Estimation of submarine groundwater discharge into Geographe Bay, Bunbury, Western Australia

A study of the submarine groundwater discharge (SGD) into Geographe Bay between Bunbury and Dunsborough in the south west of Western Australia has been carried out under the CSIRO Wealth from Oceans Flagship program. The study focused on establishing a conceptual understanding of SGD and its indirec...

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Published in:Journal of Geochemical Exploration
Main Authors: Varma, Sunil, Turner, Jeffrey, Underschultz, Jim
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier BV 2010
Subjects:
Online Access:https://espace.library.uq.edu.au/view/UQ:318734
id ftunivqespace:oai:espace.library.uq.edu.au:UQ:318734
record_format openpolar
institution Open Polar
collection The University of Queensland: UQ eSpace
op_collection_id ftunivqespace
language English
topic Submarine groundwater discharge
Numerical modeling
Satellite imagery
Southern Perth Basin
Australia
1905 Economic Geology
1906 Geochemistry and Petrology
spellingShingle Submarine groundwater discharge
Numerical modeling
Satellite imagery
Southern Perth Basin
Australia
1905 Economic Geology
1906 Geochemistry and Petrology
Varma, Sunil
Turner, Jeffrey
Underschultz, Jim
Estimation of submarine groundwater discharge into Geographe Bay, Bunbury, Western Australia
topic_facet Submarine groundwater discharge
Numerical modeling
Satellite imagery
Southern Perth Basin
Australia
1905 Economic Geology
1906 Geochemistry and Petrology
description A study of the submarine groundwater discharge (SGD) into Geographe Bay between Bunbury and Dunsborough in the south west of Western Australia has been carried out under the CSIRO Wealth from Oceans Flagship program. The study focused on establishing a conceptual understanding of SGD and its indirect quantification using hydrogeological (hydraulic) and modeling techniques. Satellite infrared images and near shore bathymetry were used to obtain evidence of the possible geographic distribution of significant SGD. The study area forms an offshore part of the Southern Perth Basin. Past studies have shown that there is substantial groundwater flow within the Superficial, Leederville and South West Yarragadee aquifers of the Southern Perth Basin in the offshore direction. The groundwater from these aquifers must ultimately discharge offshore at the seabed into Geographe Bay in the north and the Southern Ocean in the south. Some discharge also takes place onshore via rivers and drains.The results of the study show that groundwater discharge into Geographe Bay from the Superficial Aquifer between Bunbury and Busselton is 240-284m/day/km of the 67km long coastline. The offshore groundwater flow from the Leederville Aquifer along the 55km length of the coast where the aquifer occurs is estimated at 270m/d/km of the coastline. The offshore flow from the South West Yarragadee Aquifer is at the rate of 3360m/d/km of the Geographe Bay coastline. The large flow rates in the South West Yarragadee Aquifer are due to substantial downward leakage from the overlying Leederville Aquifer as well as significant recharge from rainfall in the outcropping areas. The total offshore groundwater discharge to Geographe Bay from all aquifers is estimated to be around 80million m/year on the basis of hydraulic assessment and the modeling results. Remotely sensed infrared images were analysed to detect evidence of any submarine groundwater discharge. The seasonal temperature contrast between the groundwater discharge at the seabed and the seawater makes it theoretically possible to detect areas of significant offshore groundwater seepage using suitable thermal images. ASTER thermal-infrared satellite images were acquired and analysed for this study. The ASTER images showed a low-temperature plume (21°C) in the southwest of the study area near Dunsborough Fault, possibly groundwater discharge, extending in an easterly direction and being surrounded by seawater of about 23°C. Similar cooler zones were observed along the coastline indicating groundwater discharge from the Superficial Aquifer. Following a hypothesis that former onshore coastal groundwater discharge features are likely to continue to be SGD focus areas following marine transgression, the near shore bathymetry for Geographe Bay revealed a series of ridges and troughs running sub-parallel to the present-day beach. The hillshade rendition shows a sub-parallel trough feature located about 4-5km offshore.The bathymetric features identified offshore and the low-temperature plume as observed in the satellite images provide indicators and target areas for more detailed investigation and actual measurement of SGD fluxes, for example by CTD (Conductivity, Temperature and Depth) and SSS (side-scan sonar) probing around target bathymetric features. In the interim, this study has provided valuable information about the rate of potential groundwater seepage from the Southern Perth Basin aquifers into Geographe Bay indicating the scale of possible offshore groundwater resource availability based on SGD recovery and management.
format Article in Journal/Newspaper
author Varma, Sunil
Turner, Jeffrey
Underschultz, Jim
author_facet Varma, Sunil
Turner, Jeffrey
Underschultz, Jim
author_sort Varma, Sunil
title Estimation of submarine groundwater discharge into Geographe Bay, Bunbury, Western Australia
title_short Estimation of submarine groundwater discharge into Geographe Bay, Bunbury, Western Australia
title_full Estimation of submarine groundwater discharge into Geographe Bay, Bunbury, Western Australia
title_fullStr Estimation of submarine groundwater discharge into Geographe Bay, Bunbury, Western Australia
title_full_unstemmed Estimation of submarine groundwater discharge into Geographe Bay, Bunbury, Western Australia
title_sort estimation of submarine groundwater discharge into geographe bay, bunbury, western australia
publisher Elsevier BV
publishDate 2010
url https://espace.library.uq.edu.au/view/UQ:318734
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_relation doi:10.1016/j.gexplo.2010.02.003
issn:0375-6742
orcid:0000-0003-2151-1478
op_doi https://doi.org/10.1016/j.gexplo.2010.02.003
container_title Journal of Geochemical Exploration
container_volume 106
container_issue 1-3
container_start_page 197
op_container_end_page 210
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spelling ftunivqespace:oai:espace.library.uq.edu.au:UQ:318734 2023-05-15T18:26:05+02:00 Estimation of submarine groundwater discharge into Geographe Bay, Bunbury, Western Australia Varma, Sunil Turner, Jeffrey Underschultz, Jim 2010-07-01 https://espace.library.uq.edu.au/view/UQ:318734 eng eng Elsevier BV doi:10.1016/j.gexplo.2010.02.003 issn:0375-6742 orcid:0000-0003-2151-1478 Submarine groundwater discharge Numerical modeling Satellite imagery Southern Perth Basin Australia 1905 Economic Geology 1906 Geochemistry and Petrology Journal Article 2010 ftunivqespace https://doi.org/10.1016/j.gexplo.2010.02.003 2020-09-14T23:58:02Z A study of the submarine groundwater discharge (SGD) into Geographe Bay between Bunbury and Dunsborough in the south west of Western Australia has been carried out under the CSIRO Wealth from Oceans Flagship program. The study focused on establishing a conceptual understanding of SGD and its indirect quantification using hydrogeological (hydraulic) and modeling techniques. Satellite infrared images and near shore bathymetry were used to obtain evidence of the possible geographic distribution of significant SGD. The study area forms an offshore part of the Southern Perth Basin. Past studies have shown that there is substantial groundwater flow within the Superficial, Leederville and South West Yarragadee aquifers of the Southern Perth Basin in the offshore direction. The groundwater from these aquifers must ultimately discharge offshore at the seabed into Geographe Bay in the north and the Southern Ocean in the south. Some discharge also takes place onshore via rivers and drains.The results of the study show that groundwater discharge into Geographe Bay from the Superficial Aquifer between Bunbury and Busselton is 240-284m/day/km of the 67km long coastline. The offshore groundwater flow from the Leederville Aquifer along the 55km length of the coast where the aquifer occurs is estimated at 270m/d/km of the coastline. The offshore flow from the South West Yarragadee Aquifer is at the rate of 3360m/d/km of the Geographe Bay coastline. The large flow rates in the South West Yarragadee Aquifer are due to substantial downward leakage from the overlying Leederville Aquifer as well as significant recharge from rainfall in the outcropping areas. The total offshore groundwater discharge to Geographe Bay from all aquifers is estimated to be around 80million m/year on the basis of hydraulic assessment and the modeling results. Remotely sensed infrared images were analysed to detect evidence of any submarine groundwater discharge. The seasonal temperature contrast between the groundwater discharge at the seabed and the seawater makes it theoretically possible to detect areas of significant offshore groundwater seepage using suitable thermal images. ASTER thermal-infrared satellite images were acquired and analysed for this study. The ASTER images showed a low-temperature plume (21°C) in the southwest of the study area near Dunsborough Fault, possibly groundwater discharge, extending in an easterly direction and being surrounded by seawater of about 23°C. Similar cooler zones were observed along the coastline indicating groundwater discharge from the Superficial Aquifer. Following a hypothesis that former onshore coastal groundwater discharge features are likely to continue to be SGD focus areas following marine transgression, the near shore bathymetry for Geographe Bay revealed a series of ridges and troughs running sub-parallel to the present-day beach. The hillshade rendition shows a sub-parallel trough feature located about 4-5km offshore.The bathymetric features identified offshore and the low-temperature plume as observed in the satellite images provide indicators and target areas for more detailed investigation and actual measurement of SGD fluxes, for example by CTD (Conductivity, Temperature and Depth) and SSS (side-scan sonar) probing around target bathymetric features. In the interim, this study has provided valuable information about the rate of potential groundwater seepage from the Southern Perth Basin aquifers into Geographe Bay indicating the scale of possible offshore groundwater resource availability based on SGD recovery and management. Article in Journal/Newspaper Southern Ocean The University of Queensland: UQ eSpace Southern Ocean Journal of Geochemical Exploration 106 1-3 197 210