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土壤水分有效性和根系深度作为巴塔哥尼亚木本植物水力结构的决定因素。

Soil water availability and rooting depth as determinants of hydraulic architecture of Patagonian woody species.

作者信息

Bucci Sandra J, Scholz Fabian G, Goldstein Guillermo, Meinzer Frederick C, Arce Maria E

机构信息

Comisión Nacional de Investigaciones Científicas y Técnicas (CONICET), Buenos Aires, Argentina.

出版信息

Oecologia. 2009 Jul;160(4):631-41. doi: 10.1007/s00442-009-1331-z. Epub 2009 Mar 29.

Abstract

Adaptations of species to capture limiting resources is central for understanding structure and function of ecosystems. We studied the water economy of nine woody species differing in rooting depth in a Patagonian shrub steppe from southern Argentina to understand how soil water availability and rooting depth determine their hydraulic architecture. Soil water content and potentials, leaf water potentials (Psi(Leaf)), hydraulic conductivity, wood density (rho(w)), rooting depth, and specific leaf area (SLA) were measured during two summers. Water potentials in the upper soil layers during a summer drought ranged from -2.3 to -3.6 MPa, increasing to -0.05 MPa below 150 cm. Predawn Psi(Leaf) was used as a surrogate of weighted mean soil water potential because no statistical differences in Psi(Leaf) were observed between exposed and covered leaves. Species-specific differences in predawn Psi(Leaf) were consistent with rooting depths. Predawn Psi(Leaf) ranged from -4.0 MPa for shallow rooted shrubs to -1.0 MPa for deep-rooted shrubs, suggesting that the roots of the latter have access to abundant moisture, whereas shallow-rooted shrubs are adapted to use water deposited mainly by small rainfall events. Wood density was a good predictor of hydraulic conductivity and SLA. Overall, we found that shallow rooted species had efficient water transport in terms of high specific and leaf specific hydraulic conductivity, low rho(w), high SLA and a low minimum Psi(Leaf) that exhibited strong seasonal changes, whereas deeply rooted shrubs maintained similar minimum Psi(Leaf) throughout the year, had stems with high rho(w) and low hydraulic conductivity and leaves with low SLA. These two hydraulic syndromes were the extremes of a continuum with several species occupying different portions of a gradient in hydraulic characteristics. It appears that the marginal cost of having an extensive root system (e.g., high rho(w) and root hydraulic resistance) contributes to low growth rates of the deeply rooted species.

摘要

物种为获取有限资源而进行的适应对于理解生态系统的结构和功能至关重要。我们研究了阿根廷南部巴塔哥尼亚灌木草原中9种根系深度不同的木本植物的水分经济状况,以了解土壤水分有效性和根系深度如何决定它们的水力结构。在两个夏季期间测量了土壤含水量和势、叶水势(Ψ(Leaf))、导水率、木材密度(ρ(w))、根系深度和比叶面积(SLA)。夏季干旱期间上层土壤层的水势范围为-2.3至-3.6 MPa,在150厘米以下增加到-0.05 MPa。黎明前的Ψ(Leaf)被用作加权平均土壤水势的替代指标,因为在暴露和覆盖的叶片之间未观察到Ψ(Leaf)的统计差异。黎明前Ψ(Leaf)的物种特异性差异与根系深度一致。黎明前Ψ(Leaf)范围从浅根灌木的-4.0 MPa到深根灌木的-1.0 MPa,这表明后者的根系能够获取丰富的水分,而浅根灌木则适应利用主要由小降雨事件沉积的水分。木材密度是导水率和SLA的良好预测指标。总体而言,我们发现浅根物种在高比水力导率和叶比水力导率、低ρ(w)、高SLA以及表现出强烈季节变化的低最低Ψ(Leaf)方面具有高效的水分运输,而深根灌木全年保持相似的最低Ψ(Leaf),茎具有高ρ(w)和低导水率,叶片具有低SLA。这两种水力综合征是一个连续体的极端情况,有几个物种占据了水力特征梯度的不同部分。似乎拥有广泛根系系统的边际成本(例如,高ρ(w)和根水力阻力)导致了深根物种的低生长率。

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