Journal of Radioanalytical and Nuclear Chemistry

, Volume 283, Issue 3, pp 593–596

Intertidal mangrove mudflat 240+239Pu signatures, confirming a 210Pb geochronology on the southeastern coast of Brazil

  • C. J. Sanders
  • J. M. Smoak
  • L. M. Sanders
  • M. N. Waters
  • S. R. Patchineelam
  • M. E. Ketterer
Article

DOI: 10.1007/s10967-009-0418-7

Cite this article as:
Sanders, C.J., Smoak, J.M., Sanders, L.M. et al. J Radioanal Nucl Chem (2010) 283: 593. doi:10.1007/s10967-009-0418-7

Abstract

A sediment core was taken to determine if sediment accumulation rates could be conducted using 240+239Pu signatures in the coastal mangrove mudflats of southeastern Brazil. The results from this study show that 240+239Pu fallout activities are sufficient and well preserved in the coastal sediments of this region. Sediment accumulation rates determined from the 240+239Pu signatures were 4.4 mm/year and 4.1 from 210Pb (CIC) method. A sediment mixing coefficient rate was calculated using chlorophyll-a profile (9.5 cm2).

Keywords

240+239Pu 210Pb 226Ra Brazil 

Copyright information

© Akadémiai Kiadó, Budapest, Hungary 2009

Authors and Affiliations

  • C. J. Sanders
    • 1
  • J. M. Smoak
    • 2
  • L. M. Sanders
    • 2
  • M. N. Waters
    • 3
  • S. R. Patchineelam
    • 1
  • M. E. Ketterer
    • 4
  1. 1.Departamento de GeoquímicaUniversidade Federal de Fluminense (UFF)NiteróiBrazil
  2. 2.Environmental ScienceUniversity of South Florida (USF)St. PetersburgUSA
  3. 3.Natural SciencesShorter CollegeRomeUSA
  4. 4.Department of Chemistry and BiochemistryNorthern Arizona UniversityFlagstaffUSA

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