Answers are grounded in this paper and cite their sources.
The partial molal volumes of ions in 35.1‰ salinity seawater, V*0(ion)sw, have been examined by a simple model for ion‐solvent interactions. The volume of transfer of an ion from water to seawater (ml/mol) can be represented by the equation, ΔV*0(trans) = aZ2/r + b. The V*0 of other ions in seawater have been estimated using this semiempirical equation. The effects of temperature and salinity on V*0(ions) are discussed and shown to be predictable by the proposed model.
No takes yet. Share an insight, caveat, or question.
Frank J. Millero (1969) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: