蒸腾作用
木质部
水运
水流
含水量
环境科学
水平衡
地下水补给
DNS根区域
根系
植物
土壤水分
灌溉
土壤科学
农学
生物
水文学(农业)
地质学
地下水
光合作用
岩土工程
含水层
作者
Yang Liu,Nadezhda Nadezhdina,Nan Di,Xu Ma,Jinqiang Liu,Songyan Zou,Benye Xi,Brent Clothier
出处
期刊:Plant Physiology
[Oxford University Press]
日期:2021-01-25
卷期号:186 (1): 361-372
被引量:13
标识
DOI:10.1093/plphys/kiab036
摘要
Maintaining the activity and function of the shallow root system of plants is essential for withstanding drought stress, but the associated mechanism is poorly understood. By investigating sap flow in 14 lateral roots (LRs) randomly selected from trees of a Chinese white poplar (Populus tomentosa) plantation receiving three levels of irrigation, an unknown root water transport mode of simultaneous daytime bi-directional water flow was discovered. This mode existed in five LRs confined to the surface soil without attached sinker roots. In the longer term, the bi-directional water flow was correlated with the soil water content. However, within the day, it was associated with transpiration. Our data demonstrated that bi-directional root sap flow occurred during the day, and was driven by evaporative demand, further suggesting the existence of circumferential water movement in the LR xylem. We named this phenomenon evaporation-driven hydraulic redistribution (EDHR). A soil-root water transport model was proposed to encapsulate this water movement mode. EDHR may be a crucial drought-tolerance mechanism that allows plants to maintain shallow root survival and activity by promoting root water recharge under extremely dry conditions.
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