- [Instructor] We're told that six identical
potato core cubes were isolated from a potato.
The initial weight of each cube was recorded.
Each cube was then placed in one of six open beakers,
each containing a different sucrose solution.
The cubes remained in the beakers for 24 hours
at a constant temperature of 23 degrees Celsius.
After 24 hours, the cubes were removed
from the beakers, blotted, and reweighed.
The percent change in mass,
due to a net gain or loss of water,
was calculated for each cube,
and the results are shown in the graph to the right,
so, this graph right over here.
A straight line is drawn
on the graph to help estimate results
from other sucrose concentrations not tested.
Using the straight line on the graph,
calculate the water potential, in bars,
of the potato core cubes at 23 degrees Celsius.
Give your answer to one decimal place.
So, pause this video and see if you can work that out.
All right, so, first, let's just make sure
we're understanding what's going on here.
So, there was a potato.
We took six cubes from that potato
and we stuck those six cubes
into six different sucrose molarity solutions,
and so, this data point right over here,
this was the situation where we took one of the cubes,
so, this was a sucrose solution.
This was a solution, actually, that contained no sucrose,
and so, when we put the cube in that solution,
we saw a net gain of mass.
It looks like it's about 22% gain in mass,
and so, that would have happened
because water would have flowed into the cube.
Now, at the other extreme, right over here,
this is a solution that has a lot of sucrose.
It had a very high sucrose concentration,
and when we put a cube in there,
we see that the mass of that cube went down by 25%,
and that would have been
because of the net outflow of water from that cube.
So, how do we figure out the water potential
of the core cubes at 23 degrees Celsius?
Well, we could think about a situation
where there's some sucrose concentration where,
if the cube and the sucrose solution
have the same water potential,
then you're not going to have any net inflow or outflow,
and so, where do we see that on the graph?
Well, what we'd wanna do, we have that line
where they're trying to fit the data points,
and so, where would we expect to see 0% change in mass?
So, we would go right over here to 0% change in mass.
We would go to the line right over there,
and then, we see that this line would say
that there's a 0% change in mass.
See, if this is 0.4 right over here,
this is 0.5 right over here,
so, this is about a 0.44 molar sucrose solution,
0.44 molar solution.
So, if we can figure out the water potential
of this 0.44 molar sucrose solution,
well, that's also going to be
the water potential of the potato cubes.
Well, how do we do that?
Well, we've seen the equation before
where we introduced ourselves
to the idea of water potential,
that water potential, using the Greek letter psi,
is going to be equal to the solute potential
plus the pressure potential.
Now, we're dealing with all open containers.
We don't have anything that's some piston
or something that's pressing down on these containers,
and so, because of that,
the pressure potential is going to be equal to zero,
and so, we just have to figure out the solute potential.
So, the solute potential, we have introduced ourselves
to this formula in previous videos.
It's negative i times C times R times T.
This i right over here, this is our ionization constant.
This is, since we're dealing with sucrose solutions,
it says okay, if I took sucrose and put it into water,
every one of those sucrose molecules,
does it stay one molecule, or does it disassociate?
Well, sucrose doesn't disassociate at all.
It just stays one molecule, so, this would be one.
If we were dealing with, say, sodium chloride,
each sodium chloride molecule would disassociate
into a sodium ion and a chloride ion,
and so, then, this would be two,
but this was one for sucrose.
C is the molarity of our solution,
and so, we estimated that to be 0.44,
so, let me write this down.
Our solute water potential is going
to be equal to negative one times 0.4,
0.44, I should say, and that's going to be moles.
I'll write out all the units.
Moles per liter times, it's sometimes called
the pressure constant in this context,
but this is also the universal gas constant,
and if you were doing something like the AP exam,
they would give you what this is.
So, this is 0.0831 liters times bars,
all of that over mole Kelvin.
If you're used to seeing other values of this,
it's probably because they're dealing
with other units right over here,
but this is the universal gas constant.
And then, we have to multiply that times
the temperature that we're dealing with in Kelvin.
Now, it's 23 degrees Celsius.
To convert to Kelvin, we just add to 273,
so, 273 plus 23 is going to be 296, 296 Kelvin,
and so, this is going to be equal to,
we have a negative here, and we could look at the units.
We have the liter canceling out liters,
moles canceling out with moles,
Kelvin canceling out with Kelvin,
so, we're going to get something in bars, which makes sense.
That is the unit for our water potential.
And then, we get the calculator out.
So, we have 0.44 times 0.831 times 296, 296,
is equal to, and they want us
to round our answer to one decimal place,
so, approximately 10.8,
and we already had that negative out front,
so, negative 10.8 bars, and we're done.