Accepted answer
Nobody has published a cycle count, and at 10 mg/mL the concentration tells you what a wrong guess costs: a 0.1 mL aliquot holds 1 mg and every microlitre is 10 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 10 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 10 mg/mL and the date, and never thaw a container you will refreeze.
The short version: aliquot before freezing, thaw slowly, never refreeze a thawed aliquot, and count your cycles.
The mitigation is aliquoting. Divide the reconstituted solution into single-use volumes before the first freeze, and each aliquot then experiences exactly one cycle.
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 |
Buffer salts crystallise at different points during freezing. Sodium phosphate is the classic example: the dibasic form crystallises first and the pH of the residual liquid falls by several units. That pH excursion is the real damage in many cases.
Cryoconcentration of solutes at the ice front is a well-documented mechanism in freeze-thaw damage to proteins and peptides.
Aliquot before the first freeze. That is the whole answer.
6This should be linked from the help pages. – marta_okonkwo 2 months ago add a comment