Crustal Imaging and Characterization Team
Mark Stanton
Bacteria participate in or catalyze many geochemical reactions of interest, such as oxidation of certain elements (ferrous iron, sulfur, manganese), reduction of other elements or species (ferric iron, nitrate), and organic carbon oxidation or fixation. Sorption of bacteria to mineral surfaces generally enhances their ability to accomplish a specific reaction.
The objective of the bacterial sorption task is to examine and develop methods to determine the number of bacteria (primarily iron-oxidizers) adsorbed onto sulfide mineral surfaces. Bacterial oxidation of sulfide minerals in mine wastes can lead to production of acid mine drainage (in addition to acidity that is generated by abiotic reactions). Understanding conditions that affect how bacteria attach to these minerals may be useful in mitigating acid drainage.


Left photo: Iron- and sulfur-oxidizing bacteria are generally present in metal-mine waste piles. However, their spatial locations and numbers vary widely within the mine waste pile. Right photo: Surface of a wetland adjacent to a draining mine adit in the San Juan Mountains, southwestern Colorado. The bright color results from the formation of a layer of "iron-accumulating" bacteria known as Leptothrix.
[Large version of mine waste pile photo Large version of wetland photo]
Several methods can be used to determine numbers of bacteria, such as staining used in conjunction with direct microscopic counting, or cultural techniques. The columns shown here comprise one method that is currently being examined.

Mark Stanton
Box 25046 Denver Federal Center MS 964D
Denver, CO 80225-0046
Phone: (303) 236-1924
Email: mstanton
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