确定水分和盐分胁迫对根系吸水的滞后效应

IF 5.9 1区 农林科学 Q1 AGRONOMY
Tianshu Wang , Lining Liu , Qiang Zuo , Xun Wu , Yanqi Xu , Jianchu Shi , Jiandong Sheng , Pingan Jiang , Alon Ben-Gal
{"title":"确定水分和盐分胁迫对根系吸水的滞后效应","authors":"Tianshu Wang ,&nbsp;Lining Liu ,&nbsp;Qiang Zuo ,&nbsp;Xun Wu ,&nbsp;Yanqi Xu ,&nbsp;Jianchu Shi ,&nbsp;Jiandong Sheng ,&nbsp;Pingan Jiang ,&nbsp;Alon Ben-Gal","doi":"10.1016/j.agwat.2024.109121","DOIUrl":null,"url":null,"abstract":"<div><div>Characterizing the effects of previous water and salinity stresses is critical for the evaluation of plant water status, which, in turn, is essential for understanding soil-plant water relations and optimizing irrigation schemes. Recent research has found that hysteresis of plant response following water stress alone can be described by an exponential function of the stress degree on the previous day. To explore and quantify the effects of hysteresis concerning salinity stress and combined water-salinity stress, a hydroponic experiment and a soil column experiment on winter wheat, and a field experiment on cotton were conducted. Like water stress, previous salinity stress and combined water-salinity stress also resulted in hysteretic effects on root-water-uptake. Leaf stomatal conductance and plant transpiration rate of stressed crops could only recover gradually from a previous stressed status after re-watering. When stress was mild, compensatory recovery was found, while incomplete recovery occurred when stress was severe. Although the recovery process was closely related to stress history and type, a recovery coefficient was quantified universally with an exponential function of the stress extent on the previous day (with a coefficient of determination <em>R</em><sup>2</sup> ≥ 0.60). Consideration of hysteresis for water and salinity stresses with a mathematical model led to significant improvement in the simulation of both relative transpiration rate (<em>R</em><sup>2</sup> = 0.94, root mean squared error <em>RMSE</em> = 0.04, maximal absolute error <em>MAE</em> = 0.12) and soil water content (<em>R</em><sup>2</sup> = 0.90, <em>RMSE</em> = 0.01 cm<sup>3</sup> cm<sup>–3</sup>, <em>MAE</em> = 0.03 cm<sup>3</sup> cm<sup>–3</sup>), especially during the recovery periods severely affected by historical stress. Consideration of hysteresis is expected to benefit regulation of soil water and salinity and thus enhance water use efficiency. However, the mechanisms underlying hysteresis, especially the compensatory recovery mechanisms, still need to be further investigated.</div></div>","PeriodicalId":7634,"journal":{"name":"Agricultural Water Management","volume":"305 ","pages":"Article 109121"},"PeriodicalIF":5.9000,"publicationDate":"2024-10-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Characterizing the hysteretic effects of water and salinity stresses on root-water-uptake\",\"authors\":\"Tianshu Wang ,&nbsp;Lining Liu ,&nbsp;Qiang Zuo ,&nbsp;Xun Wu ,&nbsp;Yanqi Xu ,&nbsp;Jianchu Shi ,&nbsp;Jiandong Sheng ,&nbsp;Pingan Jiang ,&nbsp;Alon Ben-Gal\",\"doi\":\"10.1016/j.agwat.2024.109121\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Characterizing the effects of previous water and salinity stresses is critical for the evaluation of plant water status, which, in turn, is essential for understanding soil-plant water relations and optimizing irrigation schemes. Recent research has found that hysteresis of plant response following water stress alone can be described by an exponential function of the stress degree on the previous day. To explore and quantify the effects of hysteresis concerning salinity stress and combined water-salinity stress, a hydroponic experiment and a soil column experiment on winter wheat, and a field experiment on cotton were conducted. Like water stress, previous salinity stress and combined water-salinity stress also resulted in hysteretic effects on root-water-uptake. Leaf stomatal conductance and plant transpiration rate of stressed crops could only recover gradually from a previous stressed status after re-watering. When stress was mild, compensatory recovery was found, while incomplete recovery occurred when stress was severe. Although the recovery process was closely related to stress history and type, a recovery coefficient was quantified universally with an exponential function of the stress extent on the previous day (with a coefficient of determination <em>R</em><sup>2</sup> ≥ 0.60). Consideration of hysteresis for water and salinity stresses with a mathematical model led to significant improvement in the simulation of both relative transpiration rate (<em>R</em><sup>2</sup> = 0.94, root mean squared error <em>RMSE</em> = 0.04, maximal absolute error <em>MAE</em> = 0.12) and soil water content (<em>R</em><sup>2</sup> = 0.90, <em>RMSE</em> = 0.01 cm<sup>3</sup> cm<sup>–3</sup>, <em>MAE</em> = 0.03 cm<sup>3</sup> cm<sup>–3</sup>), especially during the recovery periods severely affected by historical stress. Consideration of hysteresis is expected to benefit regulation of soil water and salinity and thus enhance water use efficiency. However, the mechanisms underlying hysteresis, especially the compensatory recovery mechanisms, still need to be further investigated.</div></div>\",\"PeriodicalId\":7634,\"journal\":{\"name\":\"Agricultural Water Management\",\"volume\":\"305 \",\"pages\":\"Article 109121\"},\"PeriodicalIF\":5.9000,\"publicationDate\":\"2024-10-25\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Agricultural Water Management\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0378377424004578\",\"RegionNum\":1,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"AGRONOMY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Agricultural Water Management","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0378377424004578","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"AGRONOMY","Score":null,"Total":0}
引用次数: 0

摘要

确定之前水分和盐分胁迫的影响对于评估植物水分状况至关重要,而植物水分状况又是了解土壤-植物水分关系和优化灌溉方案的关键。最近的研究发现,植物仅在水分胁迫后的滞后反应可以用前一天胁迫程度的指数函数来描述。为了探索和量化滞后对盐度胁迫和水盐联合胁迫的影响,我们对冬小麦进行了水培实验和土柱实验,并对棉花进行了田间试验。与水胁迫一样,先前的盐度胁迫和水盐联合胁迫也会对根系吸水产生滞后效应。受胁迫作物的叶片气孔导度和植物蒸腾速率只有在重新浇水后才能从之前的受胁迫状态逐渐恢复。当胁迫轻微时,会出现补偿性恢复,而当胁迫严重时,则会出现不完全恢复。虽然恢复过程与胁迫的历史和类型密切相关,但恢复系数是通过前一天胁迫程度的指数函数(决定系数 R2 ≥ 0.60)来普遍量化的。通过数学模型考虑水分和盐度胁迫的滞后性,可显著改善相对蒸腾速率(R2 = 0.94,均方根误差 RMSE = 0.04,最大绝对误差 MAE = 0.12)和土壤含水量(R2 = 0.90,均方根误差 RMSE = 0.01 cm3 cm-3,最大绝对误差 MAE = 0.03 cm3 cm-3)的模拟,尤其是在受历史胁迫严重影响的恢复期。考虑滞后因素有望有利于调节土壤水分和盐分,从而提高水分利用效率。然而,滞后的内在机制,尤其是补偿恢复机制,仍有待进一步研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Characterizing the hysteretic effects of water and salinity stresses on root-water-uptake
Characterizing the effects of previous water and salinity stresses is critical for the evaluation of plant water status, which, in turn, is essential for understanding soil-plant water relations and optimizing irrigation schemes. Recent research has found that hysteresis of plant response following water stress alone can be described by an exponential function of the stress degree on the previous day. To explore and quantify the effects of hysteresis concerning salinity stress and combined water-salinity stress, a hydroponic experiment and a soil column experiment on winter wheat, and a field experiment on cotton were conducted. Like water stress, previous salinity stress and combined water-salinity stress also resulted in hysteretic effects on root-water-uptake. Leaf stomatal conductance and plant transpiration rate of stressed crops could only recover gradually from a previous stressed status after re-watering. When stress was mild, compensatory recovery was found, while incomplete recovery occurred when stress was severe. Although the recovery process was closely related to stress history and type, a recovery coefficient was quantified universally with an exponential function of the stress extent on the previous day (with a coefficient of determination R2 ≥ 0.60). Consideration of hysteresis for water and salinity stresses with a mathematical model led to significant improvement in the simulation of both relative transpiration rate (R2 = 0.94, root mean squared error RMSE = 0.04, maximal absolute error MAE = 0.12) and soil water content (R2 = 0.90, RMSE = 0.01 cm3 cm–3, MAE = 0.03 cm3 cm–3), especially during the recovery periods severely affected by historical stress. Consideration of hysteresis is expected to benefit regulation of soil water and salinity and thus enhance water use efficiency. However, the mechanisms underlying hysteresis, especially the compensatory recovery mechanisms, still need to be further investigated.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Agricultural Water Management
Agricultural Water Management 农林科学-农艺学
CiteScore
12.10
自引率
14.90%
发文量
648
审稿时长
4.9 months
期刊介绍: Agricultural Water Management publishes papers of international significance relating to the science, economics, and policy of agricultural water management. In all cases, manuscripts must address implications and provide insight regarding agricultural water management.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信