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EC number: 239-018-0 | CAS number: 14940-41-1
- Life Cycle description
- Uses advised against
- Endpoint summary
- Appearance / physical state / colour
- Melting point / freezing point
- Boiling point
- Density
- Particle size distribution (Granulometry)
- Vapour pressure
- Partition coefficient
- Water solubility
- Solubility in organic solvents / fat solubility
- Surface tension
- Flash point
- Auto flammability
- Flammability
- Explosiveness
- Oxidising properties
- Oxidation reduction potential
- Stability in organic solvents and identity of relevant degradation products
- Storage stability and reactivity towards container material
- Stability: thermal, sunlight, metals
- pH
- Dissociation constant
- Viscosity
- Additional physico-chemical information
- Additional physico-chemical properties of nanomaterials
- Nanomaterial agglomeration / aggregation
- Nanomaterial crystalline phase
- Nanomaterial crystallite and grain size
- Nanomaterial aspect ratio / shape
- Nanomaterial specific surface area
- Nanomaterial Zeta potential
- Nanomaterial surface chemistry
- Nanomaterial dustiness
- Nanomaterial porosity
- Nanomaterial pour density
- Nanomaterial photocatalytic activity
- Nanomaterial radical formation potential
- Nanomaterial catalytic activity
- Endpoint summary
- Stability
- Biodegradation
- Bioaccumulation
- Transport and distribution
- Environmental data
- Additional information on environmental fate and behaviour
- Ecotoxicological Summary
- Aquatic toxicity
- Endpoint summary
- Short-term toxicity to fish
- Long-term toxicity to fish
- Short-term toxicity to aquatic invertebrates
- Long-term toxicity to aquatic invertebrates
- Toxicity to aquatic algae and cyanobacteria
- Toxicity to aquatic plants other than algae
- Toxicity to microorganisms
- Endocrine disrupter testing in aquatic vertebrates – in vivo
- Toxicity to other aquatic organisms
- Sediment toxicity
- Terrestrial toxicity
- Biological effects monitoring
- Biotransformation and kinetics
- Additional ecotoxological information
- Toxicological Summary
- Toxicokinetics, metabolism and distribution
- Acute Toxicity
- Irritation / corrosion
- Sensitisation
- Repeated dose toxicity
- Genetic toxicity
- Carcinogenicity
- Toxicity to reproduction
- Specific investigations
- Exposure related observations in humans
- Toxic effects on livestock and pets
- Additional toxicological data
Hydrolysis
Administrative data
Link to relevant study record(s)
Description of key information
Key value for chemical safety assessment
Additional information
An experimental study on hydrolysis as a function of pH is not available for Triiron bis(orthophosphate) (CAS 14940-41-1).
The iron transport and distribution depend on pH, Eh (redox) and the presence or absence of other dissolved constituents which form with FE(II) or FE(III) dissolved complexes, colloids or poorly soluble mineral phases (Boyd and Ellwood 2010; Konhauser et al. 2011a; Radic et al. 2011; Raiswell 2011). With increasing Eh and pH the amount if iron dissolved in groundwaters, rivers and seawater decreases (see attachment Fig. 2) (Kendall 2012).
Basically Triiron bis(orthophosphate) is subject to hydrolysis when the substance is released to water. During hydrolysis, Triiron bis(orthophosphate) decomposes into iron and orthophosphate ion, whereas Ferric iron (Fe3+) is the stable form in oxygenated waters, which forms at neutral pH highly insoluble oxides and hydroxides (Wang 1998; Simpson 2002; Zhang 1999). In anoxic waters ferrous iron (Fe2+) is stable. As dissolved ion it occurs usually in many freshwater systems. Insoluble salts will be formed in the presences of high carbonate, sulphide and orthophosphate levels (Stumm, W. and Morgan, J. J. 1981).
The 2+ and 3+ oxidation states of iron are stable over broad regions of potentials and pH. Ferric ion can be reduced by hydrogen, while ferrous ions are slowly oxidized by air. The hydrolysis of ferric ions in aqueous solutions is a complicated time-dependent system. It can be defined as hydrolysis-polymerization-precipitation. A simple mechanism describes the process into several steps: (a) primary hydrolysis giving rise to low-molecular-weight complexes (mono- and dimer), i.e., Fe(OH)2+, Fe(OH)2+, Fe2(OH)24+; (b) formation and aging of polynuclear polymers, i.e., Fen(OH)m(H2O)x(3n-m)+ or FenOm(OH)x(3n-2m-x)+; (c) precipitation of ferric oxides and hydroxides, i.e., Fe(OH)3, FeOOH, and Fe2O3. The whole process from hydrolysis to precipitation can take several years. At pH < 7, the dominant species of ferric solution are Fe(OH)2+, Fe(OH)2+, Fe2(OH)24+, Fe(OH)3, FeO(OH) and FeCl2+ (Martin, 1998).
The ferric species in the aqueous solution are theoretically dominated by the following reactions, the strengths of which vary with pH:
[Fe(H2O)n(OH)(m−1)]4−m + H2O ⇄ [Fe(H2O)n−1(OH)m]3−m + H3O+
The inorganic phosphates are normally found in different forms (see attachment). In dilute aqueous solution, phosphate exists in four forms. In strongly-basic conditions, the phosphate ion (PO43−) predominates, whereas in weakly-basic conditions, the hydrogen phosphate ion (HPO42−) is prevalent. In weakly-acid conditions, the dihydrogen phosphate ion (H2PO4−) is most common. In strongly-acid conditions, aqueous phosphoric acid (H3PO4) is the main form.
References
Boyd PW, Ellwood MJ (2010) The biogeochemical cycle of iron in the ocean. Nature Geoscience 3, 675–682.
Kendall B., Anbar A.D., Kappler A. and Konhauser K.O. (2012).The global iron cycle. In book: Fundamentals of Geobiology, Blackwell Publishing Ltd., chapter 6, 65-92
Konhauser KO, Kappler A, Roden EE (2011) Iron in microbial metabolisms. Elements 7, 89–93.
Martin, R. L., Hay, J. P., Pratt L.R. (2008). Hydrolysis of Ferric Ion in Water and Conformational Equilibrium, J. Chem. Phys., A, 1998, 102, 3565-3573
Radic A, Lacan F, Murray JW (2011) Iron isotopes in the seawater of the equatorial Pacific Ocean: new constraints for the oceanic iron cycle. Earth and Planetary Science Letters 306, 1–10.
Raiswell R (2011) Iron transport from the continents to the open ocean: the aging-rejuvenation cycle. Elements 7, 101–106.
Simpson, S.L., Rochford, L. and Birch, G.F. (2002) Geochemical influences on metal partitioning in contaminated estuarine sediments. Marine and Freshwater Research, 53, 9-17 (cited in: Xing W. and Liu G. (2011))
Stumm, W. and Morgan, J. J. (1981). Aquatic Chemistry. Wiley: New York
Wang, S.M. and Dou, H.S. (1998). Chinese Lake Notes. Science, Press: Beijing. (In Chinese) (cited in: Xing W. and Liu G. (2011))
Xing W. and Liu G. (2011) IRON BIOGEOCHEMISTRY AND IST ENVIRONMENTAL IMPACTS IN FRESHWATER LAKES. Fresenius Environmental Bulletin, Vol 20, No. 6, 1339-1345.
Zhang, X.H. (1999) Iron cycle and transformation in drinking water source. Water and wastewater, 25, 18-22. (In Chinese) (cited in: Xing W. and Liu G. (2011))
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