Journal
PLANT CELL AND ENVIRONMENT
Volume 36, Issue 6, Pages 1085-1092Publisher
WILEY-BLACKWELL
DOI: 10.1111/pce.12037
Keywords
bulk density; compaction; lubrication; mechanical impedance; rhizosphere; soil strength
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Funding
- School of Agriculture, La Trobe University
- Scottish Government's Rural and Environment Science and Analytical Services (RESAS) Division
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To penetrate soil, a root requires pressure both to expand the cavity it is to occupy, sigma n, and to overcome rootsoil friction, sigma f. Difficulties in estimating these two pressures independently have limited our ability to estimate the coefficient of soilroot friction, sr. We used a rotated penetrometer probe, of similar dimensions to a root, and for the first time entering the soil at a similar rate to a root tip, to estimate sigma n. Separately we measured root penetration resistance (PR) Qr. Root PR was between two to four times sigma n. We estimated that the coefficient of rootsoil friction (sr) was 0.210.26, based on the geometry of the root tip. This is slightly larger than the 0.050.15 characteristic of boundary lubricants. Scanning electron microscopy showed that turgid border cells lined the root channel, supporting our hypothesis that the lubricant consisted of mucilage sandwiched between border cells and the surface of the root cap and epidermis. This cellcell lubrication greatly decreased the friction that would otherwise be experienced had the surface of the root proper slid directly past unlubricated soil particles. Because rootsoil friction can be a substantial component of root PR, successful manipulation of friction represents a promising opportunity for improving plant performance.
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