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Schwertmann, U., Stanjek, H., Becher, H.-H. (2004) Long-term in vitro transformation of 2-line ferrihydrite to goethite/hematite at 4, 10, 15 and 25°C. Clay Minerals, 39 (4) 433-438 doi:10.1180/0009855043940145

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Reference TypeJournal (article/letter/editorial)
TitleLong-term in vitro transformation of 2-line ferrihydrite to goethite/hematite at 4, 10, 15 and 25°C
JournalClay Minerals
AuthorsSchwertmann, U.Author
Stanjek, H.Author
Becher, H.-H.Author
Year2004 (December)Volume39
Issue4
PublisherMineralogical Society
DOIdoi:10.1180/0009855043940145Search in ResearchGate
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Mindat Ref. ID564141Long-form Identifiermindat:1:5:564141:7
GUID0
Full ReferenceSchwertmann, U., Stanjek, H., Becher, H.-H. (2004) Long-term in vitro transformation of 2-line ferrihydrite to goethite/hematite at 4, 10, 15 and 25°C. Clay Minerals, 39 (4) 433-438 doi:10.1180/0009855043940145
Plain TextSchwertmann, U., Stanjek, H., Becher, H.-H. (2004) Long-term in vitro transformation of 2-line ferrihydrite to goethite/hematite at 4, 10, 15 and 25°C. Clay Minerals, 39 (4) 433-438 doi:10.1180/0009855043940145
In(2004, December) Clay Minerals Vol. 39 (4) Mineralogical Society

See Also

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Schwertmann, U., Friedl, J., Stanjek, H., Schulze, D. G. (2000) The effect of clay minerals on the formation of goethite and hematite from ferrihydrite after 16 years’ ageing at 25°C and pH 4 – 7. Clay Minerals, 35 (4) 613-623 doi:10.1180/000985500547034
Schwertmann, U., Carlson, L. (2005) The pH-dependent transformation of schwertmannite to goethite at 25°C. Clay Minerals, 40 (1) 63-66 doi:10.1180/0009855054010155
Schwertmann, U. (1983) Effect of pH on the Formation of Goethite and Hematite from Ferrihydrite. Clays and Clay Minerals, 31 (4) 277-284 doi:10.1346/ccmn.1983.0310405
Stanjek, H. (2002) XRD peak migration and apparent shift of cell-edge lengths of nano-sized hematite, goethite and lepidocrocite. Clay Minerals, 37 (4) 629-638 doi:10.1180/0009855023740065
Nørnberg, P., Schwertmann, U., Stanjek, H., Andersen, T., Gunnlaugsson, H.P. (2004) Mineralogy of a burned soil compared with four anomalously red Quaternary deposits in Denmark. Clay Minerals, 39 (1) 85-98 doi:10.1180/0009855043910122
Stanjek, H. (1998) The Effect of Dry Heating of Synthetic 2-line and 6-line Ferrihydrite: II. Surface Area, Porosity and Fractal Dimension. Clay Minerals, 33 (2) 277-284 doi:10.1180/claymin.1998.033.2.10
Schwertmann, U. (1988) Goethite and Hematite Formation in the Presence of Clay Minerals and Gibbsite at 25°C. Soil Science Society of America Journal, 52 (1). 288-291 doi:10.2136/sssaj1988.03615995005200010052x
Weidler, P. G., Stanjek, H. (1998) The effect of dry heating of synthetic 2-line and 6-line ferrihydrite: II. Surface area, porosity and fractal dimension. Clay Minerals, 33 (2) 277-284 doi:10.1180/000985598545471
Torrent, J., Schwertmann, U., Barron, V. (1987) The reductive dissolution of synthetic goethite and hematite in dithionite. Clay Minerals, 22 (3) 329-337 doi:10.1180/claymin.1987.022.3.07
Schwertmann, Udo (2000) The Effect of Al on Fe Oxides. XIX. Formation of Al-Substituted Hematite from Ferrihydrite at 25°C and pH 4 To 7. Clays and Clay Minerals, 48 (2) 159-172 doi:10.1346/ccmn.2000.0480202
Schwertmann, U., Fechter, H. (1994) The Formation of Green Rust and Its Transformation to Lepidocrocite. Clay Minerals, 29 (1) 87-92 doi:10.1180/claymin.1994.029.1.10
 
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