The flow rate of a river is the volume of water passing through a specific point in the river per unit of time, usually measured in cubic meters per second or cubic feet per second.
The flow rate of a river is directly related to the kinetic energy of the water within it. A higher flow rate means the water is moving faster, which increases its kinetic energy. Conversely, a lower flow rate results in slower-moving water with lower kinetic energy.
In a system, the relationship between pressure and flow rate is described by the pressure vs flow rate equation. This equation shows that as pressure increases, flow rate decreases, and vice versa. This means that there is an inverse relationship between pressure and flow rate in a system.
Mass flow rate is the amount of mass passing through a given point per unit time, while volumetric flow rate is the volume of fluid passing through a given point per unit time. The mass flow rate is calculated by multiplying the volumetric flow rate by the fluid density at that point.
The flow rate in a system is directly related to the size of the pipe. A larger pipe size allows for a higher flow rate, while a smaller pipe size restricts the flow rate. This is because a larger pipe provides more space for the fluid to flow through, reducing resistance and increasing the flow rate. Conversely, a smaller pipe size creates more resistance, limiting the flow rate.
Pressure changes with variations in flow rate in a direct relationship. As flow rate increases, pressure decreases, and as flow rate decreases, pressure increases. This is known as the Bernoulli principle, which states that as fluid velocity increases, its pressure decreases.
I'd like to know, the drought order allowed extra drainage from the river medway below normal flow rate level but how do we find out the actual flow rate?
No; in fact the rate of erosion not only varies from river to river, it depends on the type of rock the river flows over, the rate of flow and the season.
The flow rate of a river is directly related to the kinetic energy of the water within it. A higher flow rate means the water is moving faster, which increases its kinetic energy. Conversely, a lower flow rate results in slower-moving water with lower kinetic energy.
A flow regime of a river is essentially a statistical summary of how flows in a river vary over time. the amount of water and the rate of flowing water a river carries.
The average discharge into the North Sea is 70,629 cubic feet per second
the Mississippi flow rate is dependant on season, weather and observers location. Flow rates for various locations are posted on the bulletin found at the following link: http://www.mvp-wc.usace.army.mil/bulletins/daily_bulletin.shtml
the Mississippi flow rate is dependant on season, weather and observers location. Flow rates for various locations are posted on the bulletin found at the following link: http://www.mvp-wc.usace.army.mil/bulletins/daily_bulletin.shtml
A creek transitions into a river when it reaches a certain size and flow rate, typically determined by the volume of water it carries.
A hydrograph is a graph showing the rate of flow (discharge) versus time past a specific point in a river, or other channel or conduit carrying flow. The rate of flow is typically expressed in cubic meters or cubic feet per second
The flow rate of the river slows precipitously at the mouth of the river, and any carried silt drops to the bottom - where it builds up to form a delta.
The slope of land can affect the rate of deposition in a delta by influencing the speed of the river flow. A steeper slope can lead to faster river flow, carrying more sediment downstream, which can result in increased deposition. Conversely, a gentle slope may slow down river flow, allowing sediment to settle out more easily and potentially decrease deposition rates.
The East River in New York City flows at a rate of four knots or two meters per second. The East River is 16 miles long.