Question:

Which type of aquifer is more prone to contamination?

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  • Unconfined aquifers are directly connected to the surface through the unsaturated zone. Contaminants from the surface can easily infiltrate and reach the water table.
  • Confined aquifers are protected by an overlying impermeable layer, making them less susceptible to direct surface contamination.
  • Artesian aquifers are a type of confined aquifer.
  • Perched aquifers can also be vulnerable due to their shallow nature, but unconfined aquifers are generally considered most prone on a broader scale.
Updated On: June 02, 2025
  • Unconfined Aquifer
  • Confined Aquifer
  • Artesian Aquifer
  • Perched Aquifer
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The Correct Option is A

Solution and Explanation

The susceptibility of an aquifer to contamination from surface sources depends largely on its hydrogeological setting, particularly the presence or absence of protective overlying layers.
  • Unconfined Aquifer (Water Table Aquifer) (option a): An unconfined aquifer has its upper surface (the water table) directly open to the atmosphere through the unsaturated zone (vadose zone). Contaminants released at or near the ground surface can readily infiltrate through the soil and unsaturated zone and reach the water table, directly contaminating the aquifer. There is no overlying impermeable layer to protect it. Therefore, unconfined aquifers are generally more prone to contamination from surface activities.
  • Confined Aquifer (option b): A confined aquifer is overlain by an impermeable or very low permeability layer (aquitard or aquiclude). This confining layer acts as a protective barrier, restricting the downward movement of contaminants from the surface. Contamination of a confined aquifer usually occurs more slowly, perhaps through poorly constructed or abandoned wells that penetrate the confining layer, or through slow leakage through the aquitard, or in recharge areas where the aquifer may be unconfined.
  • Artesian Aquifer (option c): An artesian aquifer is simply a confined aquifer in which the water is under sufficient pressure to rise above the top of the aquifer in a well (and may even flow freely at the surface). Its susceptibility to contamination is similar to that of any confined aquifer – generally less prone than unconfined aquifers due to the overlying confining layer.
  • Perched Aquifer (option d): A perched aquifer is a localized zone of saturation above the main regional water table, formed due to an underlying lens of impermeable material. Being relatively shallow and often small in extent, perched aquifers can be quite vulnerable to surface contamination if the contaminants reach their limited recharge area. However, compared to a large regional unconfined aquifer, their overall significance might be less, but their vulnerability is high.
Considering the general types, unconfined aquifers are the most directly and widely vulnerable to contamination originating from the land surface because they lack a protective overlying impermeable layer. \[ \boxed{\text{Unconfined Aquifer}} \]
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