Drying Properties and Rice Production Potential of Cracking Soils in the Muda Irrigation Scheme
Three previously puddled rice soils, namely the Chengai, Tebengau, and Tualang series of the Muda Irrigation Scheme were studied both in the field and in the glass house. The objectives of this study were to understand the processes of drying, cracking and re-wetting and relate these to soil prop...
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Format: | Thesis |
Language: | English English |
Published: |
1999
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Online Access: | http://psasir.upm.edu.my/id/eprint/10427/1/FP_1999_5.pdf http://psasir.upm.edu.my/id/eprint/10427/ |
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Institution: | Universiti Putra Malaysia |
Language: | English English |
Summary: | Three previously puddled rice soils, namely the Chengai, Tebengau, and
Tualang series of the Muda Irrigation Scheme were studied both in the field and in the
glass house. The objectives of this study were to understand the processes of drying,
cracking and re-wetting and relate these to soil properties, to develop a simple model
for estimating bypass flow and bypass ratio of cracking soil during land soaking, and to
simulate the ORYZA_ W model for determining the optimum sowing date, quantifying
rice yield, net water use, and crop duration under future climate change scenarios, and
assessing the drought effect on irrigated rice yield. Calculated volumetric and linear
shrinkage of the Chengai and Tebengau series were similar and greater than those of
the Tualang series. The measured shrinkage geometric factor rs, with values of around
3 , indicated that shrinkage of these three series was isotropic. Comparatively faster
moisture depletion and absorption were observed in the Chengai and Tebengau series
than in the Tualang series both in the glasshouse and field conditions. Chengai and
Tebengau soils showed similar crack width, depth, area, length and volume, these
properties being significantly different from those of the Tualang soil. The deepest crack depth below the puddled layer measured by the paint method were 77, 73, and 52
cm in the Chengai, Tebengau, and Tualang series, respectively. A model was
developed to quantify bypass flow during land soaking. According to the model, the
amount of water that bypassed the topsoil of the three soil series accounted for 59-67%
of total input water. Higher yields (1 0.2 to 1 0.6 t ha-I) were predicted for the off season
(56-98 Day of the Year - DOY) than the main season (9.2 to 9.7 t ha-I during 1 96-238
DOY). The higher off season yields were associated with higher radiation and longer
crop duration. The impact of 15 different climatic scenarios was evaluated. Crop
duration (TGP) was shortened by 3 and 2 days during the off and main seasons,
respectively, following a 4°C increase in the daily maximum temperature. Increased
CO2 levels predicted an increase in yield in both seasons. The combinations of
increased CO2 levels and temperatures predicted increased yields for both seasons. The
scenarios of three General Circulation Models (GCM) predicted yield reduction in the
off season while in the main season, predicted yields were almost similar to current
yields. The net water use (NWU) increased with increase in temperature in both
seasons for all cases. Increments in CO2 level did not predict any change for NWU in
both seasons. The combinations of increased temperatures and CO2 levels, and the
scenarios of three GCMs predicted an increase of NWU in both seasons. Increased
NWU was mainly influenced by temperature increments. Yield differences between
crops temporarily stressed at mid-tillering and panicle initiation stages and nonstressed
crops were smaller. However, maturity was delayed in both seasons. Large
yield reductions were predicted for temporary drought stress at the flowering stage,
while maturity was delayed by 3 and I-day in the off and main seasons, respectively. |
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