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A quantitative study on three-dimensional pore parameters and physical properties of sodic soils restored by FGD gypsum and leaching water

机译:烟气脱硫石膏和淋洗水修复苏打土壤三维孔隙参数和物理性质的定量研究

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摘要

The application of flue gas desulfurization (FGD) gypsum has been recognized as a feasible measure in enhancing the quality of sodic soils. Quantitative evaluation of the effects of FGD gypsum on three-dimension (3D) pore characteristics is beneficial for understanding the reclamation mechanism of FGD gypsum on sodic soils. We collected intact soil cores from a sodic field at four depths (0-10, 10-20, 20-40, and 40-60 cm) in northern China to reconstruct 3D pore structures using X-ray computed tomography (CT), thus quantifying the effects of FGD gypsum (10.1 and 14.5 t hm(-2)) and leaching water (1520 and 2200 t hm(-2)) on the 3D pore characteristics and related soil physical properties. The treatments using FGD gypsum with leaching water promoted the formation of new pores and significantly (p < 0.05) increased the 3D image-based macroporosity, mesoporosity, total pore length, and number of nodes at depths of 0-20 cm, improving the permeability of sodic soils investigated, which is validated by the enhanced saturated hydraulic conductivity (K-sat). Irrigation water of 1520 t hm(-2) is demonstrated effective in assisting FGD gypsum dissolution and leaching, but excessive leaching water (2200 t hm(-2)) may reduce the permeability of 20-40 cm depth. The combined application of 14.5 t hm(-2) FGD gypsum and 1520 t hm(-2) leaching water is suggested to obtain the optimal result for the investigated sodic soils. This study offers an applicable strategy for sodic soils reclamation and provides a reference for revealing the improvement mechanism of sodic soils by FGD gypsum and leaching water.
机译:烟气脱硫(FGD)石膏的应用已被认为是提高钠盐土壤质量的可行措施。定量评估烟气脱硫石膏对三维(3D)孔隙特征的影响,有助于理解烟气脱硫石膏在苏打土壤上的复垦机理。我们从中国北方4个深度(0-10、10-20、20-40和40-60 cm)的苏打田中收集了完整的土壤核心,以使用X射线计算机断层扫描(CT)重建3D孔隙结构,因此量化FGD石膏(10.1和14.5 t hm(-2))和浸出水(1520和2200 t hm(-2))对3D孔隙特征和相关土壤物理特性的影响。 FGD石膏与浸出水的处理促进了新孔的形成,并显着(p <0.05)增加了基于3D图像的大孔,中孔,总孔长和0-20厘米深度处的节数,从而提高了渗透性的钠盐土壤进行了研究,这通过增加的饱和水导率(K-sat)得到了验证。 1520 t hm(-2)的灌溉水被证明可以有效地帮助FGD石膏溶解和浸出,但是过多的浸出水(2200 t hm(-2))可能会降低20-40 cm深度的渗透性。建议将14.5 t hm(-2)烟气脱硫石膏和1520 t hm(-2)淋洗水组合使用,以获得对所研究的钠土的最佳效果。该研究为苏打土壤复垦提供了一种可行的策略,为揭示FGD石膏和淋洗水改善苏打土壤的机理提供了参考。

著录项

  • 来源
    《Journal of Environmental Management》 |2019年第15期|109303.1-109303.10|共10页
  • 作者单位

    Tianjin Univ Sch Chem Engn & Technol Collaborat Innovat Ctr Chem Sci & Engn Tianjin Key Lab Syst Bioengn Minist Educ Tianjin 300072 Peoples R China|China Inst Water Resources & Hydropower Res Dept Irrigat & Drainage State Key Lab Simulat & Regulat Water Cycles Rive Beijing 100048 Peoples R China;

    Minist Water Resources PR China Dev Res Ctr Beijing 100038 Peoples R China;

    Penn State Univ Dept Ecosyst Sci & Management University Pk PA 16802 USA;

    China Agr Univ Coll Water Resources & Civil Engn Beijing 100083 Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Sodic soils; Gypsum; Leaching; X-ray computed tomography; 3D pore parameters;

    机译:钠土石膏;浸出X射线计算机断层扫描;3D孔参数;

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