METER SATURO User Manual

22
SYSTEM
The hydraulic conductivity is then multiplied by the difference in quasi-steady state
infiltration rate for the last pressure cycle and divided by the difference in the measured
pressure head from the last pressure cycle.
Equation 4 is equivalent to Equation 41 from Reynolds and Elrick (1990) and removes the
dependence on soil characteristics and initial water content described by λ.

METER SATURO Specifications

General

Brand	METER
Model	SATURO
Category	Measuring Instruments
Language	English