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LOSS OF NITRATE-NITROGEN BY RUNOFF AND LEACHING FOR AGRICULTURAL WATERSHEDS

机译:农村流域径流和淋溶造成硝酸盐氮的流失

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摘要

The loss of nutrients in runoff and leaching water from agricultural land is a major cause of poor water quality in the United States. Scientists (NRCS) developed a technique to estimate the impact of agricultural watersheds on natural water resources. The objectives were to apply the technique on Wagon Train (WT) watershed in Nebraska to predict: (i) loss of water by surface runoff and subsurface leaching, (ii) loss of nitrate-N from soils by runoff and leaching, and (iii) nitrate-N loading for WT reservoir. The annual loss of water was estimated at 4.32 million m3 for runoff and 0.98 million m3 for leaching. The observed annual inflow for WT reservoir was 4.25 million m3 . The predicted annual nitrate-N loss by runoff was about 7.0 Mg and could be considered the annual loading for the reservoir. The predicted nitrate-N loss by leaching was 7.73 Mg, however, the fate was not clear. The estimated average nitrate-N concentration in runoff and leaching water at field sites was 1.63 and 7.88 mg/L, respectively. The observed nitrate-N concentration in water samples taken from 12 major streams ranged between 0.37 and 1.56 mg/L with an average of 0.90 mg/L. Nitrogen uptake by algae, -weeds, and aquatic plants and emission of gaseous nitrogen oxides from fresh water under reducing conditions might explain the lower nitrate-N concentration. No attempt was made to monitor the nitrate-N concentration in soil leachate or groundwater. When factors affecting N concentration in streams are considered, the technique could provide a reasonable estimation of N concentration in stream water. We concluded that the technique could be applied to estimate the loss of nitrate-N by runoff and leaching from soils and the impact on surface waters.
机译:在美国,径流和淋溶水的营养成分流失是美国水质差的主要原因。科学家(NRCS)开发了一种技术来估算农业流域对自然水资源的影响。目的是将该技术应用在内布拉斯加州的Wagon Train(WT)分水岭上,以预测:(i)地表径流和地下淋溶损失的水,(ii)径流和淋滤从土壤中硝态氮的损失,以及(iii) )WT油藏的硝态氮负荷。估计每年的径流水损失为432万立方米,淋滤的水损失为98万立方米。观察到的WT水库年流入量为425万立方米。预测的径流造成的硝酸盐-氮年损失约为7.0 Mg,可以认为是储层的年负荷。通过浸出预测的硝酸盐氮损失为7.73 Mg,但是命运还不清楚。田间径流和浸出水中硝酸盐氮的估计平均浓度分别为1.63和7.88 mg / L。在12条主要水流中,水样中观察到的硝酸盐氮浓度在0.37至1.56 mg / L之间,平均为0.90 mg / L。藻类,杂草和水生植物吸收氮以及还原条件下淡水排放的气态氮氧化物可能解释了较低的硝态氮浓度。没有尝试监测土壤渗滤液或地下水中硝酸盐-N的浓度。当考虑影响溪流中氮浓度的因素时,该技术可以提供合理的估算溪流中氮浓度的方法。我们得出的结论是,该技术可用于估算土壤中径流和浸出以及对地表水的影响所导致的硝酸盐氮损失。

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