Institute of Geochemistry, Mineralogy and Mineral Resources, Faculty of Science, Charles University, Albertov 6, 128 00, Prague, Czech Republic.
Centre for Environmental and Marine Studies, Department of Environment and Planning, CESAM, University of Aveiro, 3810-193, Aveiro, Portugal.
Environ Monit Assess. 2022 Sep 9;194(10):755. doi: 10.1007/s10661-022-10436-7.
Mercury (Hg) concentrations in soils and Hg releases from soils during wildfires are not well characterised in Portugal, even though wildfire activity continues to increase around the Mediterranean. This study focused on the low to moderate severity wildfire in Pombal (Portugal) in 2019, which consumed 12.5 ha of maritime pine (Pinus pinaster Ait.). We evaluated Hg concentrations in soil profiles and Hg pools in organic horizons to assess the fire-induced Hg emissions. Moreover, impacts of the fire on forest floor properties were estimated. Four soil profiles were sampled, two at the burned area and two at a nearby unburned area. The soil profiles displayed a typical Hg distribution, with higher Hg concentrations (156 µg kg) in the organic horizons with a sharp decrease in the mineral layers. The bond between organic matter and Hg was evident along the profiles, with a strong correlation between TOC and Hg. Ratios of Hg/TOC in the surface layers of the soil were similar in all profiles. The mean organic Hg pool at the studied site was calculated at 10.6 g ha. The fire did not seem to affect the topsoil properties based on visual indicators and the lack of statistical differences (p > 0.05) among measured fire-sensitive chemical soil properties (pH, CEC, TOC, TS) between the topsoils of the burned and unburned areas. If we consider a hypothetical complete combustion of the organic layer (743 Mg) and unaffected topsoil, we estimated a release of 133 g of Hg from the burned area. The study emphasised the importance of the forest floor for Hg retention and its crucial role in Hg emissions during wildfires in a country increasingly affected by climate change.
在葡萄牙,土壤中的汞浓度和火灾期间土壤中汞的释放情况并没有得到很好的描述,尽管地中海周围的野火活动仍在持续增加。本研究集中于 2019 年蓬巴尔(葡萄牙)的低到中度严重野火,这场野火消耗了 12.5 公顷的海松(Pinus pinaster Ait.)。我们评估了土壤剖面中的汞浓度和有机层中的汞库,以评估火灾引起的汞排放。此外,还估计了火灾对林下地被物性质的影响。采集了四个土壤剖面,两个在燃烧区,两个在附近未燃烧区。土壤剖面显示出典型的汞分布,有机层中的汞浓度较高(156µg kg),在矿物质层中急剧下降。在整个剖面中,有机物质和汞之间的结合是显而易见的,TOC 和 Hg 之间存在很强的相关性。所有剖面中表层土壤的 Hg/TOC 比值相似。研究地点的平均有机汞库计算为 10.6g ha。根据视觉指标和燃烧敏感的土壤化学性质(pH、CEC、TOC、TS)在燃烧区和未燃烧区表土之间缺乏统计学差异(p>0.05),火灾似乎没有影响表土性质。如果我们假设有机层(743 Mg)完全燃烧且未受影响的表土,我们估计从燃烧区释放 133 克汞。该研究强调了林下地被物对汞保留的重要性及其在气候变化影响日益严重的国家野火期间汞排放的关键作用。