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A physiologically based kinetic model for bacterial sulfide oxidation.

Authors :
Klok JB
de Graaff M
van den Bosch PL
Boelee NC
Keesman KJ
Janssen AJ
Source :
Water research [Water Res] 2013 Feb 01; Vol. 47 (2), pp. 483-92. Date of Electronic Publication: 2012 Sep 17.
Publication Year :
2013

Abstract

In the biotechnological process for hydrogen sulfide removal from gas streams, a variety of oxidation products can be formed. Under natron-alkaline conditions, sulfide is oxidized by haloalkaliphilic sulfide oxidizing bacteria via flavocytochrome c oxidoreductase. From previous studies, it was concluded that the oxidation-reduction state of cytochrome c is a direct measure for the bacterial end-product formation. Given this physiological feature, incorporation of the oxidation state of cytochrome c in a mathematical model for the bacterial oxidation kinetics will yield a physiologically based model structure. This paper presents a physiologically based model, describing the dynamic formation of the various end-products in the biodesulfurization process. It consists of three elements: 1) Michaelis-Menten kinetics combined with 2) a cytochrome c driven mechanism describing 3) the rate determining enzymes of the respiratory system of haloalkaliphilic sulfide oxidizing bacteria. The proposed model is successfully validated against independent data obtained from biological respiration tests and bench scale gas-lift reactor experiments. The results demonstrate that the model is a powerful tool to describe product formation for haloalkaliphilic biomass under dynamic conditions. The model predicts a maximum S⁰ formation of about 98 mol%. A future challenge is the optimization of this bioprocess by improving the dissolved oxygen control strategy and reactor design.<br /> (Copyright © 2012 Elsevier Ltd. All rights reserved.)

Details

Language :
English
ISSN :
1879-2448
Volume :
47
Issue :
2
Database :
MEDLINE
Journal :
Water research
Publication Type :
Academic Journal
Accession number :
23177655
Full Text :
https://doi.org/10.1016/j.watres.2012.09.021