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首页> 外文期刊>Soil & Tillage Research >Puddling, irrigation, and transplanting-time effects on productivity of rice-wheat system on a sandy loam soil of Punjab, India.
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Puddling, irrigation, and transplanting-time effects on productivity of rice-wheat system on a sandy loam soil of Punjab, India.

机译:在印度旁遮普邦的沙质壤土上,水化,灌溉和移栽时间对稻麦系统生产力的影响。

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摘要

Rice-wheat productivity in irrigated tract of the Indo-Gangetic plains is constrained by water and energy limitations. In order to minimize unproductive soil water evaporation and percolation loss at a field scale, management practices include soil puddling, water-economizing irrigation schedule, and matching growth cycle with periods of low evaporative demand. This 3-year field study examines combined effects of these options on rice-wheat productivity and water-use efficiency (WUE) and energy-use efficiency (EUE) on a sandy loam soil in an irrigated semi-arid sub-tropical environment. Treatments included combinations of three puddling intensities, viz., one (P1), two (P2), and four (P4) runs of a tine cultivator in ponded water after a common pre-puddling tillage; with two irrigation regimes, viz., continuous submergence (I1) throughout the growing season, and intermittent submergence (I2) with continuous submergence for 2 weeks after transplanting followed by 2-day interval between successive irrigations, and two transplanting dates, viz., first fortnight of June (D1) and end June (D2) to impose variation in seasonal evaporative demand. Residual effect of puddling in rice on succeeding wheat was also evaluated during the 3 years. Intensive puddling and water-economizing schedule caused a significant reduction in seasonal percolation loss primarily due to puddling-induced changes in soil bulk density and hydraulic behavior. Increasing puddling intensity from P1 to P2 enhanced mean rice yield by 0.2-0.3 Mg ha-1, but additional puddling did not improve yield significantly. Mean grain yield increase with I1 over I2 ranged between 0.3 and 0.6 Mg ha-1. Interaction effect between puddling and irrigation indicate that yield benefit with I1 over I2 was greatest in P1 regime (0.6 Mg ha-1), and the effect decreased with increase in puddling intensity. Delayed transplanting caused a decline of 0.3-0.5 Mg ha-1 in rice yield. Although maximum yield was realized with combination of P2 or P)4 regime with I1 regime, but water-use efficiency was greater with I2 compared to I1 regime by 1.1 kg haSUP(-1 mm-1 in 2000 and by 0.3 kg ha-1 mm-1 in 2001. It indicates that yield gain with additional irrigation were not commensurate with additional water input. Energy analysis also showed that energy-use efficiency was 6.8, 7.2, and 6.6 kg kWh-1 for P1, P2, and P4 regimes suggesting that yield gain with P4 did not match energy input for additional puddling. Further, there was a greater risk of yield reduction of succeeding wheat with P4 (by 0.2-0.3 Mg ha-1) compared to P1 or P2 regime..
机译:印度-恒河平原灌溉区的稻麦生产率受到水和能量的限制。为了最大程度地减少田间规模的非生产性土壤水分蒸发和渗滤损失,管理措施包括土壤搅泥,节水灌溉计划以及使生长周期与低蒸发需求相匹配。这项为期3年的田间研究考察了这些选项对半干旱亚热带灌溉沙质壤土上稻麦生产率,水分利用效率(WUE)和能源利用效率(EUE)的综合影响。处理包括在普通的水耕前耕种后,在池塘水中将三种耕强度的组合,即一次(P1),两次(P2)和四个(P4)的中耕机运行。有两种灌溉方式,即在整个生长季节持续淹没(I1),在移植后2周内连续淹没(I2)连续淹没,然后连续两次灌溉之间间隔2天,两次移栽日期也就是6月的第一个两周(D1)和6月下旬(D2)施加季节性蒸发需求的变化。在这3年中,还评估了大米泥浆对后继小麦的残留影响。严格的混水和节水计划,主要是由于混水引起的土壤容重和水力行为的变化,导致季节性渗滤损失显着减少。从P1增加到P2的搅打强度可使水稻平均单产提高0.2-0.3 Mg ha-1,但增加搅打并不能显着提高产量。 I1高于I2的平均谷物单产提高幅度为0.3至0.6 Mg ha-1。混水和灌溉之间的相互作用效应表明,在P1模式下(0.6 Mg ha-1),I1高于I2的增产效益最大,且随混肥强度的增加而降低。推迟移栽造成水稻产量下降0.3-0.5 Mg ha-1。尽管P2或P)> 4方案与I1方案相结合可实现最大产量,但是与I1方案相比,I2的用水效率要高出1.1 kg ha

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