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Please be aware that this old REACH registration data factsheet is no longer maintained; it remains frozen as of 19th May 2023.

The new ECHA CHEM database has been released by ECHA, and it now contains all REACH registration data. There are more details on the transition of ECHA's published data to ECHA CHEM here.

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Environmental fate & pathways

Endpoint summary

Administrative data

Description of key information

Additional information

Triiron bis(orthophosphate) (CAS 14940-41-1) is an inorganic phosphate substance. Biotic degradation is therefore not relevant for the substance. Furthermore abiotic degradation processes like photolysis in air, water and soil are not likely. In water, soil and biological systems, dissolved Triiron bis(orthophosphate) dissociates to orthophosphate and ferrous ion (Fe2+).

“Redox transformation of iron, as well as dissolution and precipitation and thus mobilization and redistribution, are caused by chemical and to a significant extent by microbial processes (see attachment Fig. 1) (Kappler A. and Straub K. L. 2005).”

Transformations of iron by microorganisms are often much faster than the respective chemical reactions. They occur in most soils and sediments, both in freshwater and marine environments (Thamdrup 2000; Straub et al. 2001; Cornell and Schwertmann 2003).

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).

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).

Orthophosphate is available for biological metabolism without further breakdown. Besides of chemical precipitation phosphate can be biologically removed from waste water. Biological phosphate removal process is relies upon microorganisms to uptake phosphate into their cells either via anaerobic or anaerobic pathways, which is subsequently removed from the STP process as a result of sludge wasting.

 

References:

Boyd PW, Ellwood MJ (2010) The biogeochemical cycle of iron in the ocean. Nature Geoscience 3, 675–682.

Cornell R. M. and Schwertmann U. (2003).The iron Oxides: Structures, Properties, Reactions, Occurrences and Uses. Wiley-VCH, Weinheim

Kappler A. and Straub K.L. (2005). Geomicrobiological Cycling of Iron. Reviews in Mineralogy & Geochemistry, Vol. 59, pp 85-108

Konhauser KO, Kappler A, Roden EE (2011) Iron in microbial metabolisms. Elements 7, 89–93.

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

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))

Straub K. L., Benz M., Schink B. (2001).Iron metabolism in anoxic environments at near neutral pH. FEMS Microbiol Ecol 34: 181-186

Stumm, W. and Morgan, J. J. (1981). Aquatic Chemistry. Wiley: New York

Thamdrup B. (2000). Bacterial manganese and iron reduction in aquatic sediments. In: Advances in microbial ecology. Schink B. (ed) Kluwer Academic/ Plenum Publishers, New York, p 41-84

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))