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Spatio-temporal dynamics of soil moisture in silvopastoral system in the Loess Plateau of west Shanxi province

机译:西山西省黄土高原土壤水分的时空动力学

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The objective of this study was to investigate the spatio-temporal dynamics of soil moisture in silvopastoral system in the Loess Plateau of west Shanxi Province. Soil moisture in 0-100 cm layer was measured and analyzed in locust-natural grass system. The results showed as following: (1) There were significant differences of soil moisture in 0-100cm layer in different phenological phases. Soil moisture contents in different patch types were different in silvopastoral system. The soil moisture contents of the grassland were significantly greater than the forestland's. (2) There were obvious hierarchy characteristics in soil profile in locust-natural grass system. The soil moisture contents and coefficient of variation both decreased with increase of soil depth. In horizontal direction, variations of soil moisture were relatively obvious in grassland, and soil moisture increased with the increase of the distance from forest edge to grassland. In forestland, variations of soil moisture were relatively complicated and soil moisture decreased with the increase of distance. Two-dimension isogram map gave a very strong visual impression, and it obtained good results in expressing the spatial structural characters.
机译:本研究的目的是调查西山黄土高原硅质体系中土壤水分的时空动态。测量和分析在0-100cm层中的土壤水分在蝗虫 - 天然草系中分析。结果表明如下:(1)不同鉴别阶段0-100cm层中的土壤水分差异显着差异。不同斑块类型的土壤水分含量在硅晶体系统中不同。草原的土壤水分含量明显大于林地。 (2)蝗虫 - 天然草系土壤剖面中存在明显的层次特征。土壤水分含量和变异系数随着土壤深度的增加而降低。在水平方向上,草地的土壤水分的变化相对明显,土壤水分随着距离森林边缘到草地的距离而增加。在林地,土壤水分的变化相对复杂,土壤水分随着距离的增加而降低。两维表法地图给出了非常强烈的视觉印象,它获得了表达空间结构特征的良好结果。

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