The process of measuring the volume of water flowing past a specific point in a river or stream per unit of time (i.e., discharge or flow rate) is known as
stream gauging or streamflow measurement. Stream gauging involves various techniques:
- Direct methods:
- Velocity-area method: Measuring the average flow velocity and the cross-sectional area of flow. Discharge (Q) = Area (A) $\times$ Velocity (V). Velocity can be measured using current meters, ADCPs (Acoustic Doppler Current Profilers).
- Volumetric gauging: Directly measuring the volume of water collected over a period (for very small streams).
- Dilution gauging: Introducing a tracer and measuring its dilution downstream.
- Indirect methods:
- Using hydraulic structures like weirs or flumes where discharge is related to water level through a known formula.
- Using stage-discharge relationships (rating curves) where continuous measurement of water level (stage) is used to estimate discharge.
Option (c)
Stream gauging is the correct term for this process. Other options: Option (a) Rain gauging: The process of measuring the amount of rainfall using rain gauges. Option (b) Infiltration measurement: The process of measuring the rate at which water enters the soil, using instruments like infiltrometers. Option (d) Transpiration monitoring: The process of measuring the amount of water vapor released from plant leaves into the atmosphere, often done using lysimeters or sap flow sensors. \[ \boxed{\text{Stream gauging}} \]