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Measurement of micro-scale soil deformation around roots using four-dimensional synchrotron tomography and image correlation
Author(s) -
Samuel D. Keyes,
Laura Cooper,
Simon J. Duncan,
Nicolai Koebernick,
Daniel McKay Fletcher,
Callum P. Scotson,
Arjen Van Veelen,
Ian Sinclair,
Tiina Roose
Publication year - 2017
Publication title -
journal of the royal society interface
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.655
H-Index - 139
eISSN - 1742-5689
pISSN - 1742-5662
DOI - 10.1098/rsif.2017.0560
Subject(s) - soil science , digital image correlation , rhizosphere , scale (ratio) , soil structure , deformation (meteorology) , synchrotron , soil water , biological system , mathematics , environmental science , geology , materials science , biology , physics , optics , composite material , paleontology , quantum mechanics , bacteria
This study applied time lapse (four-dimensional) synchrotron X-ray computed tomography to observe micro-scale interactions between plant roots and soil. Functionally contrasting maize root tips were repeatedly imaged during ingress into soil columns of varying water content and compaction. This yielded sequences of three-dimensional densiometric data, representing time-resolved geometric soil and root configurations at the micronmetre scale. These data were used as inputs for two full-field kinematic quantification methods, which enabled the analysis of three-dimensional soil deformation around elongating roots. Discrete object tracking was used to track rigid mineral grains, while continuum digital volume correlation was used to track grey-level patterns within local sub-volumes. These techniques both allowed full-field soil displacements to be quantified at an intra-rhizosphere spatial sampling scale of less than 300 µm. Significant differences in deformation mechanisms were identified around different phenotypes under different soil conditions. A uniquely strong contrast was observed between intact and de-capped roots grown in dry, compacted soil. This provides evidence that functional traits of the root cap significantly reduce the amount of soil disturbance per unit of root elongation, with this effect being particularly significant in drier soil.

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