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Pressure is influenced by many other factors, temperature and density for example... Also the height is a factor (atmospheric pressure)
Particles settle at the mouth of a river when the river water mixes with the calmer ocean water, causing a decrease in flow velocity. This reduction in velocity leads to sediment settling as the river's capacity to transport particles decreases. Additionally, the ocean's higher salinity can also play a role in causing sediment particles to settle due to changes in water density.
The amount of sediments a river can carry is influenced by factors such as the river's velocity, volume of water, slope of the river bed, sediment particle size, and the presence of vegetation or structures that can trap sediments. Increased velocity and water volume typically result in higher sediment transport capacity.
The mouth of a river is where the river flows into another body of water, such as an ocean, sea, lake, or another river. It is typically wider than the rest of the river and marks the end of the river's journey. At the mouth, the velocity of the river's flow decreases, leading to sediment deposition.
A good sign that the velocity of running water has changed at a certain point in a river is the presence of ripples or turbulence on the surface, visible debris moving faster or slower than the surrounding water, or a change in the color or clarity of the water. These external indicators can help identify areas of differing flow velocities.
The velocity of water changes with depth due to variations in pressure and friction. Near the surface, water velocity is typically faster due to less friction, while deeper in the water column, velocity may decrease due to increased pressure from the weight of the water above. This change in velocity with depth is also influenced by factors such as the slope of the river or ocean floor and the density of the water.
You can calculate the velocity of water in a channel using the formula v = Q/A, where v is the velocity, Q is the flow rate of water, and A is the cross-sectional area of the channel through which the water is flowing. By knowing the flow rate and the cross-sectional area of the channel, you can determine the velocity of water.
To find the magnitude of the velocity vcr of the canoe relative to the river, you can use vector addition. Add the velocity of the canoe with respect to the water (vcw) to the velocity of the water with respect to the river (vwr). The formula is vcr vcw vwr.
These obstacles causes friction between water and rocks.This ultimately reduces the velocity of river water.The more roughness of the channel, the less the river`s velocity.
velocity
Increasing the gradient or slope of the river bed is most likely to increase the velocity of a river. This change allows water to flow more rapidly downhill, resulting in higher velocity.
Particles settle at the mouth of a river when the river water mixes with the calmer ocean water, causing a decrease in flow velocity. This reduction in velocity leads to sediment settling as the river's capacity to transport particles decreases. Additionally, the ocean's higher salinity can also play a role in causing sediment particles to settle due to changes in water density.
Because the velocity of the river water decreases as it enters the ocean.
Because the velocity of the river water decreases as it enters the ocean.
The velocity of a river is the speed at which the water in the river is flowing in a particular direction. It is typically measured in meters per second or feet per second. Velocity can vary at different points along a river depending on factors such as stream gradient, channel width, and flow volume.
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.
Velocity refers to the speed of water flow in a river, typically measured in meters per second. Volume, on the other hand, refers to the amount of water passing through a given point in the river over a period of time, usually measured in cubic meters per second. In essence, velocity is the speed of the water flow, while volume is the quantity of water flowing through a specific section of the river.
because pools are standing water.