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August 27, 2026Soil Research

Soil physical quality and organic carbon in agricultural systems of the Dry Chaco: influence of land use intensity and predictive models

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Authors

ANA. S. NocerezGPG. E. PeraltaHKH. Rimski Korsakov

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Overview

Observational study reveals agricultural deforestation accelerates soil compaction and organic carbon loss, indicating vegetative cover mitigates degradation.

Key Points

  • To evaluate how deforestation and agricultural management intensity alter soil physical properties and organic carbon stocks, and to develop predictive models for soil quality evolution.
  • Surveyed 113 sites across 14 farms in northwestern Argentina, measuring soil organic carbon, bulk density, macroporosity, and particle size distribution at depths of 0–10 cm and 10–20 cm alongside surface infiltration.
  • Determined soil organic carbon at equivalent soil mass and calculated a land use intensity index based on the percentage of time with vegetation cover.
  • Applied principal component analysis and linear regression models using years since deforestation, land use intensity, and soil texture as predictive variables.
  • Bulk density increased at 0.0089 Mg m⁻³ year⁻¹ and soil organic carbon declined at 0.20 g kg⁻¹ year⁻¹ after deforestation, with stronger degradation observed in soils low in clay and silt.
  • Higher land use intensity was associated with reduced compaction and greater soil organic carbon, while water infiltration declined steeply once bulk density surpassed 1.40 Mg m⁻³.
  • Predictive models accounted for 53% to 60% of the variability in soil properties using deforestation age, land use intensity, and texture.

Cite This Study

Nocerez et al. (2026) studied this question.

synapsesocial.com/papers/6a8fea3310c91c1e9262252fhttps://doi.org/10.1071/sr25213
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