Ta. Kursar et al., THE EFFECTS OF THE RAINY-SEASON AND IRRIGATION ON SOIL-WATER AND OXYGEN IN A SEASONAL FOREST IN PANAMA, Journal of tropical ecology, 11, 1995, pp. 497-515
The effects of irrigation and the rainy season on soil gases, water an
d physical properties were studied in a lowland moist forest in Panama
. Two control plots experienced a normal four-month dry season and two
experimental plots were irrigated during the dry season. The forest s
oils were well aerated. The average soil oxygen content at 20 cm never
dropped below 15%. Irrigation in the dry season resulted in treatment
effects on soil oxygen and water that persisted throughout the rainy
season. The late rainy season soil oxygen content at 20 cm was 18.2% i
n the control plots and 16.8% in the irrigated plots. The late rainy s
eason soil water content al 0-10 cm was 0.34 m(3) m(-3) in the control
plots and 0.36-0.37 m(3) m(-3) in the irrigated plots. In the control
plots, in the absence of any experimental manipulation, the soil phys
ical properties changed within a single rainy season. Specifically, so
il oxygen dropped and soil water increased during the eight-month rain
y season. The observed alterations in soil physical properties probabl
y resulted from changes in soil structure and the abundance of large p
ores. The rainy season or irrigation may decrease soil porosity by dis
persing aggregates of soil particles, whereas soil desiccation during
the dry season may enhance the formation of aggregates and large pores
. As a result, the irrigated soils held more water and were less perme
able to gas and water than soils experiencing a normal dry season. We
conclude that the dry season may play an important role in maintaining
soil structure.