Sequential spins, sorted by size
crude fractionation of a cell homogenate
A homogenate is spun at low speed to pellet the largest, heaviest structures. The supernatant is poured off and re-spun at higher speed to pellet the next size class, and so on — each round clearing out whatever is left.
A thin layer, raced through a gradient
sedimentation velocity
Sample is loaded as a narrow band on top of a pre-formed sucrose gradient, then spun for a timed interval — stopped well before equilibrium. Particles sediment at rates set by their size and shape, so they resolve into separate bands part-way down the tube.
Settling to a matching density
buoyant-density / equilibrium sedimentation
Sample is mixed throughout a steep gradient (classically CsCl) and spun until equilibrium. Each particle migrates — up or down — until the surrounding solution matches its own buoyant density, then stops moving no matter how much longer the run continues. Separation depends on density alone, not size.
Watching the boundary move
real-time optical detection
Nothing is isolated here — a spinning sample cell is scanned optically while it spins, tracking the sedimenting boundary as it moves outward from the center over time. The boundary’s speed gives the sedimentation coefficient; equilibrium runs give molecular weight, purity, and shape.