Solution Exercise 6

  1. The items and their dimensions are defined in the table of Exercise 5. Their SI units are as follows.
[latex]Q = k\frac{\rho_{fluid}g}{\mu_{fluid}}A\frac{dh}{dl}[/latex]
[latex]Q[/latex] = volumetric discharge (m3 sec-1)
[latex]k[/latex] = intrinsic permeability (m2)
[latex]\rho_{fluid}[/latex] = density of the fluid (kg m-3)
[latex]g[/latex] = gravitational acceleration (m sec-2)
A = cross‑sectional area perpendicular to flow (m2)
dh/dl = hydraulic gradient ([latex]:[/latex])
[latex]\mu_{fluid}[/latex] = viscosity of the fluid (kg m-1 sec-1)
  1. Variables are [latex]Q,\ A,\frac{dh}{dl},\ k,\ \rho_{fluid},\ \mu_{fluid}[/latex]. Constants are [latex]g[/latex].

3. Discharge is directly proportional to permeability, fluid density, gravitational acceleration, area, and hydraulic gradient. Discharge is inversely proportional to viscosity.

4. There are no exponents or logarithms in the equation; therefore, all proportionality relationships are linear.

Thought Question 19: Explain why discharge is directly proportional to density but inversely proportional to viscosity.

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Basic Hydrogeology: An Introduction to the Fundamentals of Groundwater Science Copyright © 2025 by Matthew M. Uliana. All Rights Reserved.

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