permeability
The ease with which water flows through the open spaces in a rock or sediment indicates the permeability of the rock or sediment. Permeability refers to the ability of fluids to flow through the rock or sediment. A more permeable rock or sediment will have higher porosity and allow for better fluid flow.
Streams lose their ability to carry sediment primarily due to a decrease in water flow velocity, which can occur in low-gradient areas or during periods of low rainfall. When the flow slows down, sediment settles at the bottom, leading to sedimentation and the formation of bars or islands. Additionally, vegetation growth and human interventions, such as dam construction, can further reduce sediment transport by stabilizing the riverbed and altering the natural flow dynamics. Ultimately, these changes can impact the river's ecosystem and its ability to shape the landscape.
There are actually three processes that move sediment, all involving a fluid: flowing water, blowing wind (air is a fluid), and ice movement by glaciers (also a fluid). The viscosity of the fluid determines what size of particle will be moved. Because of its low viscosity, wind will only move clay to sand size particles. Glacial ice, on the other hand, has a very high viscosity and can move house-size rocks. The particle sizes moved by water falls in between the extremes of wind and glaciers.
Increasing the size of sediment generally leads to higher permeability because larger particles create larger pore spaces between them, allowing water or air to flow more freely. However, if the sediment size becomes too large relative to the fluid's viscosity, the flow can become less efficient due to reduced surface area for interaction. Additionally, larger sediment can lead to the formation of larger voids, which may allow for more rapid drainage of fluids. Overall, while larger sediment sizes tend to enhance permeability, various factors such as sediment arrangement and fluid properties also play significant roles.
True. When a river slows down, it loses its ability to carry large sediment particles, so it deposits them first. Smaller particles settle later as the energy of the river decreases further.
The ease with which water flows through the open spaces in a rock or sediment indicates the permeability of the rock or sediment. Permeability refers to the ability of fluids to flow through the rock or sediment. A more permeable rock or sediment will have higher porosity and allow for better fluid flow.
Centrifugation is the process of separating two immiscible liquids. The fluid which is above the sediment after centrifugation, is called the supernatant.
A river delta is formed from the deposition of sediments carried by a river as the river enters an ocean, sea, lake, or another river. This is because the flow velocity decreases significantly and the fluid loses the ability to transport sediment.
When sediment collects in an area, it is called sedimentation. This process occurs when particles settle out of a fluid and accumulate on a surface, forming layers of sediment over time.
One of the definitions of 'fluid' is that the product has the ability to flow and the ability to take on the shape of a container. Ketchup is therefore a fluid
The fluid above the sediment after centrifugation is called the supernatant.
When water slows down, it loses its ability to transport sediment. As a result, the sediment will settle out of the water and accumulate on the riverbed or seafloor. This process is known as sedimentation.
looseness of sediment, speed of wave, angle of wae on sediment, angle of beach floor (as that changes the waves suction angle height and strength)
The speed at which particles of sediment fall through a still fluid is influenced by factors such as the size and density of the particles, as well as the viscosity of the fluid. This settling velocity can be calculated using Stokes' law, which takes into account these factors to determine the terminal velocity of the particles.
Ripples are caused by the flow of fluid (liquid or gas) over sediment.
Rob A. Kleijwegt has written: 'On sediment transport in circular sewers with non-cohesive deposits' -- subject(s): Sediment transport, Fluid dynamics, Sewerage
A mudflow is a mixture of sediment and water that moves down hill in a fluid manner.