1948
DOI: 10.1038/162027b0
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Evolution of Hydrogen from Ferrous Hydroxide

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Cited by 42 publications
(17 citation statements)
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“…Evidence for this viewpoint is provided by the hydrolysis property of Na-tochilinite, which releases Fe 2+ ions in dilute aqueous solutions spontaneously, and by the non-hydrolysis property of FeMgAl tochilinite (Peng et al, 2007). Thus, some of the magnetite in the matrix of CM carbonaceous chondrites may have been formed by Fe 2+ ions released from previously formed unstable phases like tochilinite and TSI when the reducing strength of the environment of the CM chondrite parent body decreased (Evans and Wanklyn, 1948;Shipko and Douglas, 1956;Schrauzer and Guth, 1976). As for pyrrhotite, some of them may have been formed from the mackinawite-like phase Fe 1Àx S dissociated from some unstable tochilinites and TSI and/or from mackinawite produced by the reaction of Fe 2+ ions released from previously formed tochilinites and TSI and S 2À ions.…”
Section: Applications To Meteoriticsmentioning
confidence: 86%
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“…Evidence for this viewpoint is provided by the hydrolysis property of Na-tochilinite, which releases Fe 2+ ions in dilute aqueous solutions spontaneously, and by the non-hydrolysis property of FeMgAl tochilinite (Peng et al, 2007). Thus, some of the magnetite in the matrix of CM carbonaceous chondrites may have been formed by Fe 2+ ions released from previously formed unstable phases like tochilinite and TSI when the reducing strength of the environment of the CM chondrite parent body decreased (Evans and Wanklyn, 1948;Shipko and Douglas, 1956;Schrauzer and Guth, 1976). As for pyrrhotite, some of them may have been formed from the mackinawite-like phase Fe 1Àx S dissociated from some unstable tochilinites and TSI and/or from mackinawite produced by the reaction of Fe 2+ ions released from previously formed tochilinites and TSI and S 2À ions.…”
Section: Applications To Meteoriticsmentioning
confidence: 86%
“…86-1346), while the N 2 H 4 IC remained unchanged. If we assume that elemental Fe first hydrolyzed to form Fe(OH) 2 , then Fe(OH) 2 transformed into Fe 3 O 4 in this reaction (Evans and Wanklyn, 1948;Shipko and Douglas, 1956;Schrauzer and Guth, 1976), we may reach a conclusion that aqueous Fe 2+ ions and Fe(OH) 2 could not reduce the intercalated N 2 H 4 into NH 3 .…”
Section: Nh 3 Icmentioning
confidence: 97%
“…All these models are based on the previous one proposed by Evans 1 for the corrosion of iron in caustic solution and assume a duplex microstructure for the growing corrosion scale combined with assumptions about transport phenomena, 2 scale dissolution 3,4 and pore blocking and precipitation. 1,5 The most recent model proposed by Gardey 6,7 for the corrosion of Alloy 600 combines the models of Evans, 1 Robertson 3,4 and Lister 5 and considers the growth of a corrosion scale consisting of three different layers, the innermost acting as a diffusion barrier and the outermost being porous.…”
Section: Introductionmentioning
confidence: 99%
“…The curves clearly reveal that u increases as the temperature increases and decreases as the concentration of CuCl 2 increases. Reaction (2) which is called the Schikorr reaction [26] has been extensively studied [27,28]. Ferrous hydroxide, Fe(OH) 2 , decomposes rapidly above 100 C [29], but relatively slowly at lower temperatures.…”
Section: Retention Coefficientmentioning
confidence: 99%