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ferrous ion

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ferrous ion

Traditional name for the divalent condition of iron, Fe2+; the modern name is iron(II). Ferrous salts are usually green, and form yellow-green solutions. FeSO4 is iron(II) sulphate (ferrous sulphate).



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In another study, we found that the mutagenic potential of mordenite was not enhanced by the addition of ferrous ion.
A low sulfur content, along with high bicarbonate and ferrous ion concentrations, was also found in Lake Monoun, hinting that the chemistries of the two lakes are similar.
Moreover, Sigurdsson's group measured exceptionally high concentrations of ferrous ions (iron atoms with a +2 charge) in the deep water and large amounts of siderite, an iron-carbonate mineral, in the bottom sediments.
 
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