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234Th sorption and export models in the water column: a review
Savoye, N.; Benitez-Nelson, C.R.; Burd, A.B.; Cochran, J.K.; Charette, M.; Buesseler, K.O.; Jackson, G.A.; Roy-Barman, M.; Schmidt, S.; Elskens, M. (2006). 234Th sorption and export models in the water column: a review. Mar. Chem. 100(3-4): 234-249.
In: Marine Chemistry. Elsevier: Amsterdam. ISSN 0304-4203, more
Peer reviewed article  

Available in Authors 
    VLIZ: Open Repository 103915 [ OMA ]

Author keywords
    234<; sup>Th; model; scavenging; export; particle dynamics

Authors  Top 
  • Savoye, N., more
  • Benitez-Nelson, C.R.
  • Burd, A.B.
  • Cochran, J.K.
  • Charette, M.
  • Buesseler, K.O.
  • Jackson, G.A.
  • Roy-Barman, M.
  • Schmidt, S.
  • Elskens, M., more

    Over the past few decades, the radioisotope pair of 238U / 234Th has been widely and increasingly used to describe particle dynamics and particle export fluxes in a variety of aquatic systems. The present paper is one of five review articles dedicated to 234Th. It is focused on the models associated with 234Th whereas the companion papers (same issue) are focused on present and future methodologies and techniques (Rutgers van der Loeff et al.), C / 234Th ratios (Buesseler et al.), 234Th speciation (Santschi et al.) and present and future applications of 234Th [Waples, J.T., Benitez-Nelson, C.R., Savoye, N., Rutgers van der Loeff, M., Baskaran, M., Gustafsson, Ö., this issue. An Introduction to the application and future use of 234Th in aquatic systems. Marine Chemistry, FATE special issue]. In this paper, we review current 234Th scavenging models and discuss the relative importance of the non-steady state and physical terms associated with the most commonly used model to estimate 234Th flux. Based on this discussion we recommend that for future work the use of models should be accompanied by a discussion of the effect that model and data uncertainty have on the model results. We also suggest that future field work incorporate repeat occupations of sample sites on time scales of 1-4 weeks in order to evaluate steady state versus non-steady state estimates of 234Th export, especially during high flux events (> ca. 800 dpm m-2 d-1). Finally, knowledge of the physical oceanography of the study area is essential, particularly in ocean margins and in areas of established upwelling (e.g., Equatorial Pacific). These suggestions will greatly enhance the application of 234Th as a tracer of particle dynamics and flux in more complicated regimes.

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