首页> 外文会议>19th International Conference on Irrigation and Drainage; 2005; Beijing(CN) >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:淋灌对中国河套灌区土壤盐分空间分布的影响

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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 Hetac 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. Aftei 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. The distribution of soil salinity was largely affected by the micro-topography of the field. As there was very little lateral movement of groundwater in this field, leaching irrigation enhanced only the vertical movement of salt in the root zone and did not reduce the heterogeneous salinity distribution in groundwater, which remained a potential salinity hazard. The heterogeneous distribution of groundwater salinity was attributed to the uneven distribution of irrigation water owing to poor land leveling. The results suggest that leaching irrigation is not efficient foreliminating soil salinity problems in poorly drained areas. The heterogeneous distribution of soil salinity may be reduced if land is leveled more carefully. Nevertheless, the main constraint remains the lack of drainage in such areas. There is an urgent need to classify the entire Hetao irrigation district according to how well areas are drained and to determine the fundamental movement of groundwater and salinity on a large scale.
机译:为了评价淋灌对土壤盐分空间分布的影响,采用电磁感应法(EIM)跟踪Hetac灌区淋灌期间排水不畅的田间盐分动态。在一个0.3公顷的研究区域中,我们观察到2002年至2003年之间的土壤盐分和微观地形超过700个点,以及地下水位和盐分在17个点。使用空间分析来确定土壤盐分的相互关系,灌溉水路径和地下水。 Aftei淋灌,根区土壤盐分暂时降低。在观测期内,土壤盐分分布没有很大变化。地下水的横向流动非常缓慢,灌溉前后的地下水盐度差异不大。地下水盐度与土壤盐度之间具有良好的相关性。土壤盐分的分布在很大程度上受田间微地形的影响。由于该田地中地下水的横向运动非常少,淋滤灌溉仅增强了根部区域盐分的垂直运动,而没有降低地下水中的非均匀盐分分布,这仍然是潜在的盐分危害。地下水盐度的非均质分布是由于土地平整度差导致灌溉水分布不均。结果表明,淋洗灌溉不能有效地消除流失较弱地区的土壤盐分问题。如果更仔细地平整土地,则可以降低土壤盐分的异质分布。然而,主要制约因素仍然是这些地区缺乏排水。迫切需要根据排水区域的好坏对整个河套灌区进行分类,并大规模确定地下水和盐分的基本运动。

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