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Soil N and salinity leaching after the autumn irrigation and its impact on groundwater in Hetao Irrigation District, China

机译:河套灌区秋季灌溉后土壤氮盐分淋失及其对地下水的影响

摘要

Soil water and salinity are crucial factors influencing crop production in arid regions. An autumn irrigation system employing the application of a large volume of water (2200-2600 m(3) ha(-1)) is being developed in the Hetao Irrigation District of China. since the 1980s with the goal to reduce salinity levels in the root zone and increase the water availability for the following spring crops. However, the autumn irrigation can cause significant quantities of NO3- to leach from the plant root zone into the groundwater. In this study. we investigated the changes in soil water content, NO3-N and salinity within a 150 cm deep soil profile in four different types of farmlands: spring wheat (F-W), maize (F-M), spring wheat-maize inter-planting (FW-M) and sunflower (F-S). Our results showed that (1) salt losses mainly occurred in the upper 60 cm of the soil and in the upper 40 cm for NO3-N; (2) the highest losses of salt and NO3-N could be observed in F-W, whereas the lowest losses were found in FW-M. NO3-N concentration, pH and electrical conductivity (EC) in the groundwater were also monitored before and after the autumn irrigation. We found that the autumn irrigation caused the groundwater concentration of NO3-N to increase from 1.73 to 21.6 mg L-1, thereby, exceeding the standards of the World Health Organization (WHO). Our results suggest that extensive development of inter-planting tillage might be a viable measure to reduce groundwater pollution, and that the application of optimized minimum amounts of water and nitrogen to meet realistic yield goals, as well as the timely application of N fertilizers and the use of slow release fertilizers can be viable measures to minimize nitrate leaching. (C) 2004 Elsevier B.V All rights reserved.
机译:土壤水和盐分是影响干旱地区农作物产量的关键因素。中国河套灌区正在开发利用大量水(2200-2600 m(3)ha(-1))的秋季灌溉系统。自1980年代以来,其目标是降低根部地区的盐度水平并增加随后春季作物的水供应。但是,秋季灌溉会导致大量的NO3-从植物根部渗入地下水。在这个研究中。我们调查了四种不同类型的农田中150厘米深土壤剖面中土壤水分,NO3-N和盐分的变化:春小麦(FW),玉米(FM),春小麦-玉米间作种植(FW-M )和向日葵(FS)。我们的结果表明:(1)盐分损失主要发生在土壤的上部60 cm,NO3-N的上部40 cm。 (2)F-W中盐和NO3-N的损失最高,而FW-M中盐和NO3-N的损失最低。在秋季灌溉前后,还监测了地下水中的NO3-N浓度,pH和电导率(EC)。我们发现秋季灌溉导致地下水中NO3-N的浓度从1.73升至21.6 mg L-1,从而超过了世界卫生组织(WHO)的标准。我们的结果表明,广泛种植间作耕作可能是减少地下水污染的可行措施,并且应用最优化的最小量的水和氮以满足实际的产量目标,并及时施用氮肥和氮肥。使用缓释肥料是减少硝酸盐浸出的可行措施。 (C)2004 Elsevier B.V保留所有权利。

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    Feng ZZ; Wang XK; Feng ZW;

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