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    基于团聚体性质的等高反坡阶改良土壤结构评价

    Structure evaluation of the improved soil with contour reverse-slope terrace based on soil aggregates property

    • 摘要: 为探明等高反坡阶(CRT)措施促进坡耕地退化土壤生态修复的机理,以云南松华坝迤者流域坡耕地为对象,测定CRT坡耕地不同位置(阶上,CRT-A;阶下,CRT-B)和土层深度的土壤团聚体性质和物理性质,并以原状坡耕地(CK)相应位置作对比,构建基于团聚体性质的土壤结构评价指标体系。结果表明:1)CRT措施可显著改善土壤孔隙状况、团聚体组成特征和稳定性;2)通过构建最小数据集,获得土壤结构评价指标体系(包括土壤密度、孔隙度、几何平均直径、稳定性团聚体、总团聚体和>2~5 mm团聚体),计算土壤结构指数评价土壤结构水平;3)土壤结构整体上表现为CRT>CK。CRT坡耕地土壤结构指数相较于CK提高23.1%~36.2%,土壤结构属于中等水平;4)CRT使坡耕地阶下土壤结构优于阶上,0~5、5~10和10~20 cm土层阶下土壤结构指数较CK分别增加25.2%、27.3%和25.7%,主要由于阶下土壤受到CRT的防冲刷保护和营养富集作用的影响。综上,CRT通过提高土壤大团聚体比例,增加土壤孔隙度,改善土壤结构,提高坡耕地土壤结构性能,促进其退化土壤的修复。

       

      Abstract:
      Background Yunnan is situated in a mountainous area, and there are only two seasons, rainy season and dry season.In rainy season, concentrated and heavy rainfall increases a great probability of soil erosion.As the main type of arable fields, sloping farmland is regarded as the key cultivated land type for soil and water loss.The contour reverse-slope terrace (CRT) increases soil water storage, root exudation, enzyme activities and reduces soil surface runoff and moisture loss, erosion and degradation, which improves the soil environment through changes of runoff and sediment yield, has been well documented, but the reasons remain unclear.In this study, we aim to elucidate the mechanisms of soil structure improvement and ecological remediation with the CRT in sloping farmland.
      Methods A field location experiment was conducted in the watershed of Yizhe in Songhua dam in Yunnan with two measures: Above and below the terrace in CK sloping farmland (CK-A, CK-B), above and below the terrace in CRT sloping farmland (CRT-A, CRT-B).The composition and stability were analyzed by measuring 0-5, 5-10, 10-20 and 20-40 cm soil mechanical-stable aggregates, physical property and constructed minimum data set to evaluate soil structure.In order to evaluate the effect of CRT on soil structure improvement in sloping farmland, a soil structure evaluation index system based on aggregates properties was constructed.
      Results 1) CRT measures improved the soil pore status, aggregates composition characteristics and stability significantly.2) Six indicators including soil bulk density, soil porosity, geometric mean diameter (GMD), stable aggregates (R0.25), total aggregates (At) and >2-5 mm soil aggregates were identified as the main indicators for soil structure evaluation in the minimum data set.The verification of total data set suggested that the minimum data set reflected the effective information and accuracy evaluation for soil structure.3) The soil structure index in CRT, compared with CK, ranging from 0.26 to 0.58, increased by 23.1% and 36.2%, indicating that soil structure was on the middle level; meanwhile, below the terrace in CRT, soil structure index in the 0-5, 5-10 and 10-20 cm soil layer increased by 25.2%, 27.3% and 25.7% compared with that in CK, respectively.It is mainly due to the erosion protection from both the upper and lower steps.
      Conclusions The CRT measures promotes soil structure via increasing the proportion of soil total aggregates and soil porosity, improving soil structure and therefore is the optimal ecological restoration measure of degraded soil ecosystem in sloping farmland.The soil structure evaluation method based on the minimum data set is applicable in this area of research and can represent the soil structure performance of sloping farmland with CRT measures accurately.

       

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