Based on realistic mechanisms of Ca2+ buffering that include both stat
ionary and mobile buffers, we derive and investigate models of Ca2+ di
ffusion in the presence of rapid buffers. We obtain a single transport
equation for Ca2+ that contains the effects caused by both stationary
and mobile buffers. For stationary buffers alone, we obtain an expres
sion for the effective diffusion constant of Ca2+ that depends on loca
l Ca2+ concentrations. Mobile buffers, such as fura-2, BAPTA, or small
endogenous proteins, give rise to a transport equation that is no lon
ger strictly diffusive. Calculations are presented to show that these
effects can modify greatly the manner and rate at which Ca2+ diffuses
in cells, and we compare these results with recent measurements by All
britton et al. (1992). As a prelude to work on Ca2+ waves, we use a si
mplified version of our model of the activation and inhibition of the
IP3 receptor Ca2+ channel in the ER membrane to illustrate the way in
which Ca2+ buffering can affect both the amplitude and existence of Ca
2+ oscillations.