Titlebook: Biomineralization and Biological Metal Accumulation; Biological and Geolo P. Westbroek,E. W. Jong Book 1983 D. Reidel Publishing Company, D

hallow

https://doi.org/10.1007/978-3-662-04416-2 element in the milieu (cf. De With, 1977). This ability is mainly attributed to the activity of a buffer system capable to remove excess Ca from the haemolymph or to release it in case of shortage. The involved deposits of Ca, mostly in the form of CaCO., are found in the shell and the soft body pa

Magisterial

,Application to Navier—Stokes Equations,tion method has been used to study the kinetics of crystallization in which the activities of ionic species in the supersaturated solutions are maintained constant by the potentiometrically controlled addition of reagents. For calcite, the rate of reaction is proportional to the square of the supers

beta-carotene

租約

Flustered

intertwine

978-94-009-7946-8D. Reidel Publishing Company, Dordrecht, Holland 1983

吊胃口

,Application to Navier—Stokes Equations,Calcium serves at least two very significant and distinct functions in Biology—one as a structural component, the other in information transfer. We are seeking unifying principles or a general conceptual framework within which we can study these phenomena. The following observations should be relevant.

緩和

ALLEY

Discretisation of the LES Models,The balance organs, Otoconia and Otoliths, of the inner ear are of interest as the only carbonitic calcified tissue of vertebrates (1). The otoconia are small and may be aragonitic or calcitic; the larger otoliths are aragonitic and grow as the fish ages (2).

manifestation