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Application of the SWAP model for sustainable agriculture in an arid region

机译:SWAP模型在干旱地区可持续农业中的应用

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Iran is located in an arid and semi-arid region of the world with average annual precipitation of about 250 mm. Due to lack of suitable water resources, many farmers are using saline river or groundwater for irrigation which causes gradual accumulation of salts in the soil. Salinity of soil and water resources is one of the major environmental factors limiting the productivity of agricultural lands and reduces land area under cultivation. For sustainable agricultural productions, appropriate irrigation management practices should be applied if the saline irrigation water is to be used for irrigation. The SWAP (soil-water-atmosphere-plant) model is a physical-based model that can be used to simulate crop yield and soil salinity, among others. To collect field data to apply to this model as input and calibrate it, a field experiment planted with wheat was conducted on a silty clay loam soil, in the central part of Iran (the Rudasht region near Isfahan with an annual average precipitation of about 80 mm), with three irrigation water salinity levels of 2, 8 and 12 dS/m with/without leaching levels of 4, 19 and 32 percent with two different irrigation water managements, using factorial design with four replications. The results showed that the model is applicable in this arid region and has low sensitivity to input data of root distribution depth and irrigation water salinity and medium sensitivity to climate data, soil surface layer hydraulic characteristics, leaf area index and amount of irrigation. The model simulated wheat yield and the calibration coefficients were obtained. The results showed that the model could be used as an effective tool for sustainable agricultural production.
机译:伊朗位于世界干旱半干旱地区,年平均降水量约为250毫米。由于缺乏合适的水资源,许多农民正在使用盐水河或​​地下水进行灌溉,这导致土壤中盐分的逐步积累。土壤和水资源盐碱化是限制农业用地生产力并减少耕地面积的主要环境因素之一。对于可持续的农业生产,如果要将盐水灌溉用水用于灌溉,则应采用适当的灌溉管理措施。 SWAP(土壤-水-大气-植物)模型是一种基于物理的模型,可以用于模拟作物产量和土壤盐分等。为了收集可用于该模型的现场数据作为输入并对其进行校准,在伊朗中部(伊斯法罕附近的Rudasht地区,年均降水量约为80)的粉质粘土壤土上进行了小麦种植试验。 (mm),采用两种重复灌溉的析因设计,三种灌溉水的盐度分别为2、8和12 dS / m,有/无浸出水平分别为4、19和32%。结果表明,该模型适用于该干旱地区,对根系分布深度和灌溉水盐分输入数据的敏感性较低,对气候数据,土壤表层水力特征,叶面积指数和灌溉量的敏感性中等。该模型模拟了小麦的产量并获得了校正系数。结果表明,该模型可以作为可持续农业生产的有效工具。

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