capacity.

00:30:26.615 --> 00:30:29.810 align:middle line:84%
It has to do with all of the
vibrational degrees of freedom

00:30:29.810 --> 00:30:30.880 align:middle line:90%
in water.

00:30:30.880 --> 00:30:35.050 align:middle line:90%
Aluminum is very small, 0.897.

00:30:35.050 --> 00:30:37.510 align:middle line:84%
So this right here is why you
can touch the aluminum foil,

00:30:37.510 --> 00:30:40.960 align:middle line:84%
but you have to avoid getting
a steam burn when you open up

00:30:40.960 --> 00:30:43.090 align:middle line:90%
the food you packed in foil.

00:30:43.090 --> 00:30:47.110 align:middle line:84%
Potato is actually
large, close to water.

00:30:47.110 --> 00:30:48.940 align:middle line:84%
Because anything
that's food-related,

00:30:48.940 --> 00:30:52.790 align:middle line:84%
basically is set by
the water content.

00:30:52.790 --> 00:30:57.620 align:middle line:84%
Cheese has a lower water
content than potato.

00:30:57.620 --> 00:30:59.210 align:middle line:90%
I grabbed the number 3.15.

00:30:59.210 --> 00:31:01.460 align:middle line:84%
If you are a gourmet
chef, you have

00:31:01.460 --> 00:31:04.340 align:middle line:84%
a table of capacities
of things like cheese.

00:31:04.340 --> 00:31:09.020 align:middle line:90%
And 3.15 is this one number.

00:31:09.020 --> 00:31:10.370 align:middle line:90%
I mean, I don't know cheddar.

00:31:10.370 --> 00:31:14.857 align:middle line:90%
But anyway, so let's move on.

00:31:14.857 --> 00:31:15.440 align:middle line:90%
Let's move on.

00:31:15.440 --> 00:31:19.410 align:middle line:90%


00:31:19.410 --> 00:31:22.230 align:middle line:84%
So, let's talk about
something really important,

00:31:22.230 --> 00:31:24.080 align:middle line:90%
the first law of thermodynamics.

00:31:24.080 --> 00:31:36.180 align:middle line:90%


00:31:36.180 --> 00:31:49.800 align:middle line:84%
So here's the first
law of thermodynamics,

00:31:49.800 --> 00:31:54.240 align:middle line:84%
as you sometimes encounter
it in a physics class.

00:31:54.240 --> 00:31:57.240 align:middle line:90%


00:31:57.240 --> 00:32:01.140 align:middle line:84%
And I'm here to tell you
this is totally useless.

00:32:01.140 --> 00:32:05.370 align:middle line:84%
Because if this is all
it were, who cares?

00:32:05.370 --> 00:32:10.730 align:middle line:84%
I mean, it's interesting,
but you can't use that.

00:32:10.730 --> 00:32:13.370 align:middle line:84%
And that's not how
we arrived at it.

00:32:13.370 --> 00:32:18.780 align:middle line:84%
Intellectually, it's sort of
intellectually being dishonest.

00:32:18.780 --> 00:32:24.490 align:middle line:84%
Because this is very
non-obvious, very non-obvious

00:32:24.490 --> 00:32:27.580 align:middle line:90%
and rather hard to prove also.

00:32:27.580 --> 00:32:28.630 align:middle line:90%
How is this useful?

00:32:28.630 --> 00:32:31.600 align:middle line:90%


00:32:31.600 --> 00:32:35.960 align:middle line:84%
The answer is because
it applies locally.

00:32:35.960 --> 00:32:40.420 align:middle line:84%
And this is where the real
intellectual thread comes from.

00:32:40.420 --> 00:32:52.250 align:middle line:90%


00:32:52.250 --> 00:33:02.320 align:middle line:84%
So we talk about the energy of
a system plus the surroundings.

00:33:02.320 --> 00:33:06.590 align:middle line:90%


00:33:06.590 --> 00:33:10.310 align:middle line:84%
System plus surroundings,
you could call universe.

00:33:10.310 --> 00:33:12.900 align:middle line:90%


00:33:12.900 --> 00:33:14.400 align:middle line:84%
It's kind of
highfalutin language.

00:33:14.400 --> 00:33:16.410 align:middle line:84%
Sometimes I'll slip,
and I'll say universe,

00:33:16.410 --> 00:33:18.810 align:middle line:90%
but I don't mean to.

00:33:18.810 --> 00:33:21.240 align:middle line:84%
Systems plus surroundings--
energy of system plus

00:33:21.240 --> 00:33:22.620 align:middle line:90%
surroundings is constant.

00:33:22.620 --> 00:33:26.740 align:middle line:90%


00:33:26.740 --> 00:33:28.940 align:middle line:90%
But here's where it gets useful.

00:33:28.940 --> 00:33:36.360 align:middle line:84%
We use the boundary
for bookkeeping.

00:33:36.360 --> 00:33:41.110 align:middle line:90%


00:33:41.110 --> 00:33:47.840 align:middle line:84%
And like it or not, a lot
of thermo is bookkeeping.

00:33:47.840 --> 00:33:59.160 align:middle line:84%
So we have a system,
we have a boundary,

00:33:59.160 --> 00:34:03.460 align:middle line:90%
and we have flows of energy.

00:34:03.460 --> 00:34:05.230 align:middle line:84%
I mean, you can
keep track of them.

00:34:05.230 --> 00:34:08.219 align:middle line:84%
And we can keep track of the
forms that energy can flow.

00:34:08.219 --> 00:34:10.230 align:middle line:84%
So there are three
ways that energy

00:34:10.230 --> 00:34:14.840 align:middle line:84%
can flow between a system
and the surroundings in 3020.

00:34:14.840 --> 00:34:17.593 align:middle line:84%
We have encountered two of them
so far about 20 minutes ago.

00:34:17.593 --> 00:34:19.760 align:middle line:84%
Somebody want to tell me
what the three of them are,

00:34:19.760 --> 00:34:20.360 align:middle line:90%
all three?

00:34:20.360 --> 00:34:25.050 align:middle line:90%


00:34:25.050 --> 00:34:28.830 align:middle line:84%
STUDENT: Convection,
radiation, and conduction.

00:34:28.830 --> 00:34:29.850 align:middle line:90%
Nope.

00:34:29.850 --> 00:34:34.350 align:middle line:84%
Sorry, so those are
forms of heat transfer.

00:34:34.350 --> 00:34:40.090 align:middle line:84%
But we are not going to
talk about fluid dynamics

00:34:40.090 --> 00:34:44.710 align:middle line:84%
or radiative processes
in any detail in 020.

00:34:44.710 --> 00:34:47.050 align:middle line:84%
So what you said was
scientifically true.

00:34:47.050 --> 00:34:49.600 align:middle line:84%
It's not specifically what
the three forms are in 020.

00:34:49.600 --> 00:34:53.120 align:middle line:84%
RAFAEL JARAMILLO: We've talked
about two of them so far.

00:34:53.120 --> 00:34:56.572 align:middle line:84%
One is heat, which is
everything you just described.

00:34:56.572 --> 00:34:58.030 align:middle line:84%
What's another way
energy can flow?

00:34:58.030 --> 00:35:00.690 align:middle line:90%


00:35:00.690 --> 00:35:01.400 align:middle line:90%
STUDENT: Work.

00:35:01.400 --> 00:35:04.880 align:middle line:84%
RAFAEL JARAMILLO: Work,
heat, work, mechanical work.

00:35:04.880 --> 00:35:08.082 align:middle line:84%
And there's a third way
that energy can flow.

00:35:08.082 --> 00:35:09.290 align:middle line:90%
We haven't introduced it yet.

00:35:09.290 --> 00:35:11.840 align:middle line:84%
Would anyone likes
to venture a guess?

00:35:11.840 --> 00:35:12.975 align:middle line:90%
STUDENT: Mass transfer.

00:35:12.975 --> 00:35:14.600 align:middle line:84%
RAFAEL JARAMILLO:
Mass transfer, right.

00:35:14.600 --> 00:35:16.260 align:middle line:90%
Matter has energy.

00:35:16.260 --> 00:35:20.438 align:middle line:84%
And so you can exchange matter
and transfer energy that way.

00:35:20.438 --> 00:35:21.980 align:middle line:84%
So this is the
bookkeeping that we're

00:35:21.980 --> 00:35:23.940 align:middle line:90%
going to do in this class.

00:35:23.940 --> 00:35:27.154 align:middle line:84%
So this gets me to first
law of bookkeeping.

00:35:27.154 --> 00:35:36.050 align:middle line:90%


00:35:36.050 --> 00:35:38.810 align:middle line:84%
I wish I had a week to
teach fluid dynamics

00:35:38.810 --> 00:35:43.910 align:middle line:84%
and talk about convection and
then talk about heat transfer,

00:35:43.910 --> 00:35:46.520 align:middle line:84%
talk about conduction,
and do radiative.

00:35:46.520 --> 00:35:49.538 align:middle line:84%
But that goes well
beyond this class.

00:35:49.538 --> 00:35:51.580 align:middle line:84%
You'll learn about those
things in other classes.

00:35:51.580 --> 00:35:54.490 align:middle line:84%
Or come to office hours, we
can talk about heat transfer.

00:35:54.490 --> 00:36:02.320 align:middle line:84%
First law bookkeeping-- this is
where we hopefully resolve some

00:36:02.320 --> 00:36:06.400 align:middle line:84%
ambiguity about 020 with the
other classes you've taken.

00:36:06.400 --> 00:36:17.050 align:middle line:84%
So types of energy include
kinetic, potential,

00:36:17.050 --> 00:36:24.340 align:middle line:90%
and internal, which we u.

00:36:24.340 --> 00:36:31.330 align:middle line:84%
So kinetic energy depends on
how fast a system is moving.

00:36:31.330 --> 00:36:33.110 align:middle line:90%
You know that.

00:36:33.110 --> 00:36:36.760 align:middle line:84%
So if your system is a
baseball, kinetic energy

00:36:36.760 --> 00:36:38.290 align:middle line:90%
is how fast it's moving.

00:36:38.290 --> 00:36:43.870 align:middle line:84%
Potential energy depends
on where a system

00:36:43.870 --> 00:36:46.900 align:middle line:90%
is in some reference frame.

00:36:46.900 --> 00:36:48.790 align:middle line:84%
So again, if your
system is a baseball,

00:36:48.790 --> 00:36:50.920 align:middle line:84%
the potential energy
depends on where

00:36:50.920 --> 00:36:53.500 align:middle line:84%
it is, relative to the
center of mass of the Earth.

00:36:53.500 --> 00:36:56.620 align:middle line:90%


00:36:56.620 --> 00:36:59.920 align:middle line:84%
Internal energy is
everything else.

00:36:59.920 --> 00:37:03.250 align:middle line:84%
It's all of the energy which
is independent of the velocity

00:37:03.250 --> 00:37:06.140 align:middle line:84%
of the system and independent
of the location of the system.

00:37:06.140 --> 00:37:08.200 align:middle line:84%
So again, if your
system is the baseball,

00:37:08.200 --> 00:37:11.170 align:middle line:84%
the internal energy is
all the molecular bonds

00:37:11.170 --> 00:37:17.760 align:middle line:84%
that make up the baseball
plus the binding energy

00:37:17.760 --> 00:37:21.370 align:middle line:90%
of the electrons to the nuclei.

00:37:21.370 --> 00:37:24.510 align:middle line:84%
So this is the one
that we use in thermo.

00:37:24.510 --> 00:37:26.850 align:middle line:84%
This is the last time we'll
talk about kinetic energy

00:37:26.850 --> 00:37:29.460 align:middle line:84%
in the last time we'll talk
about potential energy.

00:37:29.460 --> 00:37:33.090 align:middle line:84%
We might get to a 20
minutes of electrochemistry

00:37:33.090 --> 00:37:34.195 align:middle line:90%
later in the term.

00:37:34.195 --> 00:37:35.820 align:middle line:84%
And then potential
might sneak back in.

00:37:35.820 --> 00:37:43.720 align:middle line:84%
But basically, this is
where we are for 3020.

00:37:43.720 --> 00:37:56.680 align:middle line:84%
What about processes
that exchange energy?

00:37:56.680 --> 00:37:58.560 align:middle line:84%
That would just be,
we just answered.

00:37:58.560 --> 00:38:07.845 align:middle line:84%
There's heating, there's work,
and there's mass transfer.

00:38:07.845 --> 00:38:16.502 align:middle line:90%


00:38:16.502 --> 00:38:18.210 align:middle line:84%
So this is some first
law of bookkeeping.

00:38:18.210 --> 00:38:23.970 align:middle line:84%
I hope this helps a little bit
as we try to recall what counts

00:38:23.970 --> 00:38:26.070 align:middle line:84%
and what doesn't in
equilibrium thermo.

00:38:26.070 --> 00:38:30.360 align:middle line:90%


00:38:30.360 --> 00:38:34.980 align:middle line:84%
So we can do this
mathematically.

00:38:34.980 --> 00:38:39.700 align:middle line:84%
Energy is a state function,
but it's changed by processes.

00:38:39.700 --> 00:38:48.550 align:middle line:84%
So du equals change
in heat energy

00:38:48.550 --> 00:39:00.265 align:middle line:84%
plus change in mechanical
work plus something new,

00:39:00.265 --> 00:39:03.165 align:middle line:84%
a term which accounts
for a change in mass.

00:39:03.165 --> 00:39:06.020 align:middle line:90%


00:39:06.020 --> 00:39:16.950 align:middle line:84%
So dq equals heat
applied to the system.

00:39:16.950 --> 00:39:18.730 align:middle line:90%
There's a sign convention here.

00:39:18.730 --> 00:39:21.120 align:middle line:84%
We're going to follow the
sign convention in the DeHoff

00:39:21.120 --> 00:39:21.620 align:middle line:90%
textbook.

00:39:21.620 --> 00:39:23.990 align:middle line:90%


00:39:23.990 --> 00:39:26.800 align:middle line:84%
So if you're heating
a system, let's say

00:39:26.800 --> 00:39:30.280 align:middle line:84%
that's the endothermic
reaction, the instant cold pack,

00:39:30.280 --> 00:39:34.150 align:middle line:90%
then dq is positive.

00:39:34.150 --> 00:39:44.695 align:middle line:84%
Dw is work performed
on a system.

00:39:44.695 --> 00:39:47.680 align:middle line:90%


00:39:47.680 --> 00:39:50.190 align:middle line:84%
So there's a consistent
convention there.

00:39:50.190 --> 00:39:53.070 align:middle line:90%
These have the same sign.

00:39:53.070 --> 00:39:55.320 align:middle line:84%
Positive dq increases
the energy of the system,

00:39:55.320 --> 00:39:57.495 align:middle line:84%
positive dw increases
the energy of the system.

00:39:57.495 --> 00:40:02.020 align:middle line:90%


00:40:02.020 --> 00:40:07.240 align:middle line:84%
So for example,
for mechanical work

00:40:07.240 --> 00:40:16.690 align:middle line:84%
that we encounter in this class,
dw equals P dV, and here I ask

00:40:16.690 --> 00:40:19.075 align:middle line:90%
is it positive or minus?

00:40:19.075 --> 00:40:23.480 align:middle line:90%


00:40:23.480 --> 00:40:24.230 align:middle line:90%
Which one is it?

00:40:24.230 --> 00:40:27.955 align:middle line:90%


00:40:27.955 --> 00:40:28.830 align:middle line:90%
This is the pressure.

00:40:28.830 --> 00:40:32.880 align:middle line:84%
This is the change in
volume of a system.

00:40:32.880 --> 00:40:37.260 align:middle line:84%
So a positive P dV means
the system is doing work

00:40:37.260 --> 00:40:38.130 align:middle line:90%
on the surroundings.

00:40:38.130 --> 00:40:41.500 align:middle line:84%
It's expanding against
the surroundings.

00:40:41.500 --> 00:40:43.200 align:middle line:84%
So what should be the
sign here to stick

00:40:43.200 --> 00:40:46.170 align:middle line:90%
with our new convention?

00:40:46.170 --> 00:40:47.220 align:middle line:90%
STUDENT: Negative.

00:40:47.220 --> 00:40:49.770 align:middle line:84%
RAFAEL JARAMILLO: Negative
right, it's negative.

00:40:49.770 --> 00:40:54.690 align:middle line:84%
Because the system is losing
energy as it expands, negative.

00:40:54.690 --> 00:40:58.670 align:middle line:90%
So it equals minus P dV.

00:40:58.670 --> 00:41:02.860 align:middle line:90%


00:41:02.860 --> 00:41:04.940 align:middle line:84%
A little mathematical
note here--

00:41:04.940 --> 00:41:08.120 align:middle line:90%
this is a process variable.

00:41:08.120 --> 00:41:11.060 align:middle line:90%


00:41:11.060 --> 00:41:13.765 align:middle line:90%
This is a state variable.

00:41:13.765 --> 00:41:17.205 align:middle line:90%


00:41:17.205 --> 00:41:18.580 align:middle line:84%
This is not an
equation of state.

00:41:18.580 --> 00:41:21.170 align:middle line:84%
This is a differentiable
form of an equation of state.

00:41:21.170 --> 00:41:23.450 align:middle line:90%
So it's not the same thing.

00:41:23.450 --> 00:41:26.810 align:middle line:84%
But it has this funny property,
that you have on the one hand,

00:41:26.810 --> 00:41:29.300 align:middle line:84%
process variable, on the
other hand, is state variable.

00:41:29.300 --> 00:41:35.670 align:middle line:84%
This could be considered
an integration constant.

00:41:35.670 --> 00:41:40.793 align:middle line:90%


00:41:40.793 --> 00:41:43.210 align:middle line:84%
If you don't care about that
comment, ignore that comment.

00:41:43.210 --> 00:41:45.130 align:middle line:84%
We don't really talk
about integration concepts

00:41:45.130 --> 00:41:46.390 align:middle line:84%
in this class, we
don't have time.

00:41:46.390 --> 00:41:47.765 align:middle line:84%
But they are kind
of hidden there

00:41:47.765 --> 00:41:49.600 align:middle line:90%
and the structure of thermo.

00:41:49.600 --> 00:42:05.350 align:middle line:84%
All right so dq/dw and mu
i dNi equals the energy

00:42:05.350 --> 00:42:18.976 align:middle line:84%
of change dNi of
moles of component i

00:42:18.976 --> 00:42:21.350 align:middle line:84%
where i has to run over all
the different components

00:42:21.350 --> 00:42:22.680 align:middle line:90%
of the system.

00:42:22.680 --> 00:42:30.305 align:middle line:84%
So N of i equals number
moles of component i.

00:42:30.305 --> 00:42:34.250 align:middle line:90%


00:42:34.250 --> 00:42:44.070 align:middle line:84%
And mu of i is defined as
partial u, partial N of i,

00:42:44.070 --> 00:42:45.030 align:middle line:90%
for a fixed--

00:42:45.030 --> 00:42:46.440 align:middle line:90%
and we'll get to this--

00:42:46.440 --> 00:42:55.150 align:middle line:84%
entropy, volume, and
moles of j not equal to i.

00:42:55.150 --> 00:42:57.270 align:middle line:90%
I is a component label.

00:42:57.270 --> 00:43:03.860 align:middle line:90%


00:43:03.860 --> 00:43:12.350 align:middle line:84%
And this whole thing is
called the chemical potential,

00:43:12.350 --> 00:43:15.760 align:middle line:84%
which is a really central
concept for material science

00:43:15.760 --> 00:43:18.250 align:middle line:90%
and chemical engineering.

00:43:18.250 --> 00:43:23.650 align:middle line:84%
So we will be spending an entire
term on the chemical potential.

00:43:23.650 --> 00:43:27.570 align:middle line:84%
That's where I wanted
to get to today.

00:43:27.570 --> 00:43:30.000 align:middle line:90%