2013
DOI: 10.1007/s10967-013-2561-4
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Sedimentation and lateral transport of 210Pb over the East China Sea Shelf

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Cited by 8 publications
(3 citation statements)
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“…The sediment environments of the ECS are highly heterogeneous ( Dang et al, 2008 ; Fang et al, 2013 ); this characteristic has a strong influence on the spatial heterogeneity of the sediment microbial communities in the ECS, as observed in previous studies ( Dang et al, 2008 ; Feng et al, 2009 ; Chen et al, 2014 ; Ye et al, 2016 ). Based on the sediment grain size combined with the overlying water masses, the ECS can be divided into three domains: the inner shelf mud area, the outer shelf sand area, and the slope plus Okinawa Trough mud area ( Liu et al, 2006 ; Xu et al, 2016 ).…”
Section: Discussionsupporting
confidence: 56%
“…The sediment environments of the ECS are highly heterogeneous ( Dang et al, 2008 ; Fang et al, 2013 ); this characteristic has a strong influence on the spatial heterogeneity of the sediment microbial communities in the ECS, as observed in previous studies ( Dang et al, 2008 ; Feng et al, 2009 ; Chen et al, 2014 ; Ye et al, 2016 ). Based on the sediment grain size combined with the overlying water masses, the ECS can be divided into three domains: the inner shelf mud area, the outer shelf sand area, and the slope plus Okinawa Trough mud area ( Liu et al, 2006 ; Xu et al, 2016 ).…”
Section: Discussionsupporting
confidence: 56%
“…According to Stokes' Law, for particles with a median size of5.5μm (as forFFJ103), the corresponding average deposition rate is 0.65 m/day, and therefore the residence time of the particles in the water column at FFJ103 is about 100 days. This is consistent with results obtained from 210 Pb and 210 Po (Nozaki et al, 1991;Fang et al, 2013). We estimated that POP losses from the water column at FFJ103 were 46% HCHs, 40% DDTs, 36% PCBs, 17% 8PBDEs and 17% BDE-209, respectively (Figure 5).…”
Section: Spatial Variation Between Pops and Bc/toc Inventories And Th...supporting
confidence: 91%
“…In contrast, scavenging tends to enhance inventories only for 210 Pb ex in marine systems because 210 Pb ex binds rapidly and almost irreversibly to suspended particles in saline water, which then settle to the seafloor (cf. Fang et al 2013), whereas dissolved 137 Cs does not (Oguri et al 2012).…”
Section: Indications Of Riverine Inputs Focusing and Boundary Scavementioning
confidence: 94%