Freeze-thaw cycles have minimal effect on the mineralisation of low molecular weight, dissolved organic carbon in Arctic soils.

It decreased for both trialanine and amino acids significantly or almost significantly after both 1 and 3 FTC (by 0.20 ± 0.05 ( p = 0.005) and 0.08 ± 0.02 h −1 ( p = 0.103) after 1FTC and by 0.25 ± 0.06 ( p = 0.055) and 0.06 ± 0.01 h −1 ( p = 0.001) after 3FTC, for trialanine and amino acids, respectively).

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