Capturing 3D Water Flow in Rooted Soil by Ultra-fast Neutron Tomography

Abstract Water infiltration in soil is not only affected by the inherent heterogeneities of soil, but even more by the interaction with plant roots and their water uptake. Neutron tomography is a unique non-invasive 3D tool to visualize plant root systems together with the soil water distribution in...

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Main Authors: Christian Tötzke, Nikolay Kardjilov, Ingo Manke, Sascha E. Oswald
Format: Article
Language:English
Published: Nature Publishing Group 2017-07-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-017-06046-w
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spelling doaj-5270decd7a6f4fcbbb68d76f3185ad9b2020-12-08T00:11:12ZengNature Publishing GroupScientific Reports2045-23222017-07-01711910.1038/s41598-017-06046-wCapturing 3D Water Flow in Rooted Soil by Ultra-fast Neutron TomographyChristian Tötzke0Nikolay Kardjilov1Ingo Manke2Sascha E. Oswald3Institute of Earth and Environmental Science, University of PotsdamInstitute of Applied Materials, Helmholtz Centre for Materials and EnergyInstitute of Applied Materials, Helmholtz Centre for Materials and EnergyInstitute of Earth and Environmental Science, University of PotsdamAbstract Water infiltration in soil is not only affected by the inherent heterogeneities of soil, but even more by the interaction with plant roots and their water uptake. Neutron tomography is a unique non-invasive 3D tool to visualize plant root systems together with the soil water distribution in situ. So far, acquisition times in the range of hours have been the major limitation for imaging 3D water dynamics. Implementing an alternative acquisition procedure we boosted the speed of acquisition capturing an entire tomogram within 10 s. This allows, for the first time, tracking of a water front ascending in a rooted soil column upon infiltration of deuterated water time-resolved in 3D. Image quality and resolution could be sustained to a level allowing for capturing the root system in high detail. Good signal-to-noise ratio and contrast were the key to visualize dynamic changes in water content and to localize the root uptake. We demonstrated the ability of ultra-fast tomography to quantitatively image quick changes of water content in the rhizosphere and outlined the value of such imaging data for 3D water uptake modelling. The presented method paves the way for time-resolved studies of various 3D flow and transport phenomena in porous systems.https://doi.org/10.1038/s41598-017-06046-w
collection DOAJ
language English
format Article
sources DOAJ
author Christian Tötzke
Nikolay Kardjilov
Ingo Manke
Sascha E. Oswald
spellingShingle Christian Tötzke
Nikolay Kardjilov
Ingo Manke
Sascha E. Oswald
Capturing 3D Water Flow in Rooted Soil by Ultra-fast Neutron Tomography
Scientific Reports
author_facet Christian Tötzke
Nikolay Kardjilov
Ingo Manke
Sascha E. Oswald
author_sort Christian Tötzke
title Capturing 3D Water Flow in Rooted Soil by Ultra-fast Neutron Tomography
title_short Capturing 3D Water Flow in Rooted Soil by Ultra-fast Neutron Tomography
title_full Capturing 3D Water Flow in Rooted Soil by Ultra-fast Neutron Tomography
title_fullStr Capturing 3D Water Flow in Rooted Soil by Ultra-fast Neutron Tomography
title_full_unstemmed Capturing 3D Water Flow in Rooted Soil by Ultra-fast Neutron Tomography
title_sort capturing 3d water flow in rooted soil by ultra-fast neutron tomography
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2017-07-01
description Abstract Water infiltration in soil is not only affected by the inherent heterogeneities of soil, but even more by the interaction with plant roots and their water uptake. Neutron tomography is a unique non-invasive 3D tool to visualize plant root systems together with the soil water distribution in situ. So far, acquisition times in the range of hours have been the major limitation for imaging 3D water dynamics. Implementing an alternative acquisition procedure we boosted the speed of acquisition capturing an entire tomogram within 10 s. This allows, for the first time, tracking of a water front ascending in a rooted soil column upon infiltration of deuterated water time-resolved in 3D. Image quality and resolution could be sustained to a level allowing for capturing the root system in high detail. Good signal-to-noise ratio and contrast were the key to visualize dynamic changes in water content and to localize the root uptake. We demonstrated the ability of ultra-fast tomography to quantitatively image quick changes of water content in the rhizosphere and outlined the value of such imaging data for 3D water uptake modelling. The presented method paves the way for time-resolved studies of various 3D flow and transport phenomena in porous systems.
url https://doi.org/10.1038/s41598-017-06046-w
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