Chemical & Process Engineering / Sedimentation Kynch Settling
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LABORATORY 46 · CHEMICAL & PROCESS ENGINEERING

Sedimentation Kynch Settling theory

Understand sedimentation kynch settling: governing transport equations, heat and mass balances, reaction kinetics, and unit operations.

Chemical engineering transport & equilibrium foundations of Sedimentation Kynch Settling.

Sedimentation and gravity clarification are foundational mechanical separation unit operations utilized extensively in chemical manufacturing, mineral beneficiation, hydrometallurgy, water clarification, and municipal wastewater treatment. In dilute suspensions (solids volume fraction φ < 0.005), individual spherical particles settle independently without hydrodynamic particle-particle interaction according to Stokes' law: v_0 = g · d_p^2 · (ρ_p - ρ_f) / (18 · μ). However, in concentrated industrial slurries (φ > 0.05), particles settle as a collective cloud or blanket with a sharp, visible interface between the descending clarified supernatant and the concentrated suspension—a phenomenon known as hindered settling or zone settling. According to the classical sedimentation theory formulated by George J. Kynch in 1952, the local settling velocity v_s of particles in a suspension depends solely on the local solids volume concentration: v_s = f(C_s). As solids concentration increases, the upward displacement velocity of displaced fluid through the narrowing interstitial pores increases, and viscous drag is amplified by surrounding particles, causing settling velocity to decrease sharply. In the moderate concentration regime (C_s = 10.0 to 60.0 g/L), the Kynch hindered settling velocity decreases linearly with solids concentration: v_s = v_0 - S · C_s, where v_0 = 120.0000 cm/min is the unhindered terminal velocity intercept and S = 1.8500 (cm/min)/(g/L) is the Kynch hindered settling slope. Alternatively, the non-linear relationship across wide concentration ranges is described by the Richardson–Zaki correlation: v_s = v_0 · ε^n = v_0 · (1 - φ)^n, where ε is suspension voidage and n is the Richardson–Zaki exponent (~4.65 in laminar creeping flow). In continuous industrial gravity thickeners, the solid flux method (Coe & Clevenger / Yoshioka analysis) utilizes these batch settling velocity curves to identify the critical solids handling capacity (minimum flux G_min) and determine the required cross-sectional clarifier area A = F_s / G_min. In this laboratory experiment, a 1.0-meter precision glass settling column equipped with automated optical array interface detection tracks suspension interface subsidence across CaCO_3 concentrations from 10.0 to 60.0 g/L to evaluate v_s, determine S = 1.8500 (cm/min)/(g/L), and calculate continuous thickener dimensions.

v_s = -S · C_s + v_0 = -1.8500 · C_s + 120.0000

Mechanics of Particulate Sedimentation & Stokes' Law

Sedimentation describes the gravity-driven separation of solid particles suspended in a liquid medium of lower density. For an isolated, rigid spherical particle of diameter $d_p$ and density $\rho_p$ settling in an unbounded fluid of density $\rho_f$ and dynamic viscosity $\mu$, the forces acting on the particle are gravitational force $F_g$, buoyant force $F_b$, and hydrodynamic drag force $F_d$:

\[ F_g - F_b - F_d = m_p \, \frac{d v}{d t} \]

At terminal settling velocity ($d v / d t = 0$), in creeping laminar flow ($Re_p = \rho_f v d_p / \mu < 0.1$), Stokes' drag law applies ($F_d = 3 \pi \mu d_p v_0$):

\[ \frac{\pi d_p^3}{6} (\rho_p - \rho_f) g = 3 \pi \mu d_p v_0 \implies v_0 = \frac{g \, d_p^2 (\rho_p - \rho_f)}{18 \, \mu} \]

Hindered Zone Settling & Kynch Sedimentation Theory

In concentrated suspensions, particles settle collectively, forming a visible interface (mudline) separating the clarified supernatant from the suspension. George J. Kynch (1952) postulated that the local downward settling velocity $v_s$ depends solely on local solids concentration $C_s$:

\[ v_s = f(C_s) \]

In the moderate concentration regime ($C_s = 10.0$ to $60.0\text{ g/L}$), the linear hindered settling approximation models the velocity reduction caused by upward interstitial fluid displacement and multi-particle hydrodynamic interactions:

\[ v_s = v_0 - S \cdot C_s = 120.0000 - 1.8500 \cdot C_s \]

where $v_0 = 120.0000\text{ cm/min}$ is the unhindered terminal velocity intercept and $S = 1.8500\text{ (cm/min)/(g/L)}$ is the Kynch hindered settling slope.

Solids Flux & Industrial Thickener Sizing

The batch solids flux $G_s$ (mass of solids passing downward per unit cross-sectional area per unit time) is the product of concentration and settling velocity:

\[ G_s(C_s) = C_s \cdot v_s = C_s \cdot (v_0 - S \cdot C_s) \]

In a continuous thickener operating with underflow withdrawal velocity $v_u$, total solids flux is:

\[ G_{\text{total}} = C_s \cdot v_s + C_s \cdot v_u \]

By the Coe–Clevenger / Yoshioka graphical construction, the required cross-sectional thickener area $A$ for a continuous dry solids feed rate $F_s$ is dictated by the bottleneck minimum flux $G_{\text{min}}$:

\[ A = \frac{F_s}{G_{\text{min}}} \]

Viva voce questions & analytical theory

What is the difference between discrete particle settling and hindered (zone) settling?

In discrete settling (Type 1, Stokes regime), particles are far apart and settle at independent terminal velocities without mutual interference; in hindered settling (Type 2 and 3), particle concentrations exceed ~1–2 vol%, forcing fluid to flow upward through narrow interstitial channels, creating a collective settling cloud with a distinct descending mudline interface.

How does Kynch's sedimentation theory model batch settling?

Kynch assumes that settling velocity v_s depends solely on local solids concentration C_s; because mass flux is S = C_s · v_s, continuity waves of constant concentration propagate upward from the compaction zone to the descending mudline interface at wave velocity u = dS/dC_s.

Why does a batch settling curve exhibit four distinct stages over time?

1. Initial induction/flocculation period (brief aggregation); 2. Constant-rate hindered settling zone (linear subsidence as uniform slurry settles); 3. Transition/critical settling zone (rising concentration waves reach surface, slowing subsidence); 4. Compaction/compression zone (solids rest on bottom and slowly expel interstitial water under weight).

How is the Coe–Clevenger / Yoshioka flux method used to size continuous industrial thickeners?

Total solids flux is the sum of gravity flux and underflow pumping flux: G_total = C_s · v_s + C_s · v_u; the limiting flux G_min (the bottleneck minimum on the flux curve) dictates the minimum cross-sectional area required: A = F_solids / G_min.

What is the purpose of the slow-speed rake mechanism in an industrial clarifier thickener?

The slow-moving rake blades (0.1 to 2 RPM) gently stir the compression sludge blanket, creating vertical channels for trapped interstitial water to escape upward, while simultaneously plowing densified underflow slurry toward the central bottom discharge cone.

How do chemical flocculants (polyacrylamides) accelerate hindered settling rates?

High-molecular-weight polymeric flocculants adsorb onto multiple fine particles simultaneously (polymer bridging), aggregating individual micro-particles into large, porous flocs; because Stokes settling scales with floc diameter squared (d_floc^2), flocculation increases settling velocity by 10 to 100-fold.

Experimental precautions and process safety

  • Ensure the settling column is aligned strictly vertical with a precision spirit level, as a tilt of only 1° causes significant wall-effect channeling (Boycott effect).
  • Maintain slurry water temperature strictly at 20.0 ± 0.2 °C, as water viscosity changes by ~2.5% per °C, directly distorting Stokes settling rates.
  • Mix the slurry thoroughly before each run to ensure 100% uniform concentration throughout the entire column height before timing begins.
  • Never introduce air bubbles during column filling, as rising bubbles disrupt the downward zone settling interface.

Theoretical assumptions & boundary condition limits

  • The transport and thermodynamic models apply within the specified calibrated operating window (10.0 to 60.0 g/L).
  • Assumes ideal continuum flow and homogeneous phase mixing without unmodeled parasitic wall losses.
  • Continuous sensor readings reflect ordinary least-squares regression across successive observations.
  • High-temperature or extreme concentration excursions require non-ideal equation-of-state corrections.
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Connect transport theory to empirical process plant data.

Evaluated using a 100.0 cm tall, 6.0 cm ID precision graduated glass settling column with automated optical photodiode array and constant-temperature jacket at 20.0 °C. Standardized calcium carbonate slurry (mean particle diameter d_p = 25.0 μm, true solids density ρ_p = 2710 kg/m^3) in deionized water (ρ_f = 998.2 kg/m^3, μ = 1.002 mPa·s).