Soil organic matter quality interpreted thermodynamically

Soil organic matter quality in the sense of how easily carbon in the soil organic matter can be mineralised is a major determinant of soil carbon storage and rate of mineralisation of nutrients. Its origin has so far remained elusive and a number of indices, such as C-to-N-ratio, lignin concentration and other combinations of chemical constituents have been used as substitutes for quality. We suggest here that quality is the number of enzymatic steps required to release as carbon dioxide a carbon atom from an organic compound. The larger the number of steps the lower is the quality of the carbon atom. Such a measure connects quality to thermodynamics. It also explains the rapid decrease in decomposition rate with decreasing quality suggested in the q-theory of organic matter dynamics and shows that the decomposition rate of low quality substrates has a stronger temperature dependence than that of high quality substrates.