• In the tropics temperatures are high and so the
weathering reactions will occur quickly.
10oC increase in T doubles rate of most rxns
• Rainfall is
heavy and this allows constant
flushing of the
weathering material, leaching
out all but the most
insoluble material
eg. FeOOH (goethite),
Al(OH)3 (gibbsite).
• Soil humic matter is the microbially transformed, polymeric organic materials
that persists in soils (humic & fulvic acids).
• Humic matter binds to mineral surfaces thru functional groups & thru chelation to form soluble metal-humic
complexes.