According to the findings of Hjulström, a velocity of about 10 cm/second is required to maintain transport of grains with diameter of 2 mm. About 50 cm/second are required to start moving a settled grain of that size.
Note that these numbers are dependent on shape and density of the sediment. If styrofoam is your sediment the water doesn't have to flow at all to carry the grains and if you look at little gold nuggets the water has to flow significantly faster to carry the grains. This is one of the reasons why placer deposits form.
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.
Fast moving water can carry more sediment. Firstly because the potential of erosion rises with flow speed; secondly because larger grains can be transported by faster water and thirdly because the volume flow per unit time increases with flow speed. The actual amount / concentration of sediment transported by a stream is very dependent on the geology of the catchment, i.e. the amount of soft sediment available for erosion.
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.
Fast-moving water actually lifts sand and other, smaller sediment and carries it downstream. Water dissolves some sediment completely. Most large sediment falls to the bottom and moves by rolling and sliding.
A fast-moving water carries more sediments because it has more energy to erode and transport particles. Slow-moving water has less energy and is typically not able to carry as much sediment.
Fast moving rivers are capable of carrying larger rock particles than slow moving rivers.
If water is the transport medium of sediment, the grain size of sedimentary deposits most closely indicates the energy of the transporting environment. Larger grains typically suggest higher energy conditions, such as fast-flowing rivers or turbulent waters, while smaller grains indicate lower energy settings, such as calm lakes or deep ocean floors. Additionally, the sorting of sediment grains can provide insights into the distance traveled and the dynamics of the transporting medium.
Factors that affect a river's ability to erode and carry sediment include velocity of the water flow, volume of water, slope of the riverbed, geology of the surrounding area, and the presence of vegetation or obstructions along the river's path. High velocity and volume of water, steep slopes, soft rock formations, and minimal vegetation can increase erosion and sediment transport capacity.
Most rivers with a large sediment load also exhibit fast flow because swift currents are necessary to transport and suspend heavier particles. The increased velocity of the water provides the energy needed to overcome the gravitational pull on the sediment. Additionally, fast-flowing rivers often have steep gradients and turbulent flow conditions, which contribute to their ability to erode and carry sediment efficiently. This dynamic interplay between flow speed and sediment transport is crucial for shaping riverbanks and landscapes.
Fast moving. sediment is heavy it settle out in slow water. But a river that just became slow after being fast looks like it has the most, because of all the settling going on.
High gradient streams have steeper slopes, which means they have more energy and power to transport larger sediment particles. The fast flowing water in high gradient streams can effectively carry and move these large particles due to the force of the water flow.
It is called deposition. It occurs as friction or gravity overcomes the force of the moving water.