The adsorption properties of sinking particulate matter in the deep subtropical Atlantic Ocean are modeled by combining the field observations of trace metal scavenging with theoretical surface chemistry. The treatment yields equilibrium constants that define metal interactions with deep-ocean particles. These equilibrium constants can be compared with those that define metal interactions with typical metal oxides and organic compounds. The comparison indicates that metal-particulate matter interactions closely resemble the interactions between organic compounds and metals. Therefore, it is suggested that the adsorption properties of marine particulate matter are controlled by organic coatings. In addition, quantifying the surface properties of deep-ocean particles provides a means for estimating the scavenging residence times for metals for which the determination has not yet been made.
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