Lesson 5 Flashcards
Movement of water into the soil under gravity and capillary forces.
Infiltration
For excess rate of rainfall, the actual infiltration rate will follow a limiting curve called —————– curve of the soil.
infiltration capacity
The hydrologic concept of infiltration capacity is empirically based on observations at the ground surface.
Horton Equation.
The simplest method of estimating infiltration rate and is calculated by finding the loss difference between gross precipitation and observed surface runoff measured as hydrograph.
Pi - Index Method.
Developed for small basins
SCS Curve Number Method of Estima
Total rainfall P separated into 3 parts:
Direct runoff (Excess Rainfall) Pe
–Continuing Loss Fa
–Initial Loss Ia
(AMC)
Antecedent Moisture Conditions
low moisture (dry condition)
AMC I
average moisture condition (normal condition)
AMC II
high moisture, heavy rainfall over preceding few days (wet condition)
AMC III -