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Influence of Root Diameter and Soil Depth on the Xylem Anatomy of Fine- to Medium-Sized Roots of Mature Beech Trees in the Top- and Subsoil

机译:根系直径和土壤深度对表层和下层土壤中成熟山毛榉树中小型根木质部解剖的影响

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摘要

Despite their importance for water uptake and transport, the xylem anatomical and hydraulic properties of tree roots have only rarely been studied in the field. We measured mean vessel diameter (D), vessel density (VD), relative vessel lumen area (lumen area per xylem area) and derived potential hydraulic conductivity (Kp) in the xylem of 197 fine- to medium-diameter roots (1–10 mm) in the topsoil and subsoil (0–200 cm) of a mature European beech forest on sandy soil for examining the influence of root diameter and soil depth on xylem anatomical and derived hydraulic traits. All anatomical and functional traits showed strong dependence on root diameter and thus root age but no significant relation to soil depth. Averaged over topsoil and deep soil and variable flow path lengths in the roots, D increased linearly with root diameter from ∼50 μm in the smallest diameter class (1–2 mm) to ∼70 μm in 6–7 mm roots (corresponding to a mean root age of ∼12 years), but remained invariant in roots >7 mm. D never exceeded ∼82 μm in the 1–10 mm roots, probably in order to control the risk of frost- or drought-induced cavitation. This pattern was overlain by a high variability in xylem anatomy among similar-sized roots with Kp showing a higher variance component within than between root diameter classes. With 8% of the roots exceeding average Kp in their diameter class by 50–700%, we obtained evidence of the existence of ‘high-conductivity roots’ indicating functional differentiation among similar-sized roots. We conclude that the hydraulic properties of small to medium diameter roots of beech are mainly determined by root age, rendering root diameter a suitable predictor of hydraulic functioning, while soil depth – without referring to path length – had a negligible effect.
机译:尽管它们对于水的吸收和运输很重要,但在该领域中很少研究木质部的木质部解剖学和水力学特性。我们测量了197根细至中直径根部(1–10)的木质部中的平均血管直径(D),血管密度(VD),相对血管腔面积(每木质部面积的腔面积)和导出的潜在水力传导率(Kp)。毫米)在沙质土壤上成熟的欧洲山毛榉林的表层土壤和下层土壤(0–200厘米)中,用于研究根直径和土壤深度对木质部解剖学和派生水力性状的影响。所有的解剖学和功能性状都显示出对根直径的依赖性,因此对根龄的依赖性也很大,但与土壤深度没有显着关系。 D在表层土壤和深层土壤中平均,并且根中的流动路径长度可变,D随根直径的增加而线性增加,从最小直径类别(1-2 mm)中的约50μm增加到6-7 mm根中的约70μm(对应于a平均根龄约为12岁),但根> 7 mm时保持不变。在1–10 mm的根中,D从未超过〜82μm,这可能是为了控制霜冻或干旱引起的空化的风险。这种模式被相似大小的根部木质部解剖结构的高变异性所覆盖,其中Kp在内部的变异成分高于根部直径类别之间的变异成分。 8%的根在其直径类别中超过平均Kp 50-700%,我们获得了“高导电性根”的存在的证据,表明相似大小的根之间存在功能差异。我们得出的结论是,小到中等直径的山毛榉根的水力特性主要由根龄决定,这使根直径成为水力功能的合适预测指标,而土壤深度(不涉及路径长度)的影响可忽略不计。

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