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Water and salt distribution in a soil under trickle irrigation

机译:滴灌条件下土壤水盐分布

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摘要

A field study was conducted to determine water and salt distribution patterns in a soil irrigated by pairs of double-chamber, perforated polyethylene tubes. The study consisted of two experiments: a water distribution experiment and a salt distribution experiment. Both experiments were conducted at the same site with experimental plots having two perforated lines 9 m long, spaced 0.60 m. The tubing had outer orifices 0.5 mm in diameter spaced 0.30 m along the tubes. The water distribution experiment consisted of water application to the bare soil for periods of time of 3, 6, 9, and 12 hours. After each test a trench was dug normal to the irrigation tubes and samples were taken to determine soil moisture on a dry weight basis. Moisture profiles are presented for the various tests. The salt distribution experiment was conducted in the Fall of 1973 and repeated in the Spring of 1974. It consisted of four irrigation treatments comprising two irrigation levels and two levels of salt in the irrigation water (327 and 2000 milligrams per liter of salts). Experimental plots were planted with lettuce and soil samples taken after planting and after harvesting the lettuce. Soil samples were analyzed for electrical conductivity of the soil saturation extract, pH, calcium, magnesium, sodium, potassium and nitrates. Saturation extract conductivity profiles in the soil are presented for different treatments. After planting and after harvest concentrations of calcium, magnesium, sodium, potassium, nitrates and pH values are also shown. Seasonal water application and lettuce yields are presented for both trials Water movement in the soil was 2 to 3 times greater in the horizontal than in the vertical direction. Wetted soil volume showed a high positive correlation with both the volume of water applied and with time of application. Salt accumulation occurred mainly at the soil surface between the irrigation tubes and away from the main root zone of the plants. The surface accumulation was followed by a leached zone. There were no significant differences in yield among plots receiving different treatments. Seasonal water application was less than half of the seasonal amount of water normally applied for furrow irrigated lettuce in the Tucson area. It was higher than experimental determinations of seasonal consumptive use for lettuce at Mesa, Arizona. The study indicated that trickle irrigation with water of high salt content is likely to cause a high surface concentration of salts. Application of extra amounts of water by the trickle system, or another method, is recommended to leach the salts to a depth below the crop root zone.
机译:进行了一项现场研究,以确定通过成对的双腔带孔聚乙烯管灌溉的土壤中水和盐的分布模式。该研究包括两个实验:水分配实验和盐分配实验。两次实验均在同一地点进行,实验地块上有两条长9 m,间隔为0.60 m的穿孔线。管道的外孔直径为0.5毫米,沿管道的距离为0.30 m。配水实验包括向裸土上浇水3、6、9和12小时。每次测试后,在灌溉管上垂直挖一条沟渠,并取样以干重为基础确定土壤湿度。给出了各种测试的湿度曲线。盐分分布试验于1973年秋季进行,并于1974年春季重复进行。该试验由四种灌溉处理组成,包括两种灌溉水平和两种水平的灌溉水中盐分(每升盐327和2000毫克)。在试验区种植生菜,并在种植后和收获生菜后采集土壤样品。分析土壤样品的土壤饱和提取物的电导率,pH,钙,镁,钠,钾和硝酸盐。介绍了不同处理条件下土壤中饱和提取物的电导率曲线。还显示了种植后和收获后钙,镁,钠,钾,硝酸盐和pH值的浓度。两项试验均介绍了季节性施水和生菜产量。水平方向上土壤中的水分运动比垂直方向上高2至3倍。湿润的土壤体积与施水量和施药时间均呈高度正相关。盐分的积累主要发生在灌溉管之间的土壤表面,并且远离植物的主根区。表面积累之后是浸出区。在接受不同处理的地块之间,产量没有显着差异。季节性用水量少于图森地区犁沟灌溉生菜的季节性用水量的一半。它高于亚利桑那州梅萨市季节性食用生菜的实验确定值。研究表明,用高盐含量的水进行滴灌可能会导致盐的高表面浓度。建议通过滴流系统或其他方法施加额外的水,以将盐滤出至作物根部区域以下的深度。

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