Details zur Publikation

Kategorie Textpublikation
Referenztyp Zeitschriften
DOI 10.1002/elsc.200520104
Titel (primär) Bioleaching of heavy metal polluted sediment: kinetics of leaching and microbial sulfur oxidation
Autor Löser, C.; Zehnsdorf, A.; Görsch, K.; Seidel, H.
Quelle Engineering in Life Sciences
Erscheinungsjahr 2005
Department UBT; UBZ
Band/Volume 5
Heft 6
Seite von 535
Seite bis 549
Sprache englisch
Keywords Bioremediation; Heavy metals; Microorganisms; Sediments; Sulfur compounds
Abstract Remediation of heavy metal polluted sediment through bioleaching using elemental sulfur (S0) as the leaching agent can be regarded as a two-step process: firstly, the microbial oxidation of the added S0 to sulfuric acid and, secondly, the reaction of the produced acid with the sediment. Here, both subprocesses were studied in detail independently: oxidized river sediment was either suspended in sulfuric acid of various strengths, or mixed with various amounts of finely ground S0 powder (diameter of the S0 particles between 1 and 175 μm with a Rosin-Rammler-Sperling-Bennet (RRSB) distribution and an average diameter of 35 μm) and suspended in water. The leaching process was observed by repeated analysis of the suspension concerning pH, soluble sulfate and metals, and remaining S0. In the case of abiotic leaching with H2SO4, the reaction between the acid and the sediment resulted in a gradual increase in pH and a solubilization of sediment-borne heavy metals which required some time; 80 % of the finally solubilized heavy metals was dissolved after 1 h, 90 % after 10 h, and 100 % after 100 h. In the case of bioleaching, the rate of S0 oxidation was maximal at the beginning, gradually diminished with time, and was proportional to the initial amount of S0. Due to its very low solubility in water, S0 is oxidized in a surface reaction catalyzed by attached bacteria. The oxidation let the particles shrink, their surface became smaller and, thus, the S0 oxidation rate gradually decreased. The shrinking rate was time-invariant and, at 30 °C, amounted to 0.5 μm/day (or 100 μg/cm2/day). Within 21 days, 90 % of the applied S0 was oxidized. Three models with a different degree of complexity have been developed that describe this S0 oxidation, assuming S0 particles of uniform size (I), using a measured particle size distribution (II), or applying an adapted RRSB distribution (III). Model I deviated slightly from the measured data but was easy to handle, Model II fitted the measured data best but its simulation was complicated, and Model III was intermediate. The amount of soluble sulfate was smaller than the amount of H2SO4 added or microbially generated as the H2SO4 reacted with the sediment to form in part poorly soluble sulfates. A model has been developed that describes the pH and the soluble sulfate and metals at equilibrium, depending on the amount of H2SO4 applied or microbially generated, and that is based on the condition of electrical neutrality, a global metal/proton exchange reaction, and a sulfate-fixation reaction. In suspension, bioleaching with S0 required considerably more time than abiotic leaching with H2SO4, but the final pH and metal solubilization were identical when equimolar amounts of leaching agents were applied.
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Löser, C., Zehnsdorf, A., Görsch, K., Seidel, H. (2005):
Bioleaching of heavy metal polluted sediment: kinetics of leaching and microbial sulfur oxidation
Eng. Life Sci. 5 (6), 535 - 549 10.1002/elsc.200520104