首页> 外文会议>International Conference on Irrigation and Drainage >EFFECT OF LEACHING IRRIGATION ON THE SPATIAL DISTRIBUTION OF SOIL SALINITY IN THE HETAO IRRIGATION DISTRICT IN CHINA
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EFFECT OF LEACHING IRRIGATION ON THE SPATIAL DISTRIBUTION OF SOIL SALINITY IN THE HETAO IRRIGATION DISTRICT IN CHINA

机译:浸出灌溉对我国季度灌溉区土壤盐度空间分布的影响

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To evaluate the effect of leaching irrigation on the spatial distribution of soil salinity, an electromagnetic induction method (EIM) was used to track the salt dynamics of poorly drained fields during leaching irrigation in the Hetao irrigation district. In a 0.3-ha study area, we observed soil salinity and micro-topography at over 700 points, and the groundwater level and salinity at 17 points, between 2002 and 2003. Spatial analysis was used to determine the inter-relationships of soil salinity, irrigation water path, and groundwater. After leaching irrigation, soil salinity in the root zone was reduced temporarily. During the observation period, the distribution of soil salinity did not change greatly. Lateral flow of groundwater was quite slow and there was little difference in groundwater salinity before and after irrigation. There was a good correlation between groundwater salinity and soil salinity.
机译:为了评估浸出灌溉对土壤盐度空间分布的影响,使用电磁诱导方法(EIM)来追踪Hetao灌溉区浸出灌溉过程中沥干田地的盐动力学。 在0.3公顷的研究区域,我们观察到超过700点的土壤盐度和微型,以及2002年至2003年间的17分的地下水位和盐度。空间分析用于确定土壤盐度的间相互关系, 灌溉水路和地下水。 浸出灌溉后,根区的土壤盐度暂时减少。 在观察期间,土壤盐度的分布并没有大大变化。 地下水的横向流量非常缓慢,灌溉前后的地下水盐度几乎没有差异。 地下水盐度与土壤盐度之间存在良好的相关性。

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