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Risk of water contamination by nitrogen in Canada as estimated by the IROWC-N model

机译:根据IROWC-N模型估算的加拿大水被氮污染的风险

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With increasing amounts of nitrogen (N) being added to farmland in the form of fertilizer and manure to optimize crop yields, and more broadly, to meet the growing demands for food, feed and energy, there are public concerns regarding its possible negative impact on the environment. An optimal balance between N requirements for production versus efficient N use is required, so as to minimize N losses from the agricultural system. An agri-environmental indicator i.e., the Indicator of the Risk of Water Contamination by Nitrogen (IROWC-N) was developed to assess the risk of N moving from agricultural areas into ground water and/or nearby surface water bodies. The indicator linked the quantity of mineral nitrogen remaining in the soil at harvest, i.e., the Residual Soil Nitrogen (RSN) indicator, and the subsequent climatic conditions during the winter period. The results were assessed in terms of nitrate lost through leaching and nitrate concentration in the drainage water, expressed in five IROWC-N risk classes. Unlike previous versions of the indicator, the current model provided a more complete description of the soil-water balance, including the calculation of rainfall interception by crops, surface runoff, actual evapotranspiration and soil-water contents. Consequently, the current IROWC-N estimates differed markedly from those obtained previously.rnBetween 1981 and 2006, the risk of water contamination by N in Canada was small, and reflected what was happening in the three Prairie provinces where 85% of Canada's farmland is located. However, the aggregated IR0WC-N index, which is a combination of all five risk classes, increased steadily by 2.3% per year, from 6.7 in 1981 to 10.6 in 2006. The proportion of farmland in the very low IROWC-N risk class decreased from 88 to 78%; correspondingly, the proportion in the low risk class increased from 2 to 12%. The proportion of farmland in the moderate-, high- and very high-risk classes changed by less than 3% over time. The trends in IROWC-N in the Atlantic provinces were significantly worse than the national trend; for example, in Atlantic Canada, the aggregated IROWC-N index tripled from 27.8 in 1981 to 87.5 in 2006. Increases in fertilizer use (except in British Columbia), increases in livestock numbers in Manitoba and the Atlantic provinces, and an increase in legume crop acreage were the main factors that contributed to the increase in IROWC-N estimates. Climatic factors were also involved, as droughts reduced yields, N uptake and N leaching in many regions of Canada in 2001.
机译:随着氮肥以肥料和肥料的形式添加到农田中以优化农作物的产量,更广泛地说,是为了满足对食物,饲料和能源不断增长的需求,公众担心氮素对农业的负面影响环境。生产中的氮需求量与有效氮的使用量之间需要达到最佳平衡,以最大程度地减少农业系统中的氮损失。开发了一种农业环境指标,即氮污染水的风险指标(IROWC-N),以评估氮从农业区转移到地下水和/或附近地表水体中的风险。该指标将收获时土壤中残留的矿质氮量(即土壤残留氮(RSN)指标)与冬季随后的气候条件联系起来。根据浸出损失的硝酸盐和排水中硝酸盐的浓度对结果进行了评估,以五种IROWC-N风险等级表示。与该指标的先前版本不同,当前模型对土壤水平衡提供了更完整的描述,包括计算农作物截留的降雨,地表径流,实际蒸散量和土壤水含量。因此,目前的IROWC-N估算值与之前的估算值有显着差异。rn在1981年至2006年之间,加拿大的N污染水的风险很小,这反映了加拿大85%的农田所在地的三个草原省的情况。但是,综合了所有五个风险类别的IR0WC-N指数每年稳定增长2.3%,从1981年的6.7增加到2006年的10.6。在极低的IROWC-N风险类别中,耕地所占比例下降从88%降至78%;相应地,低风险类别中的比例从2%增加到12%。随着时间的推移,中,高和极高风险类别中耕地的比例变化不到3%。大西洋省份的IROWC-N趋势明显低于全国趋势;例如,在加拿大大西洋省,IROWC-N的综合指数从1981年的27.8增至2006年的87.5,增长了两倍。作物种植面积是导致IROWC-N估算值增加的主要因素。气候因素也涉及其中,因为2001年加拿大许多地区的干旱降低了单产,氮素吸收和氮素淋失。

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