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Toward a recovery time: forest herbs insight related to anthropogenic acidification

机译:争取恢复时间:与人为酸化有关的森林草药见解

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Atmospheric deposition is a global concern contributing to soil acidi?cation and biodiversity changes in forest ecosystems. Although acidifying deposition has decreased in the last decades in Europe, few evidence of ecosystem recovery from acidi?cation has been reported until now. The objective of this study was to reconstruct spatiotemporal changes in soil pH across the entire French forest territory over the last 100-year period through herb species assemblages. Data were collected from ?oristic databases resulting in a total of 120 216 plots covering French forests and spanning from 1910 to 2010. To de?ne acidity ?gures, pH values were inferred from herb assemblages for each plot of the prediction dataset based on a weighted averaging partial least squares (WA-PLS) model (R 2 = 0.80, SD = 0.59 for the validation dataset). Spatiotemporal trends of mean pH changes were obtained by comparing plots with respect to the period (mean year of the period = 1933, 1966, 1984, 1997, 2007) and substrate (acidic and nonacidic forest areas). Bioindicated pH highlighted a decrease in soil pH in both acidic and nonacidic forest areas. The sharpest and most signi?cant pH decrease occurred before 1984 in acidic areas, reaching 0.34 pH units. Subsequently, no signi?cant changes were observed, with a tendency toward stabilization. By contrast, the pH decrease reached 0.19 pH units in nonacidic areas, only reaching signi?cance between 1984 and 1997. Thereafter, we observed a slight and signi?cant pH increase. Spatially, pH trends revealed a regionalized character of acidi?cation regarding the substrate, which could not be related to the extent of deposition modeled by the European Monitoring and Evaluation Programme. Both temporal and spatial trends highlight the lagged responses of nonacidic areas compared with acidic areas. Hence, ?oristic reconstructed pH trends demonstrate a gradual cessation and recovery from acidi?cation of French forests after a period of intense atmospheric pollution.
机译:大气沉积是引起土壤酸化和森林生态系统生物多样性变化的全球关注的问题。尽管在过去的几十年中,欧洲的酸化沉积减少了,但迄今为止,鲜有生态系统从酸化中恢复的证据。这项研究的目的是通过草药物种的组合来重建整个法国森林地区在过去100年中土壤pH的时空变化。从oristic数据库中收集数据,得出覆盖法国森林的120 216个样地,时间跨度为1910年至2010年。为定义酸度数字,从草药组合推断出预测数据集每个样地的pH值,基于加权平均偏最小二乘(WA-PLS)模型(对于验证数据集,R 2 = 0.80,SD = 0.59)。通过比较各个时期(该时期的年均= 1933、1966、1984、1997、2007)和基质(酸性和非酸性林区)的图,可以获得平均pH变化的时空趋势。生物指示的pH值表明酸性和非酸性林区的土壤pH均下降。在1984年之前,酸性地区的pH下降幅度最大,幅度最大,达到0.34 pH单位。随后,未观察到明显变化,并趋于稳定。相比之下,在非酸性区域,pH降低达到0.19 pH单位,仅在1984年至1997年之间达到显着水平。此后,我们观察到pH值出现了轻微且显着的升高。从空间上看,pH趋势显示了底物酸化的区域性特征,这与欧洲监测和评估计划所模拟的沉积程度无关。与酸性区域相比,时间和空间趋势都突出了非酸性区域的滞后响应。因此,在一段时间的强烈大气污染之后,合理的pH重建趋势表明法国森林的酸化逐渐停止和恢复。

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