A laboratory simulation of the mixing of coal mine-affected water with Fitzroy Basin river water
Coal mine-affected water (CMAW) releases contribute to the total wet season stream-flow in the Fitzroy River Basin. Using data from the QLD government ‘Fitzroy River’ website, the flow attributable to CMAW releases in the Mackenzie River sub-basin were calculated as 3.75% and 2.1% in the 2012-13 and...
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ftcquniportalfig:oai:figshare.com:article/13386029 2023-05-15T17:09:40+02:00 A laboratory simulation of the mixing of coal mine-affected water with Fitzroy Basin river water Catherine Jones Victoria Vicente-Beckett 2016-01-01T00:00:00Z http://hdl.handle.net/10018/1212111 unknown https://figshare.com/articles/conference_contribution/A_laboratory_simulation_of_the_mixing_of_coal_mine-affected_water_with_Fitzroy_Basin_river_water/13386029 http://hdl.handle.net/10018/1212111 CQUniversity General 1.0 Analytical Chemistry not elsewhere classified Environmental Chemistry (incl. Atmospheric Chemistry) Copper Mixtures Coal mine-affected water releases Fitzroy River Basin Text Conference contribution 2016 ftcquniportalfig 2022-08-05T12:20:53Z Coal mine-affected water (CMAW) releases contribute to the total wet season stream-flow in the Fitzroy River Basin. Using data from the QLD government ‘Fitzroy River’ website, the flow attributable to CMAW releases in the Mackenzie River sub-basin were calculated as 3.75% and 2.1% in the 2012-13 and 2013-14 wet seasons, respectively. This study used laboratory simulation to investigate the changes in copper (Cu) composition in river water when CMAW is released in the Mackenzie sub-basin. CMAW was collected directly from a mine’s on-site holding dam. CMAW from this dam can be released into a Mackenzie River tributary when certain water quality and flow conditions are met. In April 2015 this tributary was dry, so river water was collected further downstream in the main trunk of the Mackenzie River. Changes in water quality were monitored in eight different quantities of CMAW mixed with the river water (range = 0.2-10% CMAW). Electrical conductivity increased linearly with increasing % CMAW, whereas non-linear responses and possible chemical reaction (indicated by curve inflections) were observed for pH, TSS and alkalinity in the 0.4% and 2% mixtures. Two 5L mixtures of 0.4% and 2% CMAW in river water were continually mixed at a constant speed for three days. Nine DGT samplers were placed in each mixture; temperature, EC and pH were monitored daily. A 30-mL aliquot for total dissolved Cu, a 50-mL aliquot for total alkalinity, and three DGT samplers, were removed from each mixture at three time points (24, 48 and 72 h). The suspended particulate matter (SPM) in the initial samples and final mixtures were collected and are being characterised. Total dissolved Cu concentration in the mixtures was compared to the original waters (river water = 2.2 µg/L; CMAW = 0.97 µg/L). At t=0 h the 0.4% mixture had 1.7 µg/L of Cu, while the 2% mixture had 1.9 µg/L. After 24 h both mixtures had 2.1 µg/L. Cu concentration in the 0.4% mixture was 2.0 µg/L at 48 and 72 h. Cu concentration in the 2% mixture at t=48 h dropped to 1.6 µg/L. ... Conference Object Mackenzie river CQUniversity: acquire Fitzroy ENVELOPE(-66.964,-66.964,-68.189,-68.189) Mackenzie River Waters River ENVELOPE(-137.026,-137.026,67.393,67.393) |
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CQUniversity: acquire |
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ftcquniportalfig |
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topic |
Analytical Chemistry not elsewhere classified Environmental Chemistry (incl. Atmospheric Chemistry) Copper Mixtures Coal mine-affected water releases Fitzroy River Basin |
spellingShingle |
Analytical Chemistry not elsewhere classified Environmental Chemistry (incl. Atmospheric Chemistry) Copper Mixtures Coal mine-affected water releases Fitzroy River Basin Catherine Jones Victoria Vicente-Beckett A laboratory simulation of the mixing of coal mine-affected water with Fitzroy Basin river water |
topic_facet |
Analytical Chemistry not elsewhere classified Environmental Chemistry (incl. Atmospheric Chemistry) Copper Mixtures Coal mine-affected water releases Fitzroy River Basin |
description |
Coal mine-affected water (CMAW) releases contribute to the total wet season stream-flow in the Fitzroy River Basin. Using data from the QLD government ‘Fitzroy River’ website, the flow attributable to CMAW releases in the Mackenzie River sub-basin were calculated as 3.75% and 2.1% in the 2012-13 and 2013-14 wet seasons, respectively. This study used laboratory simulation to investigate the changes in copper (Cu) composition in river water when CMAW is released in the Mackenzie sub-basin. CMAW was collected directly from a mine’s on-site holding dam. CMAW from this dam can be released into a Mackenzie River tributary when certain water quality and flow conditions are met. In April 2015 this tributary was dry, so river water was collected further downstream in the main trunk of the Mackenzie River. Changes in water quality were monitored in eight different quantities of CMAW mixed with the river water (range = 0.2-10% CMAW). Electrical conductivity increased linearly with increasing % CMAW, whereas non-linear responses and possible chemical reaction (indicated by curve inflections) were observed for pH, TSS and alkalinity in the 0.4% and 2% mixtures. Two 5L mixtures of 0.4% and 2% CMAW in river water were continually mixed at a constant speed for three days. Nine DGT samplers were placed in each mixture; temperature, EC and pH were monitored daily. A 30-mL aliquot for total dissolved Cu, a 50-mL aliquot for total alkalinity, and three DGT samplers, were removed from each mixture at three time points (24, 48 and 72 h). The suspended particulate matter (SPM) in the initial samples and final mixtures were collected and are being characterised. Total dissolved Cu concentration in the mixtures was compared to the original waters (river water = 2.2 µg/L; CMAW = 0.97 µg/L). At t=0 h the 0.4% mixture had 1.7 µg/L of Cu, while the 2% mixture had 1.9 µg/L. After 24 h both mixtures had 2.1 µg/L. Cu concentration in the 0.4% mixture was 2.0 µg/L at 48 and 72 h. Cu concentration in the 2% mixture at t=48 h dropped to 1.6 µg/L. ... |
format |
Conference Object |
author |
Catherine Jones Victoria Vicente-Beckett |
author_facet |
Catherine Jones Victoria Vicente-Beckett |
author_sort |
Catherine Jones |
title |
A laboratory simulation of the mixing of coal mine-affected water with Fitzroy Basin river water |
title_short |
A laboratory simulation of the mixing of coal mine-affected water with Fitzroy Basin river water |
title_full |
A laboratory simulation of the mixing of coal mine-affected water with Fitzroy Basin river water |
title_fullStr |
A laboratory simulation of the mixing of coal mine-affected water with Fitzroy Basin river water |
title_full_unstemmed |
A laboratory simulation of the mixing of coal mine-affected water with Fitzroy Basin river water |
title_sort |
laboratory simulation of the mixing of coal mine-affected water with fitzroy basin river water |
publishDate |
2016 |
url |
http://hdl.handle.net/10018/1212111 |
long_lat |
ENVELOPE(-66.964,-66.964,-68.189,-68.189) ENVELOPE(-137.026,-137.026,67.393,67.393) |
geographic |
Fitzroy Mackenzie River Waters River |
geographic_facet |
Fitzroy Mackenzie River Waters River |
genre |
Mackenzie river |
genre_facet |
Mackenzie river |
op_relation |
https://figshare.com/articles/conference_contribution/A_laboratory_simulation_of_the_mixing_of_coal_mine-affected_water_with_Fitzroy_Basin_river_water/13386029 http://hdl.handle.net/10018/1212111 |
op_rights |
CQUniversity General 1.0 |
_version_ |
1766065815953604608 |