Imaging of the electrical activity in the root zone under limited-water-availability stress: a laboratory study for Vitis vinifera

B. Mary, Veronika Iván, F. Meggio, Luca Peruzzo, Guillaume Blanchy, C. Chou, B. Ruperti, Yuxin Wu, Giorgio Cassiani
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Abstract

Abstract. Understanding root signals and their consequences for the whole plant physiology is one of the keys to tackling the water-saving challenge in agriculture. The implementation of water-saving irrigation strategies, such as the partial root zone drying (PRD) method, is part of a comprehensive approach to enhance water use efficiency. To reach this goal tools are needed for the evaluation of the root's and soil water dynamics in time and space. In controlled laboratory conditions, using a rhizotron built for geoelectrical tomography imaging, we monitored the spatio-temporal changes in soil electrical resistivity (ER) for more than a month corresponding to eight alternating water inputs cycles. Electrical resistivity tomography (ERT) was complemented with electrical current imaging (ECI) using plant-stem-induced electrical stimulation. To estimate soil water content in the rhizotron during the experiment, we incorporated Archie's law as a constitutive model. We demonstrated that under mild water stress conditions, it is practically impossible to spatially distinguish the limited-water-availability effects using ECI. We evidenced that the current source density spatial distribution varied during the course of the experiment with the transpiration demand but without any significant relationship to the soil water content changes. On the other hand, ERT showed spatial patterns associated with irrigation and, to a lesser degree, to RWU (root water uptake) and hydraulic redistribution. The interpretation of the geoelectrical imaging with respect to root activity was strengthened and correlated with indirect observations of the plant transpiration using a weight monitoring lysimeter and direct observation of the plant leaf gas exchanges.
有限供水压力下根区电活动成像:葡萄的实验室研究
摘要了解根系信号及其对整个植物生理的影响是应对农业节水挑战的关键之一。实施节水灌溉策略,如部分根区干燥法(PRD),是提高水资源利用效率的综合方法的一部分。要实现这一目标,需要有工具来评估根系和土壤水分在时间和空间上的动态变化。在受控的实验室条件下,我们利用为地质电子断层成像而建造的根瘤仪,监测了土壤电阻率(ER)的时空变化,监测时间长达一个多月,相当于八个交替的水输入周期。电阻率层析成像(ERT)与电流成像(ECI)通过植物茎干诱导的电刺激进行了互补。为了估算实验期间根瘤中的土壤含水量,我们采用了阿奇定律作为构成模型。我们证明,在轻微的水分胁迫条件下,使用 ECI 几乎无法在空间上区分有限水供应效应。我们发现,在实验过程中,电流源密度的空间分布随蒸腾需求而变化,但与土壤含水量的变化没有明显关系。另一方面,ERT 显示了与灌溉相关的空间模式,其次是与 RWU(根系吸水)和水力再分配相关的空间模式。利用重量监测溶液计对植物蒸腾作用进行的间接观测和对植物叶片气体交换的直接观测,加强了对根系活动的地质电学成像的解释和关联。
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