T25 The Changing Landscape of Energy Geology (Posters)

Sunday, 15 October 2023
8:00 AM - 5:30 PM
Hall B


INFLUENCE OF GALVANIC DIFFERENCE ON GROUND SUPPORT CORROSION: A CASE STUDY

Paper number: T25-12
Program: Technical Sessions
Time: 8:00 AM – 5:30 PM


Authors

  • Harper Gerfen Presenting Author
    Eastern Illinois University, Charleston, IL

Abstract

Mining is an integral part of our society, whether through processing fine materials into usable goods or assessing land areas for profitable land use. Minerals and metals found within mines are used in all types of machines and fuel operations, keeping the world running smoothly. With the recent push for green energy, minerals such as nickel and copper are in high demand. When extracting these metal resources an underground mine in Michigan observed high rates of corrosion in areas that have little to no interaction with water or atmospheric agents. This corrosion was impacting the integrity of ground support elements, which are meant to secure the surrounding rock and protect the miners from rockfall hazards. To investigate the cause of the corrosion, three samples were taken from the affected area to help determine if there was a galvanic difference between minerals causing the failures in ground support. Scrapings of the rock were subjected to a powder X-ray diffraction (PXRD) device to assess what minerals may be causing this issue. It was found that three types of graphite were present along with various iron oxides and magnetic minerals such as magnetite and Iron (II/III) oxide. The galvanic difference between the graphite variants and steel is about 0.367 volts, just under the accepted threshold of 0.5 volts that is considered safe for use. Therefore, graphite is shown to be a heavy accelerant of corrosion and due to its galvanic difference with steel, would explain the accelerated deterioration rate of surrounding support. Further testing, monitoring, and alternative ground support options are suggested to mitigate corrosion hazards and track corrosion rates in new developments.

Geological Society of America Abstracts with Programs. Vol. 55, No. 6

doi: 10.1130/abs/2023AM-391055

© Copyright 2023 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.