sorptioisotermina
Sorptioisotermina is a term used in soil physics and engineering to describe a temperature‑independent measure of moisture movement through porous media. The concept originates from the classical sorption isotherm but extends to capture the rate of water uptake by soil or concrete when the temperature remains constant. It is defined as the derivative of the water content with respect to the hydraulic gradient under isothermal conditions and is typically expressed in units of centimeters squared per hour.
Researchers have applied sorptioisotermina to predict infiltration rates in agricultural lands, to model the drying behavior
Despite its theoretical appeal, the use of sorptioisotermina remains limited to specialized research. Its calculation requires