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首页> 外文期刊>Crop science >Increased Ring-Shaped Chalkiness and Osmotic Adjustment when Growing Rice Grains under Foehn-Induced Dry Wind Condition
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Increased Ring-Shaped Chalkiness and Osmotic Adjustment when Growing Rice Grains under Foehn-Induced Dry Wind Condition

机译:Foehn引起的干风条件下种植水稻籽粒时,增加了环状的垩白度和渗透调节

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Foehn-induced dry wind during grain filling increased ring-shaped chalky kernels in rice (Oryza sativa L.) plants. The objective of this study was to determine physiological mechanisms of the occurrence of ring-shaped chalky kernels. Rice plants were subjected to water deficit in a paddy field after shade by applying dry high-speed wind. Additionally, a growth chamber experiment was conducted with plants in pots to measure the water status under the dry wind condition for 24 h by combining in situ turgor (?¨p) assay in developing endosperms with the water potential measurements. The dry (high vapor pressure deficit [VPD]) wind treatment produced the largest number of ring-shaped chalky kernels due to poor starch accumulation, compared with shade or low-VPD wind treatment. The inner endosperm cells, where a high frequency of chalkiness was observed, spatially maintained ?¨p by osmotic adjustment before the chalky formation with no decline of grain weight. Dry wind reduced photosynthesis due to a partial stomatal closure after water deficit developed. However, these responses, including those related to the plant water status, returned to a level similar to those of the control plants in a day after the dry wind was stopped. We conclude that (i) ?¨p maintenance by osmotic adjustment contributes to grain development under water deficit under foehn conditions and (ii) osmotic adjustment has a role in temporally inhibiting starch accumulation in endosperms, resulting in ring-shaped chalky kernels under foehn-induced water deficit conditions.
机译:谷物灌浆过程中,Foehn引起的干燥风增加了水稻(Oryza sativa L.)植物的环状白垩粒。这项研究的目的是确定出现环状白垩粒的生理机制。遮荫后,通过使用干燥的高速风使水稻植株在稻田中缺水。此外,还对盆栽植物进行了一个生长室实验,通过结合发育中的胚乳的原位膨大试验和水势测量来测量干旱条件下24小时的水分状况。与低阴影或低VPD风处理相比,由于淀粉积聚不良,干式(高蒸气压亏缺[VPD])风处理产生最多数量的环状白垩粒。在白垩形成之前,观察到白垩发生率很高的内胚乳细胞通过渗透调节而在空间上保持了ρp,而白垩形成没有谷物重量的下降。缺水形成后,由于部分气孔关闭,干燥风减少了光合作用。但是,这些响应(包括与植物水分状况相关的响应)在干燥风停止后的第二天恢复到与对照植物相似的水平。我们得出的结论是:(i)通过渗透调节维持磷在foehn条件下缺水时促进了谷物的发育,并且(ii)渗透调节在暂时抑制胚乳中淀粉的积累方面起作用,从而导致在foehn-条件下呈环状的白垩状谷粒。导致缺水情况。

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