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High Air Humidity Causes Atmospheric Water Absorption via Assimilating Branches in the Deep-Rooted Tree Haloxylon ammodendron in an Arid Desert Region of Northwest China

机译:高空气湿度导致西北干旱荒漠区深根树梭梭梭的同化分支吸收大气水

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摘要

Atmospheric water is one of the main water resources for plants in arid ecosystems. However, whether deep-rooted, tomentum-less desert trees can absorb atmospheric water via aerial organs and transport the water into their bodies remains poorly understood. In the present study, a woody, deep-rooted, tomentum-less plant, Haloxylon ammodendron (C.A. Mey.) Bunge, was selected as the experimental object to investigate the preconditions for and consequences of foliar water uptake. Plant water status, gas exchange, and 18O isotopic signatures of the plant were investigated following a typical rainfall pulse and a high-humidity exposure experiment. The results showed that a high content of atmospheric water was the prerequisite for foliar water uptake by H. ammodendron in the arid desert region. After atmospheric water was absorbed via the assimilating branches, which perform the function of leaves due to leaf degeneration, the plant transported the water to the secondary branches and trunk stems, but not to the taproot xylem or the soil, based on the 18O isotopic signatures of the specimen. Foliar water uptake altered the plant water status and gas exchange-related traits, i.e., water potential, stomatal conductance, transpiration rate, and instantaneous water use efficiency. Our results suggest that atmospheric water might be a subsidiary water resource for sustaining the survival and growth of deep-rooted plants in arid desert regions. These findings contribute to the knowledge of plant water physiology and restoration of desert plants in the arid regions of the planet.
机译:大气水是干旱生态系统中植物的主要水资源之一。然而,根深蒂固,无绒毛的沙漠树木能否通过空中器官吸收大气中的水分并将其输送到人体中,仍然知之甚少。在本研究中,选择了木本,根深蒂固,无绒毛的植物梭梭(C.A. Mey。)Bunge作为实验对象,研究了叶面吸水的前提条件和后果。通过典型的降雨脉冲和高湿暴露实验,研究了植物的水分状况,气体交换和植物的 18 O同位素特征。结果表明,在干旱荒漠地区,高含量的大气水是双歧杆菌吸收叶片水的前提。通过,大气中的水分通过同化分支吸收,这些同化分支由于叶片的退化而起着叶片的作用,然后植物将水分输送到次生分支和树干,而不是主根木质部或土壤。标本的18 O同位素标记。叶面水分的吸收改变了植物的水分状况和与气体交换有关的性状,即水势,气孔导度,蒸腾速率和瞬时水分利用效率。我们的结果表明,大气水可能是维持干旱沙漠地区深根植物的生存和生长的辅助水资源。这些发现有助于了解植物水分生理学以及恢复地球干旱地区的荒漠植物。

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