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Depressed hydraulic redistribution of roots more by stem refilling than by nocturnal transpiration for Populus euphratica Oliv. in situ measurement

机译:胡杨对茎的压实作用比对夜间蒸腾作用的抑制作用强。原位测量

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摘要

During the night, plant water loss can occur either through the roots, as hydraulic redistribution (HR), or through the leaves via the stoma, as nocturnal transpiration (E n), which was methodologically difficult to separate from stem refilling (R e). While HR and E n have been reported across a range of species, ecosystem, and climate zone, there is little understanding on the interactions between E n and/or R e and HR. As water movement at night occurs via gradients of water potential, it is expected that during periods of high atmospheric vapor pressure deficit (VPD), water loss via E n will override water loss via HR. To test this hypothesis, sap flow in stems and roots of Populus euphratica Oliv. trees, growing in a riparian zone in a hyperarid climate, was measured once in a year. Nocturnal stem sap flow was separated into E n and R e using the “forecasted refilling” method. Substantial nocturnal sap flow (38% of 24‐hr flux on average) was observed and positively correlated with VPD; however, the strength of the correlation was lower (R 2 = .55) than diurnal sap flow (E d) (R 2 = .72), suggesting that nocturnal stem sap flow was attributed to both water loss through the canopy and replenishment of water in stem tissues. Partitioning of nocturnal sap flow shows that R e constituted approximately 80%, and E n ~20%, of nocturnal sap flow. The amount of root sap flow attributed to redistribution was negatively related to E d (R 2 = .69) and the amount of acropetally sap flow in stems, R e (R2 = .41) and En (R2 = .14). It was suggested that the magnitude of HR is more strongly depressed by Re that was recharge to the water loss via Ed than by En. It was consistent with whole‐tree water balance theory, that the nighttime upward sap flow to xylem, stem refilling and transpiration, may depress hydraulic redistribution of roots.
机译:在夜间,植物的水分流失既可以通过水力重新分配(HR)发生在根部,也可以通过气孔通过叶片发生,例如通过夜间蒸腾(E n)发生,这在方法上很难与茎重灌装分开(R e) 。虽然已经报道了HR,E n涉及一系列物种,生态系统和气候带,但对E n和/或R e与HR之间的相互作用了解甚少。由于夜间的水运动是通过水势的梯度发生的,因此可以预期,在高大气蒸气压亏缺(VPD)期间,通过E n的水分流失将超过通过HR的水分流失。为了验证这一假设,胡杨的茎和根中的汁液流动。每年测量一次在高干旱气候下在河岸带生长的树木。使用“预填充”方法将夜间茎液流分离为E n和R e。观察到大量的夜间树液流量(平均24小时通量的38%),并且与VPD正相关;但是,相关强度低于昼夜液流(E d)(R 2 =。72)(R 2 =。55),表明是夜间茎汁液流动归因于通过冠层的水分流失和茎组织中水的补充。夜间液流的分配表明,R e约占夜间液流的80%,而E n约占20%。归因于重新分布的根液流与E d(R 2 =。69)负相关,而茎中的顶囊液流 R e(< em> R 2 =。41)和 E n( R 2 =。14)。有人建议, R 会严重抑制HR的幅度通过 E 补给失水的ed比 E n 。这与整棵树的水平衡理论是一致的,即夜间流向树木质部的树液,茎重填充和蒸腾作用可能会抑制根系的水力重新分配。

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