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Effects of decreasing acid deposition and climate change on acid extremes in an upland stream

机译:减少酸沉降和气候变化对高地河流极端酸的影响

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This study assesses the major chemical processes leading to acid extremes ina small, moorland stream in mid-Wales, UK, which has been monitored since1979. Results suggest that base cation (mainly calcium) dilution, the"sea-salt effect", and elevated nitrate pulses, are the major causes ofseasonal/episodic minima in acid neutralising capacity (ANC), and that therelative importance of these drivers has remained approximately constantduring 25 years of decreasing acid deposition and associated long-termchemical recovery. Many of the chemical variations causing short-termreductions in stream acidity, particularly base cation dilution and organicacid increases, are closely related to changes in water-flowpath andtherefore to stream discharge. Changes in the observed pH-dischargerelationship over time indicate that high-flow pH has increased more rapidlythan mean-flow pH, and therefore that episodes have decreased in magnitudesince 1980. However a two-box application of the dynamic model MAGIC, whilstreproducing this trend, suggests that it will not persist in the long term,with mean ANC continuing to increase until 2100, but the ANC of the uppersoil (the source of relatively acid water during high-flow episodes)stabilising close to zero beyond 2030. With climate change predicted to leadto an increase in maximum flows in the latter half of the century, high-flowrelated acid episodes may actually become more rather than less severe inthe long term, although the model suggests that this effect may be small.Two other predicted climatic changes could also detrimentally impact on acidepisodes: increased severity of winter "sea-salt" episodes due to higherwind speeds during winter storms; and larger sulphate pulses due tooxidation of reduced sulphur held in organic soils, during more extremesummer droughts. At the Gwy, the near-coastal location and relatively smallextent of peat soils suggest that sea-salt episodes may have the greatestinfluence.
机译:这项研究评估了自1979年以来一直受到监测的英国威尔士中部小而荒芜的溪流中导致极端酸产生的主要化学过程。结果表明,碱性阳离子(主要是钙)稀释,“海盐效应”和升高的硝酸盐脉冲是造成酸中和能力(ANC)季节性/间歇性极小值的主要原因,并且这些驱动因素的相对重要性仍然保持着大约在减少酸沉降和相关的长期化学回收的25年中保持稳定。导致溪流酸度短期降低的许多化学变化,特别是碱阳离子稀释和有机酸增加,与水流路径的变化密切相关,因此与溪流排放密切相关。随着时间的推移,观察到的pH放电关系的变化表明,高流量pH的增加比平均流量pH的增加更快,因此自1980年以来,发作的幅度有所下降。但是,动态模型MAGIC的两盒应用在再现了这种趋势的同时,这表明它不会长期持续下去,平均ANC会持续增加直到2100年,但是上层土壤(高流量事件中相对酸性水的来源)的ANC会在2030年以后稳定在接近于零的水平。为了导致本世纪后半叶的最大流量增加,从长远来看,与高流量相关的酸事件实际上可能变得更为严重而不是不那么严重,尽管该模型表明这种影响可能很小。另外两个预测的气候变化也可能对酸病的不利影响:由于冬季风暴中较高的风速,冬季“海盐”发作的严重性增加;在更极端的夏季干旱期间,由于有机土壤中所含还原硫的氧化,硫酸盐脉冲增大。在Gwy,近沿海的位置和相对较小的泥炭土壤表明海盐事件可能具有最大的影响。

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