The discharge per unit draw down at a well is known as
Specific capacity
When a well is pumped, water is removed from the aquifer. The rate at which water is pumped is called the discharge. As water is removed, the water level in the well drops below the static (non-pumping) water level. This drop in water level is called drawdown.
The relationship between the discharge rate from a well and the resulting drawdown is a key indicator of the well's performance and the aquifer's ability to supply water. This relationship is specifically defined by the term specific capacity.
Specific capacity is the discharge rate per unit of drawdown observed in a well. It is typically expressed in units like cubic meters per day per meter of drawdown ($m^3/day/m$) or gallons per minute per foot of drawdown ($gpm/ft$).
The formula for specific capacity is:
Specific Capacity $ = \frac{\text{Discharge}}{\text{Drawdown}} $
A higher specific capacity generally indicates a more efficient well or a more permeable aquifer capable of yielding more water with less drawdown.
Let's briefly look at the other options to understand why they are not the correct answer in this context:
Based on the definitions, specific capacity is the term that precisely describes the discharge per unit drawdown at a well.
The purpose of a Well Point System is-
Aquifers are generally the permeable geological formations, in which ground water occurs. Which of the following is a type of Aquifer in which ground water is confined under pressure greater than atmospheric by over-lying, relatively impermeable strata?
The number and position of bore holes vary depending on _________.
Which of the following methods can be used to lower the water table by using gravity flow?
Which of the following is just above the blank pipe in the tube well?