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Progress in drought avoidance of rainfed lowland rice

机译:雨养低地水稻避旱研究进展

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Rainfed lowland rice is grown in bunded fields covering more than 36 million hectares of South and South-east Asia. Drought stress is common, with yields averaging only 2.3 t ha~(-1). The ecosystem is characterised by fluctuating water, with soil hydrology ranging from flooded and anaerobic to droughted and aerobic. Root systems have to cope with too much and too little water at different growth stages. Drought stress may be encountered during panicle development, and especially during grain filling. These patterns vary in intensity with location, season, soil type and topographic position. Our previous research has demonstrated that cultivars differed in their patterns of adaptation to various types of rainfed environments, and this was associated in part with patterns of root behaviour during droughts. In simulated rainfed lowland conditions in the greenhouse, cultivars differed in the extent to which they could proliferate roots in, and extract water from, deeper soil layers as drought progressed. In the field, cultivars differed in the ability of their roots to penetrate hardpans and proliferate in deeper soil layers. Our most recent experiments have demonstrated that cultivars differed in the amounts of water extracted from deeper soil layers during drought. Greenhouse and field experiments have now indicated that root signals are strong in rainfed lowland rice, and are associated with increasing levels of abscisic acid in leaves as drought progresses. Cultivars varied in stomatal closure as drought progressed, with implications for rate and extent of water loss. Molecular studies have identified consistent responses in protein regulation during drought and after rewatering. In the field, the soil water from above and below the hardpan has been shown to differ in hydrogen isotope composition, raising the prospect that analysis of xylem water could be used to identify lines with a greater capacity to extract water from deeper soil layers, without destructive measurements of the root system. The implications of these results for the selection of cultivars with more efficient water use and their agronomic requirements for producing higher and more stable yields in rainfed lowland conditions are discussed.
机译:雨育的低地稻米种植在面积超过3600万公顷的南亚和东南亚的捆绑田地中。干旱胁迫很普遍,平均单产仅为2.3 t ha〜(-1)。生态系统的特征是水的波动,土壤水文范围从淹没和厌氧到干旱和需氧。根系必须在不同的生长阶段应对过多和过少的水分。在穗发育过程中,尤其是在籽粒充实过程中,可能会遇到干旱胁迫。这些模式的强度随位置,季节,土壤类型和地形位置而变化。我们以前的研究表明,不同品种对各种雨养环境的适应方式各不相同,这在某种程度上与干旱期间的根系行为有关。在模拟的雨养低地温室中,随着干旱的进行,栽培品种在深层土壤中繁殖根系并从深层土壤中提取水分的程度不同。在田间,不同品种的根部穿透硬地盘并在更深的土壤层中扩散的能力各不相同。我们最近的实验表明,干旱期间,不同品种从深层土壤中提取的水量不同。现在的温室和田间试验表明,雨养低地水稻的根部信号很强,并且随着干旱的进行与叶片中脱落酸水平的升高有关。随着干旱的进行,气孔关闭的品种也有所不同,这对水分流失的速度和程度有影响。分子研究已确定干旱期间和复水后蛋白质调节的一致反应。在田间,已证明硬顶上方和下方的土壤水在氢同位素组成方面存在差异,这提出了木质部水分析可用于识别从深层土壤中提取水的能力更高的路线的前景。根系统的破坏性测量。讨论了这些结果对选择更高效用水的品种的含义及其在雨养低地条件下产生更高和更稳定产量的农学要求。

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