心土混拌比例对白浆土水力学性质的影响

Effect of Subsoil Mixing Proportion on the Hydraulic Properties of Ablic Soil

  • 摘要:
    目的 针对白浆土中白浆层质地坚硬和水分有效性差的问题,本研究探讨了不同比例白浆层与淀积层土壤混拌后的水力学特征随容重和收缩变化的规律,以期为白浆土的机械改良提供理论支撑。
    方法 通过室内模拟实验,将白浆层与淀积层土壤按体积比3∶1、3∶2和3∶3混拌,并设置1.25 g cm−3和1.50 g cm−3两个容重,测定水分特征曲线、收缩特征及相关水力参数等。
    结果 白浆层和淀积层土壤的线性伸展系数分别为0.093和0.155,属于强胀缩性土壤。土壤收缩导致田间持水量和凋萎系数显著升高15.79%和37.51%,通气容量显著下降44.79%,大、中和有效孔隙度显著降低,小孔隙度显著提升。考虑收缩时,与白浆层比,混拌处理提高了土壤持水性以及在低吸力时的释水能力;在低容重下混拌处理的通气容量和大孔隙度显著提升了10.55% ~ 12.08%和27.47% ~ 39.56%;在高容重下混拌处理的凋萎系数和通气容量显著提升了13.39% ~ 18.41%和22.37% ~ 29.37%,大、小孔隙度显著提高了245.45% ~ 336.36%和13.95% ~ 18.59%。3∶2混拌处理的有效含水量和有效孔隙度高于其他混拌处理。
    结论 白浆层和淀积层的强收缩性显著影响土壤水力学性质和各级孔隙度;混拌处理显著改善白浆层土壤通气性,高容重下对大、小孔隙度的改善更明显,3∶2混拌比例改良水力学性质的效果最佳。

     

    Abstract:
    Objective To address the issues of heavy texture and poor water availability in the albic layer of the albic soils, this study investigated the changes in soil hydraulic properties when mixing soils in the albic and illuvial layers at varied proportions as affected by soil bulk density and shrinkage behavior, which would provide theoretical support for the mechanical amelioration of albic soils.
    Method An indoor simulation experiment was conducted, in which albic and illuvial layers were mixed at volume ratios of 3: 1, 3: 2, and 3: 3, with two bulk densities of 1.25 g cm−3 and 1.50 g cm−3. The soil water characteristic curve, shrinkage behavior and related soil hydraulic parameters were measured.
    Result The linear extensibility coefficients of the soils in the albic and illuvial layers were 0.093 and 0.155, indicating they had large shrinkage capacity. Soil shrinkage significantly increased the field capacity and wilting point by 15.79% and 37.51%, while air capacity decreased significantly by 44.79%. The porosities of macro-, meso-, and effective pores significantly decreased, whereas the micro-porosity increased. When soil shrinkage was considered, compared to the albic layer soil, the mixed treatments exhibited improved water retention and water release capability at low suction. Under low bulk density, the mixed treatments significantly enhanced the wilting point and air capacity by 13.39% - 18.41% and 22.37% - 29.37%, while increasing macro- and micro- porosities by 245.45% - 336.36% and 13.95% - 18.59%. The 3: 2 mixing treatment exhibits higher available water content and effective porosity than other mixing treatments.
    Conclusion The high soil shrinkage capacity of the albic and illuvial layers significantly affects soil hydraulic properties and pore size distribution. Mixing treatments significantly improve soil aeration in the albic layer, with more pronounced enhancements in water retention and macro- and micro-porosities under higher bulk density. The 3: 2 mixing ratio demonstrates the most effective improvement in hydraulic properties.

     

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