دورية أكاديمية
Biofilm formation on the surface of monazite and xenotime during bioleaching.
العنوان: | Biofilm formation on the surface of monazite and xenotime during bioleaching. |
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المؤلفون: | van Alin A; Curtin Medical School, Curtin University, Bentley, Western Australia, Australia.; The Institute for Geoscience Research, School of Earth and Planetary Sciences, Curtin University, Bentley, Western Australia, Australia., Corbett MK; Curtin Medical School, Curtin University, Bentley, Western Australia, Australia.; The Institute for Geoscience Research, School of Earth and Planetary Sciences, Curtin University, Bentley, Western Australia, Australia., Fathollahzadeh H; Curtin Medical School, Curtin University, Bentley, Western Australia, Australia.; The Institute for Geoscience Research, School of Earth and Planetary Sciences, Curtin University, Bentley, Western Australia, Australia., Tjiam MC; Curtin Medical School, Curtin University, Bentley, Western Australia, Australia.; Wesfarmers Centre of Vaccines and Infectious Diseases, Telethon Kids Institute, Nedlands, Western Australia, Australia.; Centre for Child Health Research, The University of Western Australia, Crawley, Western Australia, Australia., Rickard WDA; John de Laeter Centre, Curtin University, Bentley, Western Australia, Australia., Sun X; John de Laeter Centre, Curtin University, Bentley, Western Australia, Australia., Putnis A; The Institute for Geoscience Research, School of Earth and Planetary Sciences, Curtin University, Bentley, Western Australia, Australia.; Institut für Mineralogie, University of Münster, Münster, Germany., Eksteen J; WA School of Mines, Minerals, Energy and Chemical Engineering, Curtin University, Bentley, Western Australia, Australia., Kaksonen AH; WA School of Mines, Minerals, Energy and Chemical Engineering, Curtin University, Bentley, Western Australia, Australia.; CSIRO Environment, Perth, Western Australia, Australia., Watkin E; Curtin Medical School, Curtin University, Bentley, Western Australia, Australia.; The Institute for Geoscience Research, School of Earth and Planetary Sciences, Curtin University, Bentley, Western Australia, Australia.; School of Science, Edith Cowan University, Joondalup, Western Australia, Australia. |
المصدر: | Microbial biotechnology [Microb Biotechnol] 2023 Sep; Vol. 16 (9), pp. 1790-1802. Date of Electronic Publication: 2023 Jun 08. |
نوع المنشور: | Journal Article; Research Support, Non-U.S. Gov't |
اللغة: | English |
بيانات الدورية: | Publisher: Wiley-Blackwell Country of Publication: United States NLM ID: 101316335 Publication Model: Print-Electronic Cited Medium: Internet ISSN: 1751-7915 (Electronic) Linking ISSN: 17517915 NLM ISO Abbreviation: Microb Biotechnol Subsets: MEDLINE |
أسماء مطبوعة: | Publication: Hoboken, NJ : Wiley-Blackwell Original Publication: Oxford : Blackwell, c2008- |
مواضيع طبية MeSH: | Biofilms* , Minerals*, Microscopy, Confocal ; Microscopy, Electron, Scanning ; Phosphates |
مستخلص: | Microbial attachment and biofilm formation is a ubiquitous behaviour of microorganisms and is the most crucial prerequisite of contact bioleaching. Monazite and xenotime are two commercially exploitable minerals containing rare earth elements (REEs). Bioleaching using phosphate solubilizing microorganisms is a green biotechnological approach for the extraction of REEs. In this study, microbial attachment and biofilm formation of Klebsiella aerogenes ATCC 13048 on the surface of these minerals were investigated using confocal laser scanning microscopy (CLSM) and scanning electron microscopy (SEM). In a batch culture system, K. aerogenes was able to attach and form biofilms on the surface of three phosphate minerals. The microscopy records showed three distinctive stages of biofilm development for K. aerogenes commencing with initial attachment to the surface occurring in the first minutes of microbial inoculation. This was followed by colonization of the surface and formation of a mature biofilm as the second distinguishable stage, with progression to dispersion as the final stage. The biofilm had a thin-layer structure. The colonization and biofilm formation were localized toward physical surface imperfections such as cracks, pits, grooves and dents. In comparison to monazite and xenotime crystals, a higher proportion of the surface of the high-grade monazite ore was covered by biofilm which could be due to its higher surface roughness. No selective attachment or colonization toward specific mineralogy or chemical composition of the minerals was detected. Finally, in contrast to abiotic leaching of control samples, microbial activity resulted in extensive microbial erosion on the high-grade monazite ore. (© 2023 The Authors. Microbial Biotechnology published by Applied Microbiology International and John Wiley & Sons Ltd.) |
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المشرفين على المادة: | 1306-41-8 (monazite) 0 (Minerals) 0 (Phosphates) |
تواريخ الأحداث: | Date Created: 20230609 Date Completed: 20230823 Latest Revision: 20230824 |
رمز التحديث: | 20231215 |
مُعرف محوري في PubMed: | PMC10443343 |
DOI: | 10.1111/1751-7915.14260 |
PMID: | 37291762 |
قاعدة البيانات: | MEDLINE |
تدمد: | 1751-7915 |
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DOI: | 10.1111/1751-7915.14260 |