IntroductionIncreased emission of greenhouse gases such as CO 2 , methane (CH 4 ), and nitrous oxide (N 2 O) to the atmosphere is closely associated with land use change, the use of fossil fuels, forest fires, emissions from automobiles, agricultural production, and other anthropogenic activities (Sauerbeck, 2001). The CO 2 concentration of the atmosphere has changed significantly since the Industrial Revolution, increasing from 280 ppm to 390 ppm (August 2011 Mauna Loa Station, NOAA; http://co2now.org/ Current-CO2/CO2-Now/noaa-mauna-loa-co2-data. html), and it may double by the end of the 21st century if greenhouse gases continue being emitted (Lal, 2003). Soils contribute about 20% of the total CO 2 released to the atmosphere (Sauerbeck, 2001). Better management of soil organic carbon can reduce greenhouse gas emissions and increase soil fertility (Sauerbeck, 2001).Monitoring CO 2 fluxes from soils can reveal important information about microbial activity, plant root respiration, soil-atmosphere interactions, soil energy and carbon budgets, and plant production, allowing us to better understand trends and find ways to mitigate emissions (Lal, 2003). The amounts of CO 2 released from the soil to the atmosphere varies greatly based on different land use types, agricultural activities, soil characteristics, and climate (Smith et al., 2000), and it generally ranges from 0.1 to 6 g CO 2 m -2 h -1 for agricultural soils (Sauerbeck 2001). Extensive research documents how temporal and spatial variations in CO 2 emissions are controlled by soil temperature (Almaraz et al., 2009), soil water content (La Scala et al., 2006), soil organic matter content and substrate quality (Frank et al., 2006), and interaction between significant properties (Pangle and Seiler, 2002). These variables impact the activity of roots and