The role of plant species and soil condition in the structural development of the rhizosphere

A - Papers appearing in refereed journals

Helliwell, J. R., Sturrock, C. J., Miller, A. J., Whalley, W. R. and Mooney, S. J. 2019. The role of plant species and soil condition in the structural development of the rhizosphere. Plant, Cell and Environment. 42 (6), pp. 1974-1986.

AuthorsHelliwell, J. R., Sturrock, C. J., Miller, A. J., Whalley, W. R. and Mooney, S. J.

Roots naturally exert axial and radial pressures during growth which alter the structural arrangement of soil at the root-soil interface. However empirical models suggest soil densification, which can have negative impacts on water and nutrient uptake, occurs at the immediate root surface with decreasing distance from the root. Here we spatially map structural gradients in the soil surrounding roots using non-invasive imaging, to ascertain the role of root growth in early stage formation of soil structure. X-ray Computed Tomography (CT) provided a means to not only visualise a root system in situ and in 3-D but to assess the precise, root-induced alterations to soil structure close to, and at selected distances away from the root-soil interface. We spatially quantified the changes in soil structure generated by three common but contrasting plant species (Pea, Tomato and Wheat) under different soil texture and compaction treatments. Across the three plant types significant increases in porosity at the immediate root surface were found in both clay loam and loamy sand soils and not soil densification, the currently assumed norm. Densification of the soil was recorded, at some distance away from the root, dependent on soil texture and plant type. There was a significant soil texture x bulk density x plant species interaction for the root convex hull, a measure of the extent to which root systems explore the soil, which suggested pea and wheat grew better in the clay soil when at a high bulk density, compared to tomato which preferred lower bulk density soils. These results, only revealed by high resolution non-destructive imagery, show that while the root penetration mechanisms can lead to soil densification (which could have a negative impact on growth), the immediate root-soil interface is actually a zone of high porosity, which is very important for several key rhizosphere processes occurring at this scale including water and nutrient uptake and gaseous diffusion.

KeywordsRhizosphere; X-ray Computed Tomography; Soil structure; Root architecture; Compaction
Year of Publication2019
JournalPlant, Cell and Environment
Journal citation42 (6), pp. 1974-1986
Digital Object Identifier (DOI)
Open accessPublished as ‘gold’ (paid) open access
FunderBiotechnology and Biological Sciences Research Council
Funder project or codeDesigning Future Wheat - WP1 - Increased efficiency and sustainability
Publisher's version
Output statusPublished
Publication dates
Print04 Feb 2019
Publication process dates
Accepted27 Jan 2019
Copyright licenseCC BY

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