Colloid
A colloid is a heterogeneous mixture in which microscopically dispersed insoluble particles of one substance are suspended throughout another substance, with particle sizes typically ranging from 1 to 1000 nanometers, placing it intermediate between true solutions and coarse suspensions.[1] These particles remain evenly distributed without settling due to Brownian motion, the random zigzagging caused by collisions with molecules of the dispersing medium.[2] Colloids exhibit unique optical properties, such as the Tyndall effect, where they scatter light passing through them, making the beam visible—unlike true solutions that allow light to pass without scattering.[3] Colloids are classified by the phases of the dispersed and dispersing media, yielding types like sols (solid in liquid), emulsions (liquid in liquid), foams (gas in liquid), and aerosols (liquid or solid in gas).[4] Common examples include milk (fat globules in water), fog (water droplets in air), and gelatin (solid network in liquid).[5] Many colloidal particles carry electrical charges, which contribute to stability by electrostatic repulsion, preventing aggregation, though they can be destabilized by electrolytes leading to coagulation.[6] Colloid science has broad applications across industries, including food science (e.g., mayonnaise as an emulsion), pharmaceuticals (drug delivery via nanoparticles), and biotechnology (enzyme immobilization).[7] In environmental engineering, colloids play roles in water treatment through coagulation processes to remove suspended particles.[4] Emerging uses in nanotechnology leverage colloidal assemblies for advanced materials like self-propelled particles and biomedical sensors.[8]Fundamentals
Definition and Characteristics
A colloid is a type of mixture in which one substance, consisting of microscopically dispersed insoluble particles, is suspended throughout another substance, known as the continuous phase or dispersion medium.[9] The dispersed particles have at least one dimension in the approximate range of 1 nm to 1 μm (10^{-9} to 10^{-6} m), resulting in a system that appears homogeneous to the naked eye but is heterogeneous at the molecular scale.[9] The term "colloid" was coined in 1861 by Scottish chemist Thomas Graham, who used it to describe gelatinous substances like silicic acid that failed to diffuse through parchment membranes, in contrast to crystalloids that diffused readily. Key characteristics of colloids include the Tyndall effect, in which the dispersed particles scatter incident light, rendering the beam visible as a path through the medium due to the particle size being comparable to the wavelength of visible light./Physical_Properties_of_Matter/Solutions_and_Mixtures/Colloid/Tyndall_Effect) Colloids also exhibit kinetic stability, meaning the particles remain dispersed without rapid settling because Brownian motion—the random, incessant movement caused by collisions with molecules of the dispersion medium—counteracts gravitational forces.[10] This stability arises from the small particle size, which limits sedimentation velocity while promoting constant agitation. Colloids differ from true solutions, where solute particles are smaller than 1 nm and fully dissolve without scattering light or settling, and from coarse suspensions, where particles exceed 1 μm and settle quickly under gravity./07%3A_Solids_Liquids_and_Gases/7.06%3A_Colloids_and_Suspensions) Representative examples include milk, an emulsion of fat globules (approximately 0.1–10 μm) dispersed in water, and fog, an aerosol of liquid water droplets (about 1–10 μm) in air.[11]Properties and Behavior
Colloidal systems exhibit distinctive optical properties arising from the interaction of light with dispersed particles typically ranging from 1 nm to 1 μm in size. The Tyndall effect, first observed by John Tyndall in 1869, describes the scattering of light by these particles, rendering the beam visible as a cone of scattered light when passed through the colloid, in contrast to true solutions where no such scattering occurs. For particles much smaller than the wavelength of visible light (<< 400–700 nm), scattering follows Rayleigh's theory, where intensity is proportional to 1/λ⁴, leading to preferential scattering of shorter blue wavelengths, analogous to the blue sky phenomenon but intensified in colloids due to higher particle density. This effect allows direct visualization of particle motion; using an ultramicroscope invented by Richard Zsigmondy in 1903, Brownian motion appears as erratic zig-zag paths of individual particles illuminated against a dark background, confirming their kinetic agitation without sedimentation. Rheological properties of colloids are governed by particle-solvent interactions and concentration, often deviating from Newtonian behavior. Many colloidal suspensions display non-Newtonian viscosity, where flow resistance changes with shear rate; for instance, thixotropic gels, such as certain paints or drilling muds, exhibit time-dependent viscosity reduction under shear due to temporary breakdown of particle networks. In dilute suspensions of spherical particles, viscosity η increases linearly with volume fraction φ according to Einstein's 1906 derivation: \eta = \eta_0 (1 + 2.5 \phi) where η₀ is the solvent viscosity; this relation holds for φ < 0.05, highlighting how even low particle loadings enhance drag through hydrodynamic perturbations. Electrical properties stem from surface charges on colloidal particles, leading to the formation of an electrical double layer. Charged particles in a polar medium attract counterions, creating a compact Stern layer of adsorbed ions tightly bound to the surface, followed by a diffuse layer of loosely associated ions extending into the solvent.[12] The zeta potential ζ represents the effective potential at the slipping plane (interface between bound and diffuse layers), typically measured via electrophoresis; values exceeding |30| mV indicate electrostatic repulsion sufficient for stability against aggregation.[12] Thermal properties of colloids are characterized by enhanced stability against temperature-induced changes, primarily due to Brownian motion. The random collisions from solvent molecules impart kinetic energy (3/2 kT per degree of freedom) to particles, counteracting gravitational settling and maintaining dispersion even as temperature rises, provided no phase transitions occur; this agitation ensures uniformity without external mixing at ambient conditions.[13] Colloids display osmotic pressure intermediate between that of true molecular solutions and coarse suspensions. In true solutions, osmotic pressure π = cRT (from van't Hoff) arises from numerous solute molecules, yielding high values; coarse suspensions contribute negligibly due to settling and low particle count per volume. Colloidal osmotic pressure, measurable via semipermeable membranes, balances contributions from both solvent-solute and finite particle numbers, resulting in moderate values that sustain equilibrium without rapid diffusion or sedimentation.[14]Comparison with Solutions and Suspensions
Colloids occupy an intermediate position between true solutions and coarse suspensions in terms of particle size and mixture properties. In true solutions, the solute particles are molecularly dispersed with sizes less than 1 nm, resulting in a homogeneous mixture where the solute is completely dissolved and uniformly distributed at the molecular level.[15] For example, sodium chloride in water forms a true solution, exhibiting no visible boundaries between solute and solvent.[16] In contrast, coarse suspensions contain larger particles exceeding 1 μm (1000 nm) in diameter, leading to a heterogeneous mixture where the dispersed phase is distinctly visible and unevenly distributed.[17] Sand particles suspended in water exemplify a coarse suspension, appearing opaque and allowing rapid separation by gravity.[16] Colloidal dispersions, however, feature particles ranging from 1 to 1000 nm, which are large enough to influence mixture behavior but small enough to remain suspended for extended periods without immediate settling.[18] A key optical distinction arises from the Tyndall effect, where a beam of light scatters visibly in colloidal dispersions due to the size of the particles, but passes undetected through true solutions, which lack such scattering particles.[16] Coarse suspensions, while also scattering light, appear turbid overall because their larger particles block transmission more completely. Regarding settling, true solutions show no sedimentation, as solute particles do not aggregate or fall out. Coarse suspensions exhibit rapid settling under gravity, often within seconds or minutes, due to the substantial size and weight of the particles. Colloids demonstrate slow or negligible settling over time, maintaining apparent homogeneity despite their heterogeneous nature.[16] Filtration further delineates these systems: particles in true solutions and colloids pass through ordinary filter paper, but those in coarse suspensions are retained, allowing easy separation. Dialysis provides a finer distinction, employing semipermeable membranes that permit crystalloids (small molecules from true solutions) to diffuse through while retaining larger colloidal particles. This technique, introduced by Thomas Graham in 1861 through experiments separating diffusible crystalloids from non-diffusible colloids using parchment or animal bladder membranes, established the foundational boundary between these mixture types.[19] The slow settling in colloids can be quantified using Stokes' law, which describes the terminal settling velocity v of a spherical particle in a fluid as v = \frac{2}{9} \frac{(\rho_p - \rho_f) g r^2}{\eta}, where \rho_p is the particle density, \rho_f the fluid density, g gravitational acceleration, r the particle radius, and \eta the fluid viscosity.[20] For colloidal particles, the small radius r (on the order of 1-500 nm) results in a very low v, often approaching zero under ambient conditions, in contrast to the higher velocities for suspension particles with r > 500 nm. This kinetic barrier contributes to the kinetic stability of colloids, where dispersions remain dispersed despite being thermodynamically unstable and prone to eventual aggregation without stabilizing forces.[21]Classification
By Phases and Composition
Colloids are classified primarily according to the physical states of the dispersed phase and the continuous phase, which together determine their structure and behavior. This framework identifies eight principal types, each characterized by specific combinations of solid, liquid, or gas phases.[22] The following table summarizes these types, including representative examples:| Dispersed Phase | Continuous Phase | Type | Example |
|---|---|---|---|
| Gas | Liquid | Foam | Whipped cream |
| Gas | Solid | Solid foam | Styrofoam |
| Liquid | Gas | Aerosol | Fog or mist |
| Liquid | Liquid | Emulsion | Mayonnaise |
| Liquid | Solid | Gel | Gelatin dessert |
| Solid | Gas | Solid aerosol | Smoke |
| Solid | Liquid | Sol | Paint |
| Solid | Solid | Solid sol | Opal |