This study demonstrates a simple laboratory method to measure diffusion coe
fficients of reactive and nonreactive solutes in rock blocks. A demonstrati
ve diffusion measurement device consists of a small plastic cell with magne
tic stirrers, the porous rock block to be measured, and nonreactive tracer
solution. Concentrations of the tracer (as specific conductance) are measur
ed in the cell continuously with data recorded using a PC. The specific con
ductance versus time data are fitted to an analytical solution that is nume
rically inverted to estimate the diffusion coefficient. Mathematical develo
pment is demonstrated, and a sensitivity analysis shows that diffusion coef
ficient as low as 10(-9) cm(2)/s can be measured over a test period of 12 d
ays.