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 experimentPredict
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.
- 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
| added .100 M base volume (mL) | pH |
|---|---|
| 0 | 3.002171 |
| 0.5 | 3.393088 |
| 1 | 3.645664 |
| 1.5 | 3.817301 |
| 2 | 3.946461 |
| 2.5 | 4.050463 |
| 3 | 4.138041 |
| 3.5 | 4.214136 |
| 4 | 4.281797 |
| 4.5 | 4.343033 |
| 5 | 4.399238 |
| 5.5 | 4.451419 |
| 6 | 4.50033 |
| 6.5 | 4.546549 |
| 7 | 4.590533 |
| 7.5 | 4.632649 |
| 8 | 4.6732 |
| 8.5 | 4.712438 |
| 9 | 4.750578 |
| 9.5 | 4.787806 |
| 10 | 4.824288 |
| 10.5 | 4.860171 |
| 11 | 4.895587 |
| 11.5 | 4.930663 |
| 12 | 4.965517 |
| 12.5 | 5.00026 |
| 13 | 5.035006 |
| 13.5 | 5.069865 |
| 14 | 5.104951 |
| 14.5 | 5.140383 |
| 15 | 5.176284 |
| 15.5 | 5.212791 |
| 16 | 5.250051 |
| 16.5 | 5.28823 |
| 17 | 5.327517 |
| 17.5 | 5.368127 |
| 18 | 5.410318 |
| 18.5 | 5.454396 |
| 19 | 5.500735 |
| 19.5 | 5.549799 |
| 20 | 5.602182 |
| 20.5 | 5.658659 |
| 21 | 5.720272 |
| 21.5 | 5.788479 |
| 22 | 5.865406 |
| 22.5 | 5.954344 |
| 23 | 6.060795 |
| 23.5 | 6.19507 |
| 24 | 6.380298 |
| 24.5 | 6.690264 |
| 25 | 8.849498 |
| 25.5 | 10.9957 |
| 26 | 11.29244 |
| 26.5 | 11.46429 |
| 27 | 11.58503 |
| 27.5 | 11.67778 |
| 28 | 11.75285 |
| 28.5 | 11.81571 |
| 29 | 11.86967 |
| 29.5 | 11.91682 |
| 30 | 11.95861 |
| 30.5 | 11.99607 |
| 31 | 12.02996 |
| 31.5 | 12.06087 |
| 32 | 12.08922 |
| 32.5 | 12.11539 |
| 33 | 12.13966 |
| 33.5 | 12.16226 |
| 34 | 12.18339 |
| 34.5 | 12.20321 |
| 35 | 12.22185 |
| 35.5 | 12.23943 |
| 36 | 12.25606 |
| 36.5 | 12.27182 |
| 37 | 12.28679 |
| 37.5 | 12.30103 |
| 38 | 12.3146 |
| 38.5 | 12.32756 |
| 39 | 12.33995 |
| 39.5 | 12.35181 |
| 40 | 12.36318 |
| 40.5 | 12.37409 |
| 41 | 12.38458 |
| 41.5 | 12.39466 |
| 42 | 12.40437 |
| 42.5 | 12.41373 |
| 43 | 12.42276 |
| 43.5 | 12.43148 |
| 44 | 12.4399 |
| 44.5 | 12.44805 |
| 45 | 12.45593 |
| 45.5 | 12.46356 |
| 46 | 12.47096 |
| 46.5 | 12.47813 |
| 47 | 12.48509 |
| 47.5 | 12.49184 |
| 48 | 12.4984 |
| 48.5 | 12.50478 |
| 49 | 12.51098 |
| 49.5 | 12.51701 |
| 50 | 12.52288 |
| added .100 M base volume (mL) | pH |
|---|---|
| 0 | 1 |
| 0.5 | 1.017374 |
| 1 | 1.034762 |
| 1.5 | 1.052178 |
| 2 | 1.069636 |
| 2.5 | 1.08715 |
| 3 | 1.104735 |
| 3.5 | 1.122406 |
| 4 | 1.140179 |
| 4.5 | 1.158068 |
| 5 | 1.176091 |
| 5.5 | 1.194265 |
| 6 | 1.212608 |
| 6.5 | 1.231139 |
| 7 | 1.249877 |
| 7.5 | 1.268845 |
| 8 | 1.288065 |
| 8.5 | 1.307561 |
| 9 | 1.327359 |
| 9.5 | 1.347487 |
| 10 | 1.367977 |
| 10.5 | 1.38886 |
| 11 | 1.410174 |
| 11.5 | 1.431959 |
| 12 | 1.454258 |
| 12.5 | 1.477121 |
| 13 | 1.500602 |
| 13.5 | 1.524763 |
| 14 | 1.549672 |
| 14.5 | 1.575408 |
| 15 | 1.60206 |
| 15.5 | 1.629731 |
| 16 | 1.658541 |
| 16.5 | 1.688629 |
| 17 | 1.720159 |
| 17.5 | 1.753328 |
| 18 | 1.78837 |
| 18.5 | 1.825576 |
| 19 | 1.865301 |
| 19.5 | 1.907997 |
| 20 | 1.954243 |
| 20.5 | 2.004799 |
| 21 | 2.060698 |
| 21.5 | 2.123385 |
| 22 | 2.194977 |
| 22.5 | 2.278754 |
| 23 | 2.380211 |
| 23.5 | 2.50965 |
| 24 | 2.690196 |
| 24.5 | 2.995635 |
| 25 | 7 |
| 25.5 | 10.99568 |
| 26 | 11.29243 |
| 26.5 | 11.46428 |
| 27 | 11.58503 |
| 27.5 | 11.67778 |
| 28 | 11.75285 |
| 28.5 | 11.81571 |
| 29 | 11.86967 |
| 29.5 | 11.91682 |
| 30 | 11.95861 |
| 30.5 | 11.99607 |
| 31 | 12.02996 |
| 31.5 | 12.06086 |
| 32 | 12.08922 |
| 32.5 | 12.11539 |
| 33 | 12.13966 |
| 33.5 | 12.16226 |
| 34 | 12.18339 |
| 34.5 | 12.20321 |
| 35 | 12.22185 |
| 35.5 | 12.23943 |
| 36 | 12.25606 |
| 36.5 | 12.27182 |
| 37 | 12.28679 |
| 37.5 | 12.30103 |
| 38 | 12.3146 |
| 38.5 | 12.32756 |
| 39 | 12.33995 |
| 39.5 | 12.35181 |
| 40 | 12.36318 |
| 40.5 | 12.37409 |
| 41 | 12.38458 |
| 41.5 | 12.39466 |
| 42 | 12.40437 |
| 42.5 | 12.41373 |
| 43 | 12.42276 |
| 43.5 | 12.43148 |
| 44 | 12.4399 |
| 44.5 | 12.44805 |
| 45 | 12.45593 |
| 45.5 | 12.46356 |
| 46 | 12.47096 |
| 46.5 | 12.47813 |
| 47 | 12.48509 |
| 47.5 | 12.49184 |
| 48 | 12.4984 |
| 48.5 | 12.50478 |
| 49 | 12.51098 |
| 49.5 | 12.51701 |
| 50 | 12.52288 |
| Quantity | Value | Unit |
|---|---|---|
| Total mixed volume | 0.05 | L |
| Analytical acid-family concentration | 0.05 | mol/L |
| Inert sodium concentration | 0.05 | mol/L |
| Exact equilibrated pH | 8.849498 | pH units |
| Equivalence volume | 25 | mL |
| Charge-balance residual | -1.387779e-17 | mol/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.
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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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