Radial water transfer from sapwood to inner bark during day time: evidence from diurnal variations in water isotope composition and isotope tracing

IF 2.1 3区 农林科学 Q2 FORESTRY
Trees Pub Date : 2025-05-22 DOI:10.1007/s00468-025-02630-0
Daniel Epron, Yan Xia, Reno Yoshida, Masanori Katsuyama, Wakana A. Azuma, Yoshiko Kosugi, Satoshi Nagai, Masako Dannoura
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引用次数: 0

Key message

Osmotically-driven radial transfer of water from xylem to phloem occurs during the day in the branches of hinoki cypress, even though branch diameter shrinks.

Abstract

The hydraulic coupling between xylem and phloem has been explicitly included in theoretical models of phloem transport; however, the predicted radial water transfer from xylem to phloem during the day has not yet been demonstrated experimentally. In a first experiment, we tested the hypothesis of a water transfer from xylem to the inner bark during the day, assuming that, if the transfer does not occur, phloem water would be isotopically enriched due to an influx of enriched water concomitant with sugar loading in the foliage. The inner bark water from branches of mature hinoki cypress was, however, only slightly enriched in 18O in the afternoon compared to sapwood water (δ18O of − 6.3 and − 6.6‰ respectively), but much less than foliage water (16.0‰ at noon and 18.9‰ in the afternoon). This suggests that the isotopically enriched leaf water concurrently loaded with sugars in the leaf phloem was mixed with the unenriched xylem water. In a second experiment, to confirm that water transfer from xylem to the inner bark during the day occurs in branches, deuterium-enriched water was sprinkled on the soil. Concomitant deuterium enrichment of xylem and inner bark water extracted from branches was observed during the day after labelling, earlier than in leaves, when branches were still shrinking. This provides experimental support for theoretical models of phloem transport that have predicted radial transfer of water from xylem to phloem along the path.

白天从边材向树皮内部的径向水转移:来自水同位素组成和同位素示踪的日变化证据
白天,在白木柏树的树枝上,即使树枝直径缩小,水也会在木质部向韧皮部的径向转移中渗透。摘要木质部与韧皮部的水力耦合已被明确地纳入韧皮部运输的理论模型中;然而,预测的白天从木质部向韧皮部的径向水转移尚未得到实验证明。在第一个实验中,我们测试了白天水分从木质部转移到内树皮的假设,假设如果这种转移不发生,韧皮部的水将由于富含水分的流入而伴随着叶片中的糖负荷而同位素富集。成熟白木枝干树皮内水的δ18O在下午仅略高于边材水(δ18O分别为- 6.3‰和- 6.6‰),但远低于叶水(δ18O在中午和下午分别为16.0‰和18.9‰)。这表明,在叶韧皮部同时装载糖的同位素富集的叶水与未富集的木质部水混合在一起。在第二个实验中,为了证实白天从木质部到树皮内部的水分转移发生在树枝上,将富氘水洒在土壤上。在标记后的一天,从树枝中提取的木质部和树皮内部的水同时富集氘,比在树枝还在萎缩的叶子中富集氘的时间要早。这为预测水分沿路径从木质部向韧皮部径向转移的理论模型提供了实验支持。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Trees
Trees 农林科学-林学
CiteScore
4.50
自引率
4.30%
发文量
113
审稿时长
3.8 months
期刊介绍: Trees - Structure and Function publishes original articles on the physiology, biochemistry, functional anatomy, structure and ecology of trees and other woody plants. Also presented are articles concerned with pathology and technological problems, when they contribute to the basic understanding of structure and function of trees. In addition to original articles and short communications, the journal publishes reviews on selected topics concerning the structure and function of trees.
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