The structure of soils in areas of rain forest cleared for pasture is often
compacted due to trampling by animals. Then pasture is abandoned, regenera
tion of forest cover may be achieved from natural seed sources nearby. Howe
ver, the regeneration of soil structure is also important for local hydrolo
gy and successful establishment of some plant species. In this study we inv
estigated changes in soil structure and hydraulic properties in a series of
plots on volcanic soils in the San Luis Valley, Costa Rica. The plots were
current pasture, 15- and 20-year-old regenerating forest, and primary rain
forest.
Infiltration rate increased with increasing forest age and the water releas
e characteristic reverted gradually from one with greater water retention a
t all matric potentials in the pasture plot towards that found in the prima
ry forest. Compaction and low porosity were features of both the current pa
sture and 15-year-old regenerating forest in comparison to the primary fore
st.