Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/118184
Type: Thesis
Title: Tracing the groundwater inputs and water-mass mixing in the Coorong lagoons (South Australia) using strontium isotopes
Author: Kell-Duivestein, I.
Issue Date: 2015
School/Discipline: School of Physical Sciences
Abstract: Analysis of elemental concentrations of strontium [Sr] and isotope (87Sr/86Sr ratios) compositions measured in lagoonal waters sampled across the northern and southern parts of the Coorong Lagoon, South Australia are presented. These data are complemented by the analysis of major water inputs into the lagoon, including (i) Southern Ocean seawater, (ii) Murray River water, and (iii) a local groundwater source. Results of this study confirm that these different source endmembers have very distinctive 87Sr/86Sr signatures, which in turn allow quantification of their relative contributions to the water balance of the Coorong. Importantly, data confirms that at certain parts of the Coorong Lagoon (e.g., near Noonameena through Parnka Point) the magnitude of submarine groundwater discharge can be significant in localized areas, and by using 87Sr/86Sr a tracer along with bimodal isotope mixing equations, local contributions of these endmembers were able to be quantified. Specifically, results indicate that at these sites up to 38% of strontium in the North lagoon waters and up to 64% of strontium in the South lagoon waters originates from groundwater discharge, with the remaining part primarily derived from seawater. With the use of a further mass balance equation which also takes into account the Sr concentrations of the seawater and groundwater it was determined that the isotope signatures within the North Lagoon reflect groundwater inputs by volume of up to 80% in localized areas. In this contribution, we will discuss these new isotope and geochemical data within the context of the bimodal mixing processes, along with an observed initial decrease in the salinity of lagoonal waters observed in the northern parts of the Coorong before rapidly increasing to hypersaline waters further south through Parnka Channel and within the South Lagoon.
Dissertation Note: Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2015
Where: Coorong, South Australia
Keywords: Honours; Geology; Coorong; salinity; submarine groundwater discharge (SGD); strontium isotopes; hyperbolic mixing; bimodal mixing
Description: This item is only available electronically.
Provenance: This electronic version is made publicly available by the University of Adelaide in accordance with its open access policy for student theses. Copyright in this thesis remains with the author. This thesis may incorporate third party material which has been used by the author pursuant to Fair Dealing exceptions. If you are the author of this thesis and do not wish it to be made publicly available, or you are the owner of any included third party copyright material you wish to be removed from this electronic version, please complete the take down form located at: http://www.adelaide.edu.au/legals
Appears in Collections:School of Physical Sciences

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