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Twenty-five year record of chemicals in open field precipitation and throughfall from a medium-altitude forest catchment (Strengbach - NE France): An obvious response to atmospheric pollution trends

机译:25年记录的中空森林集水区露天降雨和穿透降雨中的化学物质(Strengbach-法国东北部):对大气污染趋势的明显响应

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This study concerned a 25 yr continuous record of bulk precipitation and throughfall composition in a medium-altitude forested environment. The 1986-2012 survey from the more intense acid rain period in the mid-eighties until the present allowed the quantification of the interaction between atmospheric deposition and vegetation and the long-term evolution following pollutant emission trends.The long-term monitoring evidenced some significant temporal trends (pH, conductivity, SO42-, Cl-, NO3-, Ca2+, Mg2+, and K+). Significant decreases in the concentrations and fluxes of several ions were observed (H+ and SO42-, Cl-, and Ca2+) in open field precipitation and throughfalls. The regular and strong decrease in protons and sulfate followed the decreases in anthropogenic SO2 and NOx (proton precursors) since the 1980s. The decrease in Cl- concentrations was weaker and could have been related to the regional reduction in HCl emissions and/or to changes in the precipitation regime. The annual calcium fluxes were reduced from approximately 15 to 9 and 6 to 2 kg ha(-1) under spruces and beeches, respectively, as a consequence of reductions in anthropogenic industrial dust. In such calcium-limited resource soils, the atmospheric Ca flux exceeded the Ca flux from mineral weathering and was highly bioavailable for vegetation growth. This decrease in nutrient input had strong consequences for soil nutrients and may thus have participated in forest decline.The two tree plantations had contrasting effects on the physico-chemical parameters of the incoming precipitation with higher water interception and chemical concentrations under spruces than under beeches, which underlined the role of tree species in atmospheric inputs to soils. The structure and persistence of spruce needles enhanced the capture of particles and water, accentuating the acidity of the deposition and leading to the intensification of acidification processes, nutrient leaching in soils and forest decline. In contrast, beech leaves were able to neutralize a portion of the atmospheric protons, which minimized and reduced the negative effects of acid rain. In addition, the throughfalls represented an important part of the biological cycle of trees for some elements such as K or N, as indicated by the contrasting patterns at year and long-term scales regarding the vegetation type. However, our study indicated that the influence of tree species might change over time with changes in atmospheric pollution, in precipitation regime, or in stand structure.This study outlined the importance of the long-term record of open field precipitation and throughfalls under various tree types to better evaluate the real inputs of elements to forest ecosystems and among them, essential mineral nutrients.
机译:这项研究涉及在中等海拔森林环境中连续25年连续记录的大量降水和穿透物组成。 1986-2012年的调查从80年代中期的更强烈的酸雨时期到现在,可以量化大气沉积物和植被之间的相互作用以及污染物排放趋势后的长期演变。时间趋势(pH,电导率,SO42-,Cl-,NO3-,Ca2 +,Mg2 +和K +)。在露天降雨和穿透中,观察到几种离子(H +和SO42-,Cl-和Ca2 +)的浓度和通量显着下降。自1980年代以来,质子和硫酸盐的定期而强烈的减少是由于人为的SO2和NOx(质子前体)的减少。 Cl浓度的降低较弱,可能与HCl排放量的区域减少和/或降水变化有关。由于减少了人为的工业粉尘,在云杉和山毛榉下,年钙通量分别从约15 kg减少至9 kg ha(-1)和6 kg减少至2 kg ha(-1)。在这种钙有限的资源土壤中,大气中的钙通量超过了矿物风化引起的钙通量,并且对植物生长具有很高的生物利用度。养分投入的减少对土壤养分产生了重大影响,因此可能参与了森林的衰落。这两种人工林对传入降水的理化参数产生了相反的影响,云杉下的水分截留率和化学浓度高于山毛榉,这突显了树种在大气对土壤的投入中的作用。云杉针的结构和持久性增强了对颗粒和水的捕获,增强了沉积物的酸度,并导致酸化过程的加剧,土壤中养分的淋溶和森林的衰退。相比之下,山毛榉叶能够中和一部分大气质子,从而最大程度减少并减少了酸雨的负面影响。此外,对于植物中的某些元素(例如K或N),贯穿降雨代表了树木生物循环的重要组成部分,这在年份和长期尺度上的对比模式中可以看出。然而,我们的研究表明,树木物种的影响可能会随着时间的推移而随大气污染,降水状况或林分结构的变化而变化。本研究概述了长期记录各种树木下的旷野降雨和穿透降雨的重要性类型,以更好地评估元素对森林生态系统的实际投入,其中包括必需的矿物质养分。

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