Accepted answer
Nobody has published a cycle count, and at 2.5 mg/mL the concentration tells you what a wrong guess costs: a 0.1 mL aliquot holds 0.25 mg and every microlitre is 2.5 µg. Damage from freezing is not gradual attrition — it is concentrated at the phase transitions, where ice excludes solute and the unfrozen fraction climbs well above 2.5 mg/mL for as long as the transition lasts. Two slow cycles can therefore do more than four fast ones, which is why a cycle count is the wrong unit in the first place. The way to make the number one is to make it one: split at reconstitution into single-draw aliquots, label each with 2.5 mg/mL and the date, and never thaw a container you will refreeze.
The relevant physics is ice-front concentration: as water crystallises, everything dissolved is concentrated into the shrinking liquid phase, including buffer salts.
During freezing, solutes are excluded from the ice lattice and concentrate into the residual liquid. Local concentrations can rise many-fold, which promotes aggregation independently of temperature.
Degradation pathway by condition
| Pathway | Dominant when | Detected by |
|---|
| Deamidation | Solution, neutral to alkaline pH | RP-HPLC, +1 Da on MS |
| Oxidation | Light, trace metals, peroxides | RP-HPLC, +16 Da on MS |
| Hydrolysis | Solution, extremes of pH | RP-HPLC, fragment masses |
| Aggregation | Agitation, interfaces, high concentration | SEC, visual haze; often invisible on RP-HPLC |
| Freeze-concentration damage | Freeze-thaw of buffered solution | SEC, loss of recovered content |
Let a frozen vial reach room temperature before opening it. Opening a cold vial in humid air condenses water into the cake, which raises residual moisture and undoes what lyophilisation achieved.
Aliquoting to eliminate repeated cycles is standard laboratory practice for exactly this reason.
Dry powder tolerates cycles far better than solution does.
edited 3 May 2026 by h_pergande — added a caveat about sampling