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针叶树在干旱期间依赖已建立的根系:来自碳分配和水力耦合模型的结果。

Conifers depend on established roots during drought: results from a coupled model of carbon allocation and hydraulics.

机构信息

Department of Geography, University at Buffalo, Buffalo, NY, 14261, USA.

Department of Biology, Duke University, Durham, NC, 27708, USA.

出版信息

New Phytol. 2020 Jan;225(2):679-692. doi: 10.1111/nph.16043. Epub 2019 Aug 5.

Abstract

Trees may survive prolonged droughts by shifting water uptake to reliable water sources, but it is unknown if the dominant mechanism involves activating existing roots or growing new roots during drought, or some combination of the two. To gain mechanistic insights on this unknown, a dynamic root-hydraulic modeling framework was developed that set up a feedback between hydraulic controls over carbon allocation and the role of root growth on soil-plant hydraulics. The new model was tested using a 5 yr drought/heat field experiment on an established piñon-juniper stand with root access to bedrock groundwater. Owing to the high carbon cost per unit root area, modeled trees initialized without adequate bedrock groundwater access experienced potentially lethal declines in water potential, while all of the experimental trees maintained nonlethal water potentials. Simulated trees were unable to grow roots rapidly enough to mediate the hydraulic stress, particularly during warm droughts. Alternatively, modeled trees initiated with root access to bedrock groundwater matched the hydraulics of the experimental trees by increasing their water uptake from bedrock groundwater when soil layers dried out. Therefore, the modeling framework identified a critical mechanism for drought response that required trees to shift water uptake among existing roots rather than growing new roots.

摘要

树木可能通过将水分吸收转移到可靠的水源来在长时间的干旱中存活,但尚不清楚主导机制是在干旱期间激活现有根系还是生长新根系,或者两者的某种组合。为了深入了解这种未知情况,开发了一个动态根系水力建模框架,该框架在碳分配的水力控制与根系生长对土壤-植物水力的作用之间建立了反馈。使用建立在基岩地下水上的成熟派尤恩-杜松林中进行的为期 5 年的干旱/高温野外实验对新模型进行了测试。由于单位根面积的碳成本很高,因此没有足够基岩地下水接入的模型树经历了潜在的致命水势下降,而所有实验树都保持了非致命的水势。模拟树无法快速生长根系以缓解水力压力,尤其是在温暖的干旱期间。相反,通过在土壤层变干时从基岩地下水增加水分吸收,具有基岩地下水接入权限的模型树与实验树的水力情况相匹配。因此,建模框架确定了干旱响应的关键机制,该机制要求树木在现有根系之间转移水分吸收,而不是生长新根系。

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