Mariussen Espen, Johnsen Ida Vaa, Strømseng Arnljot Einride
Norwegian Defence Research Establishment (FFI), Protection and Societal Security Division, PO Box 25, 2027, Kjeller, Norway.
The Norwegian Water Resources and Energy Directorate, P.O. Box 5091, Majorstua, 0301, Oslo, Norway.
Environ Sci Pollut Res Int. 2017 Apr;24(11):10182-10196. doi: 10.1007/s11356-017-8647-8. Epub 2017 Mar 6.
An environmental survey was performed on shooting ranges for small arms located on minerotrophic mires. The highest mean concentrations of Pb (13 g/kg), Cu (5.2 g/kg), Zn (1.1 g/kg), and Sb (0.83 g/kg) in the top soil were from a range located on a poor minerotrophic and acidic mire. This range had also the highest concentrations of Pb, Cu, Zn, and Sb in discharge water (0.18 mg/L Pb, 0.42 mg/L Cu, 0.63 mg/L Zn, and 65 μg/L Sb) and subsurface soil water (2.5 mg/L Pb, 0.9 mg/L Cu, 1.6 mg/L Zn, and 0.15 mg/L Sb). No clear differences in the discharge of ammunition residues between the mires were observed based on the characteristics of the mires. In surface water with high pH (pH ~7), there was a trend with high concentrations of Sb and lower relative concentrations of Cu and Pb. The relatively low concentrations of ammunition residues both in the soil and soil water, 20 cm below the top soil, indicates limited vertical migration in the soil. Channels in the mires, made by plant roots or soil layer of less decomposed materials, may increase the rate of transport of contaminated surface water into deeper soil layers and ground water. A large portion of both Cu and Sb were associated to the oxidizable components in the peat, which may imply that these elements form inner-sphere complexes with organic matter. The largest portion of Pb and Zn were associated with the exchangeable and pH-sensitive components in the peat, which may imply that these elements form outer-sphere complexes with the peat.
对位于贫营养泥炭沼地上的小型武器射击场进行了环境调查。表层土壤中铅(13微克/千克)、铜(5.2微克/千克)、锌(1.1微克/千克)和锑(0.83微克/千克)的最高平均浓度来自一个位于贫营养且酸性泥炭沼地上的射击场。该射击场的排放水中铅、铜、锌和锑的浓度也最高(铅0.18毫克/升、铜0.42毫克/升、锌0.63毫克/升、锑65微克/升),地下土壤水中的浓度为(铅2.5毫克/升、铜0.9毫克/升、锌1.6毫克/升、锑0.15毫克/升)。根据泥炭沼的特征,未观察到不同泥炭沼之间弹药残留物排放的明显差异。在高pH值(pH约为7)的地表水中,存在锑浓度高而铜和铅相对浓度低的趋势。表层土壤以下20厘米处的土壤和土壤水中弹药残留物浓度相对较低,表明其在土壤中的垂直迁移有限。泥炭沼中由植物根系或分解程度较低的物质的土壤层形成的通道,可能会增加受污染地表水向更深土壤层和地下水的运输速率。铜和锑的很大一部分与泥炭中的可氧化成分相关,这可能意味着这些元素与有机物形成内球络合物。铅和锌的最大部分与泥炭中的可交换和pH敏感成分相关,这可能意味着这些元素与泥炭形成外球络合物。