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The  234 Th– 238 U disequilibrium has been widely used to quantify the sinking flux of particulate organic carbon (POC) out of the upper ocean. However, the influence of the advection on the quantification is poorly understood due to the lack of  in situ  measured physical parameters. Here, a Lagrangian observation was deployed for 39 h to track the variability of  234 Th along with the current on the slope of the northeastern South China Sea (SCS). Contrasting to the general ocean interior,  234 Th showed deficits relative to  238 U in the mesopelagic waters, indicating an enhanced removal of  234 Th. Concurrently, elevated total particulate matter (TPM) and POC contents were observed in the mesopelagic waters, supporting the driving force of the cross-shelf dispersion of re-suspended shelf/slope sediments for the  234 Th removal. The widely used  234 Th-model (ignoring physical processes) produced a much lower sinking flux of POC than the sediment trap-derived POC flux during the same observation, indicating an unneglectable influence of advection and diffusion. By considering the main horizontal advection and vertical diffusion, the  234 Th– 238 U method gave rise to comparable results to sediment trap.  234 Th-derived POC fluxes showed an increased pattern from 300 to 1,000 m, consistent with the more abundant POC where. These results indicated that advection represents an unneglectable process during the quantification of the sinking flux of  234 Th over the slope of the SCS.

frontiers in marine science

Lagrangian Observation of 234Th and Its Application in Constraining the Sinking of Particulate Organic Carbon on the Slope of the Northeastern South China Sea