首页> 外文会议>International Soil Conservation Organization Conference vol.2; 20020526-31; Beijing(CN) >Soil Characteristics and Its Dynamic Variation in a Small Catchment on the Loess Plateau of China
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Soil Characteristics and Its Dynamic Variation in a Small Catchment on the Loess Plateau of China

机译:黄土高原小流域土壤特征及其动态变化

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In this paper, taking Zhifanggou small catchment, which have been integrated controlled for more than 20 years in the typical hilly-gullied Loess Plateau, as research region, selecting 20 plots of different landuse types in the whole catchment in 1999, soil anti-scourability, stable infiltration rate, soil aggregate stability, saturated soil cohesion and soil organic matter content in these plots were measured. The experiment results showed that there had significant difference of these soil characteristics in different landuse types. Shrubland had the largest mean weight diameter (MWD) of soil aggregate stability and the strongest soil anti-scourability. The anti-scourability of shrub land and natural grassland was about 70-90 times of cropland. The content of O.M in cropland and planted grassland was about 1/2-1/3 of other landuse types. The value of stable soil infiltration rate and saturated soil cohesion was the highest in natural grassland. As a whole, the measuring values of these soil characteristics in woodland with acacia, shrubland with Caragana and natural grassland were much more higher than that in planted grassland and cropland. The variation of these characteristics in soil profile (0cm-50cm) was also significant. Generally speaking, the value of soil anti-scourability, stable infiltration rate, soil aggregate stability and soil organic matter content were all decreased clearly from upper to lower position in soil profile. The decreasing extent was reduced with the soil layer becoming deeper. According to the area of different landuse types in the catchment and its change in history, by spatial and temporal up scaling, the dynamics of these soil characteristics in the catchment after years' control measurement was analyzed. All these results provided valuable basic data for soil erosion modeling and laid foundation for qualitative assessing the soil quality and ecosystem health situation in the catchment with long term controlled measurement.
机译:本文以典型的黄土高原丘陵沟壑区综合治理已有20多年的纸坊沟小流域为研究区域,1999年选择了整个流域20种不同土地利用类型的样地,土壤抗冲刷能力强。在这些样地中测量了稳定的渗透率,土壤团聚体的稳定性,饱和土壤的黏附力和土壤有机质含量。试验结果表明,不同土地利用类型的土壤特性差异显着。灌木丛具有最大的土壤团聚体平均重量直径(MWD)和最强的土壤抗冲刷性。灌木地和天然草地的抗冲刷性约为农田的70-90倍。农田和人工草地的土壤有机质含量约为其他土地利用类型的1 / 2-1 / 3。天然草地中稳定的土壤入渗率和饱和土壤黏附力的值最高。总体而言,相思林地,柠条林地灌木丛和天然草地中这些土壤特性的测量值远高于人工草地和农田。这些特征在土壤剖面(0cm-50cm)中的变化也很显着。一般来说,土壤抗冲刷性,稳定入渗速率,土壤团聚体稳定性和土壤有机质含量的值在土壤剖面中从上到下均明显降低。随着土壤层的加深,减少的程度减小。根据流域内不同土地利用类型的面积及其历史变化,通过空间和时间的按比例放大,分析了多年控制测量后流域内这些土壤特征的动态。这些结果为水土流失建模提供了有价值的基础数据,为定性评估流域土壤质量和生态系统健康状况提供了基础。

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