Interactions of fulvic acid with aluminium and a proto‐imogolite sol: the contribution of E‐horizon eluates to podzolization
- 1 June 2001
- journal article
- research article
- Published by Wiley in European Journal of Soil Science
- Vol. 52 (2) , 177-188
- https://doi.org/10.1046/j.1365-2389.2001.00377.x
Abstract
No abstract availableKeywords
This publication has 45 references indexed in Scilit:
- Distribution and mobilization of Al, Fe and Si in three podzolic soil profiles in relation to the humus layerGeoderma, 2000
- Surface reactivity of poorly-ordered minerals in podzol B horizonsGeoderma, 2000
- Low molecular weight organic acids and their Al-complexes in soil solution—composition, distribution and seasonal variation in three podzolized soilsGeoderma, 2000
- Advances in understanding the podzolization process resulting from a multidisciplinary study of three coniferous forest soils in the Nordic CountriesGeoderma, 2000
- The podzolization process. A reviewGeoderma, 2000
- The solubility characteristics of organic Al precipitates in allophanic Bs horizons could mimic those of Al hydroxides, and indicate the solubility of associated allophanesEuropean Journal of Soil Science, 1999
- Aluminium solubility characteristics of spodic B horizons containing imogolite-type materialsClay Minerals, 1998
- Synthetic Allophanes Formed in Calcareous Environments: Nature, Conditions of Formation, and TransformationsSoil Science Society of America Journal, 1991
- Iron substitution in aluminosilicate sols synthesized at low pHClay Minerals, 1984
- Chemical and colloidal stability of sols in the Al2O3‐Fe2O3‐SiO2‐H2O system: their role in podzolizationEuropean Journal of Soil Science, 1982