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For three years it has stricken a country where farming is 80percentt of the economy: blowing away seeds and soil, drying up wells and rivers, killing vegetation and livestock.
Rate of photosynthesis of AW under moderate or severe soil drying was enhanced when compared to BW or SW under similar soil drying treatments.
The fallow treatments were continuous soil flooding (flooded), soil drying with exclusion of rainfall (dry), soil drying with dry tillage (dry + tillage), and a control with soil drying and wetting from rainfall (dry and wet).
Watering and soil drying could be applied independently on either part of the soil column.
It appears that the two sensors were less responsive to the soil drying between irrigations events than gravimetric method.
Field experiments also suggest that warming and associated soil drying could reduce primary production in many temperate grasslands [80, 81].
The soil drying was carried out at a temperature of 105°C using an oven model FD 53 Binder.
Soil moisture content was determined by measuring water content after soil drying at 50°C until constant weight.
In contrast, water storage as a soil function during soil drying was not affected.
The wetted and dried sides may be shifted according to the soil drying rate and crop water requirement.
Results showed that when water consumption was reduced by 20% (moderate soil drying) and 40% (severe soil drying) through extending the watering intervals, the alternate watering (AW), or drying, on either part of the soil column largely maintained its biomass production under moderate soil drying.
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