高级检索

    黑土区坡耕地表层土壤抗冲性及团聚体流失特征

    The surface soil anti-scouribility and aggregate loss characteristics in cultivated land of the black soil area

    • 摘要: 为探明坡耕地表层土壤抗冲性及团聚体流失特征,以黑土坡耕地表层原状土(0 ~ 6 cm)为研究对象,通过室内模拟放水冲刷试验,在5种冲刷流量(6、12、18、24和30 L/min)条件下,探究土壤抗冲系数与冲刷历时、冲刷流量以及土壤团聚体流失特征之间的关系,以揭示黑土坡耕地表层土壤的抗冲性及放水冲刷前后对团聚体流失特征的影响。结果表明:1)整体上看,土壤流失总量随冲刷流量增大逐渐增加。不同冲刷流量条件下,土壤流失量随冲刷历时的延长呈指数函数递减。2)在冲刷流量6、12和18 L/min条件下,土壤抗冲系数随冲刷历时的延长呈幂函数递增。3)土壤团聚体流失特征受不同冲刷流量影响程度不同。整体上看,随着冲刷流量的增大,土壤团聚体稳定性逐渐下降,≤ 0.25 mm粒径团聚体质量分数逐渐增大。与此相反,> 2 mm粒径团聚体质量分数呈逐渐减小的趋势。> 0.5 ~ 1 mm团聚体为6、12、18 L/min冲刷流量下的主要流失粒径,流失比例为26.84% ~ 29.66%。4)在冲刷流量6、12、18 L/min条件下,≤ 0.25 mm粒径团聚体质量分数较放水冲刷前分别增加2.49、14.17和4.18倍。结果还表明:随着冲刷流量的增大,黑土坡耕地表层土壤流失总量逐渐增加,土壤抗冲性越强,土壤团聚体稳定性逐渐下降。此外,3种冲刷流量下土壤抗侵蚀能力表现为6 > 12 > 18 L/min。研究结果可为明晰黑土坡耕地表层土壤抗冲性变化和农耕地利用提供参考。

       

      Abstract:
      Background Soil erosion can cause the dispersion and breakdown of soil aggregates. One key indicator of soil erosion resistance is soil anti-scourability. In black soil regions, the surface soil of cultivated land is particularly vulnerable to the scouring effects of runoff. This runoff can further break down and disperse soil aggregates. Therefore, studying the soil’s anti-scourability, as well as the erosion characteristics of soil aggregates of different particle sizes in the surface soil of black soil cultivated land is essential.
      Methods To investigate the anti-scourability and aggregate loss characteristics of surface soil in cultivated land of the black soil area, the undisturbed soil (0-6 cm) was taken as the research object. The relationships between soil anti-scourability coefficient, scouring duration, scouring amount, and soil aggregate loss characteristics were explored, with 5 scouring amounts (6, 12, 18, 24, and 30 L/min) under indoor simulated runoff scouring experiments.
      Results 1) Overall, the total amount of soil loss gradually increased with the increase of scouring amount. The total amount of soil loss at a scouring amount of 18 L/min was 1.50 times that of 6 L/min. The soil loss decreased exponentially with decreasing scouring duration. 2) Under the conditions of scouring amounts of 6, 12, and 18 L/min, the soil anti-scourability coefficient increased as a power function with scouring duration. The soil anti-scourability coefficient was highest at a scouring amount of 18 L/min within 15 minutes, which was 2.01 and 1.38 times that at 12 and 6 L/min, respectively. 3) The loss characteristics of soil aggregates were differently affected by the scouring amount. Overall, the stability of soil aggregates gradually decreased with the increase of scouring amount, and the mass percentage of ≤ 0.25 mm aggregates gradually increased. Conversely, the mass percentage of > 2 mm aggregates gradually decreased. The fraction size of 0.5-1 mm aggregate was the main lost fraction size under different scouring amounts, accounting for 26.84%-29.66%. 4) Compared to before runoff scouring, the mass percentage of ≤ 0.25 mm aggregates under the scouring amounts of 6, 12, and 18 L/min increased by 2.49, 14.17, and 4.18 times, respectively. 5) The erosion resistance of soils gradually decreased as the scouring amount increased. The mean weight diameter of soil aggregates significantly decreased by 4.63 times than before runoff scouring under a scouring amount of 12 L/min. The fractal dimension of soil aggregates at a scouring amount of 18 L/min was 1.05 times that of 6 L/min.
      Conclusions The total amount of soil loss in the surface soil of cultivated land of the black soil gradually increased with the increase of scouring amount. At the same time, the soil anti-scourability became stronger and the stability of soil aggregates gradually decreased. Additionally, the erosion resistance of soil under the 3 scouring amounts was ranked as 6 > 12 > 18 L/min. The research results provide insights into the changes in the surface soil anti-scourability in cultivated land of black soil and offer references for agricultural land use.

       

    /

    返回文章
    返回