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水稻生长和产量对盐水灌溉的响应与植物中的 Na+/K+ 比值有关。

Rice growth and yield responses to saline water irrigation are related to Na+/K+ ratio in plants.

机构信息

Irrigation and Water Management Division, Bangladesh Rice Research Institute, Gazipur, Bangladesh.

Soil Science Division, Bangladesh Rice Research Institute, Gazipur, Bangladesh.

出版信息

PLoS One. 2024 Nov 1;19(11):e0312372. doi: 10.1371/journal.pone.0312372. eCollection 2024.

Abstract

Rice growth and yield response to salinity can be influenced by the duration and the timing of salt stress. The present study tested the effects of saline water irrigation from vegetative growth to maturity on rice growth and yield and ion concentrations in the straw and root and related them to changes in soil salinity and soil solute potential. The treatments consisted of five levels of saline water irrigation (electrical conductivity ~0.25 (control), 4, 6, 8, and 10 dS m-1) with two rice cultivars (BRRI dhan67 and BRRI dhan99) grown in pots in a rain shelter. Grain weight per pot, dry straw weight, and root weight were significantly reduced with increasing water salinity, but BRRI dhan99 was less affected. With prolonged saline water irrigation, salt concentration increased in the soil and lowered the soil solute potential. Increased saline water induced higher concentrations of Na+ in the straw (527-1200 mmol kg-1 at 4-10 dS m-1) relative to the root. By contrast, higher Cl- concentrations accumulated in the root than in the straw. The decrease of K+ in the straw and root for increasing salinity was inconsistent, but the Na+/K+ ratio sharply increased in the straw with higher water salinity. The increased Na+/K+ explained most grain weight loss due to higher salinity (R2 = 0.93) followed by Na+ (R2 = 0.87) and Cl-1 (R2 = 0.53). We conclude that the prolonged saline water irrigation has a cumulative effect on root zone salinity and solute potential that depresses grain yield in rice by increasing the Na+/K+ ratio in plants.

摘要

水稻的生长和产量对盐度的响应可以受到盐胁迫持续时间和时间的影响。本研究测试了从营养生长到成熟期间用咸水灌溉对水稻生长和产量以及秸秆和根中的离子浓度的影响,并将其与土壤盐分和土壤溶质势的变化相关联。处理包括五个咸水灌溉水平(电导率约为 0.25(对照)、4、6、8 和 10 dS m-1),使用两个水稻品种(BRRI dhan67 和 BRRI dhan99)在遮雨棚中的盆中种植。随着水盐度的增加,每盆的粒重、干秸秆重和根重显著降低,但 BRRI dhan99 的影响较小。随着咸水灌溉时间的延长,土壤中的盐分增加,土壤溶质势降低。增加的咸水导致秸秆中 Na+浓度升高(4-10 dS m-1 时为 527-1200 mmol kg-1),而相对于根,Cl-浓度升高。相反,根中的 Cl-浓度高于秸秆。随着盐度的增加,K+在秸秆和根中的减少不一致,但在较高的水盐度下,Na+/K+比值在秸秆中急剧增加。增加的 Na+/K+解释了由于较高盐度导致的大部分籽粒重量损失(R2 = 0.93),其次是 Na+(R2 = 0.87)和 Cl-1(R2 = 0.53)。我们得出结论,长时间的咸水灌溉对根区盐分和溶质势有累积效应,通过增加植物中的 Na+/K+比值,抑制水稻的籽粒产量。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0673/11530064/b5c5fcda9043/pone.0312372.g001.jpg

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