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When the discharge of a stream increases, so does it's velocity. When it decreases, so does the velocity.
The rate of stream discharge is directly related to erosion and deposition. A higher rate of discharge can increase erosion by carrying more sediment downstream. Conversely, a decrease in discharge can lead to deposition of sediment as the stream's capacity to transport sediment diminishes. Overall, stream discharge plays a crucial role in shaping the landscape through erosion and deposition processes.
When water loses its ability to hold sediment due to a decrease in velocity or capacity, it deposits the sediments it was carrying. This process is called sedimentation, and it can result in the formation of sedimentary layers over time.
The ability of a stream to erode and transport material largely depends on its velocity, gradient, and discharge. Streams with higher velocities, steeper gradients, and greater discharge have more erosive power and are better able to transport sediment.
Deltas are formed by the deposition of sediment carried by rivers as they enter an ocean or lake. The primary factors responsible for delta formation are the decrease in water velocity as the river enters a body of water and the reduction in sediment-carrying capacity due to the decrease in energy.
The carrying capacity of a stream is influenced by its discharge and velocity. Higher discharge and faster velocity can increase the stream's ability to transport sediment and debris, thus raising its carrying capacity. Conversely, lower discharge and slower velocity may result in a reduced carrying capacity as the stream has less energy to move material.
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.
The carrying capacity of a stream refers to its ability to transport sediment. Higher discharge and velocity typically increase a stream's carrying capacity as they provide more energy to move sediment. However, if the stream's carrying capacity surpasses its available sediment, deposition can occur.
When the discharge of a stream increases, so does it's velocity. When it decreases, so does the velocity.
The higher the velocity of the stream the larger carrying capacity it has.
the competence and capacity of a steam depend on a streams velocity and discharge. Because the velocity and discharge of a given stream are not constant , the competence and capacity of a stream are not constant . competence and capacity vary along a stream and change throughout the year.
The rate of stream discharge is directly related to erosion and deposition. A higher rate of discharge can increase erosion by carrying more sediment downstream. Conversely, a decrease in discharge can lead to deposition of sediment as the stream's capacity to transport sediment diminishes. Overall, stream discharge plays a crucial role in shaping the landscape through erosion and deposition processes.
Seepage velocity is the rate at which water moves through soil or rock, typically due to a pressure gradient. Discharge velocity refers to the flow velocity of water in a channel or conduit, such as a river or pipe. Seepage velocity is generally slower than discharge velocity due to the porous nature of the material through which water is moving.
When a stream's discharge increases, erosive energy increases.
Carrying power refers to a person's ability to influence or persuade others. It is the capacity to carry weight or significance in a particular situation, such as having authority or credibility in a discussion or decision-making process.
The relationship between water velocity and the rate of erosion is direct. Higher water velocity can increase the rate of erosion by carrying more sediment and debris, which can wear away the surface of land or rock more rapidly. Slower water velocity, on the other hand, may result in less erosion as it carries less sediment.
i think it is width X depth X velocity=discharge ?