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Coefficient of permeability is also referred to as ..............
Question

Coefficient of permeability is also referred to as ..............

A.

Effective porosity

B.

Field capacity

C.

Specific yield

D.

Hydraulic conductivity

Correct option is D

The correct answer is (d).

The coefficient of permeability is fundamentally synonymous with hydraulic conductivity in the context of hydrogeology and soil mechanics.

It defines the quantifiable ease with which a porous medium, like soil or rock aquifers, permits the transmission of water or other fluids under a specific hydraulic gradient.

Information Booster
  • Hydraulic conductivity is mathematically represented by the letter K in Darcy's Law, dictating the groundwater flow velocity.
  • It is typically measured in standard units of length per time, such as meters per day (m/d) or centimeters per second (cm/s).
  • The value heavily depends on both the physical properties of the porous matrix (grain size, void connectivity) and the fluid's characteristics (density, dynamic viscosity).
  • Coarse-grained materials like gravels and sands exhibit extremely high hydraulic conductivity, making them excellent, high-yielding aquifers.
  • Conversely, fine-grained materials like clays have immensely low hydraulic conductivity, acting as impermeable aquitards or aquicludes restricting water movement.
  • Pump tests and slug tests are standard field methods hydrogeologists utilize to accurately determine an aquifer's hydraulic conductivity.
  • Understanding K is crucial for designing municipal well fields, predicting contaminant plume migration, and managing sustainable groundwater extraction.
Additional Knowledge
  • Option A: Effective porosity refers exclusively to the interconnected pore space within a rock that actively contributes to fluid flow, excluding isolated or dead-end pores.
  • Option B: Field capacity denotes the specific moisture content retained in soil against the pull of gravity after excess water has completely drained away.
  • Option C: Specific yield is the precise ratio of the volume of water an unconfined aquifer releases purely by gravity drainage relative to the rock's total bulk volume.
  • Intrinsic permeability differs from hydraulic conductivity as it depends solely on the rock's properties, independent of the fluid type flowing through it.

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