Krysiak Agnieszka, Karczewska Anna
Institute of Soil Science and Agricultural Environment Protection, Wrocław University of Environmental and Life Sciences, ul. Grunwaldzka 53, 50-357 Wroclaw, Poland.
Sci Total Environ. 2007 Jul 1;379(2-3):190-200. doi: 10.1016/j.scitotenv.2006.09.031. Epub 2006 Dec 21.
Arsenic (As) concentrations in soils and waste material in two areas of former As mining and processing: Złoty Stok (Złote Mts.) and Zeleźniak (Kaczawskie Mts.), SW Poland, were measured to assess levels and environmental risk associated with possible increases in arsenic mobility under changing pH and redox conditions. Twenty six soil samples were collected from 12 sites, and represented a broad spectrum of soil properties and parent material origin, including natural soils, mine spoils, slags and tailings. Arsenic species were examined using a sequential extraction technique. The changes in As solubility were determined from extraction test solutions adjusted to solution pH values varying from 2 to 8. The effects of reducing conditions on As mobility were examined in incubation tests. Most of soils demonstrated extremely high concentrations of As, both of natural and anthropogenic origin. Total As concentrations in all samples were in the range 100-43,500 mg/kg. Sequential extraction techniques suggested that the main species of As in all soils were those bound to iron (Fe) oxides, in particular amorphous ones, whereas the contributions of mobile and specifically sorbed As forms were relatively low. In tailings and tailings-affected alluvial soils, As occurred mainly in residual forms, however these soils also had considerable amounts of mobile As. In all other soils, mobile As forms were very low. Arsenic mobilization could be possible at extremely low or high pH conditions (pH<2 or pH>8), and this may be of particular practical importance in the case of tailings, which are highly alkaline. High pH promotes solubilization of As forms in reducing conditions, whereas in neutral and acidic soils the risk of As release under reducing conditions is limited.
对波兰西南部两个前砷矿开采和加工地区(兹洛蒂斯托克(兹洛特山脉)和泽莱兹尼亚克(卡乔夫斯基山脉))的土壤和废料中的砷(As)浓度进行了测量,以评估在pH值和氧化还原条件变化的情况下,砷迁移率可能增加所带来的水平及环境风险。从12个地点采集了26个土壤样本,这些样本代表了广泛的土壤性质和母质来源,包括天然土壤、矿渣、炉渣和尾矿。采用连续提取技术对砷的形态进行了检测。通过将提取测试溶液的pH值调节至2至8来确定砷溶解度的变化。在培养试验中研究了还原条件对砷迁移率的影响。大多数土壤显示出极高浓度的砷,既有天然来源的,也有人为来源的。所有样本中的总砷浓度范围为100 - 43500毫克/千克。连续提取技术表明,所有土壤中砷的主要形态是与铁(Fe)氧化物结合的形态,特别是无定形铁氧化物,而可移动和特异性吸附的砷形态的占比相对较低。在尾矿和受尾矿影响的冲积土中,砷主要以残留形态存在,不过这些土壤中也含有相当数量的可移动砷。在所有其他土壤中,可移动砷形态的含量非常低。在极低或极高pH条件下(pH < 2或pH > 8),砷可能会发生迁移,这在尾矿这种高碱性的情况下可能具有特别重要的实际意义。高pH值会促进在还原条件下砷形态的溶解,而在中性和酸性土壤中,还原条件下砷释放的风险是有限的。