Transport Processes in Porous Media by Self-Potential Method

Table 2

Values of diffusion and longitudinal dispersivity calculated using self-potential signals registered at each electrode along the column using a hydrogeophysical inversion approach.

Tracer test	(m^2 s^−1)	(m)
6.00 (kg m^−3)		0.00186	0.986
0.95 (kg m^−3)		0.00128	0.985
0.26 (kg m^−3)		0.00114	0.984