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Sediment deposition is less in water tube boilers compared to fire tube boilers because water tube boilers have a higher water velocity that helps prevent sediment from settling on the tubes. Additionally, the design of water tube boilers allows for easier removal of any sediment that does accumulate.

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Where is deposition dominant in a stream?

Deposition is dominant in areas of a stream where the flow rate decreases, such as at the inner bends of a meander or near the mouth of the stream where it enters a larger body of water. In these locations, the stream has less energy to transport sediment, leading to deposition of the sediment it is carrying.


Does deposition occur faster or slower when water currents are slow?

Deposition occurs slower when water currents are slow because there is not enough energy to transport and deposit sediment effectively. Slow-moving water currents have less ability to erode and carry sediments, resulting in a slower rate of deposition.


Why do rivers deposit heavier sediments first and then lighter sediment?

More dense material is less buoyant in water than less dense material of equal volume. Sediment shape also plays a role in deposition sequence as material with angular irregular surfaces are more likely to be carried by water flow than smooth surfaces, due to friction with the water. Finally, the size of the sediment particle, particularly of rock material, may be most critical in the sequence of deposition; larger particles are the first to overcome the power of friction encountered in moving water, via gravity.


Does fast moving water carry less sediment than slow-moving water?

No, fast-moving water typically carries more sediment than slow-moving water because it has more energy to suspend and transport sediments. However, in very fast-flowing water, such as during a flood, sediment may be deposited when the water slows down.


Does fast moving water carry more or less sediment?

Fast moving water carries more sediment because it has more energy to erode and transport sediments from the surface of the earth. As water velocity increases, it can pick up and carry larger and heavier particles along with it.

Related Questions

How does the velocity of water affect deposition?

Water velocity affects deposition by carrying sediment along when it is fast moving, which can prevent sediment from settling and result in less deposition. When water velocity decreases, sediment will settle out of the water column and deposit due to reduced energy to keep it in suspension. High water velocity can also erode deposited sediment.


Where is deposition dominant in a stream?

Deposition is dominant in areas of a stream where the flow rate decreases, such as at the inner bends of a meander or near the mouth of the stream where it enters a larger body of water. In these locations, the stream has less energy to transport sediment, leading to deposition of the sediment it is carrying.


How does the slope of the stream affected erosion and deposition?

A steeper slope in a stream increases the velocity of the water, leading to increased erosion of sediment and rocks. This results in greater transportation of material downstream. Conversely, a gentler slope decreases the velocity of the water, causing less erosion and more deposition of sediment.


Does deposition occur faster or slower when water currents are slow?

Deposition occurs slower when water currents are slow because there is not enough energy to transport and deposit sediment effectively. Slow-moving water currents have less ability to erode and carry sediments, resulting in a slower rate of deposition.


What actions cause the deposition of sand at a delta?

Deposition of sand at a delta can be caused by the decrease in water velocity as a river enters a less energetic environment, such as a lake or ocean. Additionally, if the sediment load carried by the river exceeds its capacity due to factors like floods or high sediment supply, it can lead to deposition of sand at the delta. Finally, the presence of vegetation or obstacles in the river can slow down water flow and result in the deposition of sand.


How does building a dam effect erosion and deposition?

Building a dam can disrupt the natural flow of a river, which can affect erosion and deposition downstream. The reduced water flow can lead to decreased sediment transport, resulting in less material being deposited downstream. On the other hand, sediment buildup behind the dam can increase erosion in the immediate area.


How does a drought affect weathering erosion and deposition?

A drought can lead to decreased vegetation, which can increase weathering and erosion due to less protection from roots and vegetation to stabilize the soil. Additionally, water flow is reduced during a drought, leading to less deposition of sediment in riverbeds and coastal areas. Overall, a drought can intensify weathering and erosion processes while decreasing deposition rates.


Why do sediment settle out of flowing water as it slows down?

Because it has less energy and can carry less sediments.


What factors affect how sediments are deposited and what affect does that have on the surface features that are created?

Factors that affect sediment deposition include water velocity, sediment size, and topography. Sediments are typically deposited in areas with low velocity where energy is minimal, resulting in flat features like floodplains or deltas. In areas with high velocity, sediment is less likely to be deposited, leading to features like channels or steep riverbanks.


How does flood water and low gravity affect erosion and deposition?

Flood water can accelerate erosion by carrying away large amounts of sediment and debris. In low gravity environments, such as on Mars or the Moon, erosion is typically slower due to reduced impact forces of flowing water. Deposition in flood waters is influenced by gravity, with heavier particles settling out first, while in low gravity environments, sedimentation may be less pronounced.


Why do rivers deposit heavier sediments first and then lighter sediment?

More dense material is less buoyant in water than less dense material of equal volume. Sediment shape also plays a role in deposition sequence as material with angular irregular surfaces are more likely to be carried by water flow than smooth surfaces, due to friction with the water. Finally, the size of the sediment particle, particularly of rock material, may be most critical in the sequence of deposition; larger particles are the first to overcome the power of friction encountered in moving water, via gravity.


How does changing the slope of the stream table produce different results?

Changing the slope of the stream table affects the speed and direction of water flow. A steeper slope creates faster water flow, which can result in more erosion and deposition. Conversely, a flatter slope slows down water flow, leading to less erosion and deposition. These changes in flow dynamics can cause differences in the shape and size of channels, as well as the amount and distribution of sediment carried by the water.