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SAR also indicates irrigation water tendency to cation-exchange reactions in soil.
The sensitivity of the calculations to exchange reactions and the diffusion coefficient was tested.
The exchange reaction differs from simple sorption because it has a quantitative relationship between reacting ions.
For example, in the exchange reaction the hydrogen and deuterium switch partners.
The reaction is known as cation exchange reaction.
These reactions are known as cation anion exchange reaction.
Surface exchange reaction forward-rate constant (cm atm−0.5s−1).
Surface exchange reaction reverse-rate constant (mol cm−2s−1).
This indicates a direct base (cation anion) exchange reaction.
It shows TiChu's F-OH exchange reaction follows a compositional vector TiO2Mg-1 F-2.
The iodide ion-isotopic exchange reaction can be represented as: R − I + I * − aq.
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