00:00:15
>> Heads up of
where we are.
00:00:18
We're starting a new
chapter this morning,
00:00:21
Chapter 5, which is the
00:00:24
last of the four chapters
on heat conduction.
00:00:27
We are going to
finish about half
00:00:30
of that this morning
and the rest
00:00:31
of it on Monday after
our first mid-term.
00:00:35
This chapter is titled
Transient Conduction.
00:00:41
So now time becomes
00:00:44
one of the variables
in our solution.
00:00:47
We go back to Chapter
2 in general,
00:00:52
to get the heat
diffusion equation
00:00:54
in two dimensions.
00:00:55
We write it here for
00:00:57
constant properties
with no generation.
00:01:00
So this is the heat
diffusion equation from
00:01:02
Chapter 2 with
00:01:03
constant property
with no generation.
00:01:06
If we could solve this with
00:01:09
correct initial and
boundary conditions,
00:01:12
we would get the
temperature as
00:01:14
a function of
x, y, and time.
00:01:16
Now it can be rather
difficult, but luckily,
00:01:23
there is a possibility
we can use
00:01:26
a simpler model
to get results.
00:01:30
This model is called the
00:01:32
lumped heat capacity
model, abbreviated LHC.
00:01:36
Lumped Heat Capacity.
00:01:39
Here's what the model says,
00:01:41
take a body initially
at a temperature T_i,
00:01:45
initial temperature,
at time zero, T_i.
00:01:49
Let's say it
starts out hot,
00:01:51
just to talk
about something.
00:01:52
It starts out hot.
00:01:54
We blow a cool fluid
00:01:57
over it at T_infinity with
00:01:59
a convection coefficient
on the surface
00:02:01
of H. With time,
00:02:05
the body starts to cool.
00:02:06
Starts out hot, blow
cool fluid over it,
00:02:10
temperature of the body
starts to decline.
00:02:12
We're going to assume with
00:02:15
the simple model that
00:02:16
the temperature does not
00:02:17
vary inside the
body with x and y,
00:02:20
but it only
varies with time.
00:02:23
So now time is
not a function,
00:02:27
or temperature is not
00:02:28
a function of
x, y and time.
00:02:30
Now temperature is only
a function of time.
00:02:36
We're not going to solve
00:02:39
the differential
equation now.
00:02:41
Instead, we're
going to write
00:02:44
an energy balance
on this object.
00:02:48
So go back to the
end of Chapter 1,
00:02:54
energy balance on
a control volume.
00:02:56
E dot_in minus E dot_out
00:02:59
minus E dot_g equal
E dot_storage.
00:03:02
Problem said no generation.
00:03:05
E dot_g, zero.
00:03:08
I'm looking at the model
00:03:10
where the object starts
00:03:11
out hot is going to be
00:03:13
cooled by a colder fluid.
00:03:14
So nothing comes in,
00:03:17
but energy does go
up by convection.
00:03:21
There is a
convection leaving.
00:03:23
What happens in?
00:03:25
The body has a change
in stored energy.
00:03:28
We're taking energy
out of the body
00:03:30
by the cool fluid
blowing over it.
00:03:34
So we can then write down
00:03:37
what the convection is
00:03:39
and the change in
stored energy.
00:03:42
So we have our
convection minus
00:03:45
hA_s and T minus
T_infinity.
00:03:53
Just to review Chapter 1,
00:03:56
convection heat transfer,
00:03:57
Newton's Law of Cooling.
00:03:59
Equal the time rate
00:04:02
of change of stored energy,
00:04:04
Rho cVdT, dtime.
00:04:12
Capital V is the volume.
00:04:16
Rho times the
volume is the mass.
00:04:19
The mass times c gives me
00:04:22
a measure of
how much energy
00:04:24
the object can store.
00:04:25
Mass times c,
specific heat.
00:04:29
Units of the equation there
00:04:32
are in Watts,
both sides Watts.
00:04:35
To simplify matters, we let
00:04:39
Theta equal T
minus T_infinity.
00:04:45
Put that in the
above equation then.
00:04:48
Well, what happens,
of course,
00:04:49
is d Theta dt is
equal to dt, dt.
00:04:57
Because a differential of a
00:04:59
constant,
T_infinity is zero.
00:05:02
Put that up there.
00:05:07
Write it down,
d Theta over t.
00:05:24
There's our little
differential equation.
00:05:28
The initial condition is
00:05:36
when t equals zero,
T equals T_i.
00:05:41
So Theta is equal to
T_i minus T_infinity,
00:05:47
and we call that Theta_i.
00:05:49
So when time equals zero,
00:05:52
Theta equal Theta_i,
a constant.
00:05:55
Solve then Theta
over Theta_i,
00:06:26
and we get that
solution for
00:06:29
temperature of the object
00:06:30
as a function of time.
00:06:32
Now, just to remind you
00:06:34
what Theta over Theta_i is.
00:06:46
So Theta over Theta_i
00:06:49
is a measure of
the temperature.
00:06:59
If we want then
we could plot
00:07:01
a curve of Theta
00:07:05
over Theta_i from
zero to one.
00:07:13
This is time.
00:07:15
Start at one.
00:07:18
There's different curves,
parametric values.
00:07:23
Each particular curve is
00:07:26
a different value of the
time constant called
00:07:31
Tau, is in seconds.
00:07:49
It's Rho cV over hAs.
00:07:55
So if you want,
00:07:57
I'll just add this to it.
00:07:59
You might want to
express this as exp,
00:08:03
it's the simplified
form of this
00:08:05
then minus t over Tau.
00:08:21
>> We engineers love the
dimensionless stuff.
00:08:25
So this is
00:08:27
a dimensionless temperature
difference ratio.
00:08:30
This is dimensionless,
00:08:33
T over tau is
dimensionless.
00:08:35
T is in seconds,
00:08:36
tau is and seconds,
dimensionless,
00:08:38
so we like to
express things very
00:08:39
simply and lot of
00:08:41
times that's in
dimensionless form.
00:08:44
This is called the
time constant tau.
00:08:50
Now, let's just for
00:08:56
sake of talking
about something.
00:08:57
Let's just take
a copper sphere
00:09:00
six centimeters
in diameter.
00:09:01
I don't know if that
size is a baseball size,
00:09:04
six centimeters
in diameter,
00:09:07
initially, at 300
degrees Fahrenheit,
00:09:10
that's Ti 300, I'm
00:09:15
going to blow air over
00:09:17
it at 30 degrees
Celsius not Fahrenheit.
00:09:20
let's just say 70
degrees Fahrenheit,
00:09:22
make it English units.
00:09:25
So 300 degrees
Fahrenheit initial,
00:09:28
and now T infinity, 30
degrees Fahrenheit.
00:09:31
I blow air over
it. Of course,
00:09:32
the temperature's going
to drop with time.
00:09:34
How? Exponentially.
Yeah, drop
00:09:38
with time exponentially.
00:09:39
But these three curves,
00:09:41
let's say you take
that copper sphere
00:09:43
and put it in this
room on a stand
00:09:45
at 300 Fahrenheit and
00:09:49
the air newsroom
is really still.
00:09:51
Nobody's air's blowing,
00:09:53
air in the room
is really still.
00:09:56
H is going to
be really low,
00:09:59
time constant may
be really high.
00:10:03
This arrow means
00:10:05
high time constants,
low time constants.
00:10:07
The direction of
the arrow tells me.
00:10:09
Increasing time constant
curves this way.
00:10:11
So copper sphere
in this room,
00:10:14
it cools real slow.
00:10:18
Now, I put a floor
fan in front
00:10:21
of it, turn the
floor fan on.
00:10:23
The air blows
by really fast.
00:10:25
H becomes really big: H,
00:10:29
really big, time
constant, really small.
00:10:32
Boy, the temperature drops
00:10:33
really fast to that
copper sphere.
00:10:35
So that's the story
00:10:37
this graph is
trying to tell you.
00:10:38
You can say, "What if
the density is bigger?"
00:10:41
"What if the surface
area is smaller?"
00:10:44
You can play the same game
00:10:45
with all these
variables. So there
00:10:50
is the temperature
variation with time,
00:10:54
very simple, because it's
00:10:57
the simplest
possible model that
00:10:59
we can use in
transient studies.
00:11:02
But now we say, "Yeah,
00:11:03
but when can we use it?"
00:11:06
Well, when we can use
00:11:08
it is when something
special happens.
00:11:11
This lumped heat
capacity model
00:11:18
can be used when
00:11:22
a dimensionless parameter
00:11:25
called the Biot number,
00:11:31
defined as hlc over K
is less than one-tenth.
00:11:43
If that's satisfied, we
can take the easy way
00:11:47
out and model the problem
00:11:49
as a lumped heat
capacity model.
00:11:52
What is l sub c?
00:11:55
L sub c is called a
characteristic length.
00:12:06
It's the volume of
00:12:09
the object divided
by its surface area,
00:12:13
the area touching the
00:12:14
fluid cooling the object.
00:12:21
So there's some
simple geometries.
00:12:25
We'll put those geometries
00:12:26
up on the board here.
00:12:28
The first one is
a plane wall.
00:12:59
This particular plane wall
00:13:02
has convection
on both sides.
00:13:18
The wall is 2L thick.
00:13:22
X is measured from the
00:13:24
centerline of the wall.
00:13:25
On both sides of the wall,
00:13:28
we have convection to
a fluid at T infinity,
00:13:37
with a convection
coefficient of
00:13:40
h. L sub c
00:13:50
is equal to L.
00:13:55
It's called the
half thickness.
00:14:07
Another common geometry is
00:14:10
a cylinder whose radius
00:14:20
is r note.
00:14:22
Again, it has a fluid
blowing over it at
00:14:26
T infinity with a
convection coefficient
00:14:29
of h on the surface.
00:14:35
For this case, L sub C
00:14:39
equal the radius
divided by 2.
00:14:42
Now, we have a sphere.
00:14:53
Again, we have a
fluid blowing over
00:14:56
the sphere at
temperature T infinity,
00:14:59
with a convection
coefficient h
00:15:01
on the surface
of the sphere.
00:15:04
L sub c equal
or not over 3.
00:15:14
So those are three
common geometries
00:15:19
that we engineers study.
00:15:21
I'll tell you later
on to give you
00:15:23
some idea of what they
really couldn't be,
00:15:26
but for right
now, plane wall,
00:15:29
a cylinder, and a sphere.
00:15:37
Biot number, hlc
over K. Here's LC.
00:15:42
I don't care what
the object is,
00:15:45
you can find LC part.
00:15:48
For instance, what if I had
00:15:52
a cube of aluminum,
00:16:01
each side a, L sub c,
00:16:09
volume over surface area.
00:16:12
Volume a cubed.
How many sides?
00:16:16
Six. What's one
side? A squared.
00:16:22
L sub c, length of one
side divided by six.
00:16:26
That's what goes in
the Biot number.
00:16:29
So for any object,
00:16:30
it's the volume divided
00:16:32
by the surface area
touching the fluid.
00:16:37
Well, that's
half the story.
00:16:42
We know the full story.
00:16:43
The full story is,
00:16:44
once we get the
temperature of an object,
00:16:46
whether it's of
temperatures of function of
00:16:48
the geometry or of time,
00:16:51
the second thing is find
out something about
00:16:53
how much heat transfer
00:16:54
has occurred by convection,
00:16:56
or how much energy the body
00:16:58
has lost by convection.
00:17:02
So now, we want to
00:17:04
find the energy
lost by the body.
00:17:29
How is that energy
lost by the body?
00:17:31
Well, convection to the
fluid takes it out.
00:17:34
Now, it could
be the reverse.
00:17:36
Hot gas, initial
temperature low.
00:17:38
You heat the body.
00:17:39
Doesn't matter either way.
00:17:43
So Q equal integral
zero to time t,
00:17:51
Rho hAs, and then we
have our Theta d time.
00:18:04
Convection, by convection,
00:18:07
here's convection,
Newton's law,
00:18:09
h A Delta t.
00:18:11
Theta is Delta t. T
minus t infinity.
00:18:18
Dt, time integrate
with respect to time.
00:18:22
Where you see
Theta in here,
00:18:25
put the boxed
equation right there,
00:18:28
put that right
there, into there,
00:18:31
and integrate the
exponential function.
00:18:36
Just so you know,
the Newton's law
00:18:39
h A Delta t is in watts.
00:18:42
A watt is a joule
per second.
00:18:46
What's this guy here?
00:18:48
Seconds. When I
multiply joules
00:18:50
per second times
seconds, I get joules.
00:18:54
Capital Q is joules,
00:19:00
little q is watts.
00:19:04
Q in joules is energy,
00:19:07
and of course, watts is
00:19:09
the heat transfer,
the power watts.
00:19:12
So now, we've got two Qs,
00:19:14
a capital Q and
a lowercase q.
00:19:17
You talk about energy,
00:19:19
you talk about capital Q.
00:19:20
You talk about
heat transfer,
00:19:22
you talk about little q.
00:19:24
Put those guys in there,
00:19:26
do the integration,
I get q.
00:19:55
>> So there are the
two equations that
00:19:59
we need to solve.
00:20:09
So let's see
what I got here.
00:20:14
Any questions before
we go on now?
00:20:21
Wait, let me think
here. Here it is.
00:20:26
So we're going to
then take an example.
00:20:29
The example that
I'm going to
00:20:31
work is a copper sphere.
00:20:34
Let's put that on
the middle here.
00:20:36
So we're going to look at
00:20:38
a copper sphere
being cooled by air.
00:20:46
I might need him. I'll
leave him up here.
00:21:13
Diameter is 15 centimeters.
00:21:22
Initial temperature of 300.
00:21:30
Air temperature,
T_infinity, 30 degrees
00:21:34
C. Properties at T_average.
00:21:56
You don't want to
take the properties
00:21:58
at their starting
temperature.
00:22:00
You don't know what the
final temperature is.
00:22:04
So probably your best
guess is to take
00:22:07
the properties at the
average temperature,
00:22:10
starting temperature
plus air temperature.
00:22:12
Once you've solved
the problem,
00:22:14
go back and put
00:22:16
the right final
temperature in there.
00:22:20
I want to know how
00:22:21
the temperature
varies with time.
00:22:23
So find T as a
function of time.
00:22:29
I'll put the properties
down for copper.
00:22:55
Step 1, Chapter
5, check Biot.
00:23:01
Maybe you get lucky and
the Biot's less than
00:23:04
one-tenth and you can
00:23:06
use this model,
the simple model.
00:23:08
Biot equal hl_c
over k. H, 25;
00:23:19
k, 393; l_c from the
table geometry a sphere,
00:23:26
l_c, one-third the
radius, the radius,
00:23:30
seven and a half,
0.20 is 159,
00:23:43
which is a lot less
than one-tenth.
00:23:46
So we can use lumped
heat capacity.
00:23:54
First [inaudible]
done. I get
00:23:56
the easy about this time.
00:23:59
Here's the equation
in the box.
00:24:01
There's the equation.
00:24:28
If I want to find the
time constant Tau,
00:24:36
time constant Rho c
00:24:42
over h r_naught
over three l_c.
00:24:51
V Over As is l_c.
00:24:56
Put those numbers in there,
00:24:59
I get 3546 seconds.
00:25:05
Time constant's
almost an hour.
00:25:08
It's cooling really slow.
00:25:12
So then I know
everything here.
00:25:16
The properties, I know h,
00:25:17
I know T_infinity,
I know T_i.
00:25:19
So T as a function
00:25:21
of t then when you
put the numbers in,
00:25:36
put T in seconds,
00:25:39
and the time will come
out to be degrees
00:25:41
C. So that's my
solution then.
00:25:57
Now, if somebody asked me,
00:26:00
by the way, in the
first five minutes,
00:26:09
how much energy is lost
by the copper sphere?
00:26:12
I say, okay,
here's over here.
00:26:15
The first five minutes,
00:26:17
60 seconds per
minute times 5,
00:26:21
300 for T. I know that,
00:26:24
I know that. I know that.
00:26:25
I know that. I know Tau.
00:26:27
I just found Tau.
Put it in here.
00:26:29
So many joules of energy is
00:26:32
how much energy the sphere
00:26:34
has lost to the air.
00:26:36
Now you say, well,
00:26:37
how much heat transfer
has occurred?
00:26:41
How much energy has
going out by convection?
00:26:45
It's the same answer.
00:26:47
The change in
internal energy
00:26:49
is the same as the amount
00:26:50
of energy lost by
00:26:52
convection. Says
it right here.
00:26:54
Change in storage
is the same as
00:26:57
how much energy goes out
00:26:58
of the body by convection.
00:27:04
Any questions on that then?
00:27:07
So now of course the
obvious question is,
00:27:11
what if the Biot is
greater than one-tenth?
00:27:14
Now we got
00:27:14
much more difficulty
mathematically.
00:27:17
That's going to be Monday.
00:27:19
We'll save that
one for Monday.
00:27:21
So I want to go over
00:27:24
some things about
00:27:25
the midterm on
Friday with you.
00:27:26
So let's do that right now.
00:27:28
Any questions
before I erase
00:27:29
any of this? Yes.
00:27:32
>> Where did we get
the two [inaudible].
00:27:34
>> Which one now, here?
00:27:36
It's this guy here,
300 minus 30.
00:27:43
Let's take a look then,
00:27:46
a little bit of review.
00:27:48
It's going to be not
in great detail,
00:27:51
but just to jog
your memory of what
00:27:54
could occur on the
first midterm.
00:27:57
So here we have Chapter
1. Is Elizabeth here?
00:28:08
In front here
when were done,
00:28:10
a paper for you.
00:28:12
Let's take a look
and see Chapter 1.
00:28:17
Fourier's Law, Newton's
law, convection.
00:28:29
Fourier's law, KA over
00:28:34
L Delta T. Newton's law,
00:28:36
HAS Delta T. Radiation.
00:28:45
Small object in a
large surroundings.
00:28:50
Epsilon Sigma AT object
00:28:55
to the fourth minus
00:28:56
t surroundings
to the fourth.
00:28:59
That's for a black
body, Epsilon is 1.
00:29:03
Alpha, that's the
emissivity, is 1.
00:29:07
The Epsilon activity Alpha,
00:29:09
if you multiply the solar
input on the street
00:29:12
out there times Alpha
of black asphalt,
00:29:15
then that's how
much is absorbed
00:29:17
by the black asphalt.
00:29:19
Alpha is the absorptivity.
00:29:21
Epsilon is the emissivity.
00:29:27
Then we had,
like over here,
00:29:31
energy balance on
the control volume.
00:29:40
Then we had a surface
energy balance.
00:29:49
That gets us to Chapter 2.
00:29:56
Chapter 2, real short.
00:29:59
But Chapter 2 starts
out with the tables in
00:30:03
the back just to
00:30:11
become familiar with
what's there for you.
00:30:16
What was the solid?
00:30:18
What was the liquid?
00:30:20
What was the gas? At
what temperature?
00:30:23
All that stuff is
in the tables.
00:30:26
Then heat diffusion
equation.
00:30:37
Different versions, the
rectangular version.
00:30:41
There's one of
them right there.
00:30:43
That's the heat
diffusion equation
00:30:45
for constant properties
no generation.
00:30:48
So obviously that should
00:30:50
be on your equation sheets.
00:30:51
Rectangular, cylindrical,
spherical, three equations.
00:31:02
Know how to specify
00:31:04
initial conditions and
boundary conditions
00:31:07
to apply to the partial
00:31:10
or ordinary
differential equation.
00:31:25
>> Okay. That's Chapter 2,
00:31:27
let's go to Chapter 3.
00:31:30
Chapter 3 is our
resistances.
00:31:33
Yeah. We have
conduction resistances.
00:31:53
Again, we have plane
00:32:00
wall, cylindrical,
spherical,
00:32:10
and we have contact
resistance.
00:32:17
Then we have
convection resistance.
00:32:26
Then we put these in
00:32:29
series; parallel, series
parallel, or others.
00:32:51
We had a problem where
the heat input from
00:32:54
a chip came in to
00:32:56
a certain point
and is split,
00:32:58
and some went down,
and some went up.
00:33:00
So that's neither
of these three.
00:33:02
So there's other geometries
00:33:04
that you construct
these circuits.
00:33:12
Okay. Fins; possibly
use Table 3.4.
00:33:22
Fins of a uniform
cross section area.
00:33:25
They give you qf,
00:33:27
and that gives you
the temperature
00:33:29
of the fin as a
function of x.
00:33:37
Maybe you can
use Table 3.5.
00:33:43
Table 3.5 gives you
00:33:48
fin efficiency and then
use that to get qf.
00:34:08
But maybe you
can use Figure
00:34:11
3.19 or maybe Figure 3.20.
00:34:18
They give you a to f,
00:34:21
and put it in that
equation to get qf.
00:34:27
Then maybe you have
00:34:29
multiple fins on a surface.
00:34:39
We had problems like that.
00:34:51
Now we have Chapter 4 then.
00:34:57
Chapter 4, draw
a flux plot,
00:35:06
show the adiabats
and the isotherms.
00:35:20
Find S, conduction
shape factor.
00:35:35
Use it to solve
for heat transfer.
00:35:48
Okay. If you want
a resistance,
00:35:58
the resistance
is 1 over SK.
00:36:22
You can combine
that resistance
00:36:24
with other resistances,
00:36:26
like the convection
resistance, 1 over HA_s.
00:36:30
By the way, this
00:36:32
conduction shape
factor then,
00:36:33
you use q equal SK Delta
00:36:39
T. That's how you put
S in there to get q.
00:36:47
Now, the last half
of Chapter 4,
00:36:50
numerical methods will
not be on the midterm.
00:36:52
So stop there after
00:36:55
the conduction
shape vector, S.
00:37:09
Now, let's talk about
00:37:13
maybe what you should
look at as far
00:37:16
as example problems
in the textbook.
00:37:23
Of course, I told
00:37:25
you before and I'll
tell you again you,
00:37:26
anything I box in the
lecture probably should
00:37:29
be on your equation sheet
00:37:31
because I think it's
an important equation.
00:37:33
But beyond that,
there may be
00:37:35
equations or whatever you
00:37:36
use to solve homework.
00:37:38
If that's important, you
00:37:40
put that on your
equation sheet.
00:37:41
Not just what I
box in class,
00:37:43
but what you use to
solve homework problems.
00:37:46
So here are example
problems in the text.
00:38:02
It depends what textbook
you're looking at.
00:38:05
If it's the Heat
Transfer textbook,
00:38:07
Introduction to
Heat Transfer,
00:38:09
it's going to be
the left-hand side.
00:38:13
If it's the Heat and
Mass Transfer textbook,
00:38:17
it might be
slightly different.
00:38:19
So these are the
example problems
00:38:22
worked in the chapters in
00:38:24
the textbook that I
think probably are
00:38:25
important for you to look
00:38:26
at before the
first midterm;
00:38:29
Chapter 1, Chapter
2, Chapter 3,
00:38:54
Chapter 4.
00:38:56
Now, these same problems
00:38:59
are in the Heat and
Mass Transfer textbook,
00:39:01
but sometimes the
numbers change
00:39:03
because the author
00:39:04
changed a textbook
slightly.
00:39:05
So these are the
ones that are
00:39:07
similar to the
left hand column,
00:39:09
but they're in the Heat
00:39:10
and Mass Transfer textbook,
00:39:12
and it depends which
one you've got in
00:39:13
your hands or
on your laptop.
00:39:19
Most are the same numbers,
00:39:21
but there's a couple
00:39:22
of those slightly
different.
00:39:38
Got it.
00:39:53
Okay. So we've got 1,
00:39:56
2, 3, 4, 5, 6, 7,
00:39:58
8, 9, 10, 11, 12, 13,
00:40:00
14; 2, 4, 7,
00:40:03
9, 1, 3, 4.
00:40:07
Right. 1, 2, 3, 6.
00:40:12
Six, so it should be okay.
00:40:13
I thought I missed
one; 6, 9, 10,
00:40:16
4.1, 3.9, 3.10, 4.1.
00:40:26
Okay. Fifteen in-chapter
worked examples.
00:40:42
You've worked 18
homework problems.
00:40:52
I've worked 21 problems
worked in class.
00:41:07
You've got six previous
exam problems.
00:41:23
So you've got a
library now of
00:41:26
60 problems you can
00:41:28
review for the
first midterm.
00:41:31
If you want to
look at stuff,
00:41:36
that's what you look
at right there.
00:41:39
What's most important?
00:41:42
Well, obviously,
what I asked for
00:41:43
the last two years,
that's that one.
00:41:46
When I assign homework,
00:41:49
why do I assign
certain problems?
00:41:51
Because I think they tell
00:41:52
a really good story.
00:41:53
That's the next
important one.
00:41:55
Why I work in class?
00:41:56
Because I want to go over
00:41:57
that with you to
see if you can
00:41:58
understand what
I'm doing up here
00:41:59
in the board in class.
00:42:01
This one here, this
is worked class,
00:42:05
this in Chapter
1, that's what
00:42:07
the textbook author
thinks are important.
00:42:09
That's all right,
but that's not
00:42:11
number 1 on the list.
00:42:12
This is number 1, this
00:42:14
is number 2, this
is number 3,
00:42:16
and that's number
4, if you've got
00:42:18
prioritize your time
for looking at stuff,
00:42:20
that's what I
would suggest.
00:42:24
Any questions on that then?
00:42:27
You know what
you can bring to
00:42:28
the test on Friday,
00:42:29
what I'm going to
give you one Friday,
00:42:31
so we'll see you
on Friday then.
00:42:33
If you have any questions,
00:42:34
hang on after class,
00:42:35
I'll talk to you about
00:42:36
any questions you have.