A large area in the Mekong delta is covered by acidic sulphate soils.
Arsenic (As) and selenium (Se) are two potentially harmful elements th
at may accumulate in such sulphidic environments. Mapping of the abund
ance and fate of these elements during reclamation was therefore initi
ated. Results indicate that the soils are slightly enriched with As, b
ut not with Se. The solubility of As varied considerably within the so
il profiles and was much influenced by the redox conditions. Drainage,
therefore, resulted in a downward shift of the zone with the highest
As solubility. Selenium appeared to be practically immobile in all hor
izons studied. It was concluded that the drainage of these soils may r
esult in high initial As concentrations in the drainage water, but als
o that As becomes largely unavailable to plants.