The initial infiltration capacity in Horton model is higher for wet soil compared to that of L dry soil. 2. Interflow is the flow that reaches a stream from groundwater. T 3. The Thiessen polygon is a descriptive term for the shape of a hyetograph. 4. An increase in the relative humidity decreases evaporation. 5. When a lake is deep then the rate of evaporation decreased. 6. Manning's equation is one of the indirect methods commonly used to determine discharge.

The initial infiltration capacity in Horton model is higher for wet soil compared to that of L dry soil. 2. Interflow is the flow that reaches a stream from groundwater. T 3. The Thiessen polygon is a descriptive term for the shape of a hyetograph. 4. An increase in the relative humidity decreases evaporation. 5. When a lake is deep then the rate of evaporation decreased. 6. Manning's equation is one of the indirect methods commonly used to determine discharge.

Structural Analysis

6th Edition

ISBN:9781337630931

Author:KASSIMALI, Aslam.

Publisher:KASSIMALI, Aslam.

Chapter2: Loads On Structures

Section: Chapter Questions

Problem 1P

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