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Post-drought increase in regional-scale groundwater nitrate in southwest Germany

机译:德国西南地区地区地下水硝酸盐后期干旱后增幅

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摘要

Elevated nitrate concentrations in groundwater are a common challenge for water management. One important factor in this context is higher frequencies and intensities of wet-dry cycles that may cause increased nitrate concentrations in groundwater due to nitrate flushes after drought termination. Yet systematic studies on regional-scale impacts of droughts on groundwater nitrate concentrations are missing so far. Here we analyzed time series of 44 shallow groundwater wells and 41 springs all across the German Federal State Baden-Wuerttemberg from 2000 to 2018 to characterize patterns of post-drought nitrate increase in groundwater. In general, half of the exceptional nitrate concentrations, which exceeded the 80th percentile of long-term nitrate measurements, could be related to droughts in the research timeframe. The 2003 drought event stood out in terms of drought severity and post-drought nitrate concentration increases in our data. The great majority (91%) of all monitoring sites showed at least one exceptionally high nitrate concentration in the 4 years following the 2003 drought event. Springs were mainly located in forests of steep low mountain ranges and wells in cropland of flat river valleys. Therefore, delay times between drought intensity and nitrate concentration increases as well as magnitudes of nitrate concentration increase were diverse among wells and springs. We derived two distinct nitrate response patterns: (i) nitrate increases immediately following drought events (more common for springs and fractured rock aquifers) and (ii) delayed nitrate increases (more common for wells and porous aquifers). Springs generally showed quicker (median of 101 days) but weaker (median of +1.3 mg/L) post-drought nitrate increases than wells (185 days, +3.4 mg/L). Only few sites exhibited no post-drought nitrate increase and post-drought mean-nitrate concentrations of groundwater reservoirs were extraordinarily high in 2006. Overall, we demonstrate that post-drought nitrate increase in groundwater is omnipresent, while different landscapes and hydrogeological characteristics create a diverse regional pattern. As severe droughts become more frequent in a changing climate, post-drought nitrate increase may intensify problems regarding water quality and supply.
机译:地下水中硝酸盐浓度升高是水管理的常见挑战。这种情况下的一个重要因素是湿干循环的频率较高,湿干循环的强度可能导致在干旱终止后由于硝酸盐冲洗而导致地下水中的硝酸盐浓度增加。目前缺少对干旱对地下水硝酸盐浓度的区域规模影响的系统研究。在这里,我们分析了44个浅地下水井的时间序列,遍布德国联邦国家巴登 - Wuerttemberg的41个春季,从2000年到2018年,以对地下水的干旱后硝酸盐升高的形式。通常,出色的硝酸盐浓度的一半超过了长期硝酸盐测量的第80百分位数,可能与研究时间框架中的干旱有关。 2003年的干旱活动在干旱严重程度方面突出,硝酸后硝酸盐浓度随着我们的数据而增加。在2003年干旱事件后4年内,所有监测网站的大多数(91%)在2003年干旱事件后的4年内显示出至少一个特别高的硝酸盐浓度。 Springs主要位于陡峭的低山脉森林和河流河山谷的河流。因此,在井和弹簧之间,干旱强度和硝酸盐浓度之间的延迟时间以及硝酸盐浓度增加的幅度增加。我们衍生出两种不同的硝酸盐反应模式:(i)硝酸盐在干旱事件(弹簧和裂缝岩含水层更常见)后立即增加,(ii)延迟硝酸盐增加(对孔和多孔含水层更常见)。 Springs通常呈现更快(101天的中位数),但干旱后硝酸盐的干旱后较弱(中位数+ 3毫克/升)增加(185天,+ 3.4 mg / L)。只有少数遗址均未出现干旱后硝酸盐的增加和干旱后的地下水储层的地下水储层的浓度非常高。总体而言,我们证明了地下水的干旱后硝酸盐增加是无所不在的,而不同的景观和水文地质特征是创造的不同的区域模式。由于严重干旱在变化的气候中变得更频繁,后期硝酸盐的增加可能会加剧有关水质和供应的问题。

著录项

  • 来源
    《Hydrological Processes》 |2021年第8期|e14307.1-e14307.11|共11页
  • 作者单位

    Univ Freiburg Fac Environm & Nat Resources Hydrol D-79098 Freiburg Germany|Univ Freiburg Fac Environm & Nat Resources Environm Hydrol Syst Freiburg Germany;

    Univ Freiburg Fac Environm & Nat Resources Environm Hydrol Syst Freiburg Germany;

    Univ Freiburg Fac Environm & Nat Resources Environm Hydrol Syst Freiburg Germany;

    Univ Freiburg Fac Environm & Nat Resources Hydrol D-79098 Freiburg Germany;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Baden-Wuerttemberg; drought; Germany; groundwater; nitrate; nitrate concentration;

    机译:Baden-Wuerttemberg;干旱;德国;地下水;硝酸盐;硝酸盐浓度;

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