The settling rate of the sand particles and the flow velocity of the stream are the two main factors that determine when the sand will settle out of the stream. Higher settling rates and lower flow velocities typically lead to quicker settling of the sand particles.
The velocity of a stream is determined by factors such as the slope or gradient of the stream channel, the volume of water flowing through the stream, the shape and size of the stream channel, and the roughness of the stream bed. These factors collectively influence how fast the water moves downstream.
Two factors that determine an object's velocity are its speed (magnitude of the velocity) and direction of motion. Velocity is a vector quantity that combines both speed and direction.
The velocity of a pebble is typically much slower than the velocity of a stream. Streams can flow at varying speeds depending on factors such as gradient and volume of water, whereas a pebble would most likely only move when influenced by the force of the stream's flow.
An increase in stream velocity can be due to factors such as a steeper gradient, higher discharge, narrower channel width, or decreased channel roughness. These factors can contribute to higher flow velocities in rivers or streams.
Two factors that determine the rate of stream erosion are the velocity of the water and the amount of sediment carried by the stream. Higher velocity and increased sediment load tend to enhance erosion by allowing the stream to transport more material and exert greater cutting force on the streambed.
The settling rate of the sand particles and the flow velocity of the stream are the two main factors that determine when the sand will settle out of the stream. Higher settling rates and lower flow velocities typically lead to quicker settling of the sand particles.
The velocity of a stream is determined by factors such as the slope or gradient of the stream channel, the volume of water flowing through the stream, the shape and size of the stream channel, and the roughness of the stream bed. These factors collectively influence how fast the water moves downstream.
Two factors that determine an object's velocity are its speed (magnitude of the velocity) and direction of motion. Velocity is a vector quantity that combines both speed and direction.
it is an instrument to determine the velocity of flow at required point in a flowing stream.
The velocity of a pebble is typically much slower than the velocity of a stream. Streams can flow at varying speeds depending on factors such as gradient and volume of water, whereas a pebble would most likely only move when influenced by the force of the stream's flow.
An increase in stream velocity can be due to factors such as a steeper gradient, higher discharge, narrower channel width, or decreased channel roughness. These factors can contribute to higher flow velocities in rivers or streams.
mass and velocity
The stream velocity required to carry the smallest boulders is typically around 1 meter per second. This velocity is based on the sediment transport capacity of the stream, which is influenced by factors such as the size and weight of the boulders, as well as the stream's gradient and flow rate.
Stream velocity is the speed at which water flows in a stream or river. It is typically measured in units of distance per time (e.g. meters per second) and can vary based on factors such as gradient, channel shape, and discharge.
The two factors that determine velocity are speed (magnitude of the object's motion) and direction (the path along which the object is moving).
Mass and Velocity