Data

Data for: First continuous shipboard δ18O and δD measurements in sea water by diffusion sampling: cavity ring-down spectrometry

James Cook University
Munksgaard, Niels ; Bird, Michael ; Wurster, Chris ; Bass, Adrian
Viewed: [[ro.stat.viewed]] Cited: [[ro.stat.cited]] Accessed: [[ro.stat.accessed]]
ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=https://research.jcu.edu.au/data/published/649aab97faaf634d679f0e9f8be6d14b&rft.title=Data for: First continuous shipboard δ18O and δD measurements in sea water by diffusion sampling: cavity ring-down spectrometry&rft.identifier=https://research.jcu.edu.au/data/published/649aab97faaf634d679f0e9f8be6d14b&rft.publisher=James Cook University&rft.description=Combined measurements of salinity and the oxygen/hydrogen stable isotope composition of marine waters can characterise processes such as freshwater mixing, evaporation, precipitation and sea-ice formation. However, stable isotope data with high spatial and temporal resolution are necessary for a detailed understanding of mixed water bodies with multiple inputs. So far analysis of δ18O and δD values in water has been a relatively expensive, laboratory-based technique requiring collection of discrete samples. This has greatly limited the scope and scale of field research that can be undertaken using stable isotope analysis. Here, we report the first continuous shipboard measurements of δ18O and δD values in water by diffusion sampling-cavity ring-down spectrometry. Combined with continuous salinity recordings, a data set of nearly 6,000 measurements was made at 30-s intervals during a 3-day voyage through the Great Barrier Reef Lagoon. Our results show that continuous shipboard measurement of δ18O/δD values provides additional discriminatory power for assessing water mass formation processes and histories. Precise identification of river plumes within the Great Barrier Reef Lagoon was only possible because unique δ18O/δD–salinity relationships of individual plumes were measured at high spatial and temporal resolution. The main advantage of this new technique is the ability to collect continuous, real-time isotope data at a small fraction of the cost of traditional isotope analysis of discrete samples. Water δ18O and δD values measured by diffusion sampling-cavity ring-down spectrometry and laboratory-based isotope ratio mass spectrometry have similar accuracy and precision.Data is in excel (xls) spreadsheet format.&rft.creator=Munksgaard, Niels &rft.creator=Bird, Michael &rft.creator=Wurster, Chris &rft.creator=Bass, Adrian &rft.date=2012&rft.relation=http://dx.doi.org/10.1007/s10311-012-0371-5&rft.relation=http://dx.doi.org/10.1002/rcm.5282&rft.relation=http://dx.doi.org/10.1002/hyp.9505&rft.coverage=146.738914685,-19.1305209297 145.881981091,-17.062968503 146.013817029,-17.0209528135 146.914695935,-19.1512788295 146.738914685,-19.1305209297&rft.coverage=Great Barrier Reef, Townsville-Cairns section, North Queensland, Australia&rft_rights=&rft_subject=shipboard&rft_subject=oxygen isotopes&rft_subject=marine&rft_subject=hydrogen isotopes&rft_subject=salinity&rft_subject=cavity ring-down spectrometry&rft_subject=river&rft_subject=Great Barrier Reef lagoon&rft_subject=stable isotopes&rft_subject=water mass formation&rft_subject=plume&rft.type=dataset&rft.language=English Access the data

Access:

Open view details

Open: free access under license

Brief description

Data is in excel (xls) spreadsheet format.

Full description

Combined measurements of salinity and the oxygen/hydrogen stable isotope composition of marine waters can characterise processes such as freshwater mixing, evaporation, precipitation and sea-ice formation. However, stable isotope data with high spatial and temporal resolution are necessary for a detailed understanding of mixed water bodies with multiple inputs. So far analysis of δ18O and δD values in water has been a relatively expensive, laboratory-based technique requiring collection of discrete samples. This has greatly limited the scope and scale of field research that can be undertaken using stable isotope analysis. Here, we report the first continuous shipboard measurements of δ18O and δD values in water by diffusion sampling-cavity ring-down spectrometry. Combined with continuous salinity recordings, a data set of nearly 6,000 measurements was made at 30-s intervals during a 3-day voyage through the Great Barrier Reef Lagoon. Our results show that continuous shipboard measurement of δ18O/δD values provides additional discriminatory power for assessing water mass formation processes and histories. Precise identification of river plumes within the Great Barrier Reef Lagoon was only possible because unique δ18O/δD–salinity relationships of individual plumes were measured at high spatial and temporal resolution. The main advantage of this new technique is the ability to collect continuous, real-time isotope data at a small fraction of the cost of traditional isotope analysis of discrete samples. Water δ18O and δD values measured by diffusion sampling-cavity ring-down spectrometry and laboratory-based isotope ratio mass spectrometry have similar accuracy and precision.

Notes

Diffusion sampling - cavity ring-down spectrometry is a new technique for measuring real time δ18O and δD isotopes in sea water.

Created: 2012-11-21

Data time period: 04 2011 to 2013

This dataset is part of a larger collection

146.73891,-19.13052 145.88198,-17.06297 146.01382,-17.02095 146.9147,-19.15128 146.73891,-19.13052

146.398338513,-18.0861158215

text: Great Barrier Reef, Townsville-Cairns section, North Queensland, Australia

Subjects

User Contributed Tags    

Login to tag this record with meaningful keywords to make it easier to discover

Identifiers
  • Local : 51570a9f1a64da3fb1f983f147620bc1
  • Local : jcu.edu.au/tdh/collection/42b58145-502f-4434-94e2-b344f2a0f256
  • Local : https://research.jcu.edu.au/data/published/649aab97faaf634d679f0e9f8be6d14b