2022
DOI: 10.1016/j.clay.2022.106653
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Mechanisms of microbial-based iron reduction of clay minerals: Current understanding and latest developments

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Cited by 14 publications
(4 citation statements)
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“…Earlier studies also showed that microbial localization on mineral ores plays a crucial role in facilitating iron reduction, giving rise to the fundamental question of the ability of these two microbes to localize on the surface of the kaolin clay to facilitate iron internalization and reduction. 28 We discovered that the different culturing conditions also affect microbial localization and biofilm formation on the clay surface ( Figure S9 ). The accumulated biofilm produced by B. cereus cultured in LB and glucose medium showed 2-fold higher compared to 0.1LB medium ( Figure 5 A).…”
Section: Resultsmentioning
confidence: 98%
“…Earlier studies also showed that microbial localization on mineral ores plays a crucial role in facilitating iron reduction, giving rise to the fundamental question of the ability of these two microbes to localize on the surface of the kaolin clay to facilitate iron internalization and reduction. 28 We discovered that the different culturing conditions also affect microbial localization and biofilm formation on the clay surface ( Figure S9 ). The accumulated biofilm produced by B. cereus cultured in LB and glucose medium showed 2-fold higher compared to 0.1LB medium ( Figure 5 A).…”
Section: Resultsmentioning
confidence: 98%
“…For example, main methods of kaolin bleaching comprises flocculation with polymers, chemical solubilization, extraction, and washing (Cobos-Murcia et al, 2022). Despite iron-reducing microorganisms can also be used for this purpose (Hosseini and Ahmadi, 2015;Yong et al, 2022), few studies report the utilization of heterotrophic acidophiles for kaolin bleaching (Kupka et al, 2007). On the other hand, metallic iron may be obtained from recalcitrant ores by the sequential using of iron-reducers (González et al, 2020) and electrowinning (Mostad et al, 2008).…”
Section: Biomining and Bioremediation Processesmentioning
confidence: 99%
“…In pristine subsurface environments, there is a characteristic sequence of microbial reduction processes based on the availability of key terminal electron acceptors and donors with nitrate dominating over Fe(III), sulfate, and CO 2 when O 2 is not present (Chapelle, 2000; Meleshyn, 2014). Since nitrate is not measurable in OPA rock (Pearson et al, 2003), Fe(III) from the clay minerals can serve as the primary electron acceptor in this environment (Yong et al, 2022). Thus, Fe(III)‐reducing microorganisms can be expected to dominate and outcompete SRB, which in turn would outcompete methanogenic organisms for electron donors, thereby inhibiting sulfate reduction and/or methane production (Chapelle, 2000).…”
Section: Introductionmentioning
confidence: 99%