submerged flow उदाहरण वाक्य
उदाहरण वाक्य
- In natural stream applications, submerged flow is frequently the result of vegetative growth on the downstream channel banks, sedimentation, or subsidence of the flume.
- Submerged Flow when the water surface downstream of the flume is high enough to restrict flow through a flume, the flume is deemed to be submerged.
- Although commonly thought of as occurring at higher flow rates, It should be noted that submerged flow can exist at any flow level as it is a function of downstream conditions.
- When the downstream depth is high enough that the transition to subcritical flow advances upstream into the throat and the hydraulic jump disappears, the flume is operating in a " submerged flow " regime, and the discharge is instead given by
- Where submerged flow is or may become present, there are several methods of correcting the situation : the flume may be raised above the channel floor, the downstream channel may be modified, or a different flume type may be used ( typically a Parshall flume ).
- It is important to note that the secondary point of measurement ( Hb ) for a Parshall flume is located in the throat, measuring Hb can be difficult as flow in the throat of the flume is turbulent and prone to fluctuations in the water level . 90 % is viewed as the upper limit for which corrections for submerged flow are practical.
- Using the Parshall Flume flow equations and Tables 1-3, determine the flow type ( free flow or submerged flow ) and discharge for a 36 inch flume with an upstream depth, Ha of 1.5 ft and a downstream depth, H b of 1.4 ft . For reference of locations H a and H b, refer to Figure 1.