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A quantitative assessment of the dynamic process and potential capacity of using gypsum to reclaim sodic soil

  • Soils, Sec 3 • Remediation and Management of Contaminated or Degraded Lands • Research Article
  • Published:
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Abstract

Purpose

The effectiveness of gypsum in sodic soil amelioration has been widely recognized. The basic amelioration mechanism is well known, but quantitative details are lacking; such details would clarify the process so that gypsum can be used more rationally and efficiently in actual amelioration projects of sodic land.

Materials and methods

Sodic soil with pH, electrical conductivity (EC), exchangeable sodium percentage (ESP) and sodium adsorption ratio (SAR) values of 9.4, 0.66 mS cm–1, 43.3% and 58.6 (mmolc L−1)1/2, respectively, was sampled from the Songnen Plain. Three gypsum solutions with concentrations of 0 (CK), 1.13 (half-saturated solution; 1/2GS) and 2.26 g L–1 (saturated solution; GS) were used to leach sodic soil columns (inner diameter and depth were all 5 cm) and the variations in pH, EC and ion concentration in the leachate and soil were investigated.

Results and discussion

The eluent appeared at the bottom of the soil column after 1.8, 64.4 and 147.6 h for the GS, 1/2GS, and CK treatments, respectively. The rates of infiltration and salt leaching at a given time were always faster in the GS treatment, followed by the 1/2GS treatment. In the GS leachate, the curves of infiltration rate, pH, EC and HCO3 concentration with the cumulative volume of leachate all showed turning points at a leachate pore volume (PV) of 0.6. As leaching continued, Ca–Na exchange, followed by Ca–Mg exchange, occurred in the gypsum-treated soil. The Ca2+ utilization rate was 96.5% and 94.4% in the GS and 1/2GS treatments, respectively, in the period of Ca–Na exchange, and the rate during Ca–Mg exchange was higher in the 1/2GS than the GS treatment. When the cumulative leachate volume reached 18 and 20 PV in the GS and 1/2GS treatments, respectively, the leachate EC and pH values were stable (the errors of three consecutive leachate samples were all within 0.5% and 0.5, respectively; equilibrium state). In the gypsum treatments, the soil pH, SAR and ESP decreased by more than 1.5 units, 13.8 (mmolc L−1)1/2 and 22.3%, respectively, compared to CK.

Conclusions

To achieve rapid amelioration, efficient utilization of Ca2+, and reduced water consumption, it is suggested that the initial gypsum application rate for sodic soil amelioration be calculated on the basis of the exchangeable Na+ concentration and combined with appropriate water measures to maintain a high concentration of gypsum solution, followed by multiple applications of small amounts to create a low-concentration gypsum solution environment to reduce Mg2+.

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Funding

This research was supported by the National Key Research and Development Program of China (2022YFD1500502).

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Correspondence to Yonggan Zhao.

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Wenchao Zhang and Wenxin Zhang contributed equally to this article as first authors.

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Zhang, W., Zhang, W., Wang, S. et al. A quantitative assessment of the dynamic process and potential capacity of using gypsum to reclaim sodic soil. J Soils Sediments 23, 3082–3095 (2023). https://doi.org/10.1007/s11368-023-03535-6

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