Abstract
The remaining soil contamination after the removal of thesludge and the affected topsoil was studied in the northernpart of the Guadiamar river valley affected by the Aznalcóllartoxic spill. The easily soluble (NH4NO3-extraction)and the oxidisable fraction (H2O2/HNO3-extraction)were analysed in samples of two calcareous and two non-calcareoussoils. Correlations between soil properties and heavy metal concentrations were tested with special respect to depth distribution. The spatial distributions of the easily soluble and the oxidisable fraction were highly skewed in both examineddepths (0–20 and 20–40 cm). Easily soluble heavymetal concentrations of a high percentage of samples exceededthresholds that have been given in the German soil protectionlaw particularly in the non-calcareous soils. Within the soillayers of the non-calcareous soils, the pH seems to control theeasily soluble concentrations. However no relation between thepH and depth distribution of heavy metals within the profilescould be found. Physical properties, which determine partlypenetration depth of the sludge and soil mixing caused by theremoval may be the more important factors. Accordingly, highheavy metal concentrations are to be expected even in thesubsoils of clayey sites. As heavy metal concentrations in theoxidisable fraction are still high, further oxidationaccompanied by pH lowering has to be expected. Thus, thestudied soils show a significant risk potential of availableheavy metals even after the removal of the sludge.
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Nagel, I., Lang, F., Kaupenjohann, M. et al. Guadiamar Toxic Flood: Factors that Govern Heavy Metal Distribution in Soils. Water, Air, & Soil Pollution 143, 211–224 (2003). https://doi.org/10.1023/A:1022806209272
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DOI: https://doi.org/10.1023/A:1022806209272