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Moridis, G.J., Collett, T.S., Dallimore, S.R., Satoh, T., Hancock, S. and Weatherill, B. (2004) Numerical Studies of Gas Production from Several CH4 Hydrate Zones at the Mallik Site, Mackenzie Delta, Canada. Journal of Petroleum Science and Engineering, 43, 219-238.
https://doi.org/10.1016/j.petrol.2004.02.015

has been cited by the following article:

• TITLE: On the Galvanic Modification of Seawater

  AUTHORS: Alexander Shimkevich

  KEYWORDS: Non-Stoichiometric Seawater, Band Gap, Fermi Level, Galvanic Cell, Electron Donor, Sodium Hypochlorite

  JOURNAL NAME: World Journal of Condensed Matter Physics, Vol.9 No.4, October 30, 2019

  ABSTRACT: Chemical properties of seawater are studied at forced shifting of Fermi level εF in the band gap of liquid water due to deviation of its composition H2O1−z ( |z｜−13 ) from the stoichiometric one ( z = 0 ). It is shown that the hypo-stoichiometric state ( z > 0 ) of seawater emerges when Fermi level is shifted to the local electron level εH3O of hydroxonium H3O+ in galvanic cell with the strongly polarized anode and the quasi-equilibrium cathode. Then, each εH3O is occupied by electron and hydroxonium radicals [H3O] together with hydroxide anions [OH−]form in seawater hydrated electrons [(H2O)2−] . The opposite hyper-stoichiometric state ( z εOH for removing electron from each hydroxide ion OH− and forming hydroxyl radicals [OH] as strong oxidizers. It turned out that the ions of sodium and chlorine are connected into hydrates of sodium hypochlorite NaClO in this case.