| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | β-Ferric oxyhydroxide—akaganéite |
|---|
| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
|---|
| Authors | Mackay, A. L. | Author |
|---|
| Year | 1962 (December) | Volume | 33 |
|---|
| Issue | 259 |
|---|
| Publisher | Mineralogical Society |
|---|
| Download URL | https://rruff.info/doclib/MinMag/Volume_33/33-259-270.pdf+ |
|---|
| DOI | doi:10.1180/minmag.1962.033.259.02Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 5700 | Long-form Identifier | mindat:1:5:5700:8 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Mackay, A. L. (1962) β-Ferric oxyhydroxide—akaganéite. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (259) 270-280 doi:10.1180/minmag.1962.033.259.02 |
|---|
| Plain Text | Mackay, A. L. (1962) β-Ferric oxyhydroxide—akaganéite. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (259) 270-280 doi:10.1180/minmag.1962.033.259.02 |
|---|
| In | (1962) Mineralogical Magazine Vol. 33 (259) Mineralogical Society |
|---|
| Abstract/Notes | SummaryA new mineral, akaganéite, has been found in limonite deposits and has been shown to be identical with synthetic β-FeOOH. It contains no chlorine. The micro-morphology of β-FeOOH as it occurs as akaganéite and as it is produced by a solid-state transformation from FeCl2.4H2O , by the hydrolysis of dilute FeCl3 solutions, and by the hydrolysis of very concentrated FeCl3 a solutions, has been studied, chiefly by electron microscopy and diffraction. Some modes of colloidal association of the particles of β-FeOOH are described. |
|---|
These are possibly similar items as determined by title/reference text matching only.
