Long-Term Acid-Generating and Metal Leaching Potential of a Sub-Arctic Oil Shale

Shales are increasingly being exploited for oil and unconventional gas. Exploitation of sub-arctic oil shales requires the creation of gravel pads to elevate workings above the heaving effects of ground ice. These gravel pads can potentially generate acidic leachate, which can enhance the mobility o...

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Published in:Minerals
Main Authors: Kathryn Mumford, Brendan Pitt, Ashley Townsend, Ian Snape, Damian Gore
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2014
Subjects:
pH
Online Access:https://doi.org/10.3390/min4020293
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spelling ftmdpi:oai:mdpi.com:/2075-163X/4/2/293/ 2023-08-20T04:04:06+02:00 Long-Term Acid-Generating and Metal Leaching Potential of a Sub-Arctic Oil Shale Kathryn Mumford Brendan Pitt Ashley Townsend Ian Snape Damian Gore agris 2014-04-14 application/pdf https://doi.org/10.3390/min4020293 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/min4020293 https://creativecommons.org/licenses/by-nc-sa/3.0/ Minerals; Volume 4; Issue 2; Pages: 293-312 acid rock drainage pH oxidation reduction potential metal concentration total reflection X-ray fluorescence spectrometry (TRXRF) Text 2014 ftmdpi https://doi.org/10.3390/min4020293 2023-07-31T20:36:51Z Shales are increasingly being exploited for oil and unconventional gas. Exploitation of sub-arctic oil shales requires the creation of gravel pads to elevate workings above the heaving effects of ground ice. These gravel pads can potentially generate acidic leachate, which can enhance the mobility of metals from the shale. To examine this potential, pyrite-bearing shale originating from sub-Arctic gravel pad sites were subjected to leaching tests for 600 days at initial pH values ranging from 2 to 5, to simulate potential real world conditions. At set times over the 600 day experiment, pH, oxidation reduction potential (ORP), dissolved oxygen and temperature were recorded and small liquid samples withdrawn and analysed for elemental concentrations using total reflection X-ray fluorescence spectrometry (TRXRF). Six of eight shale samples were found to be acid generating, with pH declining and ORP becoming increasingly positive after 100 days. Two of the eight shale samples produced increasingly alkaline leachate conditions with relatively low ORP after 100 days, indicating an inbuilt buffering capacity. By 600 days the buffering capacity of all samples had been consumed and all leachate samples were acidic. TRXRF analyses demonstrated significant potential for the leaching of S, Fe, Ni, Cu, Zn and Mn with greatest concentrations found in reaction vessels with most acidic pH and highest ORP. Text Arctic MDPI Open Access Publishing Arctic Minerals 4 2 293 312
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic acid rock drainage
pH
oxidation reduction potential
metal concentration
total reflection X-ray fluorescence spectrometry (TRXRF)
spellingShingle acid rock drainage
pH
oxidation reduction potential
metal concentration
total reflection X-ray fluorescence spectrometry (TRXRF)
Kathryn Mumford
Brendan Pitt
Ashley Townsend
Ian Snape
Damian Gore
Long-Term Acid-Generating and Metal Leaching Potential of a Sub-Arctic Oil Shale
topic_facet acid rock drainage
pH
oxidation reduction potential
metal concentration
total reflection X-ray fluorescence spectrometry (TRXRF)
description Shales are increasingly being exploited for oil and unconventional gas. Exploitation of sub-arctic oil shales requires the creation of gravel pads to elevate workings above the heaving effects of ground ice. These gravel pads can potentially generate acidic leachate, which can enhance the mobility of metals from the shale. To examine this potential, pyrite-bearing shale originating from sub-Arctic gravel pad sites were subjected to leaching tests for 600 days at initial pH values ranging from 2 to 5, to simulate potential real world conditions. At set times over the 600 day experiment, pH, oxidation reduction potential (ORP), dissolved oxygen and temperature were recorded and small liquid samples withdrawn and analysed for elemental concentrations using total reflection X-ray fluorescence spectrometry (TRXRF). Six of eight shale samples were found to be acid generating, with pH declining and ORP becoming increasingly positive after 100 days. Two of the eight shale samples produced increasingly alkaline leachate conditions with relatively low ORP after 100 days, indicating an inbuilt buffering capacity. By 600 days the buffering capacity of all samples had been consumed and all leachate samples were acidic. TRXRF analyses demonstrated significant potential for the leaching of S, Fe, Ni, Cu, Zn and Mn with greatest concentrations found in reaction vessels with most acidic pH and highest ORP.
format Text
author Kathryn Mumford
Brendan Pitt
Ashley Townsend
Ian Snape
Damian Gore
author_facet Kathryn Mumford
Brendan Pitt
Ashley Townsend
Ian Snape
Damian Gore
author_sort Kathryn Mumford
title Long-Term Acid-Generating and Metal Leaching Potential of a Sub-Arctic Oil Shale
title_short Long-Term Acid-Generating and Metal Leaching Potential of a Sub-Arctic Oil Shale
title_full Long-Term Acid-Generating and Metal Leaching Potential of a Sub-Arctic Oil Shale
title_fullStr Long-Term Acid-Generating and Metal Leaching Potential of a Sub-Arctic Oil Shale
title_full_unstemmed Long-Term Acid-Generating and Metal Leaching Potential of a Sub-Arctic Oil Shale
title_sort long-term acid-generating and metal leaching potential of a sub-arctic oil shale
publisher Multidisciplinary Digital Publishing Institute
publishDate 2014
url https://doi.org/10.3390/min4020293
op_coverage agris
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Minerals; Volume 4; Issue 2; Pages: 293-312
op_relation https://dx.doi.org/10.3390/min4020293
op_rights https://creativecommons.org/licenses/by-nc-sa/3.0/
op_doi https://doi.org/10.3390/min4020293
container_title Minerals
container_volume 4
container_issue 2
container_start_page 293
op_container_end_page 312
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