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Root Osmotic Adjustment under Osmotic Stress in Maize Seedlings. 1. Transient Change of Growth and Water Relations in Roots in Response to Osmotic Stress

机译:渗透胁迫下玉米幼苗的根系渗透调节。 1.渗透胁迫对根系生长和水分关系的瞬时变化

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The transient changes in seminal root elongation rate, osmotic potential, water potential, and turgor pressure in maize after the onset of stress treatments were examined using polyethylene glycol 6000 to evaluate the process of osmotic adjustment in root. Maize seedlings were exposed to different intensities of osmotic stress for 1, 3, 5, 10, and 20 minutes, and 2, 6, 12, and 24 hours. Seminal roots shrunk immediately after the onset of the -0.41 and -0.89 MPa stress treatments, due to dehydration. However, roots gradually resumed elongation from 5 minutes after the onset of the stress treatment. The osmotic potential in the root elongating zone dropped drastically with the onset of stress followed by a gradual decrease for 6 hours. We quantitatively analyzed the relative importance of the factors that contributed to the reduction of osmotic potential, and found that 46% reduction of osmotic potential was caused by tissue dehydration and 54% by solute accumulation 20 minutes after start of -0.89 MPa treatment. At hour 12, however, only 7% reduction of osmotic potential was caused by tissue dehydration and 93% by solute accumulation. In the root elongating zone, turgor pressure decreased immediately after the onset of the stress treatment due to the larger decline of water potential than that of the osmotic potential. However, from minute 20 onwards, turgor pressure started to recover due to osmotic adjustment. These results indicated that osmotic adjustment develops immediately after exposure to osmotic stress, especially in the root elongating zone, and substantially contributed to the maintenance of turgor pressure and root growth.
机译:使用聚乙二醇6000评估了胁迫处理后玉米的精根伸长率,渗透势,水势和膨胀压力的瞬时变化,以评估根的渗透调节过程。将玉米幼苗暴露于不同强度的渗透胁迫下1、3、5、10和20分钟,以及2、6、12和24小时。在发生-0.41和-0.89 MPa应力处理后,由于脱水,生精根立即收缩。但是,从开始应力处理后的5分钟开始,根部逐渐恢复伸长。随着胁迫的开始,根部延长区中的渗透势急剧下降,随后逐渐下降6小时。我们定量分析了导致渗透压降低的因素的相对重要性,发现在-0.89 MPa处理开始后20分钟,渗透压降低的46%是由组织脱水引起的,而渗透压下降的54%是由溶质积聚引起的。然而,在第12小时,仅组织脱水导致渗透压降低了7%,而溶质积累则降低了93%。在根部延长区,由于水势的下降比渗透势的下降大,因此在应力处理开始后,膨胀压力立即降低。但是,从第20分钟开始,由于渗透调节,膨胀压力开始恢复。这些结果表明,渗透调节在暴露于渗透胁迫后立即发展,特别是在根部伸长区,并且在维持膨大压力和根生长方面起了重要作用。

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