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Water uptake and redistribution during drought in a semiarid shrub species

机译:半干旱灌木树种在干旱期间的水分吸收和再分配

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摘要

In arid systems, most plant mortality occurs during long drought periods when water is not available for plant uptake. In these systems, plants often benefit from scarce rain events occurring during drought but some of the mechanisms underlying this water use remain unknown. In this context, plant water use and redistribution after a large rain event could be a mechanism that allows deep-rooted shrubs to conservatively use water during drought. We tested this hypothesis by comparing soil and plant water dynamics in Artemisia tridentata ssp. vaseyana (Rydb.) Beetle shrubs that either received a rain event (20mm) or received no water. Soil water content (SWC) increased in shallow layers after the event and increased in deep soil layers through hydraulic redistribution (HR). Our results show that Artemisia shrubs effectively redistributed the water pulse downward recharging deep soil water pools that allowed greater plant water use throughout the subsequent drought period, which ameliorated plant water potentials. Shrubs used shallow water pools when available and then gradually shifted to deep-water pools when shallow water was being used up. Both HR recharge and the shift to shallow soil water use helped conserve deep soil water pools. Summer water uptake in Artemisia not only improved plant water relations but also increased deep soil water availability during drought
机译:在干旱系统中,大多数植物的死亡发生在长期干旱期间,因为没有足够的水吸收植物。在这些系统中,植物通常会从干旱期间发生的稀少降雨事件中受益,但是造成这种用水的某些机制仍然未知。在这种情况下,大雨后植物的水分利用和再分配可能是一种机制,可以使根深蒂固的灌木在干旱期间保守地用水。通过比较三叶蒿中土壤和植物水分动力学,我们检验了这一假设。 vaseyana(Rydb。)甲壳虫灌木丛,下雨了(20毫米)或没有积水。事件发生后,浅层土壤水分含量(SWC)增加,而水力再分配(HR)增加深层土壤水分含量。我们的结果表明,艾蒿灌木有效地重新分配了水脉冲,使深层土壤水库蓄水,从而在随后的干旱期间增加了植物用水,从而改善了植物水的潜力。灌木在可用时使用浅水池,然后在浅水用完后逐渐转移到深水池。人力资源补给和向浅层土壤水的使用都有助于保护深层土壤水库。蒿的夏季吸水不仅改善了植物的水分关系,而且增加了干旱期间深层土壤的水分供应

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