Codex @codex  0

The source may be a pipe, cistern, service connection or fitting. Robert Christison's pre-examination experiments addressed the action of different waters on metallic lead: very pure waters, including distilled water or rainwater, could attack it, whereas salts in many natural waters modified the process. This provides a contemporary basis for treating the character of the supply, as well as the material of the cistern or pipe, as important.^[ref]

The dissolving tendency is called plumbosolvency. In modern chemical terms, low pH and low alkalinity can favour the release of lead. Dissolved oxygen supports corrosion of the metal; dissolved carbon dioxide affects both acidity and carbonate chemistry. Carbonate deposits can provide a partly protective surface layer, while conditions favouring their dissolution can increase release. It is therefore misleading to say simply that all carbon dioxide prevents contamination or that all waters containing it dissolve lead to the same degree. Water hardness and alkalinity are related features of many waters but are not interchangeable quantities.^[ref]

Long contact, especially stagnation overnight or through disuse, can increase contamination. Warmer conditions, changes in the supply chemistry, disturbance of an old pipe and the condition of accumulated deposits can also matter. Water can carry dissolved lead or particles containing lead; an old apparently coated pipe is not an assurance that release has ceased. Modern supplies may additionally encounter lead-bearing solder or brass, which should be recognized as a present comparison rather than assumed to be the construction of a particular 1864 installation.^[ref]

A clear appearance and acceptable taste cannot exclude lead. Investigate the actual plumbing materials and analyse appropriately collected samples, recording the period of standing and other conditions instead of inventing a concentration. The most direct way to remove the source is replacement of lead-bearing components; treatment that controls corrosion is chemistry-dependent and is not equivalent to a universal guarantee from a hard-water scale. These considerations answer when contamination is likely without imposing an unsupported period numerical threshold.

Fresh rainwater is ordinarily soft because evaporation leaves most nonvolatile dissolved salts behind; “always” is an idealization, not an exceptionless law. Water hardness is principally caused by dissolved calcium and magnesium ions. Water vapour rising from a hard-water source does not carry these ions with it as vapour. Condensation consequently supplies low-mineral water before contact with dust, surfaces or soil. Mineral particles, sea spray and a collecting surface can add salts, so actual collected rainwater need not have zero water hardness. Nor does softness establish purity or freedom from microorganisms.^[ref]

The historically appropriate quantitative principle is soap titration of water hardness. Soluble soap reacts with hardness-producing ions to form poorly soluble salts, using up soap before a persistent lather can form. For a representative carboxylate soap,Magnesium behaves similarly. Once the dissolved hardness-producing ions have substantially reacted, additional soap can sustain the specified lather. The endpoint is therefore an operational observation under standardized shaking, standing time, temperature and sample volume; it is not the first transient bubble.

Use a measured volume of sample in a stoppered vessel with enough headspace for shaking. Add a soap solution of known strength incrementally from a burette, shaking in a reproducible way, until the chosen persistent-lather endpoint appears. Determine a blank with a corresponding amount of soft or distilled water, because some soap is needed for the lather even when no hardness salts are present. Standardize the soap against a reference solution containing a known calcium amount, expressed as an equivalent mass of calcium carbonate. This standardization is essential: the apparent strength cannot safely be inferred from the mass of an incompletely characterized commercial soap.

Let $V_s$ be the sample volume in millilitres, $V$ the soap titre in millilitres and $B$ the corresponding blank. If $f$ is the standardized capacity in milligrams of calcium carbonate equivalent per millilitre of soap solution, thenFor a standard containing $m_0$ milligrams of calcium carbonate equivalent and requiring blank-corrected titre $V_0-B_0$, $f=m_0/(V_0-B_0)$. This makes the measurement quantitative without assuming an unreported soap concentration or inventing a sample titre. Historical results could instead be stated as grains of calcium carbonate equivalent per gallon, provided the gallon convention was specified.

Repeating the examination after controlled boiling, cooling, removal of the precipitate and restoration of the original volume estimates the residual or permanent hardness. The reduction estimates the boiling-removable fraction, often called temporary hardness. A representative reaction isCarbonate equilibria and magnesium chemistry make this more subtle than assuming every dissolved salt is destroyed by boiling. Very hard samples may need measured dilution; magnesium, other metal ions and contamination can disturb the lather endpoint. Thus the soap result is an experimentally calibrated hardness equivalent, not an exact identification of every original salt.