The Effect of Extreme Temperatures on Soil Organic Matter Decomposition From Oak Forest Ecosystems

This work designs a heatwave with a calorimeter to analyse the response of soils from oak forest ecosystems to increasing temperature from 20 to 60oC and to cooling from 60  to 20oC. Calorimetry measures the heat rate of the soil organic matter decomposition and the response to increasing and decreasing temperatures directly. It was applied to soil samples representing different soil horizons with organic matter at different degree of decomposition given by their heat of combustion determined by DSC. Results showed temperature-dependent decomposition rates from 20 to 40 or 50oC typical for enzymatic activity. From 40 to 60oC changes in the rates are less predictable. Data analysis during cooling showed that all samples suffered losses of their enzymatic capacity and that only those with the heat of combustion values close to that of carbohydrates resisted the heat wave.