Anthropogenic stable cesium in water and sediment of a shallow estuary, St. Louis Bay, Mississippi

Gopal Bera, Kevin M. Yeager, Moo Joon Shim, Alan M. Shiller

Research output: Contribution to journalArticlepeer-review

7 Scopus citations


St. Louis Bay (SLB), Mississippi, is a small, shallow estuary with moderate local residential and industrial development. Dissolved, stable Cs (i.e., 133Cs) was significantly enriched in bay waters (up to 1570nM) as compared to river (<1nM) and ocean waters (2.3nM). A TiO2 refinery, located on the north shore of the bay, is the likely source of the Cs, given that the highest Cs concentrations were found in waters and in surface sediments (up to 49μg/g) near the refinery outfall. This setting presented a unique opportunity to study remobilization of Cs in a shallow estuarine system, where sediment resuspension is frequent. Remobilization (up to ~3 fold increase) of dissolved Cs was observed during sediment resuspension events. A weak correlation between Cs and clay %; strong correlations among Cs, silt % and particulate organic carbon (POC); and simple numerical approaches indicate that desorption from resuspended particulate matter is the likely mechanism of Cs remobilization. Cs-enriched SLB waters can be traced to nearshore Mississippi Sound waters, but not into Mississippi Bight waters further offshore. The findings from this study also suggest that caution needs to be taken when interpreting the radio-cesium distribution in shallow estuarine and coastal systems.

Original languageEnglish
Pages (from-to)32-41
Number of pages10
JournalEstuarine, Coastal and Shelf Science
StatePublished - May 5 2015

Bibliographical note

Publisher Copyright:
© 2015 Elsevier Ltd.


  • Cesium
  • Desorption
  • Sediment resuspension
  • Shallow estuary

ASJC Scopus subject areas

  • Oceanography
  • Aquatic Science


Dive into the research topics of 'Anthropogenic stable cesium in water and sediment of a shallow estuary, St. Louis Bay, Mississippi'. Together they form a unique fingerprint.

Cite this