In copper pipework, at work for about four years, blue coloured striat
ions or areas, mainly composed of posnjakite (Cu4(OH)6SO4.H2O), were f
ound (water chemistry (room temperature): pH = 8.1; SO4 = 24 mg/l; Cl
= 16 mg/l; O2 = 10 mg/l). Moreover cuprite, tenorite and malachite wer
e detected on the internal surfaces of copper pipeworks. After the pip
ework had been in operation for five years, an NaHCO3-dosing apparatus
was installed to treat water in all but one branch of the system. In
the section with treated water, sulphate formation decreased while mal
achite formation (Cu2CO3(OH)2) increased. Layer formation can be simul
ated in electroysis experiments. Normal tap water alone or mixed with
bicarbonate is used as an electrolyte.