WEBVTT

01-01
00:00:00.180 --> 00:00:03.785
Welcome to this practical demonstration of Lab One.

01-02
00:00:03.965 --> 00:00:09.213
In our first classroom session, you began working with the lab
independently.

01-03
00:00:09.393 --> 00:00:16.903
This video now shows the complete workflow, from choosing the system
to saving your results and reopening them.

01-04
00:00:17.083 --> 00:00:21.648
Open the demonstration guide and keep page one beside the lab.

01-05
00:00:21.828 --> 00:00:25.007
Use the Lab One link on this video page.

01-06
00:00:25.187 --> 00:00:30.349
You can pause whenever you need to enter a value or write a
calculation.

01-07
00:00:30.529 --> 00:00:36.268
The two activity stops give you time to make predictions and try a new
pressure yourself.

01-08
00:00:36.448 --> 00:00:41.525
We will study one synthetic ideal binary mixture at a fixed
temperature.

01-09
00:00:41.705 --> 00:00:46.868
Our main question is how pressure changes the liquid and vapor
amounts.

01-10
00:00:47.048 --> 00:00:55.581
We will distinguish composition from amount, check both component
balances, and preserve three cases in a comparison file.

01-11
00:00:55.761 --> 00:00:58.940
The lab contains controls for later topics.

01-12
00:00:59.120 --> 00:01:05.115
For this demonstration, stay with the ideal solution and the pressure
comparison shown here.

01-13
00:01:05.295 --> 00:01:11.460
You do not need the additional model exercises to follow this
first-week workflow.

02-01
00:01:13.990 --> 00:01:18.107
Under Chemical system, choose Teaching binary, synthetic.

02-02
00:01:18.287 --> 00:01:21.594
Under Liquid model, keep Ideal solution.

02-03
00:01:21.774 --> 00:01:27.129
The extra symbols in this option belong to notation used later in the
course.

02-04
00:01:27.309 --> 00:01:30.189
We only need the ideal assumption today.

02-05
00:01:30.369 --> 00:01:41.199
Enter three hundred fifty kelvin for Temperature, ninety-five
kilopascals for Flash pressure, and zero point five for Feed fraction,
z one.

02-06
00:01:41.379 --> 00:01:44.089
Then select Calculate equilibrium.

02-07
00:01:44.269 --> 00:01:50.199
The numerical inputs are preferable to the sliders when reproducing an
exact case.

02-08
00:01:50.379 --> 00:02:02.646
At this temperature, the selected property record defines saturation
pressures of one hundred fifty kilopascals for component A and sixty
kilopascals for component B.

02-09
00:02:02.826 --> 00:02:08.245
These are synthetic teaching values, not measurements of a real
chemical mixture.

02-10
00:02:08.425 --> 00:02:15.465
They come from the chosen system, so there are no separate
saturation-pressure boxes to fill in for this case.

02-11
00:02:15.645 --> 00:02:21.426
Keep temperature and feed composition unchanged throughout the
pressure comparison.

02-12
00:02:21.606 --> 00:02:27.217
On our one-mole feed basis, the feed contains half a mole of each
component.

02-13
00:02:27.397 --> 00:02:34.716
Record the system, ideal assumption, temperature, pressure, and feed
composition on guide page one.

03-01
00:02:37.246 --> 00:02:42.814
The lab may already display the ninety-five-kilopascal baseline when
it opens.

03-02
00:02:42.994 --> 00:02:44.551
That is expected.

03-03
00:02:44.731 --> 00:02:48.955
Our predictions concern the two pressures we have not tried yet.

03-04
00:02:49.135 --> 00:02:58.543
Before changing the pressure, use guide page one to predict what
happens at one hundred ten kilopascals and at eighty kilopascals.

03-05
00:02:58.723 --> 00:03:04.777
For each case, write whether you expect liquid only, vapor only, or
both phases.

03-06
00:03:04.957 --> 00:03:10.930
Then predict whether the vapor fraction increases or decreases
relative to the baseline.

03-07
00:03:11.110 --> 00:03:18.406
In the prediction control, consider the question about lowering
pressure at fixed temperature and feed composition.

03-08
00:03:18.586 --> 00:03:21.701
Make your own choice before checking the results.

03-09
00:03:21.881 --> 00:03:24.995
Give a short physical explanation in the guide.

03-10
00:03:25.175 --> 00:03:29.378
Do not change temperature to produce your predicted outcome.

03-11
00:03:29.558 --> 00:03:32.374
Take about two minutes for these predictions.

03-12
00:03:32.554 --> 00:03:35.477
A brief sentence for each pressure is enough.

03-13
00:03:35.657 --> 00:03:43.657
An initial prediction can be wrong and still be useful if you later
explain how the calculation changed your reasoning.

03-14
00:03:43.837 --> 00:03:47.506
Pause here and continue when both predictions are written.

04-01
00:03:50.036 --> 00:03:54.812
Select P, x, y, fixed temperature in the Diagram menu.

04-02
00:03:54.992 --> 00:03:59.088
The horizontal axis is composition of component one.

04-03
00:03:59.268 --> 00:04:01.465
The vertical axis is pressure.

04-04
00:04:01.645 --> 00:04:06.104
The solid bubble curve uses liquid composition, x one.

04-05
00:04:06.284 --> 00:04:10.401
The dashed dew curve uses vapor composition, y one.

04-06
00:04:10.581 --> 00:04:14.891
The diamond marks the overall feed at the selected pressure.

04-07
00:04:15.071 --> 00:04:18.697
Look at the two boundary results below the diagram.

04-08
00:04:18.877 --> 00:04:25.555
Bubble pressure uses liquid composition equal to the feed composition,
zero point five.

04-09
00:04:25.735 --> 00:04:31.708
Half of one hundred fifty plus half of sixty gives one hundred five
kilopascals.

04-10
00:04:31.888 --> 00:04:36.901
This is where the first vapor appears when pressure is lowered from
the liquid side.

04-11
00:04:37.081 --> 00:04:42.948
Dew pressure instead specifies vapor composition equal to zero point
five.

04-12
00:04:43.128 --> 00:04:49.315
Its reciprocal is half divided by one hundred fifty, plus half divided
by sixty.

04-13
00:04:49.495 --> 00:04:55.916
Taking the reciprocal gives approximately eighty-five point seven one
four kilopascals.

04-14
00:04:56.096 --> 00:05:00.000
These boundary calculations answer different questions.

04-15
00:05:00.180 --> 00:05:08.799
Their specified compositions are not the two endpoint compositions of
the current ninety-five-kilopascal tie line.

04-16
00:05:08.979 --> 00:05:15.123
Record both boundaries on guide page one and use them to classify our
pressure cases.

05-01
00:05:17.653 --> 00:05:19.594
Turn to guide page two.

05-02
00:05:19.774 --> 00:05:25.679
Our flash pressure is ninety-five kilopascals, between the dew and
bubble pressures.

05-03
00:05:25.859 --> 00:05:29.635
The phase label therefore reads Liquid plus vapor.

05-04
00:05:29.815 --> 00:05:32.759
Read the three large results separately.

05-05
00:05:32.939 --> 00:05:37.099
Liquid x one is about zero point three eight eight nine.

05-06
00:05:37.279 --> 00:05:41.738
Vapor y one is about zero point six one four zero.

05-07
00:05:41.918 --> 00:05:46.969
Vapor fraction, beta, is about zero point four nine three five.

05-08
00:05:47.149 --> 00:05:51.010
The first two numbers describe composition within each phase.

05-09
00:05:51.190 --> 00:05:55.307
Beta describes how much of the entire feed becomes vapor.

05-10
00:05:55.487 --> 00:06:02.037
Beta is a molar amount fraction, not the vapor composition and not a
volume fraction.

05-11
00:06:02.217 --> 00:06:12.782
On a one-mole feed basis, about zero point four nine three five moles
are vapor, and zero point five zero six five moles are liquid.

05-12
00:06:12.962 --> 00:06:18.978
The horizontal tie line connects the liquid and vapor compositions at
the same pressure.

05-13
00:06:19.158 --> 00:06:22.252
The feed composition lies between them.

05-14
00:06:22.432 --> 00:06:26.869
Component A is more concentrated in the vapor than in the liquid.

05-15
00:06:27.049 --> 00:06:32.788
Record the baseline in the guide, keeping enough digits for the
balance check that follows.

06-01
00:06:35.318 --> 00:06:39.328
Now check the answer independently on guide page two.

06-02
00:06:39.508 --> 00:06:47.060
Start with one mole of feed, containing zero point five moles of A and
zero point five moles of B.

06-03
00:06:47.240 --> 00:06:55.198
For component A, multiply the liquid amount by x one, then add the
vapor amount multiplied by y one.

06-04
00:06:55.378 --> 00:07:00.412
The liquid contains about zero point one nine six nine seven moles of
A.

06-05
00:07:00.592 --> 00:07:05.755
The vapor contains about zero point three zero three zero three moles.

06-06
00:07:05.935 --> 00:07:08.751
Their sum is zero point five moles.

06-07
00:07:08.931 --> 00:07:14.158
For component B, use one minus x one and one minus y one.

06-08
00:07:14.338 --> 00:07:20.055
The liquid contribution is about zero point three zero nine five two
moles.

06-09
00:07:20.235 --> 00:07:25.654
The vapor contribution is about zero point one nine zero four eight
moles.

06-10
00:07:25.834 --> 00:07:29.012
These also sum to zero point five moles.

06-11
00:07:29.192 --> 00:07:35.166
The two phase amounts must sum to one mole, and each phase composition
must sum to one.

06-12
00:07:35.346 --> 00:07:41.852
Small differences from these totals can arise if you calculate with
rounded screen values.

06-13
00:07:42.032 --> 00:07:45.318
Keep additional digits during the calculation.

06-14
00:07:45.498 --> 00:07:54.781
The lab's small residual checks its equations, while your hand
calculation checks that you understand the quantities being balanced.

07-01
00:07:57.311 --> 00:08:04.906
For a closer look at the amount calculation, choose Rachford, Rice,
vapor fraction in the Diagram menu.

07-02
00:08:05.086 --> 00:08:10.696
You may revisit this chapter later if you first want to complete the
practical workflow.

07-03
00:08:10.876 --> 00:08:18.279
For this ideal calculation, each K value is its saturation pressure
divided by the flash pressure.

07-04
00:08:18.459 --> 00:08:24.944
Using kilopascals for both numerator and denominator gives
dimensionless values.

07-05
00:08:25.124 --> 00:08:33.278
K one is one hundred fifty divided by ninety-five, approximately one
point five seven eight nine five.

07-06
00:08:33.458 --> 00:08:40.610
K two is sixty divided by ninety-five, approximately zero point six
three one five eight.

07-07
00:08:40.790 --> 00:08:44.630
The plotted function combines both component balances.

07-08
00:08:44.810 --> 00:08:51.572
At beta equal to zero it is approximately positive zero point one zero
five three.

07-09
00:08:51.752 --> 00:08:58.195
At beta equal to one it is approximately negative zero point one zero
eight three.

07-10
00:08:58.375 --> 00:09:01.532
The crossing between them is the physical root.

07-11
00:09:01.712 --> 00:09:11.291
That root is beta approximately zero point four nine three five, the
same vapor fraction we just checked on a one-mole feed basis.

07-12
00:09:11.471 --> 00:09:18.596
The horizontal axis here is vapor fraction, unlike the composition
axis of the pressure diagram.

07-13
00:09:18.776 --> 00:09:25.518
Return the Diagram menu to P, x, y, fixed temperature before saving
the baseline.

08-01
00:09:28.048 --> 00:09:32.186
Before changing anything, save the calculated baseline.

08-02
00:09:32.366 --> 00:09:36.121
Open Study workspace, reopen and compare cases.

08-03
00:09:36.301 --> 00:09:43.426
In Label for the next captured case, enter a clear name such as
Baseline, ninety-five kilopascals.

08-04
00:09:43.606 --> 00:09:48.790
Return to the experiment export controls and select Export experiment.

08-05
00:09:48.970 --> 00:09:59.552
This downloads a study JSON file containing inputs, calculated
results, property information, and any prediction or reflection.

08-06
00:09:59.732 --> 00:10:04.873
It also adds that exported study to the workspace comparison in this
tab.

08-07
00:10:05.053 --> 00:10:08.829
The case label helps you recognize the result later.

08-08
00:10:09.009 --> 00:10:17.606
Check that the captured baseline has pressure ninety-five kilopascals
in its inputs and the vapor fraction we just verified.

08-09
00:10:17.786 --> 00:10:21.285
Download current inputs only is a different button.

08-10
00:10:21.465 --> 00:10:26.635
It can preserve a setup, but it does not contain the calculated
result.

08-11
00:10:26.815 --> 00:10:33.450
For this exercise, use Export experiment so your evidence includes the
actual calculation.

08-12
00:10:33.630 --> 00:10:37.256
The comparison currently lives in browser memory.

08-13
00:10:37.436 --> 00:10:42.407
We will download the complete comparison after adding two more
pressures.

08-14
00:10:42.587 --> 00:10:50.118
Keep the individual study download as well, and do not assume that the
open tab alone is permanent storage.

09-01
00:10:52.648 --> 00:10:54.845
Now test your first prediction.

09-02
00:10:55.025 --> 00:11:01.745
Change only Flash pressure to one hundred ten kilopascals and select
Calculate equilibrium.

09-03
00:11:01.925 --> 00:11:10.288
Leave temperature at three hundred fifty kelvin, feed fraction at zero
point five, and the liquid model ideal.

09-04
00:11:10.468 --> 00:11:15.481
The pressure is above the bubble boundary of one hundred five
kilopascals.

09-05
00:11:15.661 --> 00:11:17.730
The result is Liquid only.

09-06
00:11:17.910 --> 00:11:21.750
Beta is zero, so all one mole of feed is liquid.

09-07
00:11:21.930 --> 00:11:27.712
Its composition is the feed composition, x one equal to zero point
five.

09-08
00:11:27.892 --> 00:11:33.012
Vapor y one displays N A, with the explanation No vapor phase.

09-09
00:11:33.192 --> 00:11:36.754
This does not mean a vapor composition of zero.

09-10
00:11:36.934 --> 00:11:42.054
There is no bulk vapor phase whose composition we can report at this
state.

09-11
00:11:42.234 --> 00:11:47.269
Compare this result with your prediction, then record it on guide page
two.

09-12
00:11:47.449 --> 00:11:53.934
In the workspace, enter a new case label such as High pressure, one
hundred ten kilopascals.

09-13
00:11:54.114 --> 00:11:58.061
Select Export experiment to capture this calculated case.

09-14
00:11:58.241 --> 00:12:03.916
We now have the two-phase baseline and one liquid-only case for
comparison.

10-01
00:12:06.446 --> 00:12:12.547
Test the second prediction by changing only Flash pressure to eighty
kilopascals.

10-02
00:12:12.727 --> 00:12:15.543
Select Calculate equilibrium again.

10-03
00:12:15.723 --> 00:12:23.446
Eighty kilopascals is below the dew boundary of about eighty-five
point seven one four kilopascals.

10-04
00:12:23.626 --> 00:12:26.762
The phase label now reads Vapor only.

10-05
00:12:26.942 --> 00:12:34.046
Beta is one, and vapor y one equals the overall feed composition, zero
point five.

10-06
00:12:34.226 --> 00:12:36.551
All one mole of feed is vapor.

10-07
00:12:36.731 --> 00:12:41.830
Liquid x one displays N A because there is no bulk liquid phase.

10-08
00:12:42.010 --> 00:12:46.746
As in the previous case, this absent composition is not zero.

10-09
00:12:46.926 --> 00:12:53.347
There is no liquid component amount to calculate because the liquid
amount itself is zero.

10-10
00:12:53.527 --> 00:12:56.983
Record the result and compare it with your prediction.

10-11
00:12:57.163 --> 00:13:08.043
At this fixed temperature, reducing pressure from one hundred ten
through ninety-five to eighty kilopascals takes us from liquid to two
phases to vapor.

10-12
00:13:08.223 --> 00:13:14.623
The vapor fraction remains zero or one while a state stays inside its
single-phase region.

10-13
00:13:14.803 --> 00:13:20.435
Label this case Low pressure, eighty kilopascals, and use Export
experiment.

10-14
00:13:20.615 --> 00:13:23.922
The workspace should now hold three distinct cases.

11-01
00:13:26.452 --> 00:13:33.748
Open the workspace comparison and find the input pressure, phase,
vapor fraction, and composition rows.

11-02
00:13:33.928 --> 00:13:40.541
Check that temperature, feed composition, and model remain the same
across all three columns.

11-03
00:13:40.721 --> 00:13:43.025
Only the flash pressure changed.

11-04
00:13:43.205 --> 00:13:47.920
The comparison displays recorded fields from the exported studies.

11-05
00:13:48.100 --> 00:13:52.345
A missing phase composition may appear as Not recorded.

11-06
00:13:52.525 --> 00:13:57.965
In the underlying JSON, the absent phase composition is null.

11-07
00:13:58.145 --> 00:14:02.540
Neither Not recorded nor null should be replaced by zero.

11-08
00:14:02.720 --> 00:14:04.960
Also inspect the pressure units.

11-09
00:14:05.140 --> 00:14:11.247
The input pressure is stored in kilopascals, but the result pressure
is stored in pascals.

11-10
00:14:11.427 --> 00:14:19.150
Ninety-five kilopascals and ninety-five thousand pascals represent the
same pressure, not a disagreement.

11-11
00:14:19.330 --> 00:14:24.258
Use Curve CSV to download the selected diagram's data.

11-12
00:14:24.438 --> 00:14:31.174
For the pressure diagram, the pressure column is labeled P underscore
P a, meaning pascals.

11-13
00:14:31.354 --> 00:14:36.852
This file is a sampled equilibrium curve, not the three-case
comparison.

11-14
00:14:37.032 --> 00:14:45.843
Because temperature and the ideal system were unchanged, the pressure
diagram itself is unchanged across our three cases.

11-15
00:14:46.023 --> 00:14:49.180
The current pressure marker and phase split move.

11-16
00:14:49.360 --> 00:14:53.904
Record a short explanation of that distinction on guide page two.

12-01
00:14:56.434 --> 00:14:58.418
Turn to guide page three.

12-02
00:14:58.598 --> 00:15:05.468
In the workspace, select Download comparison and confirm that the JSON
file is saved.

12-03
00:15:05.648 --> 00:15:08.421
Keep this file before clearing anything.

12-04
00:15:08.601 --> 00:15:13.977
For this demonstration, Clear comparison removes the three in-memory
cases.

12-05
00:15:14.157 --> 00:15:16.994
It does not delete your downloaded files.

12-06
00:15:17.174 --> 00:15:25.345
Now use Load studies or a comparison JSON and select the comparison
file you just downloaded.

12-07
00:15:25.525 --> 00:15:28.170
The three recorded cases return.

12-08
00:15:28.350 --> 00:15:32.617
Choose Restore beside the ninety-five-kilopascal baseline.

12-09
00:15:32.797 --> 00:15:35.101
This loads its saved controls.

12-10
00:15:35.281 --> 00:15:44.315
Check the system, ideal model, temperature, pressure, and feed
composition, then explicitly select Calculate equilibrium.

12-11
00:15:44.495 --> 00:15:49.338
Restoring a file and producing a fresh result are separate steps.

12-12
00:15:49.518 --> 00:15:56.984
The comparison preserves recorded evidence, while Calculate
equilibrium runs the current inputs again.

12-13
00:15:57.164 --> 00:16:04.567
Verify that the fresh result is Liquid plus vapor with beta about zero
point four nine three five.

12-14
00:16:04.747 --> 00:16:07.520
Check the two phase compositions as well.

12-15
00:16:07.700 --> 00:16:12.479
Record in the guide that you reopened the file and reproduced the
baseline.

12-16
00:16:12.659 --> 00:16:21.800
A saved file becomes useful evidence when another person, or your
future self, can recover the settings and obtain the same result.

13-01
00:16:24.330 --> 00:16:27.082
You are ready for an independent attempt.

13-02
00:16:27.262 --> 00:16:31.870
Stay on guide page three and keep the answer page closed for now.

13-03
00:16:32.050 --> 00:16:40.647
Use the same synthetic ideal mixture at three hundred fifty kelvin and
feed composition zero point five.

13-04
00:16:40.827 --> 00:16:43.728
The new pressure is ninety kilopascals.

13-05
00:16:43.908 --> 00:16:48.964
Before running the lab, classify the phase using the two boundary
pressures.

13-06
00:16:49.144 --> 00:16:54.798
Calculate liquid x one, vapor y one, and the vapor fraction by hand.

13-07
00:16:54.978 --> 00:17:06.417
Use the ideal bubble relation to find the liquid composition, the
equilibrium relation to find the vapor composition, and the component
balance to find beta.

13-08
00:17:06.597 --> 00:17:11.418
Then enter ninety kilopascals and select Calculate equilibrium.

13-09
00:17:11.598 --> 00:17:18.468
Compare your calculation with the result, and check both component
balances on a one-mole feed basis.

13-10
00:17:18.648 --> 00:17:24.237
Label and export this new study if you want to retain it with your
earlier cases.

13-11
00:17:24.417 --> 00:17:27.254
Allow about five minutes for your attempt.

13-12
00:17:27.434 --> 00:17:31.936
Write the substitutions and units, not just the final numbers.

13-13
00:17:32.116 --> 00:17:39.518
Continue to the final chapter and guide page four only after you have
tried the calculation yourself.

14-01
00:17:42.048 --> 00:17:45.547
Now open guide page four and check your attempt.

14-02
00:17:45.727 --> 00:17:52.724
Ninety kilopascals lies between the dew and bubble pressures, so both
liquid and vapor are present.

14-03
00:17:52.904 --> 00:18:01.956
From the ideal bubble relation, liquid x one equals ninety minus
sixty, divided by one hundred fifty minus sixty.

14-04
00:18:02.136 --> 00:18:04.013
The result is one third.

14-05
00:18:04.193 --> 00:18:11.745
Vapor y one equals one hundred fifty times one third, divided by
ninety, giving five ninths.

14-06
00:18:11.925 --> 00:18:19.349
The vapor fraction is the feed composition minus x one, divided by y
one minus x one.

14-07
00:18:19.529 --> 00:18:21.385
This gives three quarters.

14-08
00:18:21.565 --> 00:18:29.288
On a one-mole feed basis, the liquid amount is one quarter of a mole
and the vapor amount is three quarters.

14-09
00:18:29.468 --> 00:18:36.998
Component A contributes one twelfth of a mole in the liquid and five
twelfths in the vapor, totaling half a mole.

14-10
00:18:37.178 --> 00:18:44.261
Component B contributes one sixth in the liquid and one third in the
vapor, also totaling half a mole.

14-11
00:18:44.441 --> 00:18:50.372
If your answer differs, inspect the phase compositions and amount
fraction separately.

14-12
00:18:50.552 --> 00:18:53.666
Retain your original attempt and correction.

14-13
00:18:53.846 --> 00:19:04.023
You have now completed the practical cycle: predict, calculate, check
independently, save the evidence, and reopen it to reproduce the
result.
