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Effects of Deep Ploughing Combined with Subsurface Drainage on Soil Water–Salt Dynamics and Physical Properties in Arid Regions

Author

Listed:
  • Miao Wu

    (College of Hydraulic and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, China)

  • Yingjie Ma

    (College of Hydraulic and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, China)

  • Pengrui Ai

    (College of Hydraulic and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, China)

  • Zhenghu Ma

    (College of Hydraulic and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, China)

  • Changjiang Liu

    (College of Hydraulic and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, China)

Abstract

A two-year (2024–2025) field experiment was conducted in southern Xinjiang to alleviate soil compaction and severe salinization in saline–alkali soils and to evaluate the combined effects of tillage depth and subsurface drain spacing on soil improvement. Six treatments were established with three deep tillage depths, 70 cm (W1), 50 cm (W2), and 30 cm (W3), and two subsurface drain spacings, 20 m (S1) and 40 m (S2). Treatment effects on soil water–salt dynamics, soil physical properties and structure, ionic composition, and subsurface drainage and salt removal were analyzed. This study provides mechanistic and practical evidence that coupling deep tillage with subsurface drainage creates a more effective leaching–drainage pathway than either measure alone and enables robust optimization of design parameters (drain spacing × tillage depth) for saline–alkali land improvement in arid regions. Deep tillage in combination with subsurface drainage significantly increased soil profile water content, total porosity, and cumulative subsurface drainage and salt export, all of which reached their maxima under S1W1; it also significantly reduced bulk density, total salinity, and the concentrations of Na + , K + , Mg 2+ , Ca 2+ , Cl − , and SO 4 2− , which reached their minima under S1W1. After two spring irrigation–leaching events (in 2024 and 2025), surface salt accumulation in the soil profile was markedly alleviated, and the mean salinity in the 0–20 cm layer decreased by 45.68% across treatments. The S1W1 treatment achieved the best desalinization performance in both leaching events, with reductions of 41.36% and 44.68%, respectively. Pearson correlation analysis indicated that the desalinization effect was significantly negatively correlated with porosity and significantly positively correlated with bulk density and ionic concentrations. Overall, coupling deep tillage with subsurface drainage effectively reduced soil salinity and harmful ions, improved soil structure, and enhanced drainage-mediated salt removal, with the 70 cm tillage depth combined with a 20 cm drain spacing delivering the best performance.

Suggested Citation

  • Miao Wu & Yingjie Ma & Pengrui Ai & Zhenghu Ma & Changjiang Liu, 2026. "Effects of Deep Ploughing Combined with Subsurface Drainage on Soil Water–Salt Dynamics and Physical Properties in Arid Regions," Sustainability, MDPI, vol. 18(2), pages 1-19, January.
  • Handle: RePEc:gam:jsusta:v:18:y:2026:i:2:p:862-:d:1840636
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