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Water Uptake by Plant Roots: I – Formation and Propagation of a Water Extraction Front in Mature Root Systems as Evidenced by 2D Light Transmission Imaging

机译:植物根系对水分的吸收:I –成熟的根系中水提取前沿的形成和传播(通过二维光透射成像证明)

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摘要

Soil water extraction by plant roots results from plant and soil transport processes interacting at different space and time scales. At the single root scale, local soil hydraulic status and plant physiology strongly control water uptake. At the whole root system level, these local, spatially interacting processes, are integrated and modulated depending on the root system hydraulics and plant transpiration. Most often, architectural and physiological characteristics of the root system are poorly taken into account in water uptake studies. This work aims at (i) studying root water extraction by mature root systems from the single root to the whole root system scale and (ii) providing experimental data for the assessment of a detailed model of water transport in the soil–root system presented in a companion paper (Doussan et al., Plant Soil 2006, this issue). Based on the dynamic imaging of soil water depletion around roots, we examined the influence of root system architecture and soil hydraulic properties on water uptake. We worked with narrow-leaf lupin plants whose root system architecture ranged from taprooted to fasciculate. Plants were grown in large thin containers (rhizotron) filled with a translucent sand/clay mix growing medium. Water transfer in the soil, together with root water uptake, were monitored in laboratory experiments by means of 2D light transmission imaging. This technique enables the mapping of the soil water content at high spatial and temporal resolutions. Throughout water uptake events, we clearly observed and quantified the formation and movement of a water extraction front and of high gradients of soil water content next to the roots. The data obtained also demonstrate that water uptake is never restricted to a specific portion of a root and that the contribution of a specific portion of a root to the overall uptake varies with time and with the position of the root within the root system. Finally, we found that different root system architectures induced different water uptake patterns.
机译:植物根系提取土壤水的原因是植物和土壤的运输过程在不同的时空尺度上相互作用。在单根尺度上,当地土壤的水力状况和植物生理会强烈控制水分的吸收。在整个根系层次上,这些局部的,空间相互作用的过程将根据根系的水力学和植物的蒸腾作用进行整合和调节。多数情况下,吸水研究很少考虑根系的结构和生理特征。这项工作旨在(i)研究成熟根系从单根到整个根系规模的根系水分提取,(ii)提供实验数据,以评估土壤-根系中水分运移的详细模型。随行论文(Doussan等人,《植物土壤》 2006年,本期)。基于根周围土壤水分耗竭的动态成像,我们研究了根系结构和土壤水力学特性对水分吸收的影响。我们研究了根系结构从主根到细茎的窄叶羽扇豆植物。将植物在装满半透明沙子/粘土混合生长培养基的大型薄容器(根茎)中生长。通过2D透光成像,在实验室实验中监测土壤中的水分传输以及根系水分的吸收。这项技术可以在高空间和时间分辨率下绘制土壤水分含量图。在整个吸水事件中,我们清楚地观察并量化了水提取前沿的形成和运动以及根部附近土壤水分含量的高梯度。所获得的数据还表明,水分吸收绝不限于根的特定部分,并且根的特定部分对总吸收的贡献随时间和根在根系统中的位置而变化。最后,我们发现不同的根系体系结构会导致不同的水分吸收模式。

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