• The rates of
weathering of silicate bedrock are
dependent on the stability and solubility of the parent minerals.
•The degree of
polymerisation
controls the
stability.
• Bowen’s
reaction series
Increasing
susceptibility
to
weathering
(monomer) ionic (framework 100pm)
(chain)
(framework 102pm)
(double chain)
(framework 138pm)
(sheet)
(sheet)
(framework)
K-feldspar “cage”
H+ opens the cage