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Updated: Sep 28, 2025

Clean Sampling and Analysis of River and Estuarine Waters for Trace Metal Studies
Published on: July 1, 2016
Performance evaluations and applications of a δ13C-DIC analyzer in seawater and estuarine waters
Xue Deng1, Qian Li2, Jianzhong Su3
1School of Marine Science and Policy, University of Delaware, Newark, DE 19716, USA; Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, PR China; Key Laboratory for Ecological Environment in Coastal Areas (State Oceanic Administration), National Marine Environmental Monitoring Center, Dalian 116023, China.
Abstract:
Dissolved inorganic carbon (DIC) and its stable isotope (δ13C-DIC) are important parameters for studying carbon cycling in aquatic environments. Traditional methods based on isotope-ratio mass spectrometers are labor-intensive and not easily deployable at field sites. Here we report the performance of a method that simultaneously measures DIC concentration and its stable isotope by using a CO2 extraction device and a Cavity Ring-Down Spectroscopy (CRDS) detector. A multi-port valve is used to increase sample throughput and improve precision. The instrument achieves average precisions of better than ±1.95 μmol kg-1 and ±0.06‰, respectively, for DIC and δ13C-DIC in seawater based on three injections for each sample. We also provide recommendations on how to precisely determine δ13C-DIC samples with a wide range of DIC content in different types of waters by examining injection volume and concentration effects. This technique was applied to study carbon cycling in the Delaware Estuary. It demonstrates that a simultaneous and precise determination of both DIC and δ13C-DIC is a powerful and effective approach for constraining the processes controlling aquatic carbon cycling and CO2 fluxes. Both laboratory tests and field applications confirmed that this system can be used with high precision to study carbon cycling in various aquatic environments.

