黄土区不同龄期灌木柠条锦鸡儿根系的分布特征及其固土护坡效果

    Evaluating soil conservation from root distribution of Caragana Korshinskii Kom in the Loess region of Xining Basin

    • 摘要: 为定量评价西宁盆地黄土区优势灌木柠条锦鸡儿根系固土护坡效果,该研究以区内生长期为幼龄期(<6 a)、中龄期(6~14 a)和老龄期(>14 a)3个龄期的柠条锦鸡儿为研究对象,通过原位挖掘法与原位拉拔试验相结合的方式,调查不同龄期柠条锦鸡儿根系形态学指标和根系分布特征,并通过单根拉伸试验获得单根抗拉强度。以此为基础,利用WWM模型对不同龄期柠条锦鸡儿根系附加黏聚力进行计算,评价不同龄期柠条锦鸡儿根系对土体抗剪强度的增强效果。结合有限元数值模拟分析,定量评价不同龄期柠条锦鸡儿根系加筋和锚固作用对黄土边坡稳定性的贡献。结果表明:随着龄期的增加,柠条锦鸡儿根系埋深、根系总根长、主根根径和主根根长均逐渐增加;各龄期柠条锦鸡儿根系主要分布在0~0.6 m土层深度范围内,随着土层深度增加,幼龄期和老龄期根系根长和根数呈逐渐减少趋势;中龄期根系则呈先增大后减小趋势,根长和根数的最大值出现在0.3~0.6 m的土层深度内。幼龄期和老龄期柠条锦鸡儿根面积比和根系附加黏聚力均随着土层深度增加而逐渐减少,中龄期柠条锦鸡儿则呈先增大后减小变化趋势,且该龄期根系增强土体抗剪强度的效果相对最为显著。不同龄期柠条锦鸡儿根系均能够降低边坡坡肩、坡体中间位置总位移和最大总位移,并提高边坡稳定系数,但提升幅度有限,在0.19%~0.93%之间。随着龄期的增大,柠条锦鸡儿根系固土护坡主导力学效应由加筋作用逐渐转变为锚固作用。研究可为西宁盆地及其周边地区生态恢复、植被护坡工程的实施提供理论指导。

       

      Abstract: Caragana korshinskii Kom is one of the most important dominant shrub species in the loess region of Xining Basin. This study aims to quantitatively evaluate the mechanical effects of the roots on soil reinforcement and slope protection. Three growth stages were also selected (early age (<6 years old), middle age (6-14 years old), and old age (>14 years old)). The root morphological indexes and root geometric distribution were investigated at different ages via in situ excavation method and in situ pull-out test. The tensile strength of single roots was obtained via the single-root tensile test. In addition, the WWM model was used to evaluate the enhancement effect of roots on the soil shear strength at different growth stages. Moreover, the finite element (FE) simulation was carried out to determine the contribution of reinforcement and anchoring effect of C. korshinskii roots at different growth stages for the better stability of the loess slope. The results showed that the root depth, root width, total root length, and taproot diameter of the C. korshinskii were 3.610-5.500, 7.831-28.603 m, and 11.520-22.043 mm, respectively, indicating an increasing trend with the increase of age. Among them, the root length and root number were distributed mainly in the range of 0-0.6 m soil depth. Specifically, there was a significant decrease in the early and old age C. korshinskii with the increasing depth, whereas, the root length and root number at the middle age initially decreased with the soil depth and then increased with the turning point at the soil depth of 0.3-0.6 m. The root area ratio (RAR) and root additional cohesion at early and old age decreased with the increasing soil depth. Furthermore, the middle age C. korshinskii increased first and then decreased, indicating the most significant effect on the shear strength of the soil. The roots of C. korshinskii at different growth stages reduced the total displacement of the slope shoulder and central position of the slope, as well as the maximum total displacement of the slope. The maximum total displacements of C. korshinskii slope in early, middle and old age were 0.10%, 1.40%, and 1.88% lower than those of bare slope, respectively. The stability coefficient of the plant slope was in the range of 1.072-1.080, which was 0.19%-0.93% higher than that of the bare slope, indicating an increasing trend with the increase in plant age. The roots of C. korshinskii at different growth stages improved the slope stability coefficient, but the increase was limited. The dominant mechanical effect of C. korshinskii roots gradually evolved from the soil reinforcement to the anchoring effect from early to old age, indicating the strong influence of the plant growth stages. The finding can offer theoretical guiding to implement the ecological restoration and vegetation slope protection projects in Xining Basin and surrounding areas.

       

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