250
C. De Stefano· C. Foti . A. Gianguzza . D. Piazzese . S. Sammartano
but can be considerable for the metallic and organometallic cations. A recent investigation (Foti et al. 2000) showed that the addition of carbonate ([CO~-] + [HCO;]
= 2.7 mmol rl, for sea water 35 S) to the basic inorganic speciation model of organotins
in synthetic sea water leads to the formation (at pH = 8) of a very stable mixed species (CH3)Sn(C03)(OHh in the monomethyltin system, whilst it is absolutely negligible for the other dimethyl and trimethyltin systems at the same pH value
(see Table A9.8, Sect. A9.2 of appendix). Interactions of organotin cations and hydroxo
species with floride ions ([F-] = 0.07 mmol rI, for sea water 35 S) are very weak, and
no complex species are formed.
As concerns the possibility of having predictive relationships, we showed that
polycarboxylic anions form complexes whose stability follows very regular trends.
Moreover, apparent protonation constants can be expressed as a function of salinity
by simple polynomial equations, whose empirical parameters mainly depend on the
protonation step.
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