Lesson 5 Flashcards

1
Q

Movement of water into the soil under gravity and capillary forces.

A

Infiltration

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2
Q

For excess rate of rainfall, the actual infiltration rate will follow a limiting curve called —————– curve of the soil.

A

infiltration capacity

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3
Q

The hydrologic concept of infiltration capacity is empirically based on observations at the ground surface.

A

Horton Equation.

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4
Q

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.

A

Pi - Index Method.

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5
Q

Developed for small basins

A

SCS Curve Number Method of Estima

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6
Q

Total rainfall P separated into 3 parts:

A

Direct runoff (Excess Rainfall) Pe
–Continuing Loss Fa
–Initial Loss Ia

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7
Q

(AMC)

A

Antecedent Moisture Conditions

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8
Q

low moisture (dry condition)

A

AMC I

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9
Q

average moisture condition (normal condition)

A

AMC II

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10
Q

high moisture, heavy rainfall over preceding few days (wet condition)

A

AMC III -

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