Silver in the subarctic northeast Pacific Ocean: Explaining the basin scale distribution of silver

被引:17
|
作者
Kramer, Dennis [1 ]
Cullen, Jay T. [1 ]
Christian, James R. [2 ]
Johnson, W. Keith [2 ]
Pedersen, Thomas F. [1 ]
机构
[1] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3P6, Canada
[2] Fisheries & Oceans Canada, Sidney, BC V8L 4B2, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Silver; Marine geochemistry; Trace metal; Biogeochemical cycles; Trace metal macronutrient relationships; ATLANTIC-OCEAN; HAIDA EDDIES; PHYSICAL PROCESSES; NE PACIFIC; JAPAN SEA; TRANSPORT; DEPOSITION; SEDIMENTS; NUTRIENT; IRON;
D O I
10.1016/j.marchem.2010.11.002
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Five vertical profiles of silver (Ag) in the subarctic northeast Pacific are presented. Dissolved (<0.2 mu m) Ag concentrations within the surface mixed layer range from 6-25 pM, with the highest observed values at the most coastal site. Elevated Ag concentrations at this station are most likely attributable to the estuarine circulation in the Juan de Fuca Strait. One open-ocean station (P20) exhibited a strong surface Ag maximum. The station was located at the edge of a Haida eddy which raises the possibility that such eddies transport Ag seaward from the coastal zone. Ag concentrations in the deep waters ranged from 60-80 pM. These measurements are consistent with other recent Ag data collected in the Pacific. Ag profiles throughout the Pacific Ocean yield a strong positive correlation between Ag concentration and dissolved silicic acid concentration. However, Ag is depleted relative to silicic acid at intermediate depths where dissolved O-2 concentrations are low, implying a possible removal of Ag from oxygen-depleted waters by scavenging and/or precipitation. (C) 2010 Elsevier B.V. All rights reserved.
引用
收藏
页码:133 / 142
页数:10
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