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记录干旱期间柽柳的水分利用模式。

Patterns of Tamarix water use during a record drought.

机构信息

Department of Ecology and Evolutionary Biology, University of Kansas, Lawrence, KS 66045, USA.

出版信息

Oecologia. 2010 Feb;162(2):283-92. doi: 10.1007/s00442-009-1455-1. Epub 2009 Sep 13.

DOI:10.1007/s00442-009-1455-1
PMID:19756759
Abstract

During a record drought (2006) in southwest Kansas, USA, we assessed groundwater dynamics in a shallow, unconfined aquifer, along with plant water sources and physiological responses of the invasive riparian shrub Tamarix ramosissima. In early May, diel water table fluctuations indicated evapotranspirative consumption of groundwater by vegetation. During the summer drought, the water table elevation dropped past the lowest position previously recorded. Concurrent with this drop, water table fluctuations abruptly diminished at all wells at which they had previously been observed despite increasing evapotranspirative demand. Following reductions in groundwater fluctuations, volumetric water content declined corresponding to the well-specific depths of the capillary fringe in early May, suggesting a switch from primary dependence on groundwater to vadose-zone water. In at least one well, the fluctuations appear to re-intensify in August, suggesting increased groundwater uptake by Tamarix or other non-senesced species from a deeper water table later in the growing season. Our data suggest that Tamarix can rapidly shift water sources in response to declines in the water table. The use of multiple water sources by Tamarix minimized leaf-level water stress during drought periods. This study illustrates the importance of the previous hydrologic conditions experienced by site vegetation for controlling root establishment at depth and demonstrates the utility of data from high-frequency hydrologic monitoring in the interpretation of plant water sources using isotopic methods.

摘要

在 2006 年美国堪萨斯州西南部的一次创纪录干旱期间,我们评估了浅层无压含水层中的地下水动态,以及入侵性河岸灌木柽柳的植物水源和生理响应。在 5 月初,昼夜水位波动表明植被蒸腾消耗了地下水。在夏季干旱期间,地下水位下降到了以前记录的最低位置以下。与这一下降同时发生的是,尽管蒸腾需求不断增加,但所有先前观察到水位波动的井中的水位波动突然减少。在地下水波动减少后,体积含水量在 5 月初与毛细带特定的井深相应下降,表明从主要依赖地下水转变为非饱和带水。在至少一个井中,波动似乎在 8 月重新加剧,表明在生长季节后期,柽柳或其他未休眠物种从更深的地下水位增加了地下水的摄取。我们的数据表明,柽柳可以迅速改变水源,以应对地下水位的下降。柽柳使用多种水源最大限度地减少了干旱期间叶片水平的水分胁迫。本研究说明了先前的水文条件对控制根系在深度上的建立的重要性,并展示了高频水文监测数据在利用同位素方法解释植物水源时的实用性。

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本文引用的文献

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Invasive capacity of Tamarix ramosissima in a Mojave Desert floodplain: the role of drought.莫哈韦沙漠洪泛平原中多枝柽柳的入侵能力:干旱的作用。
Oecologia. 1997 Jun;111(1):12-18. doi: 10.1007/s004420050202.
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