Converting Cropland to Forest Improves Soil Water Retention Capacity by Changing Soil Aggregate Stability and Pore-Size Distribution

Feng Gu, Minghua Zhou (), Bo Zhu and Heng Wang
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Feng Gu: Sichuan Academy of Environmental Policy and Planning, Chengdu 610093, China
Minghua Zhou: Key Laboratory of Mountain Surface Processes and Ecological Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610299, China
Bo Zhu: Key Laboratory of Mountain Surface Processes and Ecological Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610299, China
Heng Wang: Sichuan Academy of Environmental Policy and Planning, Chengdu 610093, China

Sustainability, 2025, vol. 17, issue 10, 1-20

Abstract: The semi-arid region of North China has undergone extensive afforestation to prevent land degradation. Although afforestation was considered an effective way to improve soil water retention, the mechanism by which it affects soil hydraulic properties remained uncertain. In this study, soil water retention curve (SWRC), soil water-stable aggregates, and other soil physicochemical properties were determined in short-term abandoned cropland (AC), shrubland (SL), and woodland (WL) that had been converted from cropland for 1, 8, and 24 years, respectively. Pearson correlation analysis and partial least-squares structural equation modeling methods were used to identify the main factors affecting soil hydraulic properties. Results showed that the SWRCs of all three land uses were well-fitted by a double-exponential model. The WL and SL land uses exhibited higher soil field capacity (0.33–0.37 cm 3 cm −3 ), wilting point (0.20–0.23 cm 3 cm −3 ), and available water content (0.13–0.15 cm 3 cm −3 ). Surface soil exhibits a more pronounced trend in water retention capacity changes compared to subsoil under vegetation restoration. The WL and SL land uses showed more soil macroaggregates and intra-aggregate pores at surface layers, which mainly explained the variations in hydraulic properties. The main factors influencing soil hydraulic properties were soil aggregates, matrix and structural porosity, soil organic carbon (SOC), and soil bulk density (BD). Overall, afforestation can improve soil hydraulic properties and could be an effective practice for soil and water conservation in the semi-arid region of North China.

Keywords: land use; soil hydraulic property; hydraulic connectivity; soil aggregate; pore-size distribution (search for similar items in EconPapers)
JEL-codes: O13 Q Q0 Q2 Q3 Q5 Q56 (search for similar items in EconPapers)
Date: 2025
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