Free Standard AU & NZ Shipping For All Book Orders Over $80!
Register      Login
Soil Research Soil Research Society
Soil, land care and environmental research
RESEARCH ARTICLE

3D Cross-hole resistivity tomography to monitor water percolation during irrigation on cracking soil

A. K. Greve A B , R. I. Acworth A and B. F. J. Kelly A
+ Author Affiliations
- Author Affiliations

A Connected Waters Initiative, University of New South Wales, affiliated with the National Centre for Groundwater Research and Training, The University of New South Wales, Sydney, NSW 2052, Australia.

B Corresponding author. Email: a.greve@wrl.unsw.edu.au

Soil Research 49(8) 661-669 https://doi.org/10.1071/SR11270
Submitted: 12 October 2011  Accepted: 9 December 2011   Published: 28 December 2011

Abstract

Irrigation water entering soil cracks can quickly move past the root-zone without being utilised by plants. To assess the efficiency of irrigation practices, reliable methods to monitor water percolation are needed. Three-dimensional (3D) cross-hole electrical resistivity tomography (ERT) was carried out during three irrigation events on soil with different surface-crack intensities. Changes in the resistivity distribution during the irrigation events were related to water movement. The propagation of resistivity change during irrigation events differed for different degrees of soil cracking. For surface cracks of <2 mm width before the irrigation, the resistivity change propagated evenly down-gradient, indicating matrix flow. During irrigation on soil with 30-mm-wide surface cracks, the resistivity change first occurred in the lower parts of the profile before propagating to the top. This suggests preferential flow filling cracks from the bottom up. The differences in initial soil moisture that resulted in these two flow behaviours were reflected in the pre-irrigation resistivity profile. Subsurface temperature changes during the irrigation confirmed the different flow behaviour. 3D Cross-hole ERT allows monitoring of percolation patterns as well as the pre-irrigation moisture states that cause these patterns. This makes 3D cross-hole ERT an excellent tool for researching irrigation management.

Additional keywords: electrical resistivity, preferential flow, soil moisture, 3D tomography.


References

Acworth RI, Young RR, Bernadi AL (2005) Monitoring soil moisture status in a Black Vertosol on the Liverpool Plains, NSW, using a combination of neutron scattering and electrical image methods. Australian Journal of Soil Research 43, 105–117.
Monitoring soil moisture status in a Black Vertosol on the Liverpool Plains, NSW, using a combination of neutron scattering and electrical image methods.Crossref | GoogleScholarGoogle Scholar |

Batlle-Aguilar J, Schneider S, Pessel M, Tucholka P, Coquet Y, Vachier P (2009) Axisymetrical infiltration in soil imaged by noninvasive electrical resistivimetry. Soil Science Society of America Journal 73, 510–520.
Axisymetrical infiltration in soil imaged by noninvasive electrical resistivimetry.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BD1MXjt12rtLo%3D&md5=9d5aa254681df2d8511264e738b03247CAS |

Bell JP, Dean TJ, Hodnett MG (1987) Soil moisture measurement by an improved capacitance technique, part II. Field techniques, evaluation and calibration. Journal of Hydrology 93, 79–90.
Soil moisture measurement by an improved capacitance technique, part II. Field techniques, evaluation and calibration.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DyaL1cXhsFCjtQ%3D%3D&md5=9cbf693bda9fc96f0b8f96682ac59c58CAS |

Bing Z, Greenhalgh SA (1997) A synthetic study on cross-hole resistivity imaging with different electrode arrays. Exploration Geophysics 28, 1–5.
A synthetic study on cross-hole resistivity imaging with different electrode arrays.Crossref | GoogleScholarGoogle Scholar |

Bing Z, Greenhalgh SA (2000) Cross-hole resistivity tomography using different electrode configurations. Geophysical Prospecting 48, 887–912.
Cross-hole resistivity tomography using different electrode configurations.Crossref | GoogleScholarGoogle Scholar |

Bouma J, Dekker LW (1978) Case-study on infiltration into dry clay soil. 1. Morphological observations. Geoderma 20, 27–40.
Case-study on infiltration into dry clay soil. 1. Morphological observations.Crossref | GoogleScholarGoogle Scholar |

Bronswijk JJB (1991) Drying, cracking, and subsidence of a clay soil in a lysimeter. Soil Science 152, 92–99.
Drying, cracking, and subsidence of a clay soil in a lysimeter.Crossref | GoogleScholarGoogle Scholar |

Charlesworth PB (2005) ‘Irrigation insights. No. 1—Soil water monitoring.’ 2nd edn. National Program for Sustainable Irrigation. (Land & Water Australia: Canberra, ACT)

Dahlin T (2000) Short note on electrode charge-up effects in DC resistivity data acquisition using multi-electrode arrays. Geophysical Prospecting 48, 181–187.
Short note on electrode charge-up effects in DC resistivity data acquisition using multi-electrode arrays.Crossref | GoogleScholarGoogle Scholar |

deGroot-Hedlin C, Constable S (1990) Occam inversion to generate smooth, 2-dimensional models from magnetotelluric data. Geophysics 55, 1613–1624.
Occam inversion to generate smooth, 2-dimensional models from magnetotelluric data.Crossref | GoogleScholarGoogle Scholar |

Dey A, Morrison HF (1979) Resistivity modelling for arbitrary shaped two-dimensional structures. Geophysical Prospecting 27, 1020–1036.

Gardner W, Kirkham DON (1952) Determination of soil moisture by neutron scattering. Soil Science 73, 391–402.
Determination of soil moisture by neutron scattering.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DyaG3sXksFOqsg%3D%3D&md5=d989de009aead02cc6ef945cce06d84bCAS |

Garré S, Javaux M, Vanderborght J, Pages L, Vereecken H (2011) Three-dimensional electrical resistivity tomography to monitor root zone water dynamics. Vadose Zone Journal 10, 412–424.
Three-dimensional electrical resistivity tomography to monitor root zone water dynamics.Crossref | GoogleScholarGoogle Scholar |

Greve AK (2009) Detection of subsurface cracking depth through electrical resistivity anisotropy. PhD Thesis, The University of New South Wales, Sydney, Australia. (http://handle.unsw.edu.au/1959.4/45153).

Greve AK, Acworth RI, Kelly BFJ (2010) Detection of subsurface soil cracks by vertical anisotropy profiles of apparent electrical resistivity. Geophysics 75, WA85–WA93.
Detection of subsurface soil cracks by vertical anisotropy profiles of apparent electrical resistivity.Crossref | GoogleScholarGoogle Scholar |

Hayley K, Bentley LR, Gharibi M, Nightingale M (2007) Low temperature dependence of electrical resistivity: Implications for near surface geophysical monitoring. Geophysical Research Letters 34, L18402

Kelly BFJ, Acworth RI, Greve AK (2011) Better placement of soil moisture point measurements guided by 2D resistivity tomography for improved irrigation scheduling. Soil Research 49, 504–512.
Better placement of soil moisture point measurements guided by 2D resistivity tomography for improved irrigation scheduling.Crossref | GoogleScholarGoogle Scholar |

LaBrecque D, Daily W (2008) Assessment of measurement errors for galvanic-resistivity electrodes of different composition. Geophysics 73, F55–F64.
Assessment of measurement errors for galvanic-resistivity electrodes of different composition.Crossref | GoogleScholarGoogle Scholar |

Loke MH (2008) Res3Dinv x64 Manual. In ‘Geoelectrical Imaging 2D & 3D’. (Geotomo Software: Gelugor, Malaysia)

Loke MH, Acworth I, Dahlin T (2003) A comparison of smooth and blocky inversion methods in 2D electrical imaging surveys. Exploration Geophysics 34, 182–187.

Michot D, Benderitter Y, Dorigny A, Nicoullaud B, King D, Tabbagh A (2003) Spatial and temporal monitoring of soil water content with an irrigated corn crop cover using surface electrical resistivity tomography. Water Resources Research 39, 1138
Spatial and temporal monitoring of soil water content with an irrigated corn crop cover using surface electrical resistivity tomography.Crossref | GoogleScholarGoogle Scholar |

Miller CR, Routh PS, Brosten TR, McNamara JP (2008) Application of time-lapse ERT imaging to watershed characterization. Geophysics 73, G7–G17.
Application of time-lapse ERT imaging to watershed characterization.Crossref | GoogleScholarGoogle Scholar |

Mitchell AR, Van Genuchten MT (1993) Flood irrigation of a cracked soil. Soil Science Society of America Journal 57, 490–497.
Flood irrigation of a cracked soil.Crossref | GoogleScholarGoogle Scholar |

Rothe A, Weis W, Kreutzer K, Matthies D, Hess U, Ansorge B (1997) Changes in soil structure caused by the installation of time domain reflectometry probes and their influence on the measurement of soil moisture. Water Resources Research 33, 1585–1593.
Changes in soil structure caused by the installation of time domain reflectometry probes and their influence on the measurement of soil moisture.Crossref | GoogleScholarGoogle Scholar |

Sharma PV (1997) ‘Environmental and engineering geophysics.’ (Cambridge University Press: Cambridge, UK)

Topp GC, Davis JL, Annan AP (1980) Electromagnetic determination of soil water content: measurements in coaxial transmission lines. Water Resources Research 16, 574–582.
Electromagnetic determination of soil water content: measurements in coaxial transmission lines.Crossref | GoogleScholarGoogle Scholar |

Van Stiphout TPJ, Van Lanen HAJ, Boersma OH, Bouma J (1987) The effect of bypass flow and internal catchment of rain on the water regime in a clay loam grassland soil. Journal of Hydrology 95, 1–11.
The effect of bypass flow and internal catchment of rain on the water regime in a clay loam grassland soil.Crossref | GoogleScholarGoogle Scholar |

Vervoort W, Silburn M, Kirby M (2003) Near surface water balance in the northern Murray-Darling basin. Water Science and Technology 48, 207–214.

White EM (1970) Giant desiccation cracks in Central South-Dakota soils. Soil Science 110, 71–73.
Giant desiccation cracks in Central South-Dakota soils.Crossref | GoogleScholarGoogle Scholar |

Xu BW, Noel M (1993) On the completeness of data sets with multielectrode systems for electrical-resistivity survey. Geophysical Prospecting 41, 791–801.
On the completeness of data sets with multielectrode systems for electrical-resistivity survey.Crossref | GoogleScholarGoogle Scholar |