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Factors contributing to nitrate contamination in a groundwater recharge area of the North China Plain

机译:华北平原地下水补给区硝酸盐污染的影响因素

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摘要

Nitrate contamination is a common problem in groundwater of the North China Plain (NCP) owing to overuse of fertilizers and discharge of wastewater. Accordingly, it is important to investigate nitrate contamination in recharge areas to understand the fate of nitrate in the plains area. In this study, the spatial and temporal distribution characteristics of nitrate and factors contributing to its sources and transformation in shallow groundwater of the Beiyishui River watershed, NCP, were analysed by a combination of multiple regression and multi-tracer methods. The nitrate concentration of 79% of the samples exceeded the natural environmental standard of 13.3mgl(-1), while that of 23% of the samples exceeded the World Health Organization (WHO) drinking water standard of 50mgl(-1). Groundwater age estimation of the hill regions based on chlorofluorocarbons (CFCs) revealed a mix of young water from 1982 to 1990 and old, low CFC water. The analysis based on the variations in land use in past years revealed that part of the grassland was converted into woodland between 1980 and 1995; therefore, the land use at the recharge time was used to determine which surface conditions influence groundwater nitrate concentrations. Multiple regression analysis showed that point source pollution contributed to the high concentration of nitrate in the hill region. Fertilizer application associated with land use change from grassland to woodland was also related to the present nitrate concentration. In the plains area, the contribution of fresh water from fault fractures and denitrification led to 31 to 72% and 6 to 51% reductions in nitrate concentrations, respectively. Our results suggested that controlling point source contamination and fertilizer input to hilly regions of the study will prevent groundwater of the plains area from deterioration in future years by mixing fresh water into the aquifers and decreasing denitrification, and therefore nitrate concentrations. Copyright (c) 2015 John Wiley & Sons, Ltd.
机译:由于肥料的过量使用和废水的排放,硝酸盐污染是华北平原(NCP)地下水中的常见问题。因此,重要的是要调查补给区的硝酸盐污染,以了解平原区硝酸盐的命运。本研究采用多元回归和多示踪法相结合的方法,对北依水河流域浅层地下水中硝酸盐的时空分布特征及其来源和转化的影响因素进行了分析。 79%的样本中的硝酸盐浓度超过了13.3mgl(-1)的自然环境标准,而23%的样本中的硝酸盐浓度超过了50mgl(-1)的世界卫生组织(WHO)饮用水标准。根据氯氟烃(CFC)对丘陵地区的地下水年龄进行估算,发现1982年至1990年的年轻水和低碳的老水混合在一起。根据过去几年土地用途的变化进行的分析表明,在1980年至1995年之间,部分草地被转变为林地;因此,补给时间的土地利用被用来确定哪些表面条件影响地下水硝酸盐浓度。多元回归分析表明,点源污染造成了丘陵地区硝酸盐的高浓度。与从草地到林地的土地用途变化相关的肥料施用也与目前的硝酸盐浓度有关。在平原地区,断层裂缝和反硝化作用带来的淡水贡献分别使硝酸盐浓度降低了31%至72%和6%至51%。我们的结果表明,通过将淡水混入含水层并减少反硝化作用,从而减少硝酸盐的浓度,控制点源污染和向丘陵地区输入肥料的方法将防止平原地区地下水在未来几年内恶化。版权所有(c)2015 John Wiley&Sons,Ltd.

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