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SCIENCE · INVESTIGATE AND EXPLAIN

Cross a titration equivalence point without changing conservation laws

One charge balance can describe initial acid, buffer, equivalence and excess base.

Learning outcome: Compare initial, half-equivalence, equivalence and excess-base points. Retain dilution and charge residuals; contrast the strong-acid curve with identical starting equivalents.

Starting recap

Refresh proton equivalents, conjugate pairs, logarithmic dimensionless activity, analytical amount/volume, mass and charge balances, and bounded observational criteria.

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Try

The packet starts with .00250 mol HA. At 25.0 mL of .100 M base, total volume .0500 L and acid-family concentration .0500 M; conjugate-base hydrolysis makes equivalence basic.

Open the experiment

Predict

Why can equal acid/base equivalents leave pH above 7 in a weak-acid titration?

Experiment

Compare initial, half-equivalence, equivalence and excess-base points. Retain dilution and charge residuals; contrast the strong-acid curve with identical starting equivalents.

Follow a titration through one global charge balance

Worked teaching model · synthetic values · Fictional25.0 mL of .100 M neutral HA receives .100 M fully dissociated monobasic base with inert sodium ion; additive volumes. At each point C=.00250/(.025+Vb), Na=.100Vb/(.025+Vb); h+Na=Kw/h+C Ka/(Ka+h), Kw10⁻¹⁴. Ideal supplied packet, not an experimental procedure.

Reset keeps your prediction, captures and practice history.

pHadded .100 M base volume (mL)05012.522880
  • Weak acid exact pH: solid
  • Strong acid comparison at same amounts: long dashes

Axes rescale. A concentration scan, imposed-pH distribution and titration curve have different horizontal meanings. Read each axis and preserve the difference between an imposed condition and an inferred equilibrium.

All calculated plot coordinates
Weak acid exact pH
added .100 M base volume (mL)pH
03.002171
0.53.393088
13.645664
1.53.817301
23.946461
2.54.050463
34.138041
3.54.214136
44.281797
4.54.343033
54.399238
5.54.451419
64.50033
6.54.546549
74.590533
7.54.632649
84.6732
8.54.712438
94.750578
9.54.787806
104.824288
10.54.860171
114.895587
11.54.930663
124.965517
12.55.00026
135.035006
13.55.069865
145.104951
14.55.140383
155.176284
15.55.212791
165.250051
16.55.28823
175.327517
17.55.368127
185.410318
18.55.454396
195.500735
19.55.549799
205.602182
20.55.658659
215.720272
21.55.788479
225.865406
22.55.954344
236.060795
23.56.19507
246.380298
24.56.690264
258.849498
25.510.9957
2611.29244
26.511.46429
2711.58503
27.511.67778
2811.75285
28.511.81571
2911.86967
29.511.91682
3011.95861
30.511.99607
3112.02996
31.512.06087
3212.08922
32.512.11539
3312.13966
33.512.16226
3412.18339
34.512.20321
3512.22185
35.512.23943
3612.25606
36.512.27182
3712.28679
37.512.30103
3812.3146
38.512.32756
3912.33995
39.512.35181
4012.36318
40.512.37409
4112.38458
41.512.39466
4212.40437
42.512.41373
4312.42276
43.512.43148
4412.4399
44.512.44805
4512.45593
45.512.46356
4612.47096
46.512.47813
4712.48509
47.512.49184
4812.4984
48.512.50478
4912.51098
49.512.51701
5012.52288
Strong acid comparison at same amounts
added .100 M base volume (mL)pH
01
0.51.017374
11.034762
1.51.052178
21.069636
2.51.08715
31.104735
3.51.122406
41.140179
4.51.158068
51.176091
5.51.194265
61.212608
6.51.231139
71.249877
7.51.268845
81.288065
8.51.307561
91.327359
9.51.347487
101.367977
10.51.38886
111.410174
11.51.431959
121.454258
12.51.477121
131.500602
13.51.524763
141.549672
14.51.575408
151.60206
15.51.629731
161.658541
16.51.688629
171.720159
17.51.753328
181.78837
18.51.825576
191.865301
19.51.907997
201.954243
20.52.004799
212.060698
21.52.123385
222.194977
22.52.278754
232.380211
23.52.50965
242.690196
24.52.995635
257
25.510.99568
2611.29243
26.511.46428
2711.58503
27.511.67778
2811.75285
28.511.81571
2911.86967
29.511.91682
3011.95861
30.511.99607
3112.02996
31.512.06086
3212.08922
32.512.11539
3312.13966
33.512.16226
3412.18339
34.512.20321
3512.22185
35.512.23943
3612.25606
36.512.27182
3712.28679
37.512.30103
3812.3146
38.512.32756
3912.33995
39.512.35181
4012.36318
40.512.37409
4112.38458
41.512.39466
4212.40437
42.512.41373
4312.42276
43.512.43148
4412.4399
44.512.44805
4512.45593
45.512.46356
4612.47096
46.512.47813
4712.48509
47.512.49184
4812.4984
48.512.50478
4912.51098
49.512.51701
5012.52288
Calculated under the declared model
QuantityValueUnit
Total mixed volume0.05L
Analytical acid-family concentration0.05mol/L
Inert sodium concentration0.05mol/L
Exact equilibrated pH8.849498pH units
Equivalence volume25mL
Charge-balance residual-1.387779e-17mol/L

Stoichiometric equivalence leaves a hydrolyzing conjugate base, not necessarily neutral water.

One charge-balance equation handles initial acid, buffer region, equivalence and excess base with dilution included. Near half-equivalence the HH pH≈pKa shortcut is useful, not mathematically exact once water and residual acid ionization are retained. Strong/strong equivalence is neutral under this ideal 25°C convention; weak-acid/strong-base equivalence is basic.

These calculated packets are not performed chemical measurements. Keep feasible inventories, activity conventions, fitting observations and independent checks distinct.

Stoichiometric equivalence leaves a hydrolyzing conjugate base, not necessarily neutral water.

One charge-balance equation handles initial acid, buffer region, equivalence and excess base with dilution included. Near half-equivalence the HH pH≈pKa shortcut is useful, not mathematically exact once water and residual acid ionization are retained. Strong/strong equivalence is neutral under this ideal 25°C convention; weak-acid/strong-base equivalence is basic.

Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.

Understand

Keep amounts and volume separate

Initially 25.0 mL of .100 M HA contains .00250 mol acid family. Adding volume Vb in liters of .100 M monobasic strong base contributes .100Vb mol inert sodium ion and increases total volume to .0250+Vb L. The acid-family total concentration and sodium concentration therefore have different numerators but the same changing denominator.

For ideal activities and Kw10⁻¹⁴, solve h+Na=Kw/h+C Ka/(Ka+h). The same equation applies before and after stoichiometric equivalence. Its physical interpretation changes, but charge conservation does not switch off at a convenient region boundary.

Explain equivalence without assuming neutrality

At 25.0 mL base, the sodium and acid-family analytical concentrations are both .0500 M. The weak-acid conjugate base hydrolyzes, so equilibrium is basic. In the comparison strong-acid/strong-base packet with inert ions, equal equivalents give neutrality under the declared25°C convention.

Near half-equivalence, equal nominal HA and A− give the useful pH≈pKa relation. Residual ionization and water mean it is not an exact identity in the full model. After equivalence, excess hydroxide is a good leading approximation but dilution remains essential.

Transfer and check

For the same starting acid and 35.0 mL base, excess base is .00350−.00250=.00100 mol in .0600 L, approximately .0166667 M hydroxide. Thus pOH≈1.77815 and pH≈12.22185 at pKw 14, with a very small conjugate-base correction. Explain why dividing excess moles by the original25 mL would overstate basicity.

Source and evidence boundary

Conceptual reference checked 30 October 2026: OpenStax Chemistry 2e. Prose, numerical packets and diagrams are original. All chemistry is fictional or supplied; no substance handling, mixing, titration apparatus or health interpretation is requested. The ideal concentration approximation, fixed temperature and inert-ion assumptions are explicit, not measured calibration. Retain your charge/mass balance, prediction, changed-case check and limits.

Apply

The stoichiometric equivalence volume for 25.0 mL .100 M monoprotic acid and .100 M monobasic base is:

Public practice checks a specific claim. It does not establish independent mastery.

Why is pH≈pKa at half-equivalence a useful approximation rather than an identity under the full water/charge model?

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