Difficulty: Medium
Correct Answer: v_s = [ g * (Gs − 1) * d^2 ] / (18 * nu)
Explanation:
Introduction / Context:
Primary sedimentation and grit removal design rely on predicting particle settling velocities. For very small spherical particles at low Reynolds number (laminar regime), Stokes’ law provides a simple analytical expression relating size, fluid properties, and density contrast to settling velocity.
Given Data / Assumptions:
Concept / Approach:
Stokes’ law (laminar settling) states the drag force equals weight minus buoyancy at terminal velocity. Solving the force balance yields v_s proportional to d^2 and inversely proportional to viscosity. The density term appears as (Gs − 1) because buoyancy subtracts the fluid density from particle density.
Step-by-Step Solution:
Verification / Alternative check:
Dimensional check: numerator has L/T^2 * L^2 = L^3/T^2; denominator has L^2/T; result is L/T (velocity), consistent.
Why Other Options Are Wrong:
Option (b) inverts the relation; (c) uses d^1 not d^2; (d) uses d^3, which applies to buoyant weight but not to velocity form.
Common Pitfalls:
Applying Stokes’ law beyond its Re limit; using kinematic vs dynamic viscosity inconsistently; neglecting flocculation that changes effective particle size and density.
Final Answer:
v_s = [ g * (Gs − 1) * d^2 ] / (18 * nu)
Discussion & Comments