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Kaddijatou Jallow , Ali Eastman Oku
Faculty Mentor: Dr. Dorothy Wrigley
Minnesota State University, Mankato, Department of Biological Sciences.
Streptomyces and Bacillus Tolerance to Alkaline Conditions and Production of Calcite
Introduction
Special thanks to Dr. Dorothy Wrigley for mentoring us and allowing us to use
her lab during this research and also to the Undergraduate Research Center for
sponsoring the research.
Conclusions
Results
This document is available in alternative format to individuals with disabilities by calling
Accessibility Resources at 507-389-2825 (V), 800-627-3529 or 711 (MRS/TTY)..
.
Concrete is a major construction material consisting of Portland
cement, gravel/crushed stone, sand and water [3]. Concrete is prone to
damage (cracks) from water and these damages have been shown to
expand and worsen if not repaired immediately and properly. Some
bacteria have the ability to precipitate Calcium Carbonate/Calcite
(CaCO3) when placed in the right environmental conditions with
available resources and nutrients. This project focused on discovering
the best environmental conditions in which three strains of bacteria
could produce optimum amounts of calcite. Since the pH of concrete
is relatively alkaline, it is important that the calcite-precipitating
bacteria tolerates and maintains an alkaline environment. The three
calcite-forming bacteria used were Streptomyces 1, Streptomyces 2
and Bacillus 1.
Picture 1: Microscopic picture of bacteria and calcite precipitation
The glucose traditionally used in B4 lead to a more acidic pH. Peptone
based B4 cultures become more acidic but not as acidic as glucose based
B4 media. However , media with higher amounts of peptone media were
more alkaline . The liquid conditions described above lead to very low
precipitation of calcite in peptone and slightly higher precipitation in
glucose. The organisms were very filamentous and difficult to observe on
a plate culture. Finally, the calcium concentration in the B4 media may
be the limiting factor in the quantity of calcite formed. In conclusion, a
different media and buffer system would be required to keep the media
environment alkaline and increase calcite precipitation.
Methods
The three bacteria were cultured in different media and carefully
monitored. Bacterial growth, pH change and amount of calcite
deposited in the media were monitored. Bacterial growth was initially
monitored by measuring the turbidity of the media but was later
measured through plate count. Calcite production was measured by
passing the bacteria through a filter paper. The filter paper was dried
and weighed. The amount of calcite deposited was monitored by
calculating the change in mass of the dry filter paper. B4 media was
used for the majority of the experiment with variable sources and
concentrations of energy, amino acids, and calcium (needed for
calcite). These variable sources of energy, amino acids and calcium
utilized were glucose, yeast extract, calcium chloride, calcium
acetate, TRIS and peptone.
• Achal, V., & Pan, X. (2011). Characterization of urease and carbonic anhydrase
producing bacteria and their role in calcite precipitation. Current
Microbiology, 62, 894-902.
• De Muynck, W., Verbenken, K., De Belie, N., & Verstraete, W. (2010). Influence
of urea and calcium dosage on the effectiveness of bacterially induced
carbonate precipitation on limestone. Ecological Engineering, 36, 99-111.
• De Muynck, W., De Belie, N., & Verstraete W (2010). Microbial carbonate
precipitation in construction materials: A review. Ecological Engineering 36.
118-136.
• Hammes F, N Boon, J de Valliers, Verstraete W., & S D Silciliano (2003). Strain-
specific ureolytic microbial calcium carbonate precipitation. Applied and
environmental Microbiology. 69, 4901-4909.
• Okwadha G, J Li (2010). Optimum conditions for microbial carbonate
precipitation. Chemosphere. 81, 1143-1148.
References
Acknowledgement

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JallowOkuURC poster

  • 1. Kaddijatou Jallow , Ali Eastman Oku Faculty Mentor: Dr. Dorothy Wrigley Minnesota State University, Mankato, Department of Biological Sciences. Streptomyces and Bacillus Tolerance to Alkaline Conditions and Production of Calcite Introduction Special thanks to Dr. Dorothy Wrigley for mentoring us and allowing us to use her lab during this research and also to the Undergraduate Research Center for sponsoring the research. Conclusions Results This document is available in alternative format to individuals with disabilities by calling Accessibility Resources at 507-389-2825 (V), 800-627-3529 or 711 (MRS/TTY).. . Concrete is a major construction material consisting of Portland cement, gravel/crushed stone, sand and water [3]. Concrete is prone to damage (cracks) from water and these damages have been shown to expand and worsen if not repaired immediately and properly. Some bacteria have the ability to precipitate Calcium Carbonate/Calcite (CaCO3) when placed in the right environmental conditions with available resources and nutrients. This project focused on discovering the best environmental conditions in which three strains of bacteria could produce optimum amounts of calcite. Since the pH of concrete is relatively alkaline, it is important that the calcite-precipitating bacteria tolerates and maintains an alkaline environment. The three calcite-forming bacteria used were Streptomyces 1, Streptomyces 2 and Bacillus 1. Picture 1: Microscopic picture of bacteria and calcite precipitation The glucose traditionally used in B4 lead to a more acidic pH. Peptone based B4 cultures become more acidic but not as acidic as glucose based B4 media. However , media with higher amounts of peptone media were more alkaline . The liquid conditions described above lead to very low precipitation of calcite in peptone and slightly higher precipitation in glucose. The organisms were very filamentous and difficult to observe on a plate culture. Finally, the calcium concentration in the B4 media may be the limiting factor in the quantity of calcite formed. In conclusion, a different media and buffer system would be required to keep the media environment alkaline and increase calcite precipitation. Methods The three bacteria were cultured in different media and carefully monitored. Bacterial growth, pH change and amount of calcite deposited in the media were monitored. Bacterial growth was initially monitored by measuring the turbidity of the media but was later measured through plate count. Calcite production was measured by passing the bacteria through a filter paper. The filter paper was dried and weighed. The amount of calcite deposited was monitored by calculating the change in mass of the dry filter paper. B4 media was used for the majority of the experiment with variable sources and concentrations of energy, amino acids, and calcium (needed for calcite). These variable sources of energy, amino acids and calcium utilized were glucose, yeast extract, calcium chloride, calcium acetate, TRIS and peptone. • Achal, V., & Pan, X. (2011). Characterization of urease and carbonic anhydrase producing bacteria and their role in calcite precipitation. Current Microbiology, 62, 894-902. • De Muynck, W., Verbenken, K., De Belie, N., & Verstraete, W. (2010). Influence of urea and calcium dosage on the effectiveness of bacterially induced carbonate precipitation on limestone. Ecological Engineering, 36, 99-111. • De Muynck, W., De Belie, N., & Verstraete W (2010). Microbial carbonate precipitation in construction materials: A review. Ecological Engineering 36. 118-136. • Hammes F, N Boon, J de Valliers, Verstraete W., & S D Silciliano (2003). Strain- specific ureolytic microbial calcium carbonate precipitation. Applied and environmental Microbiology. 69, 4901-4909. • Okwadha G, J Li (2010). Optimum conditions for microbial carbonate precipitation. Chemosphere. 81, 1143-1148. References Acknowledgement