

What is the Meaning of Sedimentation?
Sedimentation can be described as the tendency for the particles which are in suspension to settle out of the fluid content. Here they are entrained and then they come to rest against a specific barrier. This happens due to their own motion through the fluid which is in the response to all the forces that are acting on them. The forces can be because of the gravitational pull, due to the centrifugal caused by acceleration or electromagnetism.
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In terms of geology, sedimentation is generally described as the opposite process of erosion that is the terminal end where the sediment transport. In this sense, it also includes the termination of the transport by the process of saltation or the true bedload transport.
What is the Process of Sedimentation?
Sedimentation is the process that allows the different particles which are in the suspended form in water to settle under the gravitational effect. The particles which settle out from the suspension become the sediment, while in water treatment this is known as sludge. When this thick sediment continues to settle, this is called consolidation. In consolidation, the sediment, or sludge, which is assisted by mechanical means is known as the process of thickening.
Sedimentation for water treatment might be used to reduce the concentration of the particles in suspension before the application of coagulation, in order to reduce the amount of coagulating which the chemicals need, or after the coagulation and, possibly after the flocculation. When the sedimentation is applied after coagulation, this purpose is done mainly to reduce the concentrated number of solids which are in suspension so that the subsequent filtration can function well.
Sedimentation is used as one of the other application methods prior to the process of filtration. While other methods include dissolving in air flotation and some other methods of filtration. The solids-liquid separation processes at times are referred to as clarification processes. While there are different processes of sedimentation like horizontal flow and others which we will discuss in our further section.
Explain Sedimentation
The Method Involved
The simplest sedimentation method is to fill a jar or a tank with water, leave that jar or tank alone, undisturbed for a longer period of time. This will allow the particles to settle and then pour the resulting water into another can. This practice is rarely viable in treating the water for townships hence, sedimentation tanks are operated continuously.
Another simple method of sedimentation is done with the process of rectangular tanks which have a horizontal flow through them. The water with the particles which are in suspension is then introduced at one end of the tank, and then when the water flows to the other end of the tank the settlement of particles in the water occurs here. The aim is simply to settle the particles and to manage the reach of the tank floor before the water is drawn out of the tank at the end. This kind of horizontal flow tank is generally built with a floor that has slopes that are flowing gently down to the inlet end of a hopper. This tank is then fitted with a mechanism that helps to scrape the sediment from the outlet end back to the inlet end and then into the hopper from where the water can be discharged hydraulically. In this design of tanks, attention has to be given to the inlet and the outlet ends to make sure that the water flows from one end to another end as uniformly as possible.
Deposition Definition Science
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A deposition is moreover a geological process where the sediments, soil, rocks get added to a landform or the landmass. The wind, ice, water, and gravity transport previously get weathered into the surface material, which in the kinetic form of energy in the fluid is being deposited and is built up in layers of sediment.
Deposition occurs when the forces responsible for sediment transportation are no longer sufficient to overcome the forces of gravity and the process of friction. This creates a resistance to motion which is known as the null-point hypothesis. This deposition can also be referred to as the build-up of the sediment from the organic derivation of matter or via the chemical process.
Types of Sedimentation Tanks
Horizontal Flow Tanks
They are rectangular in shape which has more length twice their width. This structure is designed as they need to flow more the distance and then to settle all the suspended particles.
Radial Flow Tanks
The section which is via a typical type of radial flow circular tank has the water entering this tank through the inlet pipe which is centrally located and is placed inside the deflector box.
Inclined Settling
The inclined setting device is designed to increase the settling capability of the basin. This design principle majorly utilizes the fact which the depth of a gravity settler has very little bearing on the settling capacity. These are of great importance for settling areas which are 140 square feet in each of the inclined plates.
Ballasted Sedimentation
In this type of sedimentation process, the density difference which occurs between the water and its particles produced in the water for the treatment by the coagulation, flocs, in general, is quite small. For this reason, they settle slowly. The methods of plain sedimentation (which are horizontal, radial, and inclined sedimentation) are then preceded by a slow mixing process known as flocculation.
FAQs on Sedimentation
1. What is sedimentation in simple terms?
Sedimentation is the natural process where particles suspended in a fluid, such as water or air, settle down due to gravity. These particles, called sediment, can include sand, silt, clay, or other solid materials. Over time, they come to rest and accumulate, forming layers. This is a fundamental process in both nature and industrial applications for separating solids from liquids.
2. What are some common real-world examples of sedimentation?
You can see examples of sedimentation all around you. Some common ones include:
- River Deltas: When a river flows into an ocean or lake, its speed decreases, causing the sand and silt it carries to settle and form a delta.
- Muddy Water: If you leave a glass of muddy water undisturbed, the mud particles will slowly settle to the bottom, leaving clearer water on top.
- Rock Formation: Layers of sand and organic matter settling at the bottom of oceans over millions of years lead to the formation of sedimentary rocks like sandstone and limestone.
- Water Treatment Plants: In large tanks, heavy impurities in water are allowed to settle down so they can be removed, which is a key step in purifying water.
3. What is the difference between sedimentation and decantation?
Sedimentation and decantation are two separate but sequential steps used to separate an insoluble solid from a liquid. Sedimentation is the initial step where the heavy, insoluble particles are allowed to settle down at the bottom of the container. Decantation is the subsequent step where the clear liquid is carefully poured off from the top, leaving the settled solid (the sediment) behind.
4. How do factors like particle size and density affect the rate of sedimentation?
The speed of sedimentation is directly influenced by the physical properties of the particles. Heavier and larger particles settle much more quickly than smaller, lighter ones. For instance, gravel in water will settle almost instantly, while fine clay particles can remain suspended for hours or days. Similarly, particles that are denser than the fluid they are in will settle faster. In essence, the greater the size and density, the stronger the pull of gravity on the particle, leading to a faster settling rate.
5. Why is sedimentation a crucial process for the formation of sedimentary rocks?
Sedimentation is the foundational process for creating all sedimentary rocks. It begins when sediments like sand, shells, and pebbles are transported by wind or water and settle in layers, usually at the bottom of lakes and oceans. This laying down of material is called deposition. As more and more layers accumulate, the immense weight from the upper layers puts pressure on the lower layers. This pressure, along with minerals that act like cement, compacts and hardens the loose sediment over millions of years, transforming it into solid sedimentary rock.
6. What is the main application or benefit of sedimentation?
The primary application of sedimentation is the separation of solids from liquids. Its most significant benefit is seen in water and wastewater treatment. By allowing suspended solids like dirt, grit, and other impurities to settle out of the water naturally, this process helps to clarify the water, making it easier to purify in subsequent stages. This greatly reduces the concentration of pollutants and is a cost-effective, large-scale purification method.
7. Are there different types of sedimentation?
Yes, based on the concentration of particles and how they interact, sedimentation is classified into four main types in engineering and environmental science:
- Discrete Settling: Occurs when particles are in low concentration and settle individually without affecting each other.
- Flocculent Settling: Happens when particles clump together to form larger, heavier masses called 'flocs', which then settle more rapidly.
- Hindered Settling: Takes place in higher concentrations where particles are so close they interfere with each other, causing the entire group to settle slowly as a single mass.
- Compression Settling: Occurs at very high concentrations where particles are in physical contact, and settling happens as the weight from above compresses the mass and squeezes out the water.

































