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As a particle size gets larger in a stream, the force needed to move the particle in the suspended water column is greater. The velocity dictates which size particles are able to be picked up from the bed and carried as stream load. Some particles, such as fine silts, require very little velocity and can be dissolved on their own without moving water. Larger, coarse rock particles may require extremely high velocities which may only be reached during storm events, depending on the stream of course.
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A fast-moving stream is carrying sand and gravel These particles increase the erosive power of the stream by?
Rubbing against rocks along the stream channel
What is the measure of th largest particles a stream can carry?
The measure of the largest particles that a stream can carry is typically determined by its stream power, bed material size, and flow velocity. Streams with higher stream power and flow velocity are able to transport larger particles. The largest particles a stream can carry before they settle to the streambed are usually referred to as the stream's "bedload" particles.
Which innovation was most important for American industrialization?
stream power
Does a streams slope affect its carrying capacity?
Yes, the steepness of a stream's slope can affect its carrying capacity. Generally, steeper slopes can lead to faster water flow and increased erosional power, allowing the stream to carry more sediment and potentially increase its carrying capacity. However, other factors like channel width, depth, and sediment size also play a significant role in determining the carrying capacity of a stream.
What is carrying power?
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 ability of a stream to reode and transport material depends largely on its?
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.
What is the total sediment load transported by a stream?
The total sediment load transported by a stream is the sum of the bed load, suspended load, and dissolved load. Bed load consists of larger particles that roll, slide, and bounce along the streambed. Suspended load is finer particles carried in the water column, while dissolved load is material that is dissolved in the water itself.
How is velocity related dto power?
velocity like to power becaus velocity related to power.
What factor most influence the power of a stream to erode and transport material?
The power of a stream to erode and transport material is primarily influenced by its velocity. Faster-moving water has greater kinetic energy, allowing it to dislodge and carry larger particles. Additionally, the gradient or slope of the streambed affects velocity; steeper gradients typically result in higher speeds. Other factors, such as water volume and sediment load, also play a role but are secondary to the impact of velocity.
How is power related to force and velocity?
Power is the rate at which work is done or energy is transferred. It is calculated as the product of force and velocity, where power = force x velocity. This means that power increases with both force and velocity.
What is the color of wire carrying 120W of power and 24A of current?
Typically, a wire carrying 120W of power and 24A of current would be a yellow wire, according to standard color-coding for electrical wires. However, it's important to always refer to local regulations or standards for specific color-coding guidelines to ensure safety and compliance.
A river's power to erode depends on?
A river's power to erode depends on its flow velocity, the volume of water it carries, the type and size of sediment it transports, and the slope of the river channel. These factors influence the force and effectiveness of erosion by the river.
