Question:

Darcy’s law quantifies the volume of groundwater flow

Updated On: Feb 10, 2025
  • per unit surface area of the aquifer
  • per unit time
  • per unit cross-sectional area of the aquifer
  • per unit cross-sectional area of the aquifer per unit time
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The Correct Option is B

Solution and Explanation

Darcy’s Law and Groundwater Flow

Understanding Darcy’s Law

Darcy’s Law quantifies groundwater flow as a function of:

  • Permeability (K): The ability of a porous medium to transmit fluid.
  • Hydraulic Gradient (I): The change in hydraulic head per unit distance.
  • Cross-Sectional Area (A): The area through which groundwater flows.

Mathematically, Darcy’s Law is expressed as:

\[ Q = K I A \]

where:

  • \( Q \) = Discharge (volume of water flowing per unit time)
  • \( K \) = Hydraulic conductivity (permeability)
  • \( I \) = Hydraulic gradient
  • \( A \) = Cross-sectional area

Primary Quantification

Although Darcy’s Law considers permeability, hydraulic gradient, and cross-sectional area, its primary purpose is to quantify the volume of water flowing per unit time in a porous medium.

Conclusion:

Darcy’s Law is fundamental in hydrogeology, helping estimate groundwater movement and manage water resources effectively.

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