Demineralization of an oil shale by Bacillus circulans (“siliceous bacteria”)
Samo za registrovane korisnike
1990
Članak u časopisu (Objavljena verzija)
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Experiments are presented aimed at removing the silicates from an oil shale by a chemoorganoheterotrophic bacterium, Bacillus circulans. This process was expected to substitute the drastic HF-treatment in the kerogen concentrate preparation procedure. Three Bacillus circulans strains were isolated from siliceous habitats. Tests showed that they were not using the shale organic matter as source of carbon. The substrates were the raw oil shale from Aleksinac, Yugoslavia (-0.063 mm), and the corresponding neutralized HCl- and HCl-kerogen-concentrates. The solid/liquid ratio was 1:10 (w/v), the liquid phase being 2% glycerol in distilled water. In all experiments with the shale concentrates, the pH decreased to ca 3. This resulted in a decrease of the number of bacteria and hence failure in demineralization, the lowest pH limit for the growth being ca 4. The raw shale was shown to be the most favourable substrate due to the buffer effect of the carbonates. The achieved leaching was obvious...ly much better but not yet optimal. So far the total effects were found to be 21.4, 18.7 and 17.2%, respectively. Several possible ways are suggested for improving the efficiency of the process.
Ključne reči:
Bacillus circulans / bacterial desilicification / bioleaching of silicates / oil shale from Aleksinac / silicates / siliceous bacteriaIzvor:
Organic Geochemistry, 1990, 16, 4-6, 1203-1209Izdavač:
- Elsevier
Finansiranje / projekti:
- The Research Fund of S.R. Serbia (Yugoslavia)
Institucija/grupa
IHTMTY - JOUR AU - Vrvić, Miroslav AU - Matić, Valerija AU - Vučetić, Jovan AU - Vitorović, Dragomir PY - 1990 UR - https://cer.ihtm.bg.ac.rs/handle/123456789/4738 AB - Experiments are presented aimed at removing the silicates from an oil shale by a chemoorganoheterotrophic bacterium, Bacillus circulans. This process was expected to substitute the drastic HF-treatment in the kerogen concentrate preparation procedure. Three Bacillus circulans strains were isolated from siliceous habitats. Tests showed that they were not using the shale organic matter as source of carbon. The substrates were the raw oil shale from Aleksinac, Yugoslavia (-0.063 mm), and the corresponding neutralized HCl- and HCl-kerogen-concentrates. The solid/liquid ratio was 1:10 (w/v), the liquid phase being 2% glycerol in distilled water. In all experiments with the shale concentrates, the pH decreased to ca 3. This resulted in a decrease of the number of bacteria and hence failure in demineralization, the lowest pH limit for the growth being ca 4. The raw shale was shown to be the most favourable substrate due to the buffer effect of the carbonates. The achieved leaching was obviously much better but not yet optimal. So far the total effects were found to be 21.4, 18.7 and 17.2%, respectively. Several possible ways are suggested for improving the efficiency of the process. PB - Elsevier T2 - Organic Geochemistry T1 - Demineralization of an oil shale by Bacillus circulans (“siliceous bacteria”) VL - 16 IS - 4-6 SP - 1203 EP - 1209 DO - 10.1016/0146-6380(90)90155-S ER -
@article{ author = "Vrvić, Miroslav and Matić, Valerija and Vučetić, Jovan and Vitorović, Dragomir", year = "1990", abstract = "Experiments are presented aimed at removing the silicates from an oil shale by a chemoorganoheterotrophic bacterium, Bacillus circulans. This process was expected to substitute the drastic HF-treatment in the kerogen concentrate preparation procedure. Three Bacillus circulans strains were isolated from siliceous habitats. Tests showed that they were not using the shale organic matter as source of carbon. The substrates were the raw oil shale from Aleksinac, Yugoslavia (-0.063 mm), and the corresponding neutralized HCl- and HCl-kerogen-concentrates. The solid/liquid ratio was 1:10 (w/v), the liquid phase being 2% glycerol in distilled water. In all experiments with the shale concentrates, the pH decreased to ca 3. This resulted in a decrease of the number of bacteria and hence failure in demineralization, the lowest pH limit for the growth being ca 4. The raw shale was shown to be the most favourable substrate due to the buffer effect of the carbonates. The achieved leaching was obviously much better but not yet optimal. So far the total effects were found to be 21.4, 18.7 and 17.2%, respectively. Several possible ways are suggested for improving the efficiency of the process.", publisher = "Elsevier", journal = "Organic Geochemistry", title = "Demineralization of an oil shale by Bacillus circulans (“siliceous bacteria”)", volume = "16", number = "4-6", pages = "1203-1209", doi = "10.1016/0146-6380(90)90155-S" }
Vrvić, M., Matić, V., Vučetić, J.,& Vitorović, D.. (1990). Demineralization of an oil shale by Bacillus circulans (“siliceous bacteria”). in Organic Geochemistry Elsevier., 16(4-6), 1203-1209. https://doi.org/10.1016/0146-6380(90)90155-S
Vrvić M, Matić V, Vučetić J, Vitorović D. Demineralization of an oil shale by Bacillus circulans (“siliceous bacteria”). in Organic Geochemistry. 1990;16(4-6):1203-1209. doi:10.1016/0146-6380(90)90155-S .
Vrvić, Miroslav, Matić, Valerija, Vučetić, Jovan, Vitorović, Dragomir, "Demineralization of an oil shale by Bacillus circulans (“siliceous bacteria”)" in Organic Geochemistry, 16, no. 4-6 (1990):1203-1209, https://doi.org/10.1016/0146-6380(90)90155-S . .