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钾施肥增加了桉树人工林的水力约束。

Increased hydraulic constraints in Eucalyptus plantations fertilized with potassium.

机构信息

CIRAD, UMR Eco&Sols, Montpellier, France.

Eco&Sols, Univ Montpellier, CIRAD, INRAe, IRD, Montpellier SupAgro, Montpellier, France.

出版信息

Plant Cell Environ. 2021 Sep;44(9):2938-2950. doi: 10.1111/pce.14102. Epub 2021 Jun 8.

DOI:10.1111/pce.14102
PMID:34033133
Abstract

Fertilization is commonly used to increase growth in forest plantations, but it may also affect tree water relations and responses to drought. Here, we measured changes in biomass, transpiration, sapwood-to-leaf area ratio (A :A ) and sap flow driving force (ΔΨ) during the 6-year rotation of tropical plantations of Eucalyptus grandis under controlled conditions for throughfall and potassium (K) fertilization. K fertilization increased final tree height by 8 m. Throughfall exclusion scarcely affected tree functioning because of deep soil water uptake. Tree growth increased in K-supplied plots and remained stable in K-depleted plots as tree height increased, while growth per unit leaf area increased in all plots. Stand transpiration and hydraulic conductance standardized per leaf area increased with height in K-depleted plots, but remained stable or decreased in K-supplied plots. Greater A in K-supplied plots increased the hydraulic constraints on water use. This involved a direct mechanism through halved A :A in K-supplied plots relative to K-depleted plots, and an indirect mechanism through deteriorated water status in K-supplied plots, which prevented the increase in ΔΨ with tree height. K fertilization in tropical plantations reduces the hydraulic compensation to growth, which could increase the risk of drought-induced dieback under climate change.

摘要

受精通常用于增加森林人工林的生长,但它也可能影响树木的水分关系和对干旱的响应。在这里,我们在受控条件下测量了在 6 年的桉树热带人工林轮作期间,透雨和钾(K)施肥对生物量、蒸腾、边材与叶面积比(A:A)和 sap 流驱动力(ΔΨ)的变化。K 施肥使最终树高增加了 8 米。由于深土水分吸收,透雨排除对树木功能几乎没有影响。在 K 供应的地块中,树木生长增加,而在 K 耗尽的地块中,由于树木高度增加,生长保持稳定,而单位叶面积的生长增加。在 K 耗尽的地块中,标准化为单位叶面积的林分蒸腾和水力导度随高度增加而增加,但在 K 供应的地块中保持稳定或降低。在 K 供应的地块中更大的 A 增加了对水分利用的水力限制。这涉及通过与 K 耗尽的地块相比,K 供应的地块中的 A:A 减半的直接机制,以及通过 K 供应的地块中恶化的水分状况的间接机制,这阻止了 ΔΨ 随树木高度的增加而增加。在热带人工林进行 K 施肥会减少对生长的水力补偿,这可能会增加在气候变化下因干旱导致死亡的风险。

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