G. Pihl Karlsson , P.E. Karlsson , S. Hellsten , H. Danielsson , V. Kronnäs , C. Akselsson
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引用次数: 0
Abstract
In the low deposition situation of today at many of the long-term Swedish forest monitoring sites, the deposition measured as precipitation to the open field, i.e. bulk deposition of oxidized sulphur (S) is often higher or equal to deposition of S sampled under the forest canopies, i.e. as throughfall. This suggests that the total S deposition estimated using throughfall is underestimated. The reason for this is direct exchange of S with the forest canopies, leading to an underestimation which becomes evident in low-deposition areas. We describe a new method to estimate the dry deposition of S to coniferous forest based on measurements with Teflon string samplers as surrogate surfaces, in combination with measurements of the net throughfall for sodium (throughfall subtracted with wet deposition). The wet deposition was estimated from bulk deposition measurements on the open field, corrected for dry deposition to the collectors. The method was applied for Norway spruce forests at monitoring sites across Sweden during nine years 2014–2022, and total deposition was calculated based on wet deposition and the estimated dry deposition. The estimated annual total deposition of S as a mean value for coniferous forests ranged between 0.8 and 5.2 kg S ha−1 yr−1 with lowest values in northern Sweden and highest in southwest Sweden. The share of dry deposition of the total S deposition was between 20 and 53%. The mean annual deposition of S measured as throughfall during 2014–2022 for three different regions in Sweden was between 16 and 41% lower compared to the corresponding total deposition estimated with the new method. The canopy exchange of S was analyzed on a monthly basis as the difference between the estimated total deposition and the measured throughfall deposition of S. At most sites, there was a canopy uptake of S during the summer months and a leakage of S during the winter months. This indicates that the canopy exchange of S is a phenomenon that involves some biological activity.
在瑞典许多长期森林监测点目前的低沉积情况下,以降水形式测量的空地沉积物(即氧化硫(S)的大量沉积)往往高于或等于在林冠下采样的 S 沉积物(即直降)。这表明,用直流降雨量估算的 S 沉积总量被低估了。其原因在于 S 与林冠的直接交换,从而导致低估,这在低沉积区尤为明显。我们介绍了一种估算针叶林 S 干沉降量的新方法,该方法基于以聚四氟乙烯绳采样器为替代表面的测量结果,并结合钠净通过量的测量结果(通过量减去湿沉降量)。湿沉降量是根据空地上的大量沉降测量结果估算的,并对采集器上的干沉降量进行了校正。该方法适用于 2014-2022 年九年期间瑞典各地监测点的挪威云杉林,并根据湿沉降量和估计的干沉降量计算出总沉降量。针叶林中估计的 S 年总沉积量的平均值介于 0.8 至 5.2 kg S ha-1 yr-1 之间,瑞典北部的沉积量最低,瑞典西南部的沉积量最高。干沉积物占总 S 沉积物的比例在 20% 到 53% 之间。与采用新方法估算的相应总沉积量相比,2014-2022 年期间瑞典三个不同地区通过降雨量测量的 S 年平均沉积量减少了 16% 至 41%。根据估算的总沉积量与测量的 S 径流沉积量之差,按月对 S 的冠层交换量进行了分析。这表明,树冠层的 S 交换现象涉及某种生物活动。
期刊介绍:
Atmospheric Environment has an open access mirror journal Atmospheric Environment: X, sharing the same aims and scope, editorial team, submission system and rigorous peer review.
Atmospheric Environment is the international journal for scientists in different disciplines related to atmospheric composition and its impacts. The journal publishes scientific articles with atmospheric relevance of emissions and depositions of gaseous and particulate compounds, chemical processes and physical effects in the atmosphere, as well as impacts of the changing atmospheric composition on human health, air quality, climate change, and ecosystems.