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Influence of slope steepness on ground coverage of natural grasses and soil moisture in the Loess plateau

机译:黄土高原坡面陡度对天然草木地面覆盖及土壤水分的影响

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Restoration of natural vegetation on steep slope in the gullied-hilly area of Loess Plateau is important for soil erosion control. The objective of this study was to find out the relationship between vegetation coverage /aboveground biomass and slope steepness, and the possible relations among vegetation, topographic characteristics and soil moisture. Vegetation and soil water were sampled on sites with different slope steepness ranging from 5-45° along two topographic transects. Each transect composed of two opposite slope aspects (east-west and south-north). Aboveground biomass was obtained by harvesting the current year live and dead plants and oven dried. Soil moisture was measured on moderate (10-15°), steep (20-25°) and steepest (43-45°) sites of each aspect to a depth of 3 m. Vegetation coverage and aboveground biomass were linearly related to slope steepness on east (p<0.0001), south (p<0.001) and west (p<0.0001) slopes. The slope steepness alone could explain more than 90% of ground coverage variations on the east, south and west slopes. On northern facing slope, the coverage and aboveground biomass were decreased slower than those on other aspects with increasing slope steepness. The soil moisture at the sites of northern facing slope was greater than those of other aspects. soil moistures on certain soil profiles at relatively moderate areas with higher aboveground biomass were lower than those on steeper areas with smaller aboveground biomass. This trade off relationship between above ground biomass and soil moisture may maintained the soil water balance both at moderate and steepest sites on all aspects and made the ecosystem sustainable in the water stressed typical steppe area under natural conditions.
机译:黄土高原丘陵沟壑区陡坡自然植被的恢复对土壤侵蚀的控制具有重要意义。本研究的目的是找出植被覆盖度/地上生物量与坡度之间的关系,以及植被,地形特征与土壤水分之间的可能关系。在两个坡度为5-45°的坡度不同的地点对植被和土壤水进行采样。每个断面由两个相对的坡度面组成(东西向和南北向)。地上生物量是通过收获当年的生,死植物并烘干而获得的。在每个方面的中度(10-15°),陡峭(20-25°)和最陡峭(43-45°)站点上测量土壤湿度,深度为3 m。植被覆盖度和地上生物量与东坡(p <0.0001),南坡(p <0.001)和西坡(p <0.0001)的坡度线性相关。仅斜坡陡度就可以解释东,南和西斜坡超过90%的地面覆盖变化。在北坡上,随着坡度的增加,覆盖率和地上生物量的下降速度要慢于其他方面。朝北坡位的土壤水分高于其他方面。地上生物量较高的相对温和地区某些土壤剖面的土壤水分低于地上生物量较小的较陡峭地区的土壤水分。地上生物量与土壤水分之间的这种折衷关系可以在各个方面保持适度和最陡峭位置的土壤水平衡,并在自然条件下在缺水的典型草原地区使生态系统可持续。

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