We are measuring soil nitrification potential in soil using the Griess-Ilosvay's method, according to Raglan et al., 2022 (see extract below). We have in total 360 soil samples which were stored at -20°C immediately after the harvest. In the protocol below, the rate is calculated from comparing each sample incubated at RT with a sample incubated at -20°C.

Since I work with already frozen soil samples, I am wondering how would you minimize the effect of freeze-thawing processes on the two samples?

Thank you

Method from:

Article Long Term Influence of Fertility and Rotation on Soil Nitrif...

"Briefly, 5 g of homogenized field soil in 50 mL Falcon tubes was shaken for 5 h at room temperatures after adding 1 mM (NH4)2SO4, and 1.5 M sodium chlorate. Each sample had a corresponding control sample which was treated identically, but frozen at −20°C for the 5-h incubation. 2M KCl was added after the incubation, and the tubes were manually shaken, then centrifuged for 2 min at 2,000 RPM. The supernatant was filtered using Whatman 42 filter papers. NO2-N was measured using a Genesys 20 spectrophometer (Thermo Scientific, Rochester, NY) after adding Griess-Ilosavay reagent (sulfanilamide and N-napthylethyldiamine) at 520 nm. NO2-N concentration was quantified against a NaNO2-N standard curve. Potential nitrification rates were measured as the change in NO2-N concentration between the aerated and frozen samples, by the soil gram dry weight (% dry matter) per hour."

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