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February 9, 2026Geophysical Journal International0 citationsOpen Access

Investigations of compacted soil-organics mixtures with Spectral Induced Polarisation

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TBThierry BoréThe University of QueenslandFDF. DelarueCentre National de la Recherche ScientifiqueSOSebastian Quintero OlayaThe University of Queensland

Key Points

  • To explore the relationships between soil-organic mixtures and their electrical and physical properties using SIP.
  • Investigated various organic matter types (biosolids, peat, sugar cane residue) mixed with synthetic clayey soil.
  • Analysed electrical spectral induced polarisation, mechanical, hydraulic, and chemical properties of mixtures.
  • Used inorganic clay to simulate real soil conditions for more accurate results.
  • Strong correlation found between SIP complex conductivity and total organic carbon content.
  • The slope of the relationship increased with the aromaticity of the organic matter.
  • SIP response unaffected by soil water saturation and bulk density.

Abstract

Summary In this study, we present a new integrated experimental approach to investigate simultaneously the electrical spectral induced polarisation (SIP), mechanical, hydraulic and chemical properties of synthetic clayey soil mixed with different types and quantities of organic matter. It addresses knowledge gaps that aim to advance SIP as a non-destructive analysis tool for soils. We used an inorganic clay as a proxy for clayey soil with a moderate cation exchange capacity to achieve more realistic test conditions since most studies use sand. Three organic matter (OM) types with contrasting properties, biosolids, peat and sugar cane residue, broaden the range of organic carbon materials that have been tested. Our study demonstrates a strong relationship between the imaginary part of the complex conductivity and the total organic carbon content of the soil-OM mixtures. It indicates that the relationships depend on the degree of aromaticity, with the slope angle increasing as the degree of aromaticity of the OM increases. Hence, the quantity of OM, as well as its chemical structure, plays a key role in SIP response. Interestingly, these relationships are independent of soil water saturation and bulk density. These findings are of paramount importance for enabling field-scale applications and confirm the potential of SIP as a non-invasive tool for monitoring and characterising soil in situ.

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Cite This Study

Boré et al. (2026) studied this question.

synapsesocial.com/papers/69897a25f0ec2af6756e86edhttps://doi.org/10.1093/gji/ggag021
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