Verifying through the ion-exchange reaction: Gypsum (calcium sulphate) dissolves in soil water to release Ca2+ ions.
These Ca2+ ions displace Na+ held on the soil's exchange complex, written as: Na2-Soil + Ca2+ → Ca-Soil + 2Na+.
The released Na+, now in the soil solution rather than on exchange sites, is removed by leaching with adequate drainage, lowering the exchangeable sodium percentage.
This matches exactly what Reason (R) describes, and it is the mechanism that makes Assertion (A) true, so (R) correctly explains (A).