Southern Cross GeoScience Research
Acid sulfate soils
East Trinity: a national demonstration site for innovative acid sulfate soil management
The aim of this site is to trial and assess the efficacy of innovative hydrogeochemical control methods and risk assessment methods on acid sulfate contaminant remediation on a field scale in a nationally-significant location.
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Improved laboratory test for the acid neutralising capacity of acid sulfate soils
Current methods for determining the acid neutralising capacity (ANC) of acid sulfate soils lead to an overestimation of the lime requirement for neutralisation.
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Coastal Floodplain Hydrology and Biogeochemistry
Estuarine water quality
The impact of coastal floodplain drainage systems on estuarine water quality is a significant resource management issue. The water quality of many coastal estuaries in eastern Australia is periodically degraded via acidification and deoxygenation.
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Hydrology, biogeochemistry and management of drained coastal acid sulfate soil backswamps in the lower Clarence River floodplain
Drainage systems on coastal floodplains have greatly increased the rate of acidity entering creeks and estuaries from acid sulfate soils.
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Impacts of climate change on coastal floodplain wetland biogeochemistry and surface water quality
There is broad community concern about global warming, climate change and rising sea-levels.
More about the impacts of climate change
"Chevrons" - Enigmatic littoral deposits
Chevrons are enigmatic yet understudied lancet-formed sandy sedimentary structures deposited at many coastlines of the world with lengths up to many tens of km and altitudes up to more than 200 m. This current project studies the coastlines of southern Brazil and central Chile.
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Arsenic mobility in re-flooded soils
Southern Cross GeoScience's research aims to understand the geochemical processes controlling arsenic mobility in re-flooded soils. In particular the interactions between arsenic and minerals that are common in such soils (e.g. schwertmannite).
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Iron-monosulfide formation and oxidation in acid-sulfate soils
Poor water quality in acid sulfate soil (ASS) landscapes is a widely recognised international problem. Research and management over the past three decades have focused largely on pyrite oxidation and the release of acid-sulfate leachate into floodplain waterways.
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Iron sulfide formation and element mobility in sulfidogenic environments
Understanding the formation of iron sulfides and the mobility of elements, particularly iron and arsenic, is an important aspect of managing wetland soils, benthic sediments and groundwater systems. This is a rapidly expanding area of research within Southern Cross GeoScience, supported by a 5-year Australian Research Council Project.
More about iron sulfide formation and element mobility
Schwertmannite stability in wetland soils
A research stream within Southern Cross GeoScience aims at understanding the stability of schwertmannite in acid-sulfate soil environments. Schwertmannite is a ferric-oxyhydroxysulfate mineral that forms in acidic, iron- and sulfate-rich waters.
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Biogeochemical processes in coastal wetlands are highly dynamic. They involve complex interactions between hydrology, vegetation communities, mineralogical transformations and the cycling of redox sensitive elements.
More about wetland biogeochemistry
Fluvial Geomorphology and Riverine Processes
Fluvial geomorphology and riverine processes
Fluvial depositional sequences such as alluvial floodplains and terraces are significant features in the geomorphic development of inland channel systems.
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Restoring hydrological connectivity of surface and ground waters: biogeochemical processes and environmental benefits
This project examines the restoration of lateral hydrological connectivity to improve floodplain structure and function.
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Geochronology and Archaeogeochemistry
A multidisciplinary approach to the study of stone tool economics and trade routes in the Brunswick River Valley, NSW
Research examines both coastal and upland archaeological sites, stone raw material procurement and artefact typology in the Tweed and Byron Shires of northern New South Wales (NSW).
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A new timeline for Human evolution and migration
To understand human evolution, archaeologists require precise chronologies so as to compare and contrast fossil collections. To minimise the impact of direct dating on valuable and oftentimes fragile archaeological samples, new methods and protocols for non-destructive U-Th and ESR analyses are being developed and investigated.
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Developing reliable chronologies for extinct Australian Pleistocene megafauna from museum fossil collections
Recently developed direct dating methods, particularly high-throughput MC-ICP-MS U-series dating, are used to produce reliable chronological datasets for extinct megafauna, based on fossils held in museum collections.
More about developing reliable chronologies for extinct Australian Pleistocene megafauna
Pleistocene archaeology and paleoenvironments of the Lake Victoria basin in Kenya
Lake Victoria is the largest body of water in Africa and is surrounded by a diverse mosaic of forest and grassland habitats. This dynamic environment provides the context for highly variable but still poorly documented archaeological and paleontological records of the Lake Victoria basin.
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Reconstruction of exchange and trade routes of the peri-Mediterranean obsidian archaeological assemblages
Obsidian, a volcanic glass, is a particularly well-suited tool for understanding past trade and travel networks. Each obsidian flow has a unique geochemical 'fingerprint', which allows each artefact to be traced back to its geological source and initial archaeological collection region. While most analysis techniques allow the characterisation of the main obsidian sources, some artefacts provenance remain problematic, requiring more enhanced methods.
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South American Pre-Hispanic culture (Peru): Detailed archaeogeochemical analyses of the Mochica pottery
The study focuses on improving our understanding of the fabrication technic, the material provenance and the use of raw material of the Mochica ceramic. The four sites San Josť de Moro, Dos Cabezas, Pacatnamu and Charcape are located in the lower part of the Jequetepeque Valley (Peru).
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Trace element and isotope analyses in fossil teeth: reconstructing the past with biomarkers
In the paper published by Nature in 2013, we show that these early life dietary transitions are recorded in teeth and remain stable in fossil remains from thousands of years ago. Using special analytical chemistry and microscopy techniques we are able to trace changes in the element content of teeth with precision timing.
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Terrestrial Carbon Sequestration
Long-term terrestrial carbon sequestration using phytolith occluded carbon
Atmospheric CO2 concentrations are considered to underlie dangerous climate change. This project examines the ability of plants to contribute to the long-term sequestration of carbon by the production of carbon occluding phytoliths.
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Updated: 04 November 2013