Value of Soil Organic Carbon in Agricultural Lands

Immediate efforts to increase soil carbonsequestration and minimize terrestrialgreenhouse gas emissions are needed tomitigate global warming. Whether or notterrestrial stocks become sinks or netsources of C over the next century willdepend upon how fast and at what level weare able to stabilize carbon dioxidelevels. The cost of soil C sequestrationis at present relatively low compared toother C emission reduction technologiesmaking soil C sinks an important short-termsolution to be used while competingtechnologies are developed. However,efforts to use C sequestration in soils asCO2 emissions offsets have facednumerous challenges. Difficultiesassociated with C stock validation (directmeasurement) and the impermanence andsaturability of soil C reservoirs raiseconcerns over whether soil C reservoirs aregood long-term investments. Pragmatism hasled to the development of indirectinventorying of the C reserves held atnational and regional scales. Suchindirect accounting systems will advance asvalidation methods are refined and asprocess models improve their ability toaccurately predict how existing soilcondition and specific land managementpractices will influence soil C storage andNO2 and CH4 emissions. Improveddocumentation of the value of environmentalservices and sustained productive potentialderived from optimized land use andassociated increases in soil quality willalso add to the estimated value of soil Csinks. Policies must evolve simultaneouslywith the theoretical and technical toolsneeded to promote optimization of land usepractices to mitigate climate change nowand to minimize future contributions ofsoil C to atmospheric CO2.