Puddling is used to prepare soil for irrigated rice (Oryza sativa L.) throu
ghout SE Asia creating a soft mud often over a plough pan. Whilst these con
ditions are favourable for the rice crop, they are less so for any dryland
crop, such as mungbean (Vigna radiata (L.) Wilzek) or soybean (Glycine max
L. Merr.), grown in the dry season (DS) after rice harvest leading to low o
r erratic yields. The physical properties of soils puddled for rice were me
asured as they changed in the period after draining flood water for rice ha
rvest. The experiments were run at four sites In Indonesia and the Philippi
nes for 4-6 weeks, during which they were kept free from weeds. Apart from
one site, where there were heavy rain showers, the sites received no effect
ive rainfall during the experiment, Soil moisture content and hydraulic pot
ential in the upper 40 cm were measured regularly in five replicate plots.
Evaporation from the soil was measured using mini-lysimeters, Strength prop
erties were measured using a penetrometer. Cracks were measured using an in
tercept technique. Hydraulic conductivity was calculated using a modificati
on of the instantaneous profile technique. The sites behaved in a similar f
ashion, with initial loss of water by drainage, followed by loss by evapora
tion from the surface, However, the low conductivities limited the upwards
supply of water for evaporation so that evaporation from the soil surface d
ecreased. This resulted in strong drying of the upper 5-10 cm, but much sma
ller decreases in moisture content lower down, The strength of the upper la
yers increased as they dried. The low conductivities suggest that waterlogg
ing due to heavy rain is likely to cause problems for dry season cropping.
However, the preservation or. water in the sub-soil may allow flexibility i
n the sowing dates for dry season crops to avoid periods of heavy rain or s
hortage of labour. (C) 2000 Published by Elsevier Science B.V.