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Factors controlling the distribution and fate of nitrate in the unsaturated zone and groundwater in a semiarid agriculture area

机译:在半干旱农业区控制不饱和区与地下水中硝酸盐分布和命运的因素

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Overuse of fertilizers in agriculture could cause groundwater nitrate pollution. However, this is related to nitrate input, soil moisture movement (direction and rate), and depth of water table in (semi)arid areas, where nitrate can be preserved and nitrate loss by denitrification can be limited. A 18-m soil profile to water table in Daxing, Beijing shows that the nitrate is accumulated in the upper unsaturated zone and has not reached water table; and then groundwater nitrate remains at baseline level (5.6 mg/L). The soil moisture movement velocity is 0.28 m/yr based on nitrate use history. It takes another ~35 years for the moisture with high nitrate content to reach water table and pollute groundwater, to which attention should be paid in water quality management.
机译:过度使用农业肥料可能导致地下水硝酸盐污染。然而,这与硝酸盐输入,土壤湿度运动(方向和速率)和(半)干旱区域的深度有关,其中硝酸盐可以保存,并且通过反硝化的硝酸盐损失可以限制。北京在大兴水表中的18米土壤曲线表明硝酸盐积聚在上不饱和区,并没有到达水位;然后地下水硝酸盐仍处于基线水平(5.6mg / L)。基于硝酸盐使用历史,土壤水分运动速度为0.28米/毫秒。用高硝酸盐含量的水分达到水位和污染地下水需要另外〜35年,注意应在水质管理中支付。

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