The formation and stability of Mg2+ and Ca2+–phytate complexes was studied potentiometrically using an ISE-H+ electrode. Measurements were performed at 10 °C and 25 °C in NaClaq in the ionic strength range 0.1≤I≤0.75 mol L−1. For both magnesium and calcium systems, the formation of ten MiPhyHj (12−2i−j)− species was observed in the range 3≤pH≤7 with i=1, 2, 3 and j=3, 4, 5 (and i=3, j=2). These species are quite stable; here we report for example some quantitative data for the species CaiPhyH3 (9−2i)−, i=1, 2, 3 (equilibrium iCa2++HjPhy(12−j)−= CaiPhyHj (12−j−2i)−: Kij) at I=0.25 mol L−1 and t=25 °C: logK13=3.42, logK23=6.47 and logK33=9.41. The speciation of the Ca2+–phytate system was also checked by ISE-Ca2+ measurements. Dependence on ionic strength was modeled using a simple Debye–Hückel type equation and formation constants were calculated at infinite dilution. The stability constants of complexes formed at pH>7 were estimated using an empirical predictive equation. The sequestering ability of phytate towards Mg2+ and Ca2+ was calculated in different experimental conditions and compared with those of other chelating agents.

Speciation of phytate ion in aqueous solution. Sequestration of magnesium and calcium by phytate at different teperatures and ionic strengths, in NaClaq.

CREA, PASQUALE;DE ROBERTIS, Alessandro;DE STEFANO, Concetta;SAMMARTANO, Silvio
2006-01-01

Abstract

The formation and stability of Mg2+ and Ca2+–phytate complexes was studied potentiometrically using an ISE-H+ electrode. Measurements were performed at 10 °C and 25 °C in NaClaq in the ionic strength range 0.1≤I≤0.75 mol L−1. For both magnesium and calcium systems, the formation of ten MiPhyHj (12−2i−j)− species was observed in the range 3≤pH≤7 with i=1, 2, 3 and j=3, 4, 5 (and i=3, j=2). These species are quite stable; here we report for example some quantitative data for the species CaiPhyH3 (9−2i)−, i=1, 2, 3 (equilibrium iCa2++HjPhy(12−j)−= CaiPhyHj (12−j−2i)−: Kij) at I=0.25 mol L−1 and t=25 °C: logK13=3.42, logK23=6.47 and logK33=9.41. The speciation of the Ca2+–phytate system was also checked by ISE-Ca2+ measurements. Dependence on ionic strength was modeled using a simple Debye–Hückel type equation and formation constants were calculated at infinite dilution. The stability constants of complexes formed at pH>7 were estimated using an empirical predictive equation. The sequestering ability of phytate towards Mg2+ and Ca2+ was calculated in different experimental conditions and compared with those of other chelating agents.
2006
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11570/1727768
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