Abstract

Rainfed maize production in the hilly ecosystem of Northeastern Himalayas often suffers from moisture and soil acidity induced abiotic stresses. The present study measured evapotranspiration loss (ETc) of maize crop under controlled condition (pot experiment) of water deficit (W25-25% and W50-50% of field capacity soil moistures) and well watered (W100=100% of field capacity (FC)) regimes in strong acid soils (pH=4.3) of the Northeastern Himalayan Region of India. The response of soil ameliorants (lime) and phosphorus (P) nutrition under differential water regimes on ETc losses and water use efficiency was also studied. The measured seasonal ETc loss varied from 124.3 to 270.9mm across treatment combinations. Imposition of water deficit stress resulted in significant (p<0.05) reduction (by 33-50%) of seasonal ETc losses but was at the cost of delay in tasseling to silking, 47-65% reduction in dry matter accumulation (DMA), 12-22days shortening of grain formation period, and complete kernel abortion. Liming @ 4tha-1 significantly (p<0.05) increased ETc losses and DMA across water regimes but the magnitude of increase was higher in severely water deficit (W25) regime. Unlike lime, P nutrition improved DMA only in well-watered regimes (W100) while seasonal ETc loss was unaffected. Vegetative stage (tillering to tasseling) contributed the maximum ETc losses while weekly crop ETc loss was estimated highest during 11th-14th week after sowing (coincided with blistering stage) and then declined. Water use efficiency estimated from dry matter produced per unit ETc losses and irrigation water used varied from 4.33 to 9.43gdry matterkg-1water and 4.21 to 8.56gdry matterkg-1, respectively. Among the input factors (water, P, and lime), water regime most strongly influenced the ETc loss, growth duration, grain formation, and water use efficiency of maize.

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