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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2017-07-01
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Online Access: | https://doi.org/10.1038/s41598-017-06046-w |
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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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