CALL FOR PROPOSALS:

ORGANIZERS

  • Harvey Thorleifson, Chair
    Minnesota Geological Survey
  • Carrie Jennings, Vice Chair
    Minnesota Geological Survey
  • David Bush, Technical Program Chair
    University of West Georgia
  • Jim Miller, Field Trip Chair
    University of Minnesota Duluth
  • Curtis M. Hudak, Sponsorship Chair
    Foth Infrastructure & Environment, LLC

 

Paper No. 4
Presentation Time: 9:10 AM

A SPATIAL INVESTIGATION OF METAL AND MINERAL ASSOCIATIONS IN THE MARCELLUS SHALE


FORTSON, Lauren A., Department of Geology, University at Buffalo, 411 Cooke Hall, University at Buffalo, Buffalo, NY 14260, BANK, Tracy, Geology, SUNY at Buffalo, 411 Cooke Hall, Buffalo, NY 14260 and YATZOR, Brett, Department of Chemistry, University at Buffalo, 411 Cooke Hall, University at Buffalo, Buffalo, NY 14260, laurenfo@buffalo.edu

In this study, Time-of-Flight Secondary Ion Mass Spectrometry (ToF-SIMS) was used to map the elemental compositions of core and outcrop samples of the Marcellus Shale that were collected from western NY and PA. The elements of primary interest in this study included the metals uranium and chromium as well as oxygen, hydrogen and carbon. 2-D image maps produced from ToF-SIMS analyses were analyzed by ImageJ; a computer-based program that integrates hardware and software for managing, analyzing and displaying data. Six shale samples with total organic content between 3.13 and 8.55 wt% were analyzed. Uranium concentrations ranged from 8.7 to 53.4 ppm and chromium concentrations ranged from 53 to 120 ppm. Preliminary results indicate that chromium (Cr+) has little to no negative correlation to the hydrocarbons present in the samples with correlation coefficients (R) ranging from -0.06 to -0.25. The uranium species identified include UH+, U+, and UO-. UH+ and U+ both show little to no negative or positive relationship with the hydrocarbons in the sample with correlation coefficients ranging from -0.1 to 0.22 and from -0.01 to 0.18, respectively. UO- also shows little to no positive correlation with the hydrocarbons present in the sample with correlation coefficients ranging from 0.02 to 0.23. Correlation of uranium and chromium to clay minerals present in the samples will be explored.
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