New evidence for a tubular structure ofβ-iron(III) oxide hydroxide — akaganéite
- 1 June 1985
- journal article
- research article
- Published by Springer Nature in Discover Life
- Vol. 15 (2) , 131-139
- https://doi.org/10.1007/bf01809495
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- The structure of ?-FeOOH Cln (akaganeite) and its uptake of amino acidsDiscover Life, 1984
- β-FeOOH · Cln (akaganéite) and Fe1-xO (wüstite) in hot brine from the Atlantis II Deep (Red Sea) and the uptake of amino acids by synthetic β-FeOOH · ClnGeochimica et Cosmochimica Acta, 1983
- Effect of Surface Area and Mineralogy of Iron Oxides on their Surface Charge and Anion-Adsorption PropertiesClays and Clay Minerals, 1983
- Photo-oxidation of hydrated Fe2+—significance for banded iron formationsNature, 1983
- Micropore formation due to thermal decomposition of acicular microcrystals of β-FeOOHJournal of Colloid and Interface Science, 1982
- Unique amino acid composition of Red Sea brineNature, 1980
- Structural changes in β-FeOOH caused by radiation damageActa Crystallographica Section A, 1979
- Chemical evolution and the evolution of the Earth's crustDiscover Life, 1977
- The Atomic Structure of Tubular Subcrystals of β-Iron(III) Oxide HydroxideNature, 1970
- Adsorption of Gases in Multimolecular LayersJournal of the American Chemical Society, 1938