T90 Minerals, Microbes, and Health
Monday, 1 November 2010
8:00 AM - 12:00 PM
Room 302
ANTIMICROBIAL CLAY MINERAL DEPOSITS AND FE(II) EXCHANGED SMECTITE
Paper number: T90-8
Program: Technical Sessions
Time: 9:45 AM – 10:00 AM
Authors
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Dennis D. EbrelBoulder, CO
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David W. MetgeNational Research Program, Boulder, CO
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J.C. UnderwoodBoulder, CO
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Lynda B. WilliamsArizona State University, Tempe, AZ
Abstract
Antimicrobial clay minerals were collected from the Oregon Minerals Technology (OMT) mine in Oregon approximately 20 miles east of Crater Lake. The primary rock types in the OMT deposit are dacite and andesite, which have been hydrothermally altered into mixed-layered clay minerals rich in nano-scale pyrite. Samples from OMT along with Fe(II) exchanged smectites produced in the lab were reacted with 400µL of 5x107 CFU/mL E. coli in nutrient broth with 200mg of clay and incubated for 24 hours at 37°C. After incubating 100uL of dilutions ranging from 10-5 to 10-7 were plated on nutrient agar to measure bacterial colony forming units.
Clay samples from some horizons in the deposit are antimicrobial while other horizons promote bacterial growth. Quantitative mineralogy of the OMT samples reveals that the clays consist primarily of rectorite and smectite. Natural clay samples that are antimicrobial contain pyrite while the clay deposits that promoted growth contain hematite and maghemite with no pyrite. Iron exchanged smectites completely prevented the growth of E. coli and provide evidence that soluble Fe(II) adsorbed on clay minerals in addition to pyrite is bactericidal.