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首页> 外文期刊>Hydrology and Earth System Sciences >Spatial variability of nitrate concentration in lakes in Snowdonia, North Wales, UK
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Spatial variability of nitrate concentration in lakes in Snowdonia, North Wales, UK

机译:英国北威尔士斯诺登尼亚湖泊中硝酸盐浓度的空间变异性

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摘要

At a regional scale, high nitrate (NO3‾) concentrations in upland surfacewaters generally occur in tandem with high nitrogen (N) deposition levels.However, significant differences in the patterns of surface water NO3‾concentration have been observed within areas of similar N deposition yetrelatively few studies have been undertaken which examine within-regionvariation of NO3‾ concentrations. A study of 76 lakes in Snowdonia, north Wales,an area of high deposition and sensitive catchments, was undertaken to assessvariation in surface water NO3‾ concentration across a 20 x 20 km grid squareand to identify catchments vulnerable to NO3‾ leaching. Nitrate concentrationsvary considerably, particularly during winter when values range from 0.7 to 70 μeq l-1. Although retention by vegetation and soil microbes in summer reducesthe amount of NO3‾ reaching the lakes, 37 % of sites are characterised by NO3‾concentrations greater then 4 μeq l-1. The elevated concentrations occurring insummer suggests that N breakthrough has occurred. By examining the ratio of NO3‾to total strong acid anions, it is shown that NO3‾ contributes significantly tofreshwater acidity, particularly during the winter. Redundancy analysis showsthat NO3‾ leaching is greatest, both in winter and summer, in catchments withhigh proportions of bare rock where soil and vegetation cover is limited.Nitrogen cycling in these catchments, generally at higher altitudes, may nolonger be governed by seasonal biological controls. They are likely to besaturated with respect to nitrogen (i.e. incapable of further N retention)as a result of the elevated deposition levels in the area. The contribution ofNO3‾ to acidity is also greatest at these sites. In winter, significant positiverelationships are also evident between NO3‾ concentration and soil pH andconiferous woodland. The study demonstrates the importance of catchment factorsin modifying the relationship between N deposition and N leaching in uplandcatchments.
机译:在区域范围内,高地表水的硝酸盐(NO 3 )浓度通常与高氮(N)沉积水平同时发生。在相似氮沉积区域内观察到地表水NO 3 的浓度,但是很少进行研究以研究NO 3 浓度。在北威尔士斯诺登尼亚的76个湖泊中进行了一项研究,该湖是一个高沉积和敏感集水区,以评估20 x 20范围内地表水NO 3 的变化。平方公里,并确定易受NO 3 淋洗影响的集水区。硝酸盐浓度变化很大,尤其是在冬季,当浓度范围为0.7至70μeql -1 时。尽管夏季植被和土壤微生物的滞留减少了到达湖泊的NO 3 的数量,但37%的站点具有NO 3 < sup>〜浓度大于4μeql -1 。夏季发生的浓度升高表明已经发生了氮突破。通过检查NO 3 与总强酸阴离子的比例,可以看出NO 3 的贡献显着淡化新鲜水的酸度,尤其是在冬季。冗余分析表明,在冬季和夏季,土壤和植被覆盖受限的裸岩比例高的流域,NO 3 的淋滤作用最大。 ,通常在更高的海拔,可能不再受季节性生物控制。由于该区域中沉积水平的升高,它们可能相对于氮饱和(即无法进一步保留氮)。在这些位置,NO 3 对酸度的贡献也最大。冬季,NO 3 浓度与土壤pH值和针叶林之间也存在明显的正相关关系。该研究证明了集水因子在改变旱地集水区氮沉降与氮淋失之间关系的重要性。

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