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Natural Antibacterial Clay Mineralogy~ Medical Geology ~
Clélia Tommi & Dr. Lynda Williams
School of Earth & Space Exploration
Why do Antibacterial Clay Research?
- Overuse of antibiotics around the world
- Proliferation of antimicrobial resistance strains
- Identification of new antibacterial agents
- What makes a natural clay antibacterial?
1
MRSAStaphylococcus
Buruli
First, let’s define what are clays?
Common misconceptions between
CLAY SIZE & CLAY MINERALOGY
Clays are a fine grained particlesize less than 2 µm diameter
The mineralogy of claydeposits is variable but mostly composed of phyllosilicate minerals.
What makes the structure of clays so important?
- Interlayer cations can exchange when hydrated
TETRAHEDRAL
OCTAHEDRAL
TETRAHEDRAL
Interlayer CATIONS
TETRAHEDRAL
OCTAHEDRAL
TETRAHEDRAL
What makes the structure of clays so important?
Electron Microscopy of Clay Minerals
How does clay interact with the bacteria?
- Metals have been used as antimicrobial agentssince antiquity
- Studies indicate that different metals cause discrete and distinct types of cell damage
http://www.nature.com/nrmicro/journal/v11/n6/full/nrmicro3028.html
Experimental Methods
In Vitro Antibacterial Testing
- Bacterial Plate Counting
- Disk Diffusion
Testing clays for their antibacterial properties
Rhodes Clays, North CarolinaOMT Clays, Oregon
Greeney’s Clays, New YorkWalker’s Clays, Nevada
Mineral Analysis
-X-Ray Diffraction
-RockJock Analysis
In Vitro Antibacterial Susceptibility Testing
- Bacterial Plate Counts
Summary of bar graph showing E.coli growth in sample incubated with clay minerals
- Disk Diffusion
In Vitro Antibacterial Susceptibility Testing
Petri dishes showing the zone of inhibition for the OMT clay (24 mm), compared to the
Rhodes clay that is not antibacterial
Petri dishes showing zone of inhibition
- 0 mm Rhodes- 0 mm Greeney- 24 mm OMT- 50 mm Walker
XRD Mineral Analysis
- Random powder X-Ray Diffraction pattern of the Greeney Clays
Sample name: Greeney
Full pattern degree of fit: 0.2121
Mineral Weight %
NON-CLAYS
Quartz 59.0Kspar (ordered Microcline)
3.0
Plagioclase (albite, var. cleavelandite)
8.5
Calcite (Mg-rich) 0.2
Halite 0.0
Gypsum 0.0
Total non-clays 70.8
CLAYS
Smectite (Na-Kinney) 3.9
Illite (1Md) 4.3
Chlorite (Mg; Luzenac) 2.2
Muscovite (2M1) 5.2
Illite (R0; 5%I) 4.3
Total clays 19.9
TOTAL 90.7
XRD Mineral Analysis
Fit With Quartz Walker
Full pattern degree of fit: 0.1974
Mineral Weight %
NON-CLAYS Quartz 10.7Plagioclase (albite, var.) 5.0Plagioclase (oligoclase) 8.8Gypsum 3.7Jarosite (Mex) 9.1 Total non-clays 37.3
CLAYS Kaolinite (disordered) 6.0Smectite (Na-Kinney) 53.3Chlorite (CMM) 3.4Chlorite (Mg; Luzenac) 0.0 Total clays 62.7
TOTAL 100.0
- Random powder X-Ray Diffraction pattern of the Walker Clay
Conclusions
- Antibacterial testing showed that the Rhodes and the Greeney clay are not antibacterial, but the OMT and Walker clay are.
- XRD shows the presence of goethite and anhydrite in the Rhodes and Greeney clay, suggesting oxidation. Other minerals are igneous and metamorphic assemblages.
- The antibacterial clays (OMT and Walker) are hydrothermally altered deposits that contain reduced metals (e.g., pyrite).
- The oxidation state (Eh) and acidity (pH) of the clays equilibrated with water is important to the antibacterial effect.
Questions?
- Disk Diffusion
Thank you!