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首页> 外文期刊>Hydrology and Earth System Sciences >Future recovery of acidified lakes in southern Norway predicted by the MAGIC model
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Future recovery of acidified lakes in southern Norway predicted by the MAGIC model

机译:MAGIC模型预测的挪威南部酸化湖泊的未来恢复

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The acidification model MAGIC was used to predict recovery of small lakes in southernmost Norway to future reduction of acid deposition. A set of 60 small headwater lakes was sampled annually from either 1986 (35 lakes) or 1995 (25 lakes). Future acid deposition was assumed to follow implementation of current agreed legislation, including the Gothenburg protocol. Three scenarios of future N retention were used. Calibration of the sites to the observed time trends (1990–1999) as well as to one point in time considerably increased the robustness of the predictions. The modelled decline in SO4* concentrations in the lakes over the period 1986–2001 matched the observed decline closely. This strongly suggests that soil processes such as SO4 adsorption/desorption and S reduction/oxidation do not delay the response of runoff by more than a few years. The slope of time trends in ANC over the period of observations was less steep than that observed, perhaps because the entire soil column does not interact actively with the soilwater that emerges as runoff. The lakes showed widely differing time trends in NO3 concentrations over the period 1986–2000. The observed trends were not simulated by any of the three N scenarios. A model based on the C/N ratio in soil was insufficient to account for N retention and leaching at these sites. The large differences in modelled NO3, however, produced only minor differences in ANC between the three scenarios. In the year 2050, the difference was only about 5 μeq l-1. Future climate change entailing warming and increased precipitation could also increase NO3 loss to surface waters. SO4* concentrations in the lakes were predicted to decrease in parallel with the future decreases in S deposition. Fully 80% of the expected decline to year 2025, however, had already occurred by the year 2000. Similarly, ANC concentrations were predicted to increase in the future, but again about 67% of the expected change has already occurred over the past 20 years. The recovery of ANC was predicted to be incomplete. Even after the CLE scenario (for future acid deposition) is implemented, the chemical conditions in about one-third of the lakes were predicted to be insufficient to support trout populations in the future. Thus, additional measures will be required if these lakes are to be restored. style="line-height: 20px;">Keywords: acid deposition, lakes, model, Norway, recovery
机译:酸化模型MAGIC用于预测挪威最南端的小湖的恢复情况,以减少将来的酸沉降。每年从1986年(35个湖泊)或1995年(25个湖泊)中抽取60个小型上游水源湖泊。假定未来的酸沉积将遵循包括哥德堡议定书在内的当前商定法规的执行。使用了未来保留氮的三种方案。根据观测到的时间趋势(1990-1999年)以及某一时间点对站点进行校准,大大提高了预测的可靠性。 1986年至2001年期间,湖泊中SO 4 * 浓度的模拟下降趋势与观测到的下降趋势非常吻合。这强烈表明,土壤过程如SO 4 的吸附/解吸和S的还原/氧化不会将径流的响应延迟超过几年。在整个观测期间,ANC的时间趋势斜率不如观测到的陡峭,这可能是因为整个土壤柱不会与径流产生的土壤水积极相互作用。在1986-2000年期间,湖泊中NO 3 浓度的时间趋势差异很大。这三个N个场景中的任何一个都没有模拟观察到的趋势。基于土壤中C / N比的模型不足以说明这些位置的氮保留和浸出。但是,在这三种情况下,建模的NO 3 的巨大差异在ANC中仅产生了微小的差异。在2050年,差异仅为5μeql -1 。未来的气候变化将导致变暖和降水增加,也可能增加NO 3 向地表水的损失。预测湖泊中SO 4 * 的浓度会随着未来S沉积量的减少而降低。到2000年,到2025年的预期下降的全部80%已经发生。类似地,预计ANC的浓度在未来会增加,但是在过去20年中,大约有67%的预期变化已经发生。 。预计ANC的恢复不完全。甚至在实施了CLE情景(用于未来的酸沉积)之后,预计未来约有三分之一的湖泊的化学条件不足以支持鳟鱼种群。因此,如果要恢复这些湖泊,就需要采取其他措施。 style =“ line-height:20px;”> 关键字:酸沉降,湖泊,模型,挪威,恢复

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