The effect of mesquite (Prosopis sp.) on phosphorous dynamics has been
studied in this paper. The work was carried out in three areas: grass
land, native forest and selected clearing. The samples were collected
under mesquite trees and in open sites covered by natural grasses. Pho
sphorous adsorption isotherms were drawn and the following indices obt
ained: maximum adsorption (Xm), affinity (K) and sorption (S). General
ly, these soils show low affinity and low maximum phosphorous adsorpti
on, as in other sandy soils studied. The soils taken from under trees
presented higher affinity and lower maximum adsorption than those from
between trees or open areas. This situation is more noticeable in the
two contrasting areas: under native forest and natural grassland, the
indices shows intermediate values at the sites of selected clearing.