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5-FeOOH

Magnetic properties of feroxyhyte (8-FeOOH) Phys. Chem. Min. 22 333-341 Bender-Koch, C. Morup, S Madsen, M.B. ... [Pg.559]

Ishikawa, T. Cai,W.Y. Kandori, K. (1992) Characterization of the thermal decomposition products of 8-FeOOH by Eourier-trans-form infrared spectroscopy and N2 adsorption. J. Chem. Soc. Faraday Trans. I. 88 1173-1177... [Pg.591]

Patrat, G. Debergevin, F. Pemet, M. Joubert, J.C. (1983) Structural locale de 8-FeOOH. [Pg.615]

Schwertmann, U. Carlson, L. (1980) Natural occurrence of feroxyhite (8- FeOOH). Clays Clay Min. 28 272-280... [Pg.624]

Other candidate Fe(III) oxides not listed include magnetite (Fe304) feroxyhyte, 8 -FeOOH ferrihydrite, Fe507(0H).4H20. [Pg.419]

In addition to a-FeOOH, (/8, y, 8)-FeOOH have been synthesized. The last varieties apparently are metastable and convert to hematite a-Fe203 when boiled, with a-FeOOH formed as an intermediate phase (Butler and Ison, 1965). All the other mineral species (limonite, turgite, hydrogoethite) are goethite with a variable amount of adsorbed water, or mixtures of goethite, amorphous iron hydroxides, and sometimes hematite. [Pg.274]

FIG. 6 Frequency dependence of electric birefringence Kic from NaCMC solution, , and electric light scattering a from 8-FeOOH suspension, stabilized by addition... [Pg.318]

Then, they prepared the catalysts using ruthenium carbonyl [22]. They found that for two iron oxides (a- and 8-FeOOH) the reaction rate constants are considerably higher than those of reactions with other catalysts based on RuCla. [Pg.28]

TABLE 2.1 Conversion Degree (%) in the Water-Gas Shift Reaction, RuCla-Impregnated Iron Oxide-Hydroxide Catalysts (a- and 8-FeOOH) 03 g of the Catalyst, Reaction Temperature 350 °C... [Pg.29]

Gotic, M., Popovic, S., Music, S. Formation and characterization of 8-FeOOH. Mater. Lett. [Pg.363]

Feroxyhyte (8-FeOOH) occurs naturally in soils in poorly crystallised (disordered) form, but is more common as a synthetic phase, belonging to the hexagonal system (Cornell and Schwertmann, 1996). Natural feroxyhytes occur above weathered basalts and have so far only been identified on Hawaii (Parfitt et al, 1988). Synthetic feroxyhyte may be produced by titrating iron(II) chloride with sodium hydroxide and water (Schwertmann and Cornell, 2000). Identifications in works of art are not yet known. [Pg.156]

Figure 5.16 Sirucuires of (a) gocihiie a-FeOOH and (b) akaganeiie /8-FeOOH... Figure 5.16 Sirucuires of (a) gocihiie a-FeOOH and (b) akaganeiie /8-FeOOH...

See other pages where 5-FeOOH is mentioned: [Pg.11]    [Pg.22]    [Pg.64]    [Pg.105]    [Pg.378]    [Pg.385]    [Pg.574]    [Pg.592]    [Pg.421]    [Pg.160]    [Pg.5]    [Pg.148]    [Pg.241]    [Pg.254]    [Pg.309]    [Pg.395]    [Pg.317]    [Pg.793]    [Pg.6]    [Pg.8]    [Pg.127]    [Pg.471]    [Pg.471]    [Pg.474]    [Pg.490]    [Pg.200]    [Pg.429]    [Pg.429]   
See also in sourсe #XX -- [ Pg.6 , Pg.22 , Pg.57 , Pg.94 , Pg.105 , Pg.125 , Pg.359 , Pg.378 ]




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8-FeOOH Neel temperature

8-FeOOH cation substitution

8-FeOOH colour

8-FeOOH crystal structure

8-FeOOH dehydroxylation

8-FeOOH formation

8-FeOOH magnetic properties

8-FeOOH surface area

8-FeOOH unit cell

A-FeOOH

A-FeOOH samples

Atmospheric corrosion FeOOH

Dehydroxylation of FeOOH

FeOOH and feroxyhyte

FeOOH structures

FeOOH, precipitation

FeOOH, precipitation oxyhydroxides

Ferric oxides 6-FeOOH

Goethite a-FeOOH

High pressure FeOOH

Iron -oxide.hydroxide FeOOH

Iron oxide, hydrated form [FeOOH

Iron oxyhydroxide FeOOH

Lepidocrocite (7-FeOOH)

Lepidocrocite y-FeOOH

Magnetic particles FeOOH

Oxidation FeOOH

P-FeOOH

Precipitation of Iron Oxides from Dense p-FeOOH Suspensions

Y-FeOOH

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