2004
DOI: 10.1016/j.still.2004.07.012
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Structural heterogeneity of the soil tilled layer as characterized by 2D electrical resistivity surveying

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Cited by 112 publications
(98 citation statements)
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“…The electrical resistivity of air is virtually infinite; therefore, a dry porous soil is in general more resistive than a compacted one. Besson et al (2004) used surface twodimensional ER tomography with the same settings as those adopted in our study to map soil structure in tilled layers. In their tomograms, soil compaction resulting from wheel traffic was clearly detected, and the plough pan was visible.…”
Section: Resultsmentioning
confidence: 99%
“…The electrical resistivity of air is virtually infinite; therefore, a dry porous soil is in general more resistive than a compacted one. Besson et al (2004) used surface twodimensional ER tomography with the same settings as those adopted in our study to map soil structure in tilled layers. In their tomograms, soil compaction resulting from wheel traffic was clearly detected, and the plough pan was visible.…”
Section: Resultsmentioning
confidence: 99%
“…In some cases, soil texture can dominate the resistivity pattern overshadowing soil structure and water-related properties (Banton et al 1997). For a given texture, though, soil structural state variation, by altering the proportions between water and air filled porosity, can exert a strong effect on resistivity; this is at the base of the successful use of high resolution resistivity tomography for mapping soil alterations induced by tillage (Besson et al 2004;Basso et al 2010). Basso and coauthors (2010) found that resistivity mapping allowed to discern between tilled, freshly tilled, and untilled soils better than penetrometry.…”
Section: Principles Of Geophysical Techniques For Agriculturementioning
confidence: 99%
“…Measurement of parameters describing soil mechanical behaviour, such as shear strength and resistance to penetration, is also commonly used in soil compaction (Horn and Fleige 2003). Geophysical methods are increasingly applied in soil compaction studies, as non-invasive and less time and labour consuming (e. g., electrical resistivity tomography -ERT (Besson et al 2004) and apparent electrical conductivity -EC a (Al-Gaadi 2012;Brevik and Fenton 2004). ERT has been used to study the spatial and temporal variability of many soil physical properties (Samouelian et al 2005).…”
mentioning
confidence: 99%
“…ERT has been used to study the spatial and temporal variability of many soil physical properties (Samouelian et al 2005). It has been also applied to detect the effects of tillage in soil physical properties (Besson et al 2013;Rossi et al 2013), to describe soil tilled layer (Besson et al 2004), to estimate soil water content (Samouelian et al 2005;Seladji et al 2010;Dafonte et al 2013) and saturated hydraulic conductivity (Farzamian et al 2015). Electric conduction occurs within the water-filled pores and at the surface of clay particles.…”
mentioning
confidence: 99%
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