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In Oxisols, Fe(III) substitution for Al is observed in kaolinite. Develop a balanced chemical reaction for the incongruent dissolution of ferri-kaolinite [Si4(Al1yFey)4O10(OH)8], assuming the principal

In Oxisols, Fe(III) substitution for Al is observed in kaolinite. Develop a balanced chemical reaction for the incongruent dissolution of ferri-kaolinite [Si4(Al1–yFey)4O10(OH)8], assuming the principal weathering products to be goethite, gibbsite, and silicic acid

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