Zero-valent iron for the in situ remediation of Antarctic contaminated sites

© 2015 Dr. Tom M. Statham To successfully remediate contaminated areas in Antarctica and other cold regions there is a requirement to develop suitable heavy metal containment and treatment technologies. Potential contaminant technologies for the remediation of Antarctic contaminated sites were asses...

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Main Author: STATHAM, THOMAS
Format: Doctoral or Postdoctoral Thesis
Language:unknown
Published: 2015
Subjects:
PRB
Online Access:http://hdl.handle.net/11343/51012
id ftumelbourne:oai:jupiter.its.unimelb.edu.au:11343/51012
record_format openpolar
spelling ftumelbourne:oai:jupiter.its.unimelb.edu.au:11343/51012 2023-05-15T13:55:52+02:00 Zero-valent iron for the in situ remediation of Antarctic contaminated sites STATHAM, THOMAS 2015 http://hdl.handle.net/11343/51012 unknown http://hdl.handle.net/11343/51012 permeable reactive barrier PRB mass transfer heavy metal low temperature contamination Wilkes Station ground water remediation PhD thesis 2015 ftumelbourne 2019-10-15T12:11:44Z © 2015 Dr. Tom M. Statham To successfully remediate contaminated areas in Antarctica and other cold regions there is a requirement to develop suitable heavy metal containment and treatment technologies. Potential contaminant technologies for the remediation of Antarctic contaminated sites were assessed and the results indicate that a granular zero-valent iron (ZVI) permeable reactive barrier (PRB) is appropriate for the treatment of heavy metal contamination. This containment and ground/surface water treatment approach could complement either dig-and-haul or stabilisation/fixation remediation methods. A mass transport model was developed that accounts for (i) aqueous-phase dispersion processes, (ii) film diffusion of contaminant ions to the reacting surface and (iii) the reactive mechanism itself. Regression of a series of dynamic flow-kinetic experiments suggest that the removal of Cu2+ and Zn2+ ions would be controlled by mass transfer to a small reacting proportion of the iron oxyhydroxide surface area. Designing water treatment systems with contamination removal based on ZVI requires an understanding of the formation of a series of iron oxyhydroxides produced during corrosion of the thermodynamically unstable ZVI core. X-ray diffractometry (XRD) and geochemical modelling were used to investigate the mechanisms of copper and zinc removal and the formation of iron oxyhydroxides in batch experiments at 4 and 25 °C over 349 days. Copper removal was predominantly associated with a mineral product, which was unstable in an aerobic environment. Zinc and some copper were sequestered into the iron oxyhydroxide structure and did not redissolve when the pH was reduced. When located in a cold region exposed to freeze-thaw cycling, solution-media interactions may be detrimental to PRB performance. A laboratory based simulation of PRB performance was conducted within Darcy Boxes under freeze-thaw conditions. The reactive contaminants, Cu2+ and Zn2+ ions, were removed from the pore water during solution flow and freeze-thaw cycling. The retention time within the reactive media, assessed by a conservative tracer, decreased by 15–18% during the set first freeze-thaw cycling and remained constant then on during the set second freeze-thaw cycling. Agglomeration of particles was observed during an experimental freeze-thaw ZVI PRB simulation. However, there was no significant change in the hydraulic conductivity. The < 212 µm particles produced during the flow of solution and freeze-thaw cycling did not contain concentrated levels of the treated contaminant metals. Based on the laboratory results, a media sequence for the treatment of both hydrocarbon and heavy metal contamination was installed within an existing PRB at Casey Station, Antarctica. Results from two seasons of monitoring indicate that the media achieved a greater chemical phosphorus removal capacity when compared to previous Antarctic PRB designs. However, non-idea flow was observed during the second season. Geophysical studies and an excavator based subsurface site assessment were conducted to continue the development of a conceptual site model for the Wilkes Tip Site, a contaminated site in Antarctica. The potential remediation directions of this site were also discussed. Doctoral or Postdoctoral Thesis Antarc* Antarctic Antarctica The University of Melbourne: Digital Repository Antarctic Casey Station ENVELOPE(110.528,110.528,-66.282,-66.282)
institution Open Polar
collection The University of Melbourne: Digital Repository
op_collection_id ftumelbourne
language unknown
topic permeable reactive barrier
PRB
mass transfer
heavy metal
low temperature
contamination
Wilkes Station
ground water remediation
spellingShingle permeable reactive barrier
PRB
mass transfer
heavy metal
low temperature
contamination
Wilkes Station
ground water remediation
STATHAM, THOMAS
Zero-valent iron for the in situ remediation of Antarctic contaminated sites
topic_facet permeable reactive barrier
PRB
mass transfer
heavy metal
low temperature
contamination
Wilkes Station
ground water remediation
description © 2015 Dr. Tom M. Statham To successfully remediate contaminated areas in Antarctica and other cold regions there is a requirement to develop suitable heavy metal containment and treatment technologies. Potential contaminant technologies for the remediation of Antarctic contaminated sites were assessed and the results indicate that a granular zero-valent iron (ZVI) permeable reactive barrier (PRB) is appropriate for the treatment of heavy metal contamination. This containment and ground/surface water treatment approach could complement either dig-and-haul or stabilisation/fixation remediation methods. A mass transport model was developed that accounts for (i) aqueous-phase dispersion processes, (ii) film diffusion of contaminant ions to the reacting surface and (iii) the reactive mechanism itself. Regression of a series of dynamic flow-kinetic experiments suggest that the removal of Cu2+ and Zn2+ ions would be controlled by mass transfer to a small reacting proportion of the iron oxyhydroxide surface area. Designing water treatment systems with contamination removal based on ZVI requires an understanding of the formation of a series of iron oxyhydroxides produced during corrosion of the thermodynamically unstable ZVI core. X-ray diffractometry (XRD) and geochemical modelling were used to investigate the mechanisms of copper and zinc removal and the formation of iron oxyhydroxides in batch experiments at 4 and 25 °C over 349 days. Copper removal was predominantly associated with a mineral product, which was unstable in an aerobic environment. Zinc and some copper were sequestered into the iron oxyhydroxide structure and did not redissolve when the pH was reduced. When located in a cold region exposed to freeze-thaw cycling, solution-media interactions may be detrimental to PRB performance. A laboratory based simulation of PRB performance was conducted within Darcy Boxes under freeze-thaw conditions. The reactive contaminants, Cu2+ and Zn2+ ions, were removed from the pore water during solution flow and freeze-thaw cycling. The retention time within the reactive media, assessed by a conservative tracer, decreased by 15–18% during the set first freeze-thaw cycling and remained constant then on during the set second freeze-thaw cycling. Agglomeration of particles was observed during an experimental freeze-thaw ZVI PRB simulation. However, there was no significant change in the hydraulic conductivity. The < 212 µm particles produced during the flow of solution and freeze-thaw cycling did not contain concentrated levels of the treated contaminant metals. Based on the laboratory results, a media sequence for the treatment of both hydrocarbon and heavy metal contamination was installed within an existing PRB at Casey Station, Antarctica. Results from two seasons of monitoring indicate that the media achieved a greater chemical phosphorus removal capacity when compared to previous Antarctic PRB designs. However, non-idea flow was observed during the second season. Geophysical studies and an excavator based subsurface site assessment were conducted to continue the development of a conceptual site model for the Wilkes Tip Site, a contaminated site in Antarctica. The potential remediation directions of this site were also discussed.
format Doctoral or Postdoctoral Thesis
author STATHAM, THOMAS
author_facet STATHAM, THOMAS
author_sort STATHAM, THOMAS
title Zero-valent iron for the in situ remediation of Antarctic contaminated sites
title_short Zero-valent iron for the in situ remediation of Antarctic contaminated sites
title_full Zero-valent iron for the in situ remediation of Antarctic contaminated sites
title_fullStr Zero-valent iron for the in situ remediation of Antarctic contaminated sites
title_full_unstemmed Zero-valent iron for the in situ remediation of Antarctic contaminated sites
title_sort zero-valent iron for the in situ remediation of antarctic contaminated sites
publishDate 2015
url http://hdl.handle.net/11343/51012
long_lat ENVELOPE(110.528,110.528,-66.282,-66.282)
geographic Antarctic
Casey Station
geographic_facet Antarctic
Casey Station
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_relation http://hdl.handle.net/11343/51012
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