1996
On the role of colloids in trace metal solid-solution partitioning in continental shelf waters: a comparison of model results and field data
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Cited by 67 publications
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Abstract
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“…The log K OC of THg in the SSF is 7.2 ± 0.3 in the open ocean and 6.6 ± 0.5 in the upwelling region. This is in line with the previous finding of Cui et al that the open ocean generally exhibits higher K d values when compared to the coastal regions ( p -value < 0.05) due to the so-called particle concentration effect where K d displays an inverse relationship with particle mass. , Notably, the upwelling region shows a higher POC concentration ( p -value < 0.05), averaging 28.1 μg/L, compared to the open ocean (7.6 μg/L), showing a concentration gradient that is consistent with the particle concentration effect on K OC values (Figure S1). Additionally, the value of K OC in the SSF is comparable to that in the LSF in both regions (LSF log K OC , upwelling: 6.6 ± 0.4; open ocean: 7.42 ± 0.1) ( t test; P -value > 0.05).…”
Section: Results
supporting
confidence: 91%