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In part I of this paper the electric behaviour of pure water is described byan interstitial-ice model, the so-called Protonic-SemiconductorInterstitial-Ice or PSII model. Liquid water consists of an intact ice-likelattice with a significant percentage of both vacant lattice positions andwater molecules filling the interstitial sites of the open ice-like lattice. Itis shown that not the Grotthuss mechanism is dominant in water but athermally-induced hopping mechanism of the H$^+$ and OH$^-$ ions linked tovacancies. In part II this hopping mechanism is further explored and confrontedto the small Hall mobilities of the ions, still unexplained with mainstreammodels. Two types of complexes are found. The first type is composed of eithercharged vacancies with the opposite charge of the ion (H$^+$VL and OH$^-$VD) orneutral vacancies (H$^+$V and OH$^-$V). These complexes are responsible for themajor part of the mobility of the ions. However, their movement is changing theelectric polarisation density of the lattice structure blocking the Hall effectof these complexes. The second type of complexes contains a vacancy chargedsimilar as the ion (H$^+$VD and OH$^-$VL). This second type is responsible foronly a small fraction of the electric mobility (10-20%), but their movement isnot altering the electric polarisation of the lattice structure. They areresponsible for the measured small Hall mobilities of the ions.

A new and coherent interstitial-ice model for pure water part II: explaining the conflicting Hall data