The alteration process of natural oxidation of magnetite from the capping of magnetite deposits at Takanokura Mine, Fukushima Prefecture may be induced as follows : chemical formula The natural oxidation of magnetite from all other deposits in Japan may be taken to have followed some part of the above formula. In this report, the mineralogical properties of some minerals altered from magnetite, namely, hydrous magnetite, maghemite and goethite, are also described
Fe(III) ratio (x) was varied from 0.10 to 0.50. After stabilization by aging at pH- ~ 8 in anaerobic...
Microscope studies of a wide range of ores and fresh, oxidized, or partly iron-enriched, banded iron...
Two kinds of magnetites, one dense lumps (magnetite I) and the other with conspicuous parting in the...
Hematite changes, under the influence of meteoric and underground water, into hydrous hematite somew...
Mineralogical study was made of one sample each of weathering products of siderite and ferroan rhodo...
application/pdfHematite changes, under the influence of meteoric and underground water, into hydrous...
Some varieties of hydrated ferric oxides altered from pure Japanese pyrrhotite consist chiefly of go...
Hydrated iron oxide minerals (so-called limonite) formed under oxidizing conditions at ordinary temp...
Hydrous iron oxides altered from the titaniferous iron sands from 4 different localities in Aomori P...
Pure α-Fe_2O_3 powder prepared by oxidation of Fe(CO)_5, was reduced to Fe_3O_4 by the hydrogen stre...
ABSTRACT: Small amounts of Fe(IlI) induce precipitation f Fe(II) from carbonate solutions around neu...
Abstract--In the absence of oxygen, Fe(II) chloride, sulfate, and carbonate solutions react at pH 6....
In natural systems iron oxides and hydroxides are frequently associated with a variety of cations wh...
the stages involved in the oxidation of magnetite. Mr. Gokhale's failure to consider all of the...
Data on the phases and transformations in the iron oxide -water systems are collected. Measurements ...
Fe(III) ratio (x) was varied from 0.10 to 0.50. After stabilization by aging at pH- ~ 8 in anaerobic...
Microscope studies of a wide range of ores and fresh, oxidized, or partly iron-enriched, banded iron...
Two kinds of magnetites, one dense lumps (magnetite I) and the other with conspicuous parting in the...
Hematite changes, under the influence of meteoric and underground water, into hydrous hematite somew...
Mineralogical study was made of one sample each of weathering products of siderite and ferroan rhodo...
application/pdfHematite changes, under the influence of meteoric and underground water, into hydrous...
Some varieties of hydrated ferric oxides altered from pure Japanese pyrrhotite consist chiefly of go...
Hydrated iron oxide minerals (so-called limonite) formed under oxidizing conditions at ordinary temp...
Hydrous iron oxides altered from the titaniferous iron sands from 4 different localities in Aomori P...
Pure α-Fe_2O_3 powder prepared by oxidation of Fe(CO)_5, was reduced to Fe_3O_4 by the hydrogen stre...
ABSTRACT: Small amounts of Fe(IlI) induce precipitation f Fe(II) from carbonate solutions around neu...
Abstract--In the absence of oxygen, Fe(II) chloride, sulfate, and carbonate solutions react at pH 6....
In natural systems iron oxides and hydroxides are frequently associated with a variety of cations wh...
the stages involved in the oxidation of magnetite. Mr. Gokhale's failure to consider all of the...
Data on the phases and transformations in the iron oxide -water systems are collected. Measurements ...
Fe(III) ratio (x) was varied from 0.10 to 0.50. After stabilization by aging at pH- ~ 8 in anaerobic...
Microscope studies of a wide range of ores and fresh, oxidized, or partly iron-enriched, banded iron...
Two kinds of magnetites, one dense lumps (magnetite I) and the other with conspicuous parting in the...