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首页> 外文期刊>Hydrology and Earth System Sciences >Climate change as a confounding factor in reversibility of acidification: RAIN and CLIMEX projects
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Climate change as a confounding factor in reversibility of acidification: RAIN and CLIMEX projects

机译:气候变化是酸化可逆性的一个混杂因素:RAIN和CLIMEX项目

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The RAIN and CLIMEX experiments atRisdalsheia, southernmost Norway, together cover 17 years (1984-2000) of whole-catchmentmanipulation of acid deposition and climate. A 1200 m2 roofplaced over the forest canopy at KIM catchment excluded about 80% of ambientacid deposition; clean rain was sprinkled under the roof. Aclimate change treatment (3.7°C increase in air temperature and increase in aircarbon dioxide concentrations to 560 ppmv) was superimposed onthe clean rain treatment for four years (1995-1998). Sea-salt inputs and temperatureare climate-related factors that influence water chemistry and can confoundlong-term trends caused by changes in deposition of sulphurand nitrogen. The RAIN and CLIMEX experiments at Risdalsheia provided directexperimental data that allow quantitative assessment ofthese factors. Run-off chemistry responded rapidly to the decreased aciddeposition. Sulphate concentrations decreased by 50% within threeyears; nitrate and ammonium concentrations decreased to new steady-state levelswithin the first year. Acid neutralising capacity increasedand hydrogen ion and inorganic aluminium decreased. Similar recovery fromacidification was also observed at the reference catchment,ROLF, in response to the general 50% reduction in sulphate deposition oversouthern Norway in the late 1980s and 1990s. Variations insea-salt deposition caused large variations in run-off chemistry at thereference catchment ROLF and the year-to-year noise in acidneutralising capacity was as large as the overall trend over the period. Thesevariations were absent at KIM catchment because the sea-salt inputswere held constant over the entire 17 years of the clean rain treatment. Theclimate change experiment at KIM catchment resulted inincreased leaching of inorganic nitrogen, probably due to increasedmineralisation and nitrification rates in the soils. style="line-height: 20px;">Keywords: acid deposition, global change, water, soil, catchment, experiment, Norway.
机译:在挪威最南端的里斯达希亚(Risdalsheia)进行的RAIN和CLIMEX实验共进行了17年(1984-2000)的全流域酸沉降和气候调控。在KIM集水区的森林冠层上方的1200 m 2 屋顶排除了大约80%的环境酸沉积。屋檐下洒了干净的雨。四年(1995-1998年)的清洁雨水处理叠加了气候变化处理(气温升高3.7°C,空气中二氧化碳浓度增加到560 ppmv)。海盐输入和温度是与气候相关的因素,会影响水的化学作用,并可能混淆由硫和氮沉积变化引起的长期趋势。 Risdalsheia的RAIN和CLIMEX实验提供了直接的实验数据,可以对这些因素进行定量评估。径流化学对减少的酸沉积反应迅速。三年内硫酸盐浓度降低了50%;在第一年内,硝酸盐和铵的浓度下降到新的稳态水平。酸中和能力增加,氢离子和无机铝减少。在1980年代末期和1990年代后期,在挪威南部,硫酸盐沉积总体减少了50%,在参考流域ROLF也观察到了类似的酸化回收。海盐沉积的变化导致参考流域ROLF的径流化学变化很大,酸中和能力的年比噪声与该时期的总体趋势一样大。在KIM集水区没有这些变化,因为在整个整整17年的雨水处理过程中,海盐输入量都保持恒定。 KIM集水区的气候变化实验导致无机氮的淋溶增加,这可能是由于土壤中的矿化和硝化速率增加所致。 style =“ line-height:20px;”> 关键字:酸沉降,全球变化,水,土壤,流域,实验,挪威。

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