WEBVTT

01-01
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Welcome to Week Three.

01-02
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This lesson begins with a question raised by our work in Lab Eight.

01-03
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If a model fits the observations closely, how much confidence should
we place in those observations?

01-04
00:00:14.096 --> 00:00:24.229
We will examine thermodynamic consistency first, then move to a
different question: when does a liquid mixture separate into two
stable liquids?

01-05
00:00:24.409 --> 00:00:28.676
The lesson replaces our classroom session during the holiday.

01-06
00:00:28.856 --> 00:00:38.627
Allow about three hours altogether, including watching, calculations,
Lab investigations, a break, and the closing reflection.

01-07
00:00:38.807 --> 00:00:41.879
The recording is only one part of that time.

01-08
00:00:42.059 --> 00:00:46.773
Keep your own answers and pause whenever an activity is assigned.

02-01
00:00:49.303 --> 00:00:54.573
Start by opening the four-page practice worksheet and the three-page
Lab guide.

02-02
00:00:54.753 --> 00:00:57.910
Their links are on the lesson page and this slide.

02-03
00:00:58.090 --> 00:01:05.339
You can print the worksheet, annotate the PDF, or write in a notebook
using the same question labels.

02-04
00:01:05.519 --> 00:01:07.482
Have a calculator ready.

02-05
00:01:07.662 --> 00:01:12.953
Keep the slide deck available beside the video so that you can follow
its links.

02-06
00:01:13.133 --> 00:01:16.098
The worked solutions are a separate document.

02-07
00:01:16.278 --> 00:01:21.846
Open the relevant section only after you have attempted the
corresponding questions.

02-08
00:01:22.026 --> 00:01:28.831
The background reading is optional; you do not need to complete
another reading assignment before starting.

02-09
00:01:29.011 --> 00:01:33.513
All preparation belongs inside today's first fifteen minutes.

02-10
00:01:33.693 --> 00:01:38.535
Pause here briefly to arrange the files, then continue to the
schedule.

02-11
00:01:38.715 --> 00:01:42.129
You can work through the entire lesson independently.

03-01
00:01:44.659 --> 00:01:49.715
The times on the slides are elapsed study time, not video timestamps.

03-02
00:01:49.895 --> 00:01:53.159
They include both listening and doing the work.

03-03
00:01:53.339 --> 00:01:59.525
During the first fifteen minutes, review Lab Eight and calculate one
activity coefficient.

03-04
00:01:59.705 --> 00:02:04.820
Next, spend twenty minutes on the Gibbs-Duhem constraint and its
assumptions.

03-05
00:02:05.000 --> 00:02:09.309
A fifteen-minute hand calculation prepares you for Lab Three.

03-06
00:02:09.489 --> 00:02:14.439
The Lab comparison and interpretation take you to minute ninety.

03-07
00:02:14.619 --> 00:02:16.816
Then take a ten-minute break.

03-08
00:02:16.996 --> 00:02:24.399
From minute one hundred, examine stability and the lever rule before
carrying out the Lab Four investigation.

03-09
00:02:24.579 --> 00:02:29.799
The final fifteen minutes are for self-review, the exit ticket, and
feedback.

03-10
00:02:29.979 --> 00:02:32.987
Use these times as approximate guides.

03-11
00:02:33.167 --> 00:02:40.804
A pause for calculation uses the remaining time in its block; it is
not added on top of three hours.

03-12
00:02:40.984 --> 00:02:44.781
Move forward when you have recorded the required evidence.

04-01
00:02:47.311 --> 00:02:50.895
Turn to page one, questions A one through A three.

04-02
00:02:51.075 --> 00:02:55.052
First, define x, y, z, and gamma in your own words.

04-03
00:02:55.232 --> 00:02:59.691
Keep phase composition separate from the overall mixture composition.

04-04
00:02:59.871 --> 00:03:05.476
Next, calculate gamma one from the supplied synthetic Lab Eight
observation.

04-05
00:03:05.656 --> 00:03:14.381
Multiply the vapor mole fraction by total pressure, then divide by the
liquid mole fraction times the saturation pressure.

04-06
00:03:14.561 --> 00:03:18.487
Both pressures are in kilopascals, so their units cancel.

04-07
00:03:18.667 --> 00:03:25.195
Use the full values printed on the worksheet rather than trying to
copy every digit from the narration.

04-08
00:03:25.375 --> 00:03:29.279
Compare your answer with the exponential given in A two.

04-09
00:03:29.459 --> 00:03:35.112
Finally, answer whether a small fitting error proves thermodynamic
consistency.

04-10
00:03:35.292 --> 00:03:41.884
If you need a reminder, use one relevant chapter of the Lab Eight
walkthrough within this review block.

04-11
00:03:42.064 --> 00:03:47.013
Pause now and finish your attempt before the next slide reveals the
check.

05-01
00:03:49.543 --> 00:03:52.317
Compare these statements with your answers.

05-02
00:03:52.497 --> 00:04:00.859
X one describes component one's mole fraction in the liquid, and y one
describes its mole fraction in the vapor.

05-03
00:04:01.039 --> 00:04:04.090
Z one refers to the overall mixture.

05-04
00:04:04.270 --> 00:04:14.873
Gamma one is an activity coefficient: multiplying it by the liquid
mole fraction gives liquid activity on the chosen pure-liquid standard
state.

05-05
00:04:15.053 --> 00:04:20.471
The calculated gamma is about one point four nine one five four five.

05-06
00:04:20.651 --> 00:04:29.718
Taking the exponential of the rounded logarithm gives essentially the
same answer; the final-digit difference comes from rounding.

05-07
00:04:29.898 --> 00:04:35.103
This inference uses ideal vapor and a negligible Poynting correction.

05-08
00:04:35.283 --> 00:04:42.259
For A three, a close fit shows that the selected model reproduces the
observations under its assumptions.

05-09
00:04:42.439 --> 00:04:48.839
Consistency asks whether the inferred properties obey a thermodynamic
relationship.

05-10
00:04:49.019 --> 00:04:53.499
Keep any correction beside your original answer, then continue.

06-01
00:04:56.029 --> 00:05:00.445
Now consider a binary liquid at fixed temperature and pressure.

06-02
00:05:00.625 --> 00:05:05.745
The Gibbs-Duhem equation connects changes in its two activity
coefficients.

06-03
00:05:05.925 --> 00:05:12.005
If one coefficient changes with composition, the other cannot be
chosen independently.

06-04
00:05:12.185 --> 00:05:16.943
Their mole-fraction-weighted logarithmic changes must sum to zero.

06-05
00:05:17.123 --> 00:05:25.827
This is a constraint on a collection of composition-dependent
properties, rather than a test of one isolated gamma value.

06-06
00:05:26.007 --> 00:05:33.879
The second equation defines dimensionless excess Gibbs energy by
weighting the two log activity coefficients.

06-07
00:05:34.059 --> 00:05:43.445
Under the same fixed conditions, the slope of that excess-energy curve
equals the logarithm of gamma one divided by gamma two.

06-08
00:05:43.625 --> 00:05:47.935
That slope relationship will give us a local diagnostic.

06-09
00:05:48.115 --> 00:05:55.005
We can compare the slope inferred from the weighted properties with
the log ratio at the same composition.

06-10
00:05:55.185 --> 00:05:57.660
Complete B one on page one.

06-11
00:05:57.840 --> 00:06:02.363
State the fixed conditions and explain the connection in one sentence.

07-01
00:06:04.893 --> 00:06:11.997
Experimental vapor-liquid data do not always follow a path with both
temperature and pressure fixed.

07-02
00:06:12.177 --> 00:06:21.009
In an isothermal experiment, temperature stays constant while the
equilibrium pressure generally changes with composition.

07-03
00:06:21.189 --> 00:06:28.442
The more general relationship therefore contains a pressure term
involving molar excess volume.

07-04
00:06:28.622 --> 00:06:32.526
Our teaching calculation neglects that contribution.

07-05
00:06:32.706 --> 00:06:36.653
This approximation must accompany the interpretation.

07-06
00:06:36.833 --> 00:06:41.803
In an isobaric experiment, pressure is fixed but temperature changes.

07-07
00:06:41.983 --> 00:06:46.314
The local relationship then needs an excess-enthalpy correction.

07-08
00:06:46.494 --> 00:06:54.793
For real measurements, we need independent excess-enthalpy information
before assigning that corrected local verdict.

07-09
00:06:54.973 --> 00:06:59.303
A missing correction is not evidence that the measurements failed.

07-10
00:06:59.483 --> 00:07:06.417
Lab Three also supplies synthetic excess enthalpy for its generated
isobaric cases.

07-11
00:07:06.597 --> 00:07:12.847
That value comes from the generator; it is not an independent
calorimetric measurement.

07-12
00:07:13.027 --> 00:07:20.942
Complete B two: identify the omitted pressure contribution and the
property needed for the temperature correction.

08-01
00:07:23.472 --> 00:07:27.184
The four approaches ask related but different questions.

08-02
00:07:27.364 --> 00:07:34.425
The isothermal area method integrates the log-activity ratio across
the full composition range.

08-03
00:07:34.605 --> 00:07:37.891
Contributions of opposite sign can cancel.

08-04
00:07:38.071 --> 00:07:49.299
The local differential method compares a slope relationship at
individual interior compositions, but numerical differentiation is
sensitive to noise and spacing.

08-05
00:07:49.479 --> 00:07:55.389
Herington supplies an empirical allowance for an isobaric boiling-
temperature range.

08-06
00:07:55.569 --> 00:07:59.537
That allowance does not replace measured excess enthalpy.

08-07
00:07:59.717 --> 00:08:08.442
The Van Ness-type approach asks whether a selected activity model can
reproduce the observed pressure and vapor composition.

08-08
00:08:08.622 --> 00:08:17.027
Before interpreting any result, check whether the method applies to
the data path and whether the required information is available.

08-09
00:08:17.207 --> 00:08:22.221
Not applicable, not assessed, and not run are not synonyms for failed.

08-10
00:08:22.401 --> 00:08:25.003
They are also not successful tests.

08-11
00:08:25.183 --> 00:08:27.146
Read the stated reason.

08-12
00:08:27.326 --> 00:08:32.211
Complete B three on page one, using guide page two if needed.

08-13
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You do not need to operate the Lab yet.

09-01
00:08:37.737 --> 00:08:42.388
We will first make the area calculation small enough to check by hand.

09-02
00:08:42.568 --> 00:08:53.683
Page one, section C, gives five equally spaced compositions and five
values of L, the natural logarithm of the activity-coefficient ratio.

09-03
00:08:53.863 --> 00:08:57.703
Treat neighboring points as the ends of a straight segment.

09-04
00:08:57.883 --> 00:09:03.237
For each interval, multiply its width by the average of the two
endpoint values.

09-05
00:09:03.417 --> 00:09:08.665
Keep the sign: a segment below zero contributes a negative signed
area.

09-06
00:09:08.845 --> 00:09:11.811
Add the four contributions for C one.

09-07
00:09:11.991 --> 00:09:19.116
For C two, increase every L value by zero point two and calculate the
signed sum again.

09-08
00:09:19.296 --> 00:09:25.693
For C three, explain what this integral cannot establish about
individual observations.

09-09
00:09:25.873 --> 00:09:31.164
These are synthetic values whose endpoint limits are supplied
analytically.

09-10
00:09:31.344 --> 00:09:34.266
We are not inventing endpoint measurements.

09-11
00:09:34.446 --> 00:09:40.548
Stop the video here and complete C one through C three before opening
the solution slide.

10-01
00:09:43.078 --> 00:09:56.076
The four baseline contributions are zero point three seven five, zero
point one two five, minus zero point one two five, and minus zero
point three seven five.

10-02
00:09:56.256 --> 00:10:03.872
The positive area is one half, the signed negative area is minus one
half, and the total is zero.

10-03
00:10:04.052 --> 00:10:13.161
Raising the entire curve by zero point two adds a rectangle of height
zero point two over a composition interval of one.

10-04
00:10:13.341 --> 00:10:17.096
The new signed integral is therefore zero point two.

10-05
00:10:17.276 --> 00:10:23.584
Lab Three calls the signed integral I and also reports a normalized
score, D.

10-06
00:10:23.764 --> 00:10:31.166
D compares the magnitudes of the positive and negative areas; it is
not the signed integral itself.

10-07
00:10:31.346 --> 00:10:35.762
The teaching area criterion is D below five percent.

10-08
00:10:35.942 --> 00:10:40.486
If both magnitudes vanish, that normalization is undefined.

10-09
00:10:40.666 --> 00:10:43.760
Check your work and keep the distinction visible.

10-10
00:10:43.940 --> 00:10:50.894
Real interior measurements still cannot establish missing endpoint
intervals without an extra assumption.

11-01
00:10:53.424 --> 00:10:58.608
Open Lab Three and guide page one, with worksheet page two beside
them.

11-02
00:10:58.788 --> 00:11:04.079
Before changing a control, understand what the local residual
represents.

11-03
00:11:04.259 --> 00:11:10.766
It subtracts the log-activity ratio from the slope of dimensionless
excess Gibbs energy.

11-04
00:11:10.946 --> 00:11:18.846
Under our isothermal pressure-term approximation, a consistent
continuous description makes that difference vanish.

11-05
00:11:19.026 --> 00:11:22.760
The Lab estimates slopes numerically at interior points.

11-06
00:11:22.940 --> 00:11:30.001
Its teaching score is one hundred times the mean absolute residual,
with a threshold of five.

11-07
00:11:30.181 --> 00:11:36.282
That scaled score is not a probability or a percentage of incorrect
observations.

11-08
00:11:36.462 --> 00:11:43.225
Numerical differentiation can create a small residual even for clean
generated data.

11-09
00:11:43.405 --> 00:11:46.699
Also, an average can dilute a narrow peak.

11-10
00:11:46.879 --> 00:11:49.482
Inspect the shape as well as the score.

11-11
00:11:49.662 --> 00:11:59.283
This finite-difference diagnostic is distinct from the fitted Padé
slope used in the NIST and Kojima point-test implementation.

12-01
00:12:01.813 --> 00:12:05.376
For D one, make the initial state reproducible.

12-02
00:12:05.556 --> 00:12:09.934
Select Synthetic, isothermal, three hundred fifty kelvin.

12-03
00:12:10.114 --> 00:12:15.058
Choose Consistent reference, and explicitly select forty-one points.

12-04
00:12:15.238 --> 00:12:20.528
The page normally starts with eighty-one points, so do not skip that
change.

12-05
00:12:20.708 --> 00:12:25.615
Under Inspect, choose Log-activity ratio and integrated area.

12-06
00:12:25.795 --> 00:12:30.894
Record the signed integral, the normalized D score, and the area
status.

12-07
00:12:31.074 --> 00:12:38.410
Then switch Inspect to Local Gibbs-Duhem residual and record its
score, status, and general shape.

12-08
00:12:38.590 --> 00:12:41.875
The results update when you change these controls.

12-09
00:12:42.055 --> 00:12:46.663
Amplitude is disabled for the clean reference, which is expected.

12-10
00:12:46.843 --> 00:12:52.923
These data use Lab Three's own generator, not the Lab Eight
demonstration dataset.

12-11
00:12:53.103 --> 00:12:57.818
Save the reference evidence with Export all results or a screenshot.

12-12
00:12:57.998 --> 00:13:00.664
Rename the JSON clearly.

12-13
00:13:00.844 --> 00:13:04.023
Wait until D four to run the model fit.

12-14
00:13:04.203 --> 00:13:08.512
Pause now and complete D one before changing the perturbation.

13-01
00:13:11.042 --> 00:13:16.440
For D two, keep the temperature path and forty-one-point sampling
unchanged.

13-02
00:13:16.620 --> 00:13:21.569
Change Controlled perturbation to Canceling errors, zero net area.

13-03
00:13:21.749 --> 00:13:25.226
Check that the amplitude is zero point two five.

13-04
00:13:25.406 --> 00:13:30.654
This construction adds a cosine-shaped term to the log-activity ratio.

13-05
00:13:30.834 --> 00:13:39.226
Its integral across the full composition range is exactly zero,
although the term is not zero at every composition.

13-06
00:13:39.406 --> 00:13:46.019
The weighted changes to the two log activity coefficients cancel in
the excess-energy value.

13-07
00:13:46.199 --> 00:13:51.447
This is designed to separate a global integral from a local
relationship.

13-08
00:13:51.627 --> 00:13:55.766
Inspect the area plot and then the local residual plot.

13-09
00:13:55.946 --> 00:14:02.495
Record their scores and statuses without turning them into a single
overall pass or fail.

13-10
00:14:02.675 --> 00:14:05.214
Explain what each actually tests.

13-11
00:14:05.394 --> 00:14:10.236
Save this case under a different filename so that you retain the
reference.

13-12
00:14:10.416 --> 00:14:15.003
Pause here and finish D two before moving to the localized defect.

14-01
00:14:17.533 --> 00:14:25.384
For D three, change only the perturbation to Localized defect near x
one equals zero point three five.

14-02
00:14:25.564 --> 00:14:29.852
Keep amplitude zero point two five and forty-one points.

14-03
00:14:30.032 --> 00:14:35.493
This time the discrepancy occupies a narrow part of the composition
range.

14-04
00:14:35.673 --> 00:14:42.286
Locate it on the local residual plot, then compare its appearance with
the single averaged score.

14-05
00:14:42.466 --> 00:14:51.064
For these exact settings, both aggregate criteria are met, even though
the residual plot shows the localized defect.

14-06
00:14:51.244 --> 00:14:57.132
Do not assume that deliberately introducing a defect must make every
badge change.

14-07
00:14:57.312 --> 00:15:02.240
Record what the Lab actually reports and explain the scope of the
average.

14-08
00:15:02.420 --> 00:15:04.958
Save the localized case separately.

14-09
00:15:05.138 --> 00:15:13.443
If you have spare time inside this activity block, compare one hundred
sixty-one points, then return to forty-one.

14-10
00:15:13.623 --> 00:15:21.538
That optional resolution check changes the numerical sampling; it does
not create new experimental evidence.

14-11
00:15:21.718 --> 00:15:23.787
Pause and complete D three.

15-01
00:15:26.317 --> 00:15:34.616
For the one required modeling run, return to Consistent reference at
three hundred fifty kelvin and forty-one points.

15-02
00:15:34.796 --> 00:15:39.340
Click Run modeling test once and wait for the convergence message.

15-03
00:15:39.520 --> 00:15:42.101
Then inspect Modeling residuals.

15-04
00:15:42.281 --> 00:15:48.041
Record the pressure error in percent and the vapor-composition error
in percentage points.

15-05
00:15:48.221 --> 00:15:52.872
These are different quantities, even though both are scaled by one
hundred.

15-06
00:15:53.052 --> 00:16:01.713
The Lab fits two constant N R T L parameters with the nonrandomness
parameter fixed at zero point four seven.

15-07
00:16:01.893 --> 00:16:08.485
Its teaching criteria require both reported errors to be below one in
their stated units.

15-08
00:16:08.665 --> 00:16:20.868
The clean fit should give near-zero errors because it reproduces its
own generating model; that is a check of model reproduction, not a
certificate for real measurements.

15-09
00:16:21.048 --> 00:16:25.570
Herington is not applicable because this case is isothermal.

15-10
00:16:25.750 --> 00:16:29.825
Its boiling-range allowance belongs to an isobaric path.

15-11
00:16:30.005 --> 00:16:32.224
Pause now to finish D four.

15-12
00:16:32.404 --> 00:16:38.249
If the fit does not converge, record no modeling verdict instead of
guessing a result.

16-01
00:16:40.779 --> 00:16:45.067
Compare your D one and D two records with these two plots.

16-02
00:16:45.247 --> 00:16:54.122
The teal reference and amber canceling-error curves have different
log-activity ratios, yet both meet the area criterion.

16-03
00:16:54.302 --> 00:16:58.590
Their positive and negative contributions nearly balance.

16-04
00:16:58.770 --> 00:17:01.735
The local residual tells a different story.

16-05
00:17:01.915 --> 00:17:09.062
The reference remains close to zero, while the canceling-error
residual oscillates across the composition range.

16-06
00:17:09.242 --> 00:17:19.780
The reference D score is about zero point zero seven nine percent, and
the canceling-case score is about zero point zero seven four percent.

16-07
00:17:19.960 --> 00:17:30.264
Those similarly small area scores conceal a large difference in the
local score: roughly zero point one one eight versus fifteen point
six.

16-08
00:17:30.444 --> 00:17:35.202
Read that contrast from the numerical records and the plotted shape.

16-09
00:17:35.382 --> 00:17:37.878
Complete E one in your own words.

16-10
00:17:38.058 --> 00:17:43.967
Describe how cancellation can occur globally while a local
relationship is violated.

16-11
00:17:44.147 --> 00:17:47.688
Pause before continuing to the interpretation check.

17-01
00:17:50.218 --> 00:17:57.728
Your explanation should connect the two observations rather than rank
the methods as universally good or bad.

17-02
00:17:57.908 --> 00:18:04.734
The cosine perturbation integrates to zero, so the area method misses
that particular discrepancy.

17-03
00:18:04.914 --> 00:18:08.776
The local relationship retains a structured departure.

17-04
00:18:08.956 --> 00:18:16.444
For E two, write a supported claim, give the numerical or graphical
evidence, and state one limitation.

17-05
00:18:16.624 --> 00:18:25.438
Include the dataset, forty-one-point sampling, and perturbation
amplitude so another person could reproduce the comparison.

17-06
00:18:25.618 --> 00:18:32.530
Mention the assumptions behind inferred activities or the sensitivity
of derivatives to sampling.

17-07
00:18:32.710 --> 00:18:38.832
Keep the localized case in mind: even a mean local score can hide a
narrow feature.

17-08
00:18:39.012 --> 00:18:45.455
After writing your own explanation, compare it with sections D and E
of the worked solutions.

17-09
00:18:45.635 --> 00:18:48.707
Save the baseline and changed-case evidence.

17-10
00:18:48.887 --> 00:18:57.911
This constructed exercise demonstrates limitations of diagnostics; it
does not estimate experimental uncertainty.

18-01
00:19:00.441 --> 00:19:02.532
Take a ten-minute break now.

18-02
00:19:02.712 --> 00:19:05.442
Save your work and leave the files open.

18-03
00:19:05.622 --> 00:19:10.998
Step away from the screen, then return to this point with worksheet
page three ready.

18-04
00:19:11.178 --> 00:19:14.162
After the break, we will change the question.

18-05
00:19:14.342 --> 00:19:19.782
A model can obey Gibbs-Duhem and still favor separation into two
liquids.

18-06
00:19:19.962 --> 00:19:24.762
We will use Gibbs energy to determine which liquid state is stable.

19-01
00:19:27.292 --> 00:19:37.298
At fixed temperature and pressure, stable equilibrium is the
admissible state with the lowest total Gibbs energy, subject to the
material balance.

19-02
00:19:37.478 --> 00:19:45.008
For a binary mixture, the mixing-energy curve contains the ideal
mixing terms plus the excess contribution.

19-03
00:19:45.188 --> 00:19:53.252
This curve can become nonconvex even when the activity model satisfies
the Gibbs-Duhem identity exactly.

19-04
00:19:53.432 --> 00:19:58.616
That is why consistency does not imply a stable homogeneous liquid.

19-05
00:19:58.796 --> 00:20:04.514
Equality of chemical potentials identifies candidate coexisting
phases.

19-06
00:20:04.694 --> 00:20:11.862
We must still ask whether that candidate provides the lowest energy
when all allowed compositions are considered.

19-07
00:20:12.042 --> 00:20:17.780
In a binary plot, a globally supporting common tangent supplies that
comparison.

19-08
00:20:17.960 --> 00:20:22.931
The line represents the energy of a mixture of the two endpoint
liquids.

19-09
00:20:23.111 --> 00:20:32.284
Complete F one on page three: explain what remains to be checked after
a solver has found equal chemical potentials.

19-10
00:20:32.464 --> 00:20:36.688
Pause briefly before continuing to the geometric condition.

20-01
00:20:39.218 --> 00:20:45.853
A common tangent touches the curve at two distinct compositions and
has the same slope at both.

20-02
00:20:46.033 --> 00:20:53.777
Its slope must also equal the rise between the two energy values
divided by the distance between the compositions.

20-03
00:20:53.957 --> 00:21:00.182
Those local equalities are necessary, but the word supporting adds a
global requirement.

20-04
00:21:00.362 --> 00:21:06.976
Across the entire admitted composition range, the line must remain at
or below the curve.

20-05
00:21:07.156 --> 00:21:15.817
If it crosses above the curve somewhere, another allowed state can
lower the energy and the candidate is not globally stable.

20-06
00:21:15.997 --> 00:21:22.653
Similarly, a solution whose two endpoints coincide does not establish
two distinct liquids.

20-07
00:21:22.833 --> 00:21:31.302
Positive curvature at one composition is only a local statement; it
cannot by itself prove global stability.

20-08
00:21:31.482 --> 00:21:34.234
Keep this condition ready for F three.

20-09
00:21:34.414 --> 00:21:39.854
First, move to the next slide and attempt the lever-rule calculation
in F two.

21-01
00:21:42.384 --> 00:21:53.264
For F two, suppose a stable tie line has already been established with
liquid compositions zero point two zero and zero point eight zero.

21-02
00:21:53.444 --> 00:22:00.186
These values are supplied for a hand example; they are not the
endpoints you should expect from Lab Four.

21-03
00:22:00.366 --> 00:22:12.206
Calculate the fraction of the component-one-rich liquid by subtracting
the lower endpoint from the overall composition, then dividing by the
distance between the endpoints.

21-04
00:22:12.386 --> 00:22:16.183
The other liquid fraction is one minus that result.

21-05
00:22:16.363 --> 00:22:24.064
Do this first for an overall composition of zero point five zero, then
for zero point three five.

21-06
00:22:24.244 --> 00:22:31.668
Reconstruct each overall composition from the fractions and endpoint
compositions to check your balance.

21-07
00:22:31.848 --> 00:22:36.072
Here beta names the richer liquid, not a vapor fraction.

21-08
00:22:36.252 --> 00:22:41.479
Pause now and calculate both feeds before the next slide shows the
answers.

22-01
00:22:44.009 --> 00:22:48.020
For the central feed, the two liquid fractions are equal.

22-02
00:22:48.200 --> 00:22:57.458
For an overall composition of zero point three five, the rich-liquid
fraction is one quarter and the other fraction is three quarters.

22-03
00:22:57.638 --> 00:23:06.918
The balance is three quarters times zero point two, plus one quarter
times zero point eight, which returns zero point three five.

22-04
00:23:07.098 --> 00:23:16.869
The coexisting compositions remain the same because we have kept the
coexistence conditions fixed and moved the feed within the same tie
line.

22-05
00:23:17.049 --> 00:23:19.396
The phase amounts change instead.

22-06
00:23:19.576 --> 00:23:26.893
Correct your F two calculation, then answer F three using the global
supporting-tangent condition.

22-07
00:23:27.073 --> 00:23:33.388
Touching the curve twice is not enough if the line rises above an
admissible part of it.

22-08
00:23:33.568 --> 00:23:37.344
Open Lab Four and guide page three when you are ready.

22-09
00:23:37.524 --> 00:23:42.900
The next investigation uses the model's actual calculated endpoints.

23-01
00:23:45.430 --> 00:23:49.675
For G one, predict the phase state before reading the result.

23-02
00:23:49.855 --> 00:23:58.474
In Lab Four, open Explore a state and choose Unstable, A equals three,
z one equals zero point five zero.

23-03
00:23:58.654 --> 00:24:08.278
Verify the controls: one-parameter Margules, interaction parameter
three, and feed mole fraction zero point five zero.

23-04
00:24:08.458 --> 00:24:12.597
Choose Gibbs energy and common tangent in the View control.

23-05
00:24:12.777 --> 00:24:18.900
If you type values instead of selecting the preset, click Find
equilibrium to apply them.

23-06
00:24:19.080 --> 00:24:25.181
Record the calculated coexisting compositions and both liquid
fractions in the table.

23-07
00:24:25.361 --> 00:24:31.462
Write the Gibbs-energy decrease divided by R T beside G four or below
the table.

23-08
00:24:31.642 --> 00:24:41.050
The parameters represent a hypothetical model at fixed conditions;
this Lab has no physical temperature or pressure input boxes.

23-09
00:24:41.230 --> 00:24:44.494
Keep the same model throughout this comparison.

23-10
00:24:44.674 --> 00:24:52.589
Pause now to make your prediction, run the baseline, and complete G
one using the actual displayed outputs.

24-01
00:24:55.119 --> 00:25:00.858
Before changing the feed, save the baseline with Export study JSON.

24-02
00:25:01.038 --> 00:25:06.328
Give the file a name that identifies the feed as zero point five zero.

24-03
00:25:06.508 --> 00:25:14.338
For G two, change only Feed mole fraction to zero point three five,
then click Find equilibrium.

24-04
00:25:14.518 --> 00:25:18.294
Leave the model and interaction parameter unchanged.

24-05
00:25:18.474 --> 00:25:22.143
Record the same outputs beside your baseline values.

24-06
00:25:22.323 --> 00:25:26.376
Compare the endpoint compositions separately from the fractions.

24-07
00:25:26.556 --> 00:25:35.986
Ask whether each liquid's composition changed, whether its amount
changed, and whether the result still reconstructs the overall feed.

24-08
00:25:36.166 --> 00:25:39.494
Use the endpoints calculated by this model.

24-09
00:25:39.674 --> 00:25:47.546
Substituting zero point two and zero point eight from the earlier hand
example would test a different tie line.

24-10
00:25:47.726 --> 00:25:53.507
Pause here and record the changed-feed result before checking the
balance independently.

25-01
00:25:56.037 --> 00:26:02.586
Now verify G three with your calculator, not simply by copying the
Lab's residual.

25-02
00:26:02.766 --> 00:26:12.516
Use the actual lower and upper coexistence compositions to calculate
the rich-liquid fraction for the feed of zero point three five.

25-03
00:26:12.696 --> 00:26:16.557
Then obtain the other fraction by subtraction from one.

25-04
00:26:16.737 --> 00:26:22.476
Reconstruct the feed by weighting each endpoint composition by its
phase fraction.

25-05
00:26:22.656 --> 00:26:27.690
Check that both fractions lie between zero and one and that they sum
to one.

25-06
00:26:27.870 --> 00:26:33.865
If the displayed endpoints are rounded, a small final-digit mismatch
is expected.

25-07
00:26:34.045 --> 00:26:39.805
You can use the additional digits in the JSON export for a tighter
check.

25-08
00:26:39.985 --> 00:26:46.108
A successful balance verifies that the reported amounts and
compositions match the feed.

25-09
00:26:46.288 --> 00:26:49.829
It does not establish global stability by itself.

25-10
00:26:50.009 --> 00:26:54.425
Pause now and show the substituted calculation on page three.

26-01
00:26:56.955 --> 00:27:02.011
Complete G four by combining the numerical and graphical evidence.

26-02
00:27:02.191 --> 00:27:08.676
Open Verify the equilibrium, then inspect the full Gibbs-energy and
common-tangent plot.

26-03
00:27:08.856 --> 00:27:21.352
Confirm that the liquids have distinct compositions, their chemical
potentials agree within the reported numerical tolerance, and the
common tangent supports the whole admitted curve.

26-04
00:27:21.532 --> 00:27:25.074
Add your independent feed balance to this evidence.

26-05
00:27:25.254 --> 00:27:34.214
The Gibbs-energy decrease shows how much the equilibrium split lowers
the energy relative to the hypothetical homogeneous feed.

26-06
00:27:34.394 --> 00:27:40.175
Do not confuse the homogeneous-feed label with the final equilibrium
phase count.

26-07
00:27:40.355 --> 00:27:47.139
An unstable homogeneous feed can produce a stable equilibrium
consisting of two liquids.

26-08
00:27:47.319 --> 00:27:53.527
Explain which quantities stayed fixed when only the feed changed and
which quantities changed.

26-09
00:27:53.707 --> 00:28:01.899
Pause to write this reasoning, using the tangent and the energy
comparison rather than relying only on a phase badge.

27-01
00:28:04.429 --> 00:28:09.506
Compare G one through G four with section G of the worked solutions.

27-02
00:28:09.686 --> 00:28:20.801
Check that your record identifies one-parameter Margules with A equal
to three, both overall feed compositions, and the actual coexistence
endpoints.

27-03
00:28:20.981 --> 00:28:30.712
Keep phase composition separate from phase fraction: composition
describes each liquid, while fraction tells us how much of that liquid
is present.

27-04
00:28:30.892 --> 00:28:38.871
If a result differs, first compare the model settings, check that
typed values were applied, and inspect any rounding.

27-05
00:28:39.051 --> 00:28:44.363
Save the changed-feed JSON and a comparison table or plot.

27-06
00:28:44.543 --> 00:28:50.068
Retain your balance calculation and stability explanation with those
files.

27-07
00:28:50.248 --> 00:28:53.043
The required investigation ends here.

27-08
00:28:53.223 --> 00:29:00.562
LLE fitting and vapor-liquid-liquid equilibrium are optional
extensions for later study.

27-09
00:29:00.742 --> 00:29:04.774
Open page four of the worksheet for the short self-review.

28-01
00:29:07.304 --> 00:29:11.933
Answer H one through H four without consulting the solutions.

28-02
00:29:12.113 --> 00:29:18.513
Use a sentence or two for each explanation and include the brief
calculation in H four.

28-03
00:29:18.693 --> 00:29:25.008
First, decide whether meeting an area criterion guarantees all local
relationships.

28-04
00:29:25.188 --> 00:29:31.844
Second, explain what you should check before blaming a differential
discrepancy on experimental error.

28-05
00:29:32.024 --> 00:29:38.473
Third, state what a small fitting error can establish and whether that
is predictive validation.

28-06
00:29:38.653 --> 00:29:48.851
Finally, return to the supplied illustrative endpoints zero point two
and zero point eight, with feed composition zero point three five.

28-07
00:29:49.031 --> 00:29:55.921
Calculate the rich-liquid fraction and say what establishes stable
coexistence beyond the balance.

28-08
00:29:56.101 --> 00:29:58.171
Preserve your first answers.

28-09
00:29:58.351 --> 00:30:03.065
Pause now and finish all four before continuing to the review check.

29-01
00:30:05.595 --> 00:30:13.894
For H one, opposite local errors can cancel in the integral, so a
small area is not a guarantee about every point.

29-02
00:30:14.074 --> 00:30:25.173
For H two, examine the thermodynamic path, required excess-property
corrections, phase and property assumptions, and the numerical
differentiation.

29-03
00:30:25.353 --> 00:30:32.457
If essential information is missing, the appropriate result may be not
assessed rather than a failed test.

29-04
00:30:32.637 --> 00:30:40.061
For H three, a small residual demonstrates reproduction by the
selected model on those observations.

29-05
00:30:40.241 --> 00:30:44.551
It does not independently establish accuracy for new data.

29-06
00:30:44.731 --> 00:30:52.923
For H four, the rich-liquid fraction is zero point two five and the
balance returns zero point three five.

29-07
00:30:53.103 --> 00:31:00.932
A stable two-liquid interpretation also needs distinct phases and a
globally supporting common tangent.

29-08
00:31:01.112 --> 00:31:04.803
Correct your answers in a different color or add a note.

29-09
00:31:04.983 --> 00:31:08.780
Keep the original attempt so you can see what changed.

30-01
00:31:11.310 --> 00:31:18.201
Open the existing Session Three exit-ticket and feedback form using
the link or QR code.

30-02
00:31:18.381 --> 00:31:22.626
Section I on worksheet page four gives the same instructions.

30-03
00:31:22.806 --> 00:31:34.299
In the concept response, answer the LLE question: explain when a
calculated split represents stable equilibrium, using your Lab Four
reasoning.

30-04
00:31:34.479 --> 00:31:42.373
In the numerical-evidence response, describe the Lab Three comparison
between the area and local diagnostics.

30-05
00:31:42.553 --> 00:31:49.373
Identify the case, sampling and amplitude, and include the results
that support your statement.

30-06
00:31:49.553 --> 00:31:52.753
You may add your Lab Four balance if useful.

30-07
00:31:52.933 --> 00:31:57.839
Use your own explanation rather than copying the example conclusion.

30-08
00:31:58.019 --> 00:32:03.246
This form is anonymous and does not identify individual attendance.

30-09
00:32:03.426 --> 00:32:10.146
Pause to enter the exit-ticket responses, then continue to the
feedback fields in the same form.

31-01
00:32:12.676 --> 00:32:16.324
Finish the feedback fields and submit the form once.

31-02
00:32:16.504 --> 00:32:25.101
Tell us whether the pace and Lab access worked for independent study,
and name one explanation or instruction that could be clearer.

31-03
00:32:25.281 --> 00:32:28.993
Wait for the message Response received before leaving.

31-04
00:32:29.173 --> 00:32:41.681
Then check your own saved work: the completed worksheet with
corrections, the Lab Three comparison and exports or screenshots, and
both Lab Four cases with the independent balance.

31-05
00:32:41.861 --> 00:32:48.389
Exporting a Lab study saves a local file; it does not submit your
assignment to a server.

31-06
00:32:48.569 --> 00:32:54.094
Keep these files together and follow any separately announced
submission arrangements.

31-07
00:32:54.274 --> 00:32:56.578
This completes the three-hour route.

31-08
00:32:56.758 --> 00:33:00.726
No additional compulsory homework follows this lesson.

31-09
00:33:00.906 --> 00:33:09.269
Your evidence should now distinguish model reproduction, thermodynamic
consistency, and stable phase equilibrium.
