The soil which can store water and allow a small quantity to flow thro...
Different types of geological formations:
- Aquitard: These are porous but less permeable geological formations from which water cannot flow but instead sieves through it. A good example of aquitard is silty clay material.
- Aquifers: These are porous and permeable geological formations from which sufficient discharge can be extracted. It generally comprises layers of sand and gravel and fractured bedrock.
- Aquiclude: These are porous but impermeable geological formations from which discharge cannot be extracted. A good example of aquiclude is clay.
- Aquifuge: These are neither porous nor permeable geological formations. A good example of it is a massive compact rock.
The soil which can store water and allow a small quantity to flow thro...
Introduction:
In the field of civil engineering, it is important to have a good understanding of the properties and characteristics of soil. One important characteristic of soil is its ability to store and transmit water. Different types of soils have different water storage and transmission capacities. In this context, the soil which can store water and allow a small quantity to flow through it over a long period is called an Aquitard.
Aquitard:
An Aquitard is a type of soil or rock layer that has a relatively low permeability, which means it restricts the flow of water. However, it still has the ability to store water within its pore spaces. Aquitards are typically composed of clay, silt, or compacted fine-grained materials. They have a lower hydraulic conductivity compared to aquifers, which are more porous and allow the easy movement of water.
Properties of Aquitards:
1. Low permeability: Aquitards have a low hydraulic conductivity, which means they have a low ability to transmit water. This is due to the fine-grained nature of the soil or rock particles, which creates small gaps and restricts the flow of water.
2. Water storage capacity: Aquitards have the ability to retain water within their pore spaces. This water storage capacity is important in areas where water availability is limited and can help sustain vegetation and ecosystems over a longer period.
3. Transient flow: While aquitards restrict the flow of water, they still allow a small quantity of water to flow through them over a long period. This is known as transient flow and occurs due to the pressure gradient between the aquifer and the surrounding aquitard. The movement of water through aquitards is much slower compared to aquifers.
Importance of Aquitards:
1. Groundwater protection: Aquitards act as a barrier between aquifers, which are important sources of groundwater, and potential sources of contamination. Their low permeability restricts the movement of pollutants and helps protect the quality of groundwater.
2. Water resource management: Understanding the properties of aquitards is crucial in water resource management. Aquitards can act as natural storage reservoirs, slowly releasing water to adjacent aquifers and maintaining a sustainable water supply over a longer period.
3. Construction considerations: Aquitards play a significant role in civil engineering projects, especially those involving the construction of underground structures. They can affect the stability of excavations and the flow of groundwater, and need to be properly identified and characterized during the design and construction phases.
In conclusion, an Aquitard is a soil or rock layer with low permeability that can store water and allow a small quantity to flow through it over a long period. Aquitards are important in groundwater protection, water resource management, and construction considerations.
To make sure you are not studying endlessly, EduRev has designed Civil Engineering (CE) study material, with Structured Courses, Videos, & Test Series. Plus get personalized analysis, doubt solving and improvement plans to achieve a great score in Civil Engineering (CE).