P. Unconfined aquifer - 3. Water Table aquifer
An unconfined aquifer is a water-bearing stratum where the upper water surface (the water
table) is at atmospheric pressure. Because its upper boundary is the water table, it is
commonly called a water table aquifer.
Q. Confined aquifer - 4. Artesian aquifer
A confined aquifer is sandwiched between two impermeable layers, keeping the water inside
under pressure greater than atmospheric pressure. When a well penetrates this layer, water
rises above the aquifer level, which is why it is called an artesian aquifer.
R. Aquitard - 1. Insignificant yield
An aquitard is a saturated, poorly permeable geological formation (like sandy clay). While it
can store water and allow slow seepage between aquifers, it cannot transmit water fast
enough to provide an adequate supply to wells, resulting in an insignificant yield.
S. Aquiclude - 2. Impermeable to flow of water
An aquiclude is a highly porous formation that contains a large amount of water but is
completely impermeable to its flow due to extremely small pore sizes (like pure clay).
It prevents any effective movement or transmission of groundwater.