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首页> 外文期刊>Hydrological Processes >Chronic and episodic acidification of streams along the Appalachian Trail corridor, eastern United States
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Chronic and episodic acidification of streams along the Appalachian Trail corridor, eastern United States

机译:美国东部阿巴拉契亚小径走廊沿线河流的慢性和间歇性酸化

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摘要

Acidic atmospheric deposition has adversely affected aquatic ecosystems globally. As emissions and deposition of sulfur (S) and nitrogen (N) have declined in recent decades across North America and Europe, ecosystem recovery is evident in many surface waters. However, persistent chronic and episodic acidification remain important concerns in vulnerable regions. We evaluated acidification in 269 headwater streams during 2010-2012 along the Appalachian Trail (AT) that transits several ecoregions and is located downwind of high levels of S and N emission sources. Discharge was estimated by matching sampled streams to those of a nearby gaged stream and assuming equivalent daily mean flow percentiles. Charge balance acid-neutralizing capacity (ANC) values were adjusted to the 15th (Q15) and 85th flow percentiles (Q85) by applying the ANC/discharge slope among sample pairs collected at each stream. A site-based approach was applied to streams sampled twice or more and a second regression-based approach to streams sampled once to estimate episodic acidification magnitudes as the ANC difference from Q15 to Q85. Streams with ANC <0 mu eq/L doubled from 16% to 32% as discharge increased from Q15 to Q85 according to the site-based approach. The proportion of streams with ANC <0 mu eq/L at low flow and high flow decreased from north to south. Base cation dilution explained the greatest amount of episodic acidification among streams and variation in sulfate (SO42-) concentrations was a secondary explanatory variable. Episodic SO42- patterns varied geographically with dilution dominant in northern streams underlain by soils developed in glacial sediment and increased concentrations dominant in southern streams with older, highly weathered soils. Episodic acidification increased as low-flow ANC increased, exceeding 90 mu eq/L in 25% of streams. Episodic increases in ANC were the dominant pattern in streams with low-flow ANC values <30 mu eq/L. Chronic and episodic acidification remain an ecological concern among AT streams. The approach developed here could be applied to estimate the magnitude and extent of chronic and episodic acidification in other regions recovering from decreasing levels of atmospheric S and N deposition.
机译:酸性大气沉积对全球的水生生态系统产生了不利影响。由于近几十年来北美和欧洲的硫(S)和氮(N)的排放和沉积下降,许多地表水域的生态系统恢复显而易见。但是,持续的慢性和偶发性酸化仍然是脆弱地区的重要关切。我们评估了2010-2012年沿穿越多个生态区域且位于高硫和氮排放源顺风的阿巴拉契亚小径(AT)269条上游水源中的酸化程度。通过将采样流与附近量具流的采样流匹配并假设等效的每日平均流量百分位数来估算流量。通过在每个流中收集的样品对之间应用ANC /放电斜率,将电荷平衡酸中和能力(ANC)值调整为第15个(Q15)和第85个流动百分位数(Q85)。将基于站点的方法应用于两次或更多次采样的流,并将基于回归的第二种方法应用于一次采样的流,以估计从Q15到Q85的ANC差异的情景酸化幅度。根据基于站点的方法,随着排放量从Q15增加到Q85,ANC <0μeq / L的水流从16%增至32%。低流量和高流量时,ANC <0μeq/ L的水流比例从北向南降低。碱性阳离子稀释解释了流中最大的间歇性酸化,而硫酸盐(SO42-)浓度的变化是次要解释变量。情景上SO42-的分布格局在地理上有所不同,在北部河流中,稀释作用占主导地位,而在冰川沉积物中发育的土壤则在其下游;而在南部河流中,浓度较高的条件是年龄较老,风化的土壤。间歇性酸化随着低流量ANC的增加而增加,在25%的物流中超过90μeq/ L。在低流量ANC值<30μeq/ L的水流中,ANC的增加是主要的模式。长期和间歇酸化仍然是AT流中的生态问题。此处开发的方法可用于估算从大气S和N沉积物水平下降中恢复的其他地区的慢性和间歇酸化的程度和程度。

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