Radioisotopes and coastal research in the Great Barrier Reef

Stieglitz, T.C., Hancock, G., Clarke, J., and Cook, P.G. (2011) Radioisotopes and coastal research in the Great Barrier Reef. In: Abstracts from 11th Australasian Environmental Isotopes Conference and 4th Australasian Hydrogeology Research Conference. pp. 106-107. From: 11th Australasian Environmental Isotopes Conference and 4th Australasian Hydrogeology Research Conference, 12-14 July 2011, Cairns, QLD, Australia.

[img] PDF (Published Version) - Published Version
Download (36kB)
View at Publisher Website: http://www.jcu.edu.au/ees/seminars/JCUPR...
 
53


Abstract

Radioisotopes are efficient tracers of coastal processes on various spatial and temporal scales. The isotopes of radon and radium are particularly useful tools to understand hydrological land-ocean interaction because (a) activities of these isotopes are elevated in groundwater by two to three orders of magnitude in comparison with seawater, and (b) these isotopes have half-lives similar to the time scales of coastal hydrological processes such as river and groundwater discharge to the ocean, as well as coastal ocean mixing (or residence) time.

The application of these isotopes to studies of land-ocean interaction in the central Great Barrier Reef region (Townsville to Cooktown) is illustrated in three recent studies: (1) coastal mapping of radon on a regional scale improves the understanding of the spatial variability of river and groundwater fluxes to the Great Barrier Reef lagoon; (2) quantification of tidal water exchange between mangrove forests and creeks demonstrates the significant contributions this process makes to water flux and associated geochemical fluxes along tropical coastlines; (3) estimates of coastal water residence time contribute to the understanding of the fate of land-derived solutes in the Great Barrier Reef Lagoon.

Concurrent mapping of 222Rn (half-life 3.8 days) and salinity allows an efficient qualitative assessment of land–ocean interaction on various spatial and temporal scales. From shore-parallel transects along the Central Great Barrier Reef coastline with a surface-towed and continuously recording multi-detector system, numerous locations of elevated radon activities can be identified as terrestrially-derived submarine groundwater discharge, riverine sources, and the recirculation of seawater through crustacean burrows in mangrove forests. Variations in the inverse relationship of 222Rn and salinity in different tropical wet seasons reveal ‘timing’ aspects of large-scale freshwater input during the tropical wet season into the lagoon.

Subsequently, 222Rn was used together with radium isotopes to quantify the tidal water exchange between a mangrove forest on Hinchinbrook Island and the ocean. Significant export of these radio-nuclides from the forest into a tidal creek indicates continuous tidally-driven circulation through animal burrows in the forest. The forest floor is efficiently flushed, with water flux of about 30 L m-2 day-1 of forest floor, which is equivalent to about 10% of the total burrow volume in the forest per tidal cycle. This work illustrates the physical process which supports export of organic and inorganic matter from mangrove forests to the coastal zone. Importantly, annual average circulation fluxes through mangrove forest floors are of the same order as annual river discharge in the central GBR.

Finally, an improved understanding of the fate of land-derived waters is of great importance to current discussions about water quality management in the Great Barrier Reef. The mixing of coastal waters is an important parameter influencing the health of these ecosystems. Time constants associated with the decay of four naturally-occurring isotopes of radium span large time scales; 224Ra, 223Ra, 228Ra and 226Ra have half-lives of 4 days, 11 days, 6 years and 1620 years respectively. The radium quartet has been used to determine time scales of mixing of near-shore water and deep ocean water. This study demonstrates that central GBR water within 20 km of the coast is flushed with outer lagoon water on a timescale of 18–45 days, with the flushing time increasing northward. This difference likely reflects the different reef matrix density in the two zones, affecting exchange with offshore Coral Sea water.

Item ID: 21456
Item Type: Conference Item (Abstract / Summary)
Date Deposited: 03 Apr 2012 01:14
FoR Codes: 04 EARTH SCIENCES > 0402 Geochemistry > 040203 Isotope Geochemistry @ 30%
04 EARTH SCIENCES > 0406 Physical Geography and Environmental Geoscience > 040603 Hydrogeology @ 40%
04 EARTH SCIENCES > 0405 Oceanography > 040503 Physical Oceanography @ 30%
SEO Codes: 96 ENVIRONMENT > 9605 Ecosystem Assessment and Management > 960503 Ecosystem Assessment and Management of Coastal and Estuarine Environments @ 50%
96 ENVIRONMENT > 9611 Physical and Chemical Conditions of Water > 961102 Physical and Chemical Conditions of Water in Coastal and Estuarine Environments @ 50%
Downloads: Total: 53
Last 12 Months: 4
More Statistics

Actions (Repository Staff Only)

Item Control Page Item Control Page