Soil Carbon
E. Berryman, Jeffrey Hatten, Deborah S. Page‐Dumroese, Katherine Heckman, David V. D’Amore, Jennifer Puttere, Michael Sanclements, Stephanie Connolly, Charles H. Perry, Grant M. Domke
Abstract
Abstract Soil organic matter (OM) is a pervasive material composed of carbon (C) and other elements. It includes the O horizon (e.g., litter and duff), senesced plant materials within the mineral soil matrix, dead organisms (including macroorganisms and microorganisms), microbial and root exudates, and organic materials adhering to mineral surfaces. Soil organic carbon (SOC) is a very dynamic component of the soil; each year, the amount of SOC processed by microorganisms within the soil is roughly equal to the amount of inputs from plant detritus. The pervasive dynamic nature of SOC is key to the ecosystem service, or “the benefits people obtain from ecosystems” (Millennium Ecosystem Assessment 2003), that SOC provides.