A logarithmic graph would best represent the relationship between stream velocity and the size of particles it can carry downstream. As velocity increases, the stream can carry larger particles due to increased erosion and transport capacity. However, there will be a limit to the size of particles carried downstream as velocity continues to increase.
To prevent particles of 0.01 cm from settling downstream, a minimum stream velocity of 0.02 m/s is required, based on Stokes' law calculations for settling velocity.
In cylindrical coordinates, vorticity is related to the velocity by the curl of the velocity field. The vorticity vector is the curl of the velocity vector, which represents the local rotation of the fluid at a point in the flow.
In calculus, the relationship between velocity and time is represented by the derivative dv/dt. This derivative represents the rate of change of velocity with respect to time. It shows how quickly the velocity of an object is changing at any given moment.
The relationship between acceleration, velocity, and time can be expressed graphically by plotting acceleration on the y-axis, velocity on the x-axis, and time changing over the course of the graph. This can show how changes in acceleration affect velocity over time. The slope of the velocity-time graph represents acceleration.
A stream's velocity typically increases downstream due to the accumulation of water volume and slope gradient. This leads to higher flow rates and faster-moving water.
To prevent particles of 0.01 cm from settling downstream, a minimum stream velocity of 0.02 m/s is required, based on Stokes' law calculations for settling velocity.
Yes, the average sediment size tends to decrease downstream due to the sorting process during transportation. As water flow velocity decreases, it can no longer carry larger particles, leading to their deposition closer to the source. Smaller particles are carried farther downstream before settling due to their lighter weight.
In cylindrical coordinates, vorticity is related to the velocity by the curl of the velocity field. The vorticity vector is the curl of the velocity vector, which represents the local rotation of the fluid at a point in the flow.
In calculus, the relationship between velocity and time is represented by the derivative dv/dt. This derivative represents the rate of change of velocity with respect to time. It shows how quickly the velocity of an object is changing at any given moment.
The relationship between acceleration, velocity, and time can be expressed graphically by plotting acceleration on the y-axis, velocity on the x-axis, and time changing over the course of the graph. This can show how changes in acceleration affect velocity over time. The slope of the velocity-time graph represents acceleration.
It is a direct relationship as the velocity of the water increases , the rate of erosion also increases. As the velocity increases it will pick up larger objects such as boulders and cobble but remember the biggest objects always get deposited first.
A stream's velocity typically increases downstream due to the accumulation of water volume and slope gradient. This leads to higher flow rates and faster-moving water.
Average velocity increases downstream because of the overall flow of the river. As the river moves in the downstream direction, the volume of water increases due to tributaries adding water along the way. This increase in water volume results in a higher average velocity as the same amount of water needs to flow through a larger channel.
In the context of the load-velocity relationship, the relationship between load and velocity is inverse. This means that as the load increases, the velocity at which the load can be moved decreases, and vice versa.
The carrying capacity of a stream is influenced by its discharge and velocity. A higher discharge and velocity typically allow a stream to transport larger sediments and materials downstream, increasing its carrying capacity. Conversely, lower discharge and velocity may limit the stream's ability to carry sediment and materials.
If the boat is moving downstream, you add the speed of the boat with the speed of the river flow. Therefore, the velocity of the boat downstream is 18 km/h. If the boat is moving upstream, you subtract the river flow speed from the boat's speed, so in this case, it would be 12 km/h.
Linear velocity is directly proportional to the radius at which the object is moving and the angular velocity of the object. The equation that represents this relationship is v = rω, where v is the linear velocity, r is the radius, and ω is the angular velocity. As the angular velocity increases, the linear velocity also increases, given the same radius.