Department of Earth and Environmental Sciences, Division of Soil and Water Management, Katholieke Universiteit Leuven , Kasteelpark Arenberg, 20, 3001 Heverlee, Belgium.
Environ Sci Technol. 2011 Feb 15;45(4):1616-22. doi: 10.1021/es104000m. Epub 2011 Jan 4.
The red mud accident of October 4, 2010, in Ajka (Hungary) contaminated a vast area with caustic, saline red mud (pH 12) that contains several toxic trace metals above soil limits. Red mud was characterized and its toxicity for plants was measured to evaluate the soil contamination risks. Red mud radioactivity (e.g., (238)U) is about 10-fold above soil background and previous assessments revealed that radiation risk is limited to indoor radon. The plant toxicity and trace metal availability was tested with mixtures of this red mud and a local noncontaminated soil up to a 16% dry weight fraction. Increasing red mud applications increased soil pH to maximally 8.3 and soil solution EC to 12 dS m(-1). Shoot yield of barley seedlings was affected by 25% at 5% red mud in soil and above. Red mud increased shoot Cu, Cr, Fe, and Ni concentrations; however, none of these exceed toxic limits reported elsewhere. Moreover, NaOH amended reference treatments showed similar yield reductions and similar changes in shoot composition. Foliar diagnostics suggest that Na (>1% in affected plants) is the prime cause of growth effects in red mud and in corresponding NaOH amended soils. Shoot Cd and Pb concentrations decreased by increasing applications or were unaffected. Leaching amended soils (3 pore volumes) did not completely remove the Na injury, likely because soil structure was deteriorated. The foliar composition and the NaOH reference experiment allow concluding that the Na salinity, not the trace metal contamination, is the main concern for this red mud in soil.
2010 年 10 月 4 日,匈牙利阿格卡(Ajka)的赤泥事故污染了大片土地,导致腐蚀性、含盐量高的赤泥(pH 值为 12)泛滥,其中含有多种超过土壤限量的有毒痕量金属。本研究对赤泥进行了特性分析,并对其植物毒性进行了测量,以评估土壤污染风险。赤泥的放射性(例如,(238)U)比土壤背景高出约 10 倍,此前的评估表明,辐射风险仅限于室内氡。本研究用这种赤泥和当地未受污染的土壤混合物进行了植物毒性和痕量金属有效性测试,赤泥在土壤中的添加比例高达干重的 16%。随着赤泥的不断添加,土壤 pH 值最高可增加到 8.3,土壤溶液电导率增加到 12 dS m(-1)。土壤中赤泥添加量达到 5%时,会对大麦幼苗的地上部生物量产生 25%的抑制作用。赤泥增加了植株的 Cu、Cr、Fe 和 Ni 浓度;然而,没有一种浓度超过其他地方报道的有毒浓度限值。此外,用 NaOH 处理的对照实验显示出类似的减产和类似的地上部组成变化。叶片诊断表明,在赤泥和相应的 NaOH 处理土壤中,起主要生长抑制作用的是 Na(受影响植物中含量超过 1%)。随着赤泥添加量的增加,植株的 Cd 和 Pb 浓度降低,或不受影响。用淋洗法处理添加了赤泥的土壤(淋洗 3 倍孔隙体积)并不能完全去除 Na 伤害,可能是因为土壤结构遭到破坏。叶片组成和 NaOH 对照实验表明,对于这种赤泥在土壤中的应用,主要关注的是 Na 盐度,而不是痕量金属污染。