Maize, sorghum, and millet monoculture effects on soil properties of a Typi
c Ustipsamment in the semiarid pampa of Argentina were evaluated after 27 y
ears in a plot experiment. A permanent Eragrostis curvula pasture was used
as a reference. Miller was the most destructive crop to the soil because it
decreased dry aggregate stability by 10%, soil organic matter (OM) by 30%,
extractable K by 20%, available P by 44%, inorganic P by 11%, available Fe
by 20%, available Zn more than 90%, available Cu by 30%, and available Mn
by 26%, and it increased wet aggregate instability by 75%. Grain sorghum wa
s less destructive to the soil than millet because it only decreased OM by
30% and extractable K by 24%. All studied crops decreased the cation exchan
ge capacity of the soil between 20 and 30%, the pH values, and the concentr
ation of soil extractable Mg2+ by 38 to 63%. Soil extractable Ca2+ was decr
eased 30% by the Eragrostis pasture and 40% by maize. The negative effect o
f millet and grain sorghum on OM was attributed to a low coverage of the so
il with plant residues left by these crops as well as the long exposition o
f the bare soil during temperate and wet periods. Decreases of soil nutrien
t contents were attributed to plant uptake in all cases, except the Zn conc
entrations, which were related to variations on soil pH and phosphate conce
ntrations. It was concluded that maize, the most commonly cultivated crop i
n the region studied, did not affect physical and chemical soil properties
to a large extent. Conversely, millet had the most negative effect on physi
cal and chemical properties of the soil.