Origin and hydrodynamics of xylem sap in tree stems, and relationship to root uptake of soil water

Abstract Although 10 years have passed since Japan’s Fukushima nuclear accident, the future radiation risk from 137Cs contamination of wood via root uptake is a serious concern. We estimated the depth at which the roots of evergreen coniferous sugi (Cryptomeria japonica) and broadleaf deciduous kona...

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Main Authors: Yasunori Mahara, Tomoko Ohta, Jyunichi Ohshima, Kazuya Iizuka
Format: Article
Language:English
Published: Nature Publishing Group 2021-04-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-021-87397-3
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spelling doaj-3a97bbb32f4d412b889d0d3ab89fbd3b2021-04-18T11:33:48ZengNature Publishing GroupScientific Reports2045-23222021-04-0111111410.1038/s41598-021-87397-3Origin and hydrodynamics of xylem sap in tree stems, and relationship to root uptake of soil waterYasunori Mahara0Tomoko Ohta1Jyunichi Ohshima2Kazuya Iizuka3Kyoto UniversityGraduate School of Engineering, Nagaoka University of TechnologyUtsunomiya University Forest, Utsunomiya UniversityUtsunomiya University Forest, Utsunomiya UniversityAbstract Although 10 years have passed since Japan’s Fukushima nuclear accident, the future radiation risk from 137Cs contamination of wood via root uptake is a serious concern. We estimated the depth at which the roots of evergreen coniferous sugi (Cryptomeria japonica) and broadleaf deciduous konara (Quercus serrata) trees actively take up soil water by using positive δD values from the artificial D2O tracer and seasonal changes in the δ18O values of soil water as a natural environmental tracer. We compared the tracer concentration changes in xylem sap with those in the soil water and ascertained that both tree species primarily took up water from a depth of 20 cm, though with mixing of water from other depths. Using sap hydrodynamics in tree stems, we found that water circulation was significantly slower in heartwood than in sapwood. Heartwood water was not supplied by direct root uptake of soil water. The measured diffusion coefficients for D2O, K+, Cs+, and I− in xylem stems were greater in sapwood than in heartwood, and their magnitude was inversely correlated with their molecular weights. The distribution of D2O and 137Cs concentrations along the radial stem could be explained by simulations using the simple advective diffusion model.https://doi.org/10.1038/s41598-021-87397-3
collection DOAJ
language English
format Article
sources DOAJ
author Yasunori Mahara
Tomoko Ohta
Jyunichi Ohshima
Kazuya Iizuka
spellingShingle Yasunori Mahara
Tomoko Ohta
Jyunichi Ohshima
Kazuya Iizuka
Origin and hydrodynamics of xylem sap in tree stems, and relationship to root uptake of soil water
Scientific Reports
author_facet Yasunori Mahara
Tomoko Ohta
Jyunichi Ohshima
Kazuya Iizuka
author_sort Yasunori Mahara
title Origin and hydrodynamics of xylem sap in tree stems, and relationship to root uptake of soil water
title_short Origin and hydrodynamics of xylem sap in tree stems, and relationship to root uptake of soil water
title_full Origin and hydrodynamics of xylem sap in tree stems, and relationship to root uptake of soil water
title_fullStr Origin and hydrodynamics of xylem sap in tree stems, and relationship to root uptake of soil water
title_full_unstemmed Origin and hydrodynamics of xylem sap in tree stems, and relationship to root uptake of soil water
title_sort origin and hydrodynamics of xylem sap in tree stems, and relationship to root uptake of soil water
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2021-04-01
description Abstract Although 10 years have passed since Japan’s Fukushima nuclear accident, the future radiation risk from 137Cs contamination of wood via root uptake is a serious concern. We estimated the depth at which the roots of evergreen coniferous sugi (Cryptomeria japonica) and broadleaf deciduous konara (Quercus serrata) trees actively take up soil water by using positive δD values from the artificial D2O tracer and seasonal changes in the δ18O values of soil water as a natural environmental tracer. We compared the tracer concentration changes in xylem sap with those in the soil water and ascertained that both tree species primarily took up water from a depth of 20 cm, though with mixing of water from other depths. Using sap hydrodynamics in tree stems, we found that water circulation was significantly slower in heartwood than in sapwood. Heartwood water was not supplied by direct root uptake of soil water. The measured diffusion coefficients for D2O, K+, Cs+, and I− in xylem stems were greater in sapwood than in heartwood, and their magnitude was inversely correlated with their molecular weights. The distribution of D2O and 137Cs concentrations along the radial stem could be explained by simulations using the simple advective diffusion model.
url https://doi.org/10.1038/s41598-021-87397-3
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