Calculate infiltration rate f = K(1 + ψΔθ/F) using Green-Ampt model. Cumulative infiltration F solved iteratively. Soil parameters from texture class. Used in hydrologic modeling when ponding time matters.
2D stress state at a point. All stresses in MPa.
Calculate infiltration rate f = K(1 + ψΔθ/F) using Green-Ampt model. Cumulative infiltration F solved iteratively. Soil parameters from texture class. Used in hydrologic modeling when ponding time matters
Each component has a specific meaning:
Note: Interpret the green-ampt result against the clinical thresholds and context described above.
Enter the Green-Ampt model for the patient or scenario you are assessing. Calculate infiltration rate f = K(1 + ψΔθ/F) using Green-Ampt model. Cumulative infiltration F solved iteratively. Soil parameters from texture class. Used in hydrologic modeling when ponding time matters. Use the green-ampt result to inform your clinical assessment.