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Trends in surface water chemistry of acidified UK Freshwaters, 1988-2002

机译:1988-2002年英国酸化淡水的地表水化学趋势

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Analysis of water chemistry data from 15 years of monitoring at 22 acid-sensitive lakes and streams in the UK reveals coherent national chemical trends indicative of recovery from acidification. Excess sulphate and base cations exhibit significant decline, often accompanied by an increase in an alkalinity-based determination of acid neutralising capacity (AB-ANC) and, at fewer sites, a decline in hydrogen and labile aluminium. Acid neutralising capacity determined by "charge-balance" (CB-ANC) exhibits few trends, possibly due to compound errors associated with its determination. Trend slopes in excess sulphate correlate with those for base cations, hydrogen ion and AB-ANC, with between-site variability linked to catchment hydrology, sea-salt inputs and forestry. Nitrate concentrations have not changed significantly but show high sensitivity to varying climate. Trends in AB-ANC are influenced by significant increases in dissolved organic carbon, the cause of which it is vital to establish before trends in the former can definitively be attributed to decreasing acidic deposition.
机译:对英国22个对酸敏感的湖泊和溪流进行15年监测以来对水化学数据的分析表明,国家化学趋势具有连贯性,可指示从酸化中恢复的趋势。过量的硫酸根和阳离子显着下降,通常伴随着基于碱度的酸中和能力(AB-ANC)测定的增加,而在更少的位置,氢和不稳定铝的减少。由“电荷平衡”(CB-ANC)确定的酸中和能力显示出很少的趋势,这可能是由于与其确定相关的化合物误差所致。过量硫酸盐的趋势斜率与碱性阳离子,氢离子和AB-ANC的趋势斜率相关,并且场间变异与流域水文学,海盐输入和林业有关。硝酸盐浓度变化不大,但对气候变化敏感。 AB-ANC的趋势受溶解有机碳显着增加的影响,因此,必须先确定其原因,才能确定前者的趋势可以肯定地归因于酸性沉积的减少。

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