| Northeastern Section (39th Annual) and Southeastern Section (53rd Annual) Joint Meeting (March 25–27, 2004) | |
| Paper No. 58-6 | |
| Presentation Time: 1:00 PM-5:00 PM | ||
ACTION OF A NATURAL BATERIAL CONSORTIA ON ACID MINE DRAINAGE FROM THE KEMPTON MINE COMPLEX: A SMALL COMPONENT OF UNDERSTANDING OF ONE OF THE LARGE COAL MINES IN MARYLAND | ||
|
BOWLES, Graeme C.1, PICCOLI, Philip M.2, LOWER, Steven K.3, and CANDELA, Philip A.2, (1) Department of Geology, Univ of Maryland, Department of Geology, University of Maryland, College Park, MD 20742-4211, gbowles@geotransinc.com, (2) Laboratory for Mineral Deposits Research, Department of Geology, University of Maryland, College Park, MD 20742, (3) Department of Geosciences, The Ohio State University, Columbus, OH 43210-1308 The Kempton Mine operated in western Maryland and northern West Virginia between 1914 and 1950 and primary extraction of the ~60 inch thick Upper Freeport coal bed. Closure of the mine was followed by rapid filling of the complex with groundwater. For over 50 years, water has been flowing primarily from the man shaft and bore hole edifices of the mine, into Laurel Run at the headwaters of the Potomac River. Effluent is being released into the environment at a rate of ~6 million gallons per day, and a pH of ~ 3.45, with a relatively constant ion load. A variety of remediation efforts have been attempted to rectify the problem with variable success. In this study, we have attempted to investigate the influence of microorganisms on acid mine drainage (AMD) generation. To this end, water and sediment samples were collected aseptically from Kempton effluent vents, in addition to a sample from a coal seam. The following information was also collected at the sample sites: temperature, total dissolved solids, dissolved oxygen, pH, sulfate, ferric and ferrous iron.. Water and sediment samples were examined in the laboratory using a microscope and found to contain a variety of motile organisms. These samples were used as an inoculum for nineteen experiments containing a defined base media, 15 mg of crushed pyrite, and addition of ~1 cm pyrite cubes. Products of the experiments were then analyzed for pH, and bacteria-mineral relationships using a FE-SEM. The following results were obtained: 1) well developed biofilms on mineral surfaces that appear to be dominated by polysaccharide polymers, 2) bacterial consortia exhibiting three common morphological forms (cocci, rods, and spirillum), and 3) pH values ranging from 1.0 to 1.5. These observations provide evidence that natural bacterial species from the mine are able to form prolific biofilms in association with sulfide minerals, and that the bacteria play a role in the kinetics and extent to which pyrite is reduced in the production of AMD in the system. | ||
|
Northeastern Section (39th Annual) and Southeastern Section (53rd Annual) Joint Meeting (March 25–27, 2004)
General Information for this Meeting | ||
| Session No. 58--Booth# 52 Undergraduate Research (Posters) II Hilton McLean Tysons Corner: Ballrooms A and B 1:00 PM-5:00 PM, Friday, March 26, 2004 Geological Society of America Abstracts with Programs, Vol. 36, No. 2, p. 125 | ||
© Copyright 2004 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions. | ||