Author/Authors :
Kobe، نويسنده , , S. and Dra?i?، نويسنده , , G. and McGuiness، نويسنده , , P.J. and Meden، نويسنده , , T. and Sarantopoulou، نويسنده , , E. and Kollia، نويسنده , , Z. and Cefalas، نويسنده , , A.C.، نويسنده ,
Abstract :
The influence of the magnetic field and the water flow on the crystal form of calcium carbonate precipitated from low-concentration water solution was followed systematically. By changing the strength of the field, the calcite/aragonite/vaterite ratio varied. The crystal form and the particle size distribution of the precipitated calcium carbonate were determined by using X-ray analyses and transmission electron microscopy (TEM). A simple hydrodynamical model, using the Navier–Stokeʹs and Maxwellʹs equations, predicts that there is a strong energy coupling and transfer between turbulent flow and the magnetic fields, which can be amplified to high values. Since the formation of aragonite is enhanced in the presence of magnetic field, scaling is prevented in turbulent flow.