Magiera Tadeusz, Kapicka Ales, Petrovský Eduard, Strzyszcz Zygmunt, Fialová Hana, Rachwał Marzena
Institute of Environmental Engineering PAS, M. Sklodowskiej-Curie 34, 41-819 Zabrze, Silesian, Poland.
Environ Pollut. 2008 Dec;156(3):618-27. doi: 10.1016/j.envpol.2008.06.030. Epub 2008 Aug 6.
Previous investigations revealed a strong magnetic anomaly due to soil magnetic enhancement in the industrialized cross-border area of Upper Silesia (Poland) and Northern Moravia (Czech Republic). Since industrial and urban dusts contain magnetic particles, this soil magnetic enhancement is assumed to be of anthropogenic origin, caused by a high concentration of atmospherically deposited magnetic particles, accumulated in topsoil layers. This assumption is proved by investigations of vertical profiles of magnetic susceptibility along a transect crossing the border area of the two countries. The results show that the population of magnetic minerals in the organic horizon is different from that in the mineral horizons. The vertical distribution of magnetic susceptibility and thermomagnetic analysis suggests negligible lithogenic contribution. The observed relationship between magnetic susceptibility and some heavy metals, confirmed by micromorphological observations and microchemical analysis of magnetic particles separated from the organic horizons of forest topsoil, has proved the usefulness of soil magnetometry for pollution study.
先前的调查显示,在上西里西亚(波兰)和北摩拉维亚(捷克共和国)工业化的跨境地区,由于土壤磁性增强而出现强烈的磁异常。由于工业和城市灰尘含有磁性颗粒,这种土壤磁性增强被认为是人为来源,由大气中沉积的高浓度磁性颗粒在表层土壤层中积累所致。对一条穿越两国边境地区的样带进行的磁化率垂直剖面调查证实了这一假设。结果表明,有机层中的磁性矿物种群与矿质层中的不同。磁化率的垂直分布和热磁分析表明岩源贡献可忽略不计。通过对从森林表层土壤有机层中分离出的磁性颗粒进行微观形态观察和微化学分析,证实了磁化率与某些重金属之间的观测关系,证明了土壤磁测在污染研究中的有用性。