Construct water-ion evidence without assuming neutral means pH 7
Build independent pH and pOH proposals, repair their product and compare temperature-dependent neutral references.
Learning outcome: Use logarithms and a stated water-ionization reference to distinguish equal ion activities, equilibrium consistency and acidity relative to neutrality.
Starting recap
pH is the negative base-10 logarithm of hydronium activity. Lowering pH by one multiplies that activity by ten. Neutrality compares hydronium and hydroxide; equilibrium also constrains their product.
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Try
At 50°C propose pH 7 and pOH 7. The two activities are equal. Does their product match the reference pKw 13.26?
Open the experimentPredict
Predict whether equality alone is sufficient. Predict the neutral pH at 50°C, then whether a consistent pH 7 solution is acidic or basic there.
Experiment
Repair both independent choices to 6.63 at 50°C. Next hold pH 7 and repair only pOH. Change to 0°C without changing either proposal, diagnose the mismatch and repair pOH again. Compare consistent pH 6 and pH 7 pairs at a fixed temperature and explain the tenfold activity change. Capture a failed and a repaired construction.
Construct a consistent water-ion pair
Calculated reference values · original ion-pair construction · Rounded IAPWS 2024 reference pKw values; original ideal dilute activity construction. Water activity is approximated as 1 and ionic activity coefficients as 1. Activities are dimensionless; the source ionic standard is molal, 1 mol/kg. This checks one equilibrium relation, not full solution composition, charge balance or a measured pH determination.
Reset keeps your prediction, captures and practice history.
Both proposals stay fixed when you change temperature. They are your constructed values, not newly measured samples.
| Check | Your construction | Interpretation |
|---|---|---|
| Equal activities? | pH 7 versus pOH 7 | Equal; this alone is insufficient. |
| Water equilibrium? | 7 + 7 = 14.000; pKw = 13.26 | Does not match the central rounded model. |
| Activity product | 1.000000e-7 × 1.000000e-7 = 1.000000e-14 | Kw = 5.495409e-14; product/Kw = 0.181970 |
| Hydronium / hydroxide | 1.000000 | No equilibrium-solution classification is assigned to the inconsistent pair. |
At 50°C, neutrality in this ideal dilute model requires pH = pOH = pKw/2 = 6.630. Equilibrium also requires aH × aOH = Kw. Activity is dimensionless: aH and aOH are the hydronium and hydroxide activities. At fixed Kw, a tenfold increase in aH requires a tenfold decrease in aOH.
Connect the reference to the classroom approximation
The source reaction is 2H₂O ⇌ H₃O⁺ + OH⁻, with Kw = aH × aOH / aWater². We approximate water activity as 1. Ionic activities use the molal standard: a = γm/m°, with m° = 1 mol/kg and γ approximated as 1 here. This does not equate mol/kg with mol/L. The familiar classroom concentration formulas additionally use a dilute-solution approximation.
A nonneutral solution needs other ions to balance charge. Passing the water relation alone does not supply those ions, establish complete composition or validate a preparation. No acid concentration or salt inventory is inferred.
Calculated source values, conditions and precision
IAPWS R11-24 (2024), Table 3, page 6: 0°C: pKw 14.95; 25°C: pKw 13.99; 50°C: pKw 13.26. Footnote b specifies liquid density at 0.1 MPa for these temperatures. These rounded values come from a reference formulation, not three newly measured samples. The full formulation is not implemented; there is no interpolation or extrapolation.
The neutral central value 6.995 at 25°C follows the printed 13.99. Its extra arithmetic digit is not measurement precision; it does not establish a resolvable experimental difference from the classroom pH 7 approximation. The source describes typical agreement with data, not a guaranteed uncertainty bound for each row. A numerical match here is an arithmetic test of the declared inputs.
This proposal does not satisfy the central rounded water-equilibrium model.
pH + pOH = 14.000 versus pKw 13.26. Ion activities are equal; the neutral reference is 6.630. Numerical matching is not experimental validation.
Captures retain your constructed pH/pOH pair and the selected calculated reference. They are not measured pH samples or validation of complete solution composition.
Understand
Apply
Public practice checks a specific claim. It does not establish independent mastery.
Show both the sum of logarithms and product of activities. Distinguish an exact arithmetic check of rounded inputs from a measured pH conclusion. Explain the water-activity approximation and why passing this one relation does not establish the full ionic composition.
Continue
Completion requires a saved prediction, at least one capture and a reflection. Presence checks do not grade your reasoning.
Skipping retains experiments and awards no mastery.
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