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Modelling acidification, recovery and target loads for headwater catchments in Nova Scotia, Canada

机译:对加拿大新斯科舍省上游水源的酸化,回收和目标负荷进行建模

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摘要

The response of twenty acid-sensitive headwater catchments in Nova Scotia toacidic deposition was investigated for the period 1850–2100 using a dynamichydrochemical model (MAGIC: Model of Acidification of Groundwater inCatchments). To ensure robust model simulation, MAGIC was calibrated to thelong-term chemical trend in annual lake observations (13–20 years). Modelsimulations indicated that the surface waters of all twenty catchmentsacidified to the 1970s but showed subsequent recovery (increases in acidneutralising capacity (ANC) and pH) as sulphate deposition decreased.However, under proposed future emissions reductions (approximately 50% ofcurrent deposition) simulated ANC and pH will not return to estimatedpre-industrial levels by 2100. An ANC of 20 μmolc L−1 and pHof 5.4 were defined as acceptable chemical thresholds (or critical chemicallimits) for aquatic organisms in the current study. Under the proposedemissions reductions only one catchment is predicted to remain below thecritical limit for ANC by 2100; three additional catchments are predicted toremain below the critical limit for pH. Dynamic models may be used toestimate target loads, i.e., the required deposition reductions to achieverecovery within a given time. Setting target loads at approximately 30%of current depositions would allow three of the four lakes to reach thechemical criteria by 2030. In contrast to the generally good prognosis forsurface waters, soils lost an average of 32% of estimated initial basesaturation and recovery is estimated to be very slow, averaging 23% lowerthan pre-acidification levels in 2100.
机译:使用动态水化学模型(MAGIC:集水区地下水酸化模型)研究了新斯科舍省20个酸敏感源区对酸性沉积的响应。为了确保强大的模型仿真,将MAGIC校准为年度湖泊观测(13–20年)中的长期化学趋势。模型模拟表明,到1970年代酸化的所有20个集水区的地表水都显示出随后的回收率(酸中和能力(ANC)和pH值的增加)随着硫酸盐沉积的减少而降低,但是在拟议的未来减排量中(大约当前沉积的50%),模拟了ANC和pH值到2100年不会恢复到工业化之前的估计水平。ANC为20μmol c L -1 且pH值为5.4被定义为可接受的化学阈值(或临界化学极限)当前研究中的水生生物。根据拟议的减排量,到2100年,仅一个流域预计将保持低于ANC的临界限值;预计另外三个流域将保持在pH的临界限值以下。可以使用动态模型来估计目标负荷,即,在给定时间内实现恢复所需的沉积减少量。将目标负荷设定为当前沉积的大约30%,到2030年将使四个湖泊中的三个达到化学标准。与通常对地表水的良好预后形成对比的是,土壤平均损失了估计的初始基础饱和度的32%,恢复量估计为速度非常慢,平均比2100年的酸化前水平低23%。

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