Record number :
2253955
Title of article :
Dissolution kinetics of biogenic silica collected from the water column and sediments of three Southern California borderland basins
Author/Authors :
Cheng، نويسنده , , Tao and Hammond، نويسنده , , Douglas E. and Berelson، نويسنده , , William M. and Hering، نويسنده , , Janet G. and Dixit، نويسنده , , Suvasis Dixit، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2009
Pages :
9
From page :
41
To page :
49
Abstract :
Understanding biogenic silica (bSi) dissolution kinetics in margin environments is important in assessing the global silicon cycle, a cycle closely linked to the global carbon cycle. This understanding is also essential to answer the question of whether bSi content in marine sediment is a valid indicator of productivity in the overlying surface ocean. In this study, plankton tow, sediment trap, and sediment samples were collected at sites in three Southern California borderland basins. Batch dissolution experiments with plankton tow and sediment trap materials (conducted in the laboratory at 22 °C) showed linear dissolution kinetics, from which mean dissolution rate constants of 0.05 d− 1 for plankton tow samples and 0.07 d− 1 for sediment trap samples could be calculated. The dissolution rate constants for both types of samples showed seasonal variability but not the same seasonal patterns. Faster dissolution was observed with sediment trap samples collected at 800 m than at 550 m. With sediment multi-core samples, non-linear dissolution kinetics was observed, which complicates the direct comparison of dissolution rates. Nonetheless, dissolution appeared to be slower for the sediments samples than for samples collected from the water column and to decrease with depth in the sediments. Rate constants for surface sediment (0–0.5 cm) were at least 3–5 times less, and sediments at depths > 2 cm had rate constants at least 6–13 times less than those for material sinking to the sediment surface at these sites. Dissolution experiments conducted with Santa Barbara Basin surface sediment samples amended with dissolved aluminum (Al) and San Pedro Basin trap samples amended with enriched detrital materials (obtained by leaching bSi from sediment samples) suggested that dissolution was inhibited by Al and that the sediments from the different basins varied in the extent of Al release.
Keywords :
sediment trap , Detrital material , Sediment multi-core , Plankton tow , Batch dissolution experiments , opal
Journal title :
Marine Chemistry
Journal title :
Marine Chemistry
Serial Year :
2009
Link To Document :
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