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Electrical resistivity tomography as a non‐destructive method for mapping root biomass in an orchard
Author(s) -
Rossi R.,
Amato M.,
Bitella G.,
Bochicchio R.,
Ferreira Gomes J. J.,
Lovelli S.,
Martorella E.,
Favale P.
Publication year - 2011
Publication title -
european journal of soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.244
H-Index - 111
eISSN - 1365-2389
pISSN - 1351-0754
DOI - 10.1111/j.1365-2389.2010.01329.x
Subject(s) - electrical resistivity tomography , orchard , soil science , electrical resistivity and conductivity , soil water , bulk density , environmental science , soil test , organic matter , agronomy , ecology , biology , physics , quantum mechanics
Multi‐electrode soil electrical resistivity ( ρ ) tomography was used for the non‐invasive study of tree roots in situ and their spatial distribution in an agricultural soil. The quantitative relations of ρ and root biometry and the contribution of different root size classes were investigated with two‐ and three‐dimensional 48‐electrode tomograms in an orchard in southern Italy on a Typic haploxeralf fine, mixed termic soil. Root biomass density ( RD ) and root length density ( RLD ) were measured destructively on coarse (>2 mm diameter) and fine roots, and soil paste electrical conductivity, water content, stone content, texture, organic matter and pH were measured on soil samples taken up to 0.48‐m deep. Areas of large ρ values (up to 460 ohm m) were found close to tree trunks and variability in ρ was related to RD (0–0.137 Mg m −3 ) only; the resistive response was from coarse roots. The effect of other soil variables on ρ was overshadowed by the presence of roots and therefore no significant multivariate relationship was found. A highly significant ρ ‐ RD gamma GLM model used to fit positively skewed data provides a useful framework for regression analysis when ρ is dominated by roots. Soil electrical resistivity is promising as a proxy for RD in orchards, but not for RLD , and the effect of tree roots on ρ needs to be taken into account in electrical surveys of soils.

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