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Mobility of major ions and nutrients in the unsaturated zone during paddy cultivation: a field study and solute transport modelling approach

机译:水稻种植过程中非饱和区主要离子和养分的迁移:田间研究和溶质运移建模方法

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Study of the movement of water and solute within soil profiles is important for a number of reasons. Accumulation of prominent contaminants from agricultural chemicals in the unsaturated zone over the years is a major concern in many parts of the world. As a result, the unsaturated zone has been a subject of great research interest during the past decade. Hence, an intensive field study was conducted in a part of Palar and Cheyyar river basins to understand the variation of major ions and nutrients in the soil zone during paddy cultivation. The chloride and nitrate data were used to model the movement of these chemicals in the unsaturated zone using the HYDRUS-2D model. The field study shows that fertilizer application and irrigation return flow increases the major ions and nutrients concentration in the unsaturated zone. Further, the nutrient concentrations are regulated by plant uptake, fertilizer application and infiltration rate. Additionally, denitrification and soil mineralization processes also regulate the nitrogen concentration in the unsaturated zone. The solute transport modelling study concluded that the simulated results match reasonably with the observed trends. Simulated concentrations of chloride and nitrate for a 5-year period indicate that the concentrations of these ions fluctuate in a cyclic manner (from 60 to 68 mg l~(-1) and from 3·4 to 3·5 mg l~(-1) respectively in groundwater) with no upward and downward trend. The influence of excessive fertilizer application on groundwater was also modelled. The model predicts an increase of about 17 mg l~(-1) of chloride and 2·3 mg l~(-1) of nitrogen in the groundwater of this area when the application of fertilizers is doubled. The model indicates that the present level of use of agrochemicals is no threat to the groundwater quality.
机译:由于多种原因,研究水和溶质在土壤剖面中的运动很重要。多年来,来自不饱和地区农用化学品的主要污染物的积累是世界许多地方的主要关注点。结果,在过去的十年中,非饱和带一直是研究热点。因此,在帕拉尔河和奇亚尔河流域的一部分进行了深入的田间研究,以了解水稻种植过程中土壤区域主要离子和养分的变化。使用HYDRUS-2D模型,使用氯化物和硝酸盐数据来模拟这些化学物质在不饱和区的运动。田间研究表明,施肥和灌溉回流增加了非饱和区的主要离子和养分含量。此外,养分浓度受植物吸收,肥料施用和渗透率的调节。另外,反硝化和土壤矿化过程也调节不饱和区的氮浓度。溶质运移模型研究得出结论,模拟结果与观察到的趋势合理匹配。模拟5年的氯化物和硝酸盐浓度表明,这些离子的浓度呈周期性波动(从60到68 mg l〜(-1)和从3·4到3·5 mg l〜(- 1)分别在地下水中)没有上升和下降的趋势。还模拟了过量施肥对地下水的影响。该模型预测,当肥料用量增加一倍时,该地区地下水中的氯化物增加约17 mg l〜(-1)和2·3 mg l〜(-1)。该模型表明,目前使用农药的水平对地下水质量没有威胁。

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