Thermodynamic Control of the Carbon Budget of a Peatland

The transformations and transitions of organic matter into, through, and out of an ecosystem must obey the second law of thermodynamics. This study considered the transition in the solid components of the organic matter flux through an entire ecosystem. Organic matter samples were taken from each organic matter reservoir and fluvial transfer pathway in a 100% peat-covered catchment (Moor House National Nature Reserve, North Pennines, UK) and were analyzed by elemental analysis and bomb

calorimetry. The samples analyzed were as follows: bulk aboveground and belowground biomass; individual plant functional types (heather, mosses, and sedges); plant litter layer; peat soil; and samples of particulate and dissolved organic matter (POM and DOM). Samples were compared to standards of lignin, cellulose, and plant protein. It was possible to calculate: enthalpy of formation (ΔHƒOM); entropy of formation (ΔSƒOM); and Gibbs free energy of formation (ΔGƒOM)

for each of the samples and standards. The increase (decreasing

negative values) in ΔGƒOM through the ecosystem mean that for all but litter production, the transformations through the system must be balanced by production of low (large negative values) ΔGƒOM products, not only CO₂ or CH₄ but also DOM. The change in ΔGƒOM down the peat profile shows that reaction of the soil organic matter decreases or even ceases at depth and the majority of the reaction has occurred above 40 cm below the surface. This approach represents a new objective way to test and trace organic matter transformations in and through an ecosystem.