548 Micro-and Nanomanufacturing
approximately a few micrometers in thickness, and is caused by the
use of a high clay content bonding system. High glass content bond-
ing systems tend to aggressively decompose the surface of silicon
carbide abrasive grains. In vitrified corundum grinding wheels, high
glass content bonding systems are used extensively and lead to
bonding layers in excess of one hundred micrometers in thickness.
In addition to the formation of very thin bonding layers in
vitrified silicon carbide grinding wheels, the use of high clay content
bonding systems implies that there is an increase in the amount of
quartz in the bond bridges between abrasive grains. Although the
likelihood of decomposition of silicon carbide surfaces is reduced,
the probability of bond bridge failure is increased due to the in-
creased quartz content. Therefore, the dissolution of quartz is of
paramount importance in order to compensate for thinner interfacial
bonding layers.
The dissolution of quartz in a liquid phase does not require a
nucleation step. One process that determines the rate of the overall
reaction is the phase-boundary reaction rate that is fixed by the
movement of ions across the interface. However, reaction at the
phase boundary leads to an increased concentration at the interface.
Ions must diffuse away from the reaction interface so that the reac-
tion can continue. The rate of material transfer and the diffusion rate
are controlled by molecular diffusion in the presence of a high-
viscosity liquid phase. For a stationary solid in an unstirred liquid,
or in a liquid with no fluid flow produced by hydrodynamic insta-
bilities, the rate of dissolution is governed by molecular diffusion.
The effective diffusion length over which mass is transported
is proportional to ^Dt, where D is the diffusion coefficient and / is
time,
and therefore the change in thickness of the solid, which is
proportional to the mass dissolved, varies with Natural, or free,
convection occurs because of hydrodynamic instabilities in the liq-
uid which gives rise to fluid flow over the solid. This enhances the
kinetics of dissolution. Generally, a partially submerged solid un-
dergoes more dissolution near to the solid-liquid interface. Below
this interface the kinetics of dissolution of the solid can be analyzed
using the principles of free convection.
The boundary layer thickness is determined by the hydrody-
namic conditions of fluid flow. Viscous liquids form much thicker