The experimental and mechanistic approaches available for the study of the
kinetics of in vitro biogenic silica dissolution are synthesised to provide
rigorous guidance for future investigation. Batch and flow-through reactor
s are discussed, as are the four mechanisms which have been proposed previo
usly within the marine domain. In recognition of success with similar probl
ems in mineral weathering and hydrometallurgy, the applicability of the Act
ivated Complex Theory is also considered. Full mathematical derivations are
presented for the mechanisms before they are evaluated according to contem
porary needs. At each stage the problems inherent in fitting mathematical m
odels to experimental data are highlighted. The decrease in reaction rate w
ith time observed in batch reactors is discussed in terms of both the appro
ach towards saturation and decrease in surface area of the dissolving frust
ules. In appreciating this distinction, optimum combinations of experimenta
l design are suggested for mimicking silica dissolution in either the water
column or sediment. The role of organic frustule components, micro-organis
ms and faecal pellets in the dissolution process are discussed. (C) 2001 El
sevier Science Ltd. All rights reserved.