Dissolution of biogenic silica (BSi) in coastal environments is important for marine productivity. Understanding this process is central to assessing the global silicon cycle, which is closely linked to the global carbon cycle. BSi dissolution experiments were conducted to explore factors influencing this process, and to better understand the regeneration of silicic acid in Jiaozhou Bay sediments. The results showed that the BSi content in sediments varied from 0.44% to 2.73% (average, 1.90%). The horizontal distribution of BSi was slightly greater in the north of the bay than in the south, and was similar to the distributions of Chl-a and phytoplankton abundance. Experiments conducted under continuous flow conditions showed that the dissolution kinetics of BSi was non-linear; based on these data the mean solubility of BSi was calculated to be 277μM-Si for sediment samples, 297μM-Si for sediment trap samples and 559μM-Si for diatom–sediment mixture. The dissolution rate constant for BSi in surface sediments varied from 1.7 to 6.8yr−1. The highest rate was found for tidal flat sediments, and the lowest rate was found in the mouth of the bay; these values for sediment material are higher than those reported for sediments from the Arabian, Scotia and Norwegian seas. For the sediment trap samples the dissolution rate constant ranged from 1.5 to 3.0yr−1, and showed no obvious variation among the different sampling periods. Structural incorporation of trace aluminum to the BSi surface, and the specific surface area and the reactivity of BSi affected both the solubility and dissolution dynamics of BSi in Jiaozhou Bay sediment. BSi dissolution in the water column and sediment appears to be the key process that sustains diatoms as the dominant phytoplankton species in Jiaozhou Bay.
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