Vander Linden, Charles
[UCL]
Li, Zimin
[UCL]
Iserentant, Anne
[UCL]
Delvaux, Bruno
[UCL]
Dissolving primary silicates release solutes (Si, Al, Fe…) that recombine to form secondary clay minerals and/or (Al, Fe) oxides. In perhumid conditions, most of H4SiO4 can be leached out whereas gibbsite (Al(OH)3) forms. Gibbsite is thus a pertinent indicator of desilication intensity and Si bioavailability
Bibliographic reference |
Vander Linden, Charles ; Li, Zimin ; Iserentant, Anne ; Delvaux, Bruno. Rainfall as the major driver of plant Si availability in gibbsitic Andosols.EGU 2020 (Vienna, Austria, du 04/05/2020 au 08/05/2020). |
Permanent URL |
http://hdl.handle.net/2078.1/230622 |