interactions of ferric and ferrous irons and organic matter in water

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Geochemical Journal, Vol. 7, pp. 167 to 177, 1973 Interactions of ferric and ferrous irons and organic matter in water environment TOSHIKO AKIYAMA Department of Chemistry, Tokyo Metropolitan University, Setagaya, Tokyo 158, Japan (Received March 13, 1972; in revised form July 2, 1973) Abstract -Coprecipitation of organic matter with ferric and ferrous hydroxide, and iron holding in solution containing organic matter were experimentally studied. The dissolved organic matter from bacterial degradation of green algae was used. The results of the experiments showed that ferrous iron, as well as ferric iron, coprecipitate organic matter under reduced conditions, and that ferric and ferrous irons selectively co- precipitate proteinous materials. On the contrary, pigment and lipid materials are rarely coprecipitated, and hold ferric iron in dissolved form probably by forming water soluble iron-organic complexes . These results show the significance of the interaction of organic matter and iron in the cycle of them in the hydrosphere.

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Page 1: Interactions of ferric and ferrous irons and organic matter in water

Geochemical Journal, Vol. 7, pp. 167 to 177, 1973

Interactions of ferric and ferrous irons andorganic matter in water environment

TOSHIKO AKIYAMA

Department of Chemistry, Tokyo MetropolitanUniversity, Setagaya, Tokyo 158, Japan

(Received March 13, 1972; in revised form July 2, 1973)

Abstract -Coprecipitation of organic matter with ferric and ferrous hydroxide, andiron holding in solution containing organic matter were experimentally studied. Thedissolved organic matter from bacterial degradation of green algae was used. The resultsof the experiments showed that ferrous iron, as well as ferric iron, coprecipitate organicmatter under reduced conditions, and that ferric and ferrous irons selectively co-precipitate proteinous materials. On the contrary, pigment and lipid materials are rarelycoprecipitated, and hold ferric iron in dissolved form probably by forming water solubleiron-organic complexes.

These results show the significance of the interaction of organic matter and ironin the cycle of them in the hydrosphere.

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