Nucleic Acid Isolation, PCR Technology, and Probe Labeling

Cellular Fractionation

1. Cellular Fractionation

Homogenization Techniques & Lysis Buffer Design — Foundations of Subcellular Isolation

1. Introduction to Cellular Fractionation

Cellular fractionation is a fundamental process in biochemistry and cell biology that involves breaking open cells (homogenization) and separating their individual organelles, membrane vesicles, and macromolecules based on physical characteristics such as size, shape, and buoyant density. To study metabolic pathways, organelle-specific enzyme activities, or macromolecular structures, the target components must first be isolated from the highly complex, crowded cellular interior — a two-stage process of first breaking the cell open, and then separating what spills out.

1.1 Mechanics of Cell Disruption (Homogenization)

The first critical step in cellular fractionation is homogenization: breaking open the plasma membrane while preserving the structural and functional integrity of the subcellular organelles. The choice of technique depends strictly on the source material — animal tissue, plant tissue, bacteria, yeast, or cultured cells each demand a different disruption strategy.

Dounce Homogenizer Manual shear through 0.05–0.1 mm gap Best for: Fragile animal tissue (liver, brain) French Press Extrusion through a valve at up to 20,000 psi (138 MPa) Best for: Tough bacterial walls (e.g. E. coli) Sonication Ultrasonic cavitation (20–50 kHz) — bubble implosion shear Best for: Bacteria & cultured mammalian cells Grinding (Abrasives) Friction with sand, alumina or glass beads Best for: Plant cells & yeast (rigid walls) Enzymatic Digestion Wall-degrading enzymes, then gentle osmotic lysis Best for: Protoplast / spheroplast generation

Figure: Five approaches to cell disruption. The physical or chemical strategy chosen for homogenization is dictated by the mechanical resilience of the starting material — from the delicate plasma membranes of animal tissue, which tolerate only gentle shear, to the rigid, wall-protected cells of bacteria, plants, and yeast, which require high pressure, abrasion, or targeted enzymatic digestion before they will lyse.

  1. Mechanical Shearing (Dounce Homogenizer): A glass pestle is manually moved up and down within a precision-bored glass cylinder. The clearance between the pestle and the cylinder is extremely small, typically 0.05 to 0.1 mm. As the pestle moves, the liquid suspension is forced through this narrow gap, subjecting the cells to high shear forces.
    This is the preferred method for fragile animal cells and soft tissues (such as liver or brain), because it breaks the plasma membrane while leaving the nuclei, mitochondria, and lysosomes intact.
  2. High-Pressure Extrusion (French Press): The French pressure cell forces a suspension of cells through a tiny, needle-valve orifice at extremely high pressures — up to 20,000 psi (138 MPa). As the cells pass through the valve into atmospheric pressure, they experience massive shear forces and a rapid drop in pressure, causing them to burst.
    Highly effective for breaking tough cell walls, such as those of Escherichia coli and other Gram-negative or Gram-positive bacteria.
  3. Sonication (Ultrasonic Cavitation): High-frequency sound waves (20 to 50 kHz), emitted from a metal probe immersed in the cell suspension, create localized high- and low-pressure zones. During the low-pressure cycle, microscopic vapor bubbles grow; during the high-pressure cycle, they implode violently — a process called cavitation. The resulting shockwaves and shear forces tear the cell membranes apart.
    Heat caution: sonication generates significant heat and can easily denature proteins, so the sample must be kept in an ice bath and sonicated in short pulses.
  4. Grinding with Abrasives (Mortar and Pestle): For plant tissues protected by rigid cellulose cell walls, or yeast cells protected by thick glucan/mannan walls, manual grinding in a mortar and pestle with dry abrasives — fine sand, alumina, or glass beads — is often required. The physical friction breaks the cell walls, releasing the intracellular contents into the buffer.
  5. Enzymatic Digestion (Protoplast Generation): Chemical or enzymatic pretreatments can selectively degrade the cell wall before lysis. Lysozyme hydrolyzes the β(1→4) glycosidic bonds of bacterial peptidoglycan; cellulases and pectinases digest plant cell walls; zymolyase or lyticase acts on yeast cells.
    Once the rigid wall is removed, the resulting fragile cell — a protoplast or spheroplast — can be easily lysed by gentle osmotic shock.
MethodPhysical mechanismTypical application
Dounce homogenizerManual shear through a 0.05–0.1 mm pestle–cylinder clearanceFragile animal tissue (liver, brain); preserves nuclei, mitochondria, lysosomes
French pressHigh-pressure extrusion through a needle-valve orifice (≤20,000 psi)Tough Gram-negative/positive bacterial walls (e.g. E. coli)
SonicationUltrasonic cavitation (20–50 kHz); bubble implosion shearBacteria, cultured mammalian cells; requires ice bath & pulsing
Grinding (abrasives)Mechanical friction with sand, alumina, or glass beadsPlant cells (cellulose walls), yeast (glucan/mannan walls)
Enzymatic digestionWall-degrading enzymes (lysozyme, cellulase/pectinase, zymolyase) + osmotic shockGenerating protoplasts/spheroplasts prior to gentle lysis

1.2 Osmotic, pH, and Chemical Composition of Lysis Buffers

Once the cells are disrupted, the released organelles must be stabilized in a specialized suspension medium called the homogenization buffer or lysis buffer. If the buffer composition is incorrect, the organelles will quickly swell, lyse, or aggregate. A standard homogenization buffer is built from five functional components layered together.

Homogenization Buffer pH 7.4, isotonic Osmotic Stabilizer Sucrose (~0.25 M), mannitol, sorbitol, or glycerol Prevents osmotic swelling & lysis of released organelles pH Buffer HEPES or Tris-HCl (10–50 mM) Holds pH at 7.4 despite acidic lysosomal/vacuolar release Chelating Agent EDTA (Ca²⁺/Mg²⁺) or EGTA (Ca²⁺-selective), 1–5 mM Blocks metalloprotease & nuclease activity Protease Inhibitors PMSF, leupeptin, pepstatin, aprotinin (fresh cocktail) Protects proteins from lysosomal protease attack Reducing Agent DTT or β-mercaptoethanol (0.1–1.0 mM) Keeps –SH groups reduced, blocks stray disulfide bonds

Figure: Anatomy of a homogenization buffer. Five functional components are combined around an isotonic, pH-controlled base: an osmotic stabilizer to prevent organelle swelling, a zwitterionic pH buffer to hold physiological pH, a chelating agent to disarm destructive metal-dependent enzymes, a protease-inhibitor cocktail to protect released proteins, and a reducing agent to preserve free thiol groups.

  1. Osmotic Stabilizers (Osmolytes): The intracellular fluid is highly concentrated and exerts significant osmotic pressure. In a hypotonic medium such as pure water, water rapidly diffuses into organelles by osmosis, causing them to swell and burst. Sucrose (typically 0.25 M) is the most widely used osmolyte because it is chemically inert, inexpensive, and does not easily cross organelle membranes; mannitol, sorbitol, or glycerol are alternatives, especially for plant or bacterial cells.
  2. Hydrogen Ion Buffers (pH Control): Biological membranes and enzymes are highly sensitive to pH fluctuations. Homogenization buffers are typically adjusted to physiological pH (7.4) using highly stable, non-reactive zwitterionic buffers such as HEPES or Tris-HCl (usually 10 to 50 mM), which maintain a stable pH despite the release of acidic compounds from damaged vacuoles or lysosomes.
  3. Chelating Agents: When cells are lysed, intracellular metalloproteases and nucleases are activated, and heavy metal contaminants can catalyze protein oxidation. EDTA or EGTA is added at 1 to 5 mM.
    EDTA vs. EGTA: EDTA chelates both Ca²⁺ and Mg²⁺, essential cofactors for many destructive enzymes (DNases, calcium-dependent proteases). EGTA is highly selective for Ca²⁺, making it ideal when Mg²⁺ must be preserved.
  4. Protease Inhibitors: To protect extracted proteins from degradation by lysosomal proteases (such as cathepsins) released during lysis, a cocktail is added immediately before homogenization.
    PMSF — irreversible inhibitor of serine proteases. Leupeptin / pepstatin — reversible inhibitors of lysosomal acid proteases. Aprotinin — inhibits trypsin and related serine proteases.
  5. Reducing Agents: The cytoplasm is a highly reducing environment that keeps protein sulfhydryl (–SH) groups reduced. On exposure to atmospheric oxygen during homogenization, these groups can oxidize and form incorrect intermolecular disulfide bonds, inactivating enzymes. Low concentrations (0.1 to 1.0 mM) of DTT (dithiothreitol) or β-mercaptoethanol are included to maintain a reducing environment.
ComponentPurposeCommon reagentsTypical concentration
Osmotic stabilizerKeeps medium isotonic/hypertonic to prevent organelle swelling & lysisSucrose, mannitol, sorbitol, glycerol~0.25 M (sucrose)
pH bufferMaintains physiological pH despite acidic lysosomal/vacuolar releaseHEPES, Tris-HCl10–50 mM, pH 7.4
Chelating agentSequesters Ca²⁺/Mg²⁺ that activate metalloproteases & nucleasesEDTA (broad), EGTA (Ca²⁺-selective)1–5 mM
Protease inhibitorsBlocks proteolytic degradation by released lysosomal proteasesPMSF, leupeptin, pepstatin, aprotininFresh cocktail, µM–mM range
Reducing agentPreserves –SH groups; prevents aberrant disulfide bondsDTT, β-mercaptoethanol0.1–1.0 mM
Physical Principles of Centrifugation

2. Physical Principles of Centrifugation

Force Balance, Sedimentation Theory & RCF Calculations — Quantitative Foundations of Centrifugal Separation

2. Physical Principles of Centrifugation

Centrifugation is a physical method that uses high-speed rotation to subject suspended particles to a radial centrifugal force. This force accelerates the natural sedimentation rate of particles — molecules, organelles, or whole cells — suspended in a liquid medium, allowing them to be separated based on their physical properties: mass, size, shape, and density.

2.1 Complete Force Balance Equations (Fc, Fb, Ff)

A particle suspended in a liquid medium inside a rotating centrifuge tube is subject to three primary, competing physical forces.

ω Axis of rotation r (radius) Centrifuge tube particle Fc Fb Ff

Figure: Force balance on a sedimenting particle. The centrifugal force (Fc) pushes the particle radially outward, away from the axis of rotation at angular velocity ω. Opposing it are the buoyant force (Fb), acting inward per Archimedes' principle, and the frictional/drag force (Ff), which opposes the particle's net motion through the fluid and grows with velocity until the three forces balance at terminal velocity.

  1. Centrifugal Force (Fc): Acts radially outward from the axis of rotation. It is directly proportional to the particle's mass, the square of the rotor's angular velocity, and the particle's distance from the axis.
    Fc = mω²r
    • m — actual mass of the particle (g)
    • ω — angular velocity of the rotor (rad/s)
    • r — radial distance from the axis to the particle (cm)
  2. Buoyant Force (Fb): By Archimedes' principle, any object immersed in a fluid experiences an upward (radially inward) force equal to the weight of fluid it displaces.
    Fb = m0ω²r

    Here m0 is the mass of displaced solvent. The displaced volume equals the particle's volume, expressible as mv, where v is the partial specific volume (mL of solvent displaced per gram of solute). Multiplying by solvent density ρ gives:

    m0 = mvρ

    Substituting back:

    Fb = mvρω²r
  3. Frictional Force (Ff): As the particle moves through the fluid it experiences hydrodynamic drag, opposing its net motion and proportional to its sedimentation velocity.
    Ff = fv
    • f — frictional coefficient (depends on size, shape, solvent viscosity)
    • v — sedimentation velocity of the particle (cm/s)

2.2 Mathematical Derivation of Sedimentation Velocity (v)

When the rotor starts spinning, Fc exceeds Fb and the particle accelerates outward. As velocity increases, the opposing Ff grows proportionally, until within microseconds the system reaches a dynamic equilibrium (terminal velocity) where the net force is zero.

  1. Set the forces in balance at terminal velocity:
    Ff = FcFb
  2. Substitute the force equations from 2.1:
    fv = mω²rmvρω²r
  3. Factor out the common terms (m, ω²r):
    fv = mω²r (1 − vρ)
  4. Re-express particle mass in macroscopic terms — molar mass M (g/mol) divided by Avogadro's number N (6.022×10²³ /mol):
    m = MN
  5. Substitute and solve for the terminal sedimentation velocity:
    fv = MNω²r (1 − vρ)
    v = Mω²r (1 − vρ)N f

This final equation reveals three governing physical factors:

FactorRelationshipPhysical meaning
Mass & sizevMLarger, heavier particles sediment faster than smaller, lighter ones
Viscosity & shapev ∝ 1/fCompact spherical particles (low f) sediment faster than elongated or denatured ones (high f) of the same mass
Density difference(1 − vρ) — the buoyancy factorSee the three cases below
ConditionBuoyancy factorOutcome
Particle denser than solvent (1/v > ρ)PositiveParticle sediments outward, toward the tube bottom
Particle less dense than solvent (1/v < ρ)NegativeParticle floats inward, toward the tube top
Densities equal (1/v = ρ)ZeroVelocity is zero — particle stays stationary regardless of rotor speed

2.3 Sedimentation Coefficient (s), Svedberg Units (S), and Non-Additivity in Complexes

The sedimentation coefficient is defined as sedimentation velocity per unit of centrifugal acceleration:

s = vω²r

Substituting the derived expression for v (from 2.2):

s = M (1 − vρ)N f
Svedberg unit: because biological macromolecules have extremely small s values (typically ~10⁻¹³ seconds), the Svedberg unit (S) was established in honor of Theodor Svedberg, the pioneer of ultracentrifugation: 1 S = 1×10⁻¹³ seconds.
Small subunit 40S Large subunit 60S + associate 80S ribosome buried interface (hidden from solvent)

Figure: Why sedimentation coefficients don't add. When the 40S and 60S ribosomal subunits associate, their masses simply sum — but the newly buried interface removes surface area that no longer contacts solvent, so the frictional coefficient of the 80S complex is smaller than the sum of the two individual coefficients. Since sM/f, a disproportionately smaller f alongside an additive M yields an 80S particle, not a 100S one.

SystemSubunitsComplexWhy not additive
Eukaryotic ribosome40S + 60S80SMass adds; buried surface area lowers f disproportionately
Bacterial ribosome30S + 50S70SSame principle — compact packing reduces total frictional drag

2.4 Thermodynamic & Hydrodynamic Standardization to s20,w

Because solvent density (ρ) and viscosity (η) are highly temperature- and salt-dependent, an experimentally measured sedimentation coefficient (sexp) must be converted to a standard reference state — pure water at 20°C — before it can be compared across laboratories.

s20,w = sexp × 1 − vρ20,w1 − vρexp × ηexpη20,w
  • sexp — sedimentation coefficient observed under experimental conditions
  • ηexp, η20,w — viscosity of the experimental solvent vs. water at 20°C
  • ρexp, ρ20,w — density of the experimental solvent vs. water at 20°C
  • v — partial specific volume of the macromolecule
This equation mathematically "corrects" the experimental value, stripping away the fluid-dynamic artifacts of the specific buffer and temperature used, and allowing direct comparison of structural properties across different laboratories.

2.5 Mathematical Relationship of RCF to rpm and Radius (r)

Earth's gravitational acceleration is roughly g = 980 cm/s². To sediment small biological molecules, a centrifuge must generate accelerations thousands of times stronger than gravity — this multiplier is the Relative Centrifugal Field (RCF), or g-force:

RCF = centrifugal accelerationgravitational acceleration = rω²g

To calculate RCF from standard instrument parameters — rotor radius r (cm) and rotational speed in rpm:

  1. Convert rpm to angular velocity ω (one revolution = 2π radians, one minute = 60 s):
    ω = 2π × rpm60 rad/s
  2. Substitute into the RCF equation:
    RCF = r (2π × rpm / 60)² / g
  3. Expand using g = 980 cm/s² and simplify the constants:
    RCF = r980 × 4π² × (rpm)²3600
RCF = 1.118 × 10⁻⁵ × r × (rpm)²

This is the practical working formula — the one used directly in the sample calculations below.

ω Axis of rotation Fixed-angle rotor tube rmin = 6 cm (top) 15,093 × g rmax = 12 cm (bottom) 30,186 × g

Figure: RCF varies with radial position. At 15,000 rpm in a fixed-angle rotor with rmin = 6 cm and rmax = 12 cm, a particle at the bottom of the tube experiences roughly twice the g-force of a particle at the top — RCF scales linearly with r. (In a real fixed-angle rotor the tube sits at an angle rather than perfectly vertical, but the radial distance — and therefore the g-force — still increases continuously from the top of the tube to the bottom.)

2.6 High-Yield Sample Calculations

Problem 1 — Calculating g-force (RCF)

A fixed-angle rotor has rmax = 12 cm and rmin = 6 cm, operated at 15,000 rpm. Find the RCF at the bottom and top of the tube.

At the bottom (rmax = 12 cm):

RCF = 1.118×10⁻⁵ × 12 × (15,000)² = 1.118×10⁻⁵ × 12 × 2.25×10⁸ = 1.118 × 12 × 2250
30,186 × g

At the top (rmin = 6 cm):

RCF = 1.118×10⁻⁵ × 6 × (15,000)² = 1.118 × 6 × 2250
15,093 × g
Takeaway: g-force varies linearly with distance from the axis of rotation — a particle at the bottom of the tube experiences roughly twice the sedimenting force of one at the top.
Problem 2 — Calculating Sedimentation Velocity

A spherical virus with s = 100 S sits in a rotor generating ω²r = 10⁷ cm/s² at the tube center. Find the sedimentation velocity in cm/hour.

Step 1 — convert S to seconds:

s = 100 × 10⁻¹³ s = 10⁻¹¹ s

Step 2 — use s = v / ω²r to solve for v:

v = s × (ω²r) = 10⁻¹¹ s × 10⁷ cm/s² = 10⁻⁴ cm/s

Step 3 — convert to cm/hour (1 hour = 3600 s):

v = 10⁻⁴ cm/s × 3600 s/hour
0.36 cm/hour
Centrifugation Instrumentation and Rotor Dynamics

3. Centrifugation Instrumentation and Rotor Dynamics

Rotor Geometry, Vacuum Engineering & Sedimentation Physics

3. Centrifugation Instrumentation and Rotor Dynamics

Centrifugation instruments are highly engineered devices capable of spinning rotors at extreme speeds. Because the forces generated are immense — in the largest ultracentrifuges, hundreds of thousands of times the force of gravity — rotor safety, aerodynamic friction, and temperature control are critical engineering challenges that shape every part of the instrument's design.

3.1 Structural and Operational Differences: Low-Speed, High-Speed, and Ultracentrifuges

Centrifuges are classified into three broad instrument classes based on the rotational speeds and forces they can safely generate.

ParameterLow-speed centrifugesHigh-speed centrifugesUltracentrifuges
Max rotational speed1,000–6,000 rpm10,000–25,000 rpm50,000–150,000 rpm
Max relative centrifugal field (RCF)up to 6,000 × gup to 60,000 × gup to 1,000,000 × g
Temperature controlAmbient (unrefrigerated) or simple coolingRefrigerated (4°C to 20°C)Precision refrigeration (0°C to 4°C)
Atmospheric chamberOpen to ambient airSealed, normal atmospheric pressureHigh vacuum (<0.13 Pa, or 10−3 torr)
Drive systemDirect-drive AC/DC motorHigh-torque brushless induction motorVariable-frequency induction or magnetic drive
Primary biological usesPelleting whole cells, red blood cells, large precipitatesHarvesting bacterial cells, yeast, nuclei, large chloroplastsIsolating proteins, ribosomes, nucleic acid conformations, lipid fractions

3.2 Why Does an Ultracentrifuge Require a Vacuum?

At speeds exceeding 30,000 rpm, the outer edge of a metal rotor travels faster than the speed of sound. The friction between the spinning rotor and surrounding air molecules generates extreme heat — enough to instantly cook and denature biological samples — while the air resistance itself places immense mechanical strain on the drive motor. To eliminate this aerodynamic drag and the heat it generates, ultracentrifuges are fitted with a heavy-duty vacuum pump that evacuates the rotor chamber to pressures below 10−3 torr before the run begins.

Without Vacuum With Vacuum (<10⁻³ torr) Air friction → heat → sample denatures PUMP No air molecules → no frictional heating

Figure: Why ultracentrifuges run under vacuum. In open air (left), rotor tip speeds above the speed of sound cause constant collisions with air molecules, generating heat that would denature the sample and straining the motor. Evacuating the chamber (right) removes the air molecules entirely, eliminating both the drag and the heat.

Threshold to remember: the vacuum requirement is a direct consequence of speed — below roughly 30,000 rpm the tip speed stays subsonic and a sealed, unevacuated chamber is sufficient, which is why only true ultracentrifuges (not high-speed centrifuges) need a vacuum pump.

3.3 Physics of Rotor Geometries: Swing-Bucket vs. Fixed-Angle vs. Vertical Rotors

The physical path a sedimenting particle takes, and the efficiency with which a pellet or gradient band forms, are dictated entirely by the geometry of the rotor.

Swing-Bucket Rotor AT REST SPINNING centrifugal force tubes swing to 90° Pellet forms symmetrically at tube bottom — straight radial path, no wall contact Fixed-Angle Rotor AT REST SPINNING angle constant (14–40°) short radial path to wall Particles strike the outer wall, then slide down — fastest pelleting, but wall contact Vertical Rotor AT REST SPINNING ~1–2 cm to wall tubes stay vertical Long thin pellet along the entire outer wall — fastest gradient separations

Figure: The three rotor geometries. A swing-bucket rotor's tubes hang vertically at rest and swing outward to a full 90° once spinning, so particles travel straight down the tube length. A fixed-angle rotor holds tubes rigidly at a permanent angle whether at rest or spinning, giving particles only a short radial distance to travel before hitting the wall. A vertical rotor holds tubes fully parallel to the spin axis at all times, so particles need to cross only the tube's diameter to reach the wall.

  1. Swing-Bucket Rotors (Horizontal Rotors): The rotor has individual hinges holding metal buckets. At rest the buckets hang vertically; as the rotor accelerates, centrifugal force swings them outward until they sit horizontally, at 90° to the vertical axis of rotation. Particles then travel along a straight path down the length of the tube, parallel to the tube walls, and the pellet forms symmetrically at the absolute center-bottom of the tube.
    Advantages: because particles never collide with the tube walls during their descent, there is no convective mixing or wall disturbance — this makes swing-bucket rotors ideal for density gradient centrifugation, both rate-zonal and isopycnic, where clean, discrete bands must be preserved.
    Disadvantages: the long sedimentation path means pelleting times are relatively slow, and the swung-out buckets create high aerodynamic drag, which limits the maximum achievable speed.
  2. Fixed-Angle Rotors: Centrifuge tubes sit in rigid cavities bored into a solid block of metal (aluminum or carbon fiber) at a permanent fixed angle, typically 14–40° from the central vertical axis. Particles travel only a short distance radially outward before striking the outer wall of the tube, lose their kinetic energy there, and slide down the wall to accumulate as a compact pellet at the bottom-side of the tube.
    Advantages: the sedimentation distance is often less than half that of a swing-bucket rotor, dramatically cutting the run time needed to form a pellet; the solid, aerodynamic block can also withstand much higher rotational speeds and forces.
    Disadvantages: particles sliding down the tube wall cause frictional heating and convective mixing, which makes fixed-angle rotors unsuitable for high-resolution rate-zonal gradients.
  3. Vertical Rotors: Tubes are held completely parallel to the vertical axis of rotation, at 0°. Because centrifugal force acts perpendicular to the tube's length, particles travel only a tiny distance — roughly the tube's diameter, about 1–2 cm — before reaching the outer wall, sliding down it to form a long, thin pellet along the entire outer wall of the tube.
    Advantages: the minimal sedimentation distance gives the fastest possible separation times, which makes vertical rotors especially useful for rapid plasmid DNA preparation in CsCl gradients.
    Disadvantages: as the rotor slows down, the bands that formed vertically along the width of the tube must reorient to a horizontal position under gravity, which can cause significant band-broadening and contamination.

3.4 Wall Effects, Thermal Convection, and Heat Generation

Beyond rotor geometry itself, several physical phenomena can degrade centrifugation efficiency if left unmanaged.

Wall Effect (Fixed-Angle / Vertical) particles pile up at the wall dense plume plunges through the gradient, disrupting bands Thermal Convection warm inner wall → mixing currents

Figure: Two failure modes of an unmanaged spin. Left — in fixed-angle and vertical rotors, particles striking the tube wall can stick and pile up into a locally concentrated, denser zone that plunges rapidly to the bottom in a convective plume, disrupting the carefully separated bands. Right — without adequate refrigeration, a temperature gradient develops across the tube; because fluid density falls as temperature rises, a warm zone at the inner radius sets up convective currents that mix and destroy the bands.

Wall effects: in fixed-angle and vertical rotors, particles striking the tube wall can stick or accumulate, creating localized zones that are denser than the surrounding fluid and so plunge rapidly to the tube bottom in convective plumes, disrupting the gradient separation.
Thermal convection: if the rotor chamber is not properly refrigerated, temperature gradients develop across the tube; since fluid density decreases with temperature, a warm zone at the inner radius creates convective currents that mix and destroy separated bands. Precision temperature sensors and microprocessors are required to keep the rotor isothermal to within ±0.1°C.

3.5 Rotor Selection at a Glance

GoalBest rotorWhy
Preserve clean gradient bands (rate-zonal or isopycnic)Swing-bucketNo wall contact; straight, parallel sedimentation path
Fastest pelleting of a crude sampleFixed-angleShortest radial path; withstands the highest speeds
Fastest possible gradient run (e.g. plasmid DNA prep)VerticalSedimentation distance is only the tube diameter
Routine bacterial or yeast harvestingHigh-speed fixed-angleBest balance of run time, capacity, and cost
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