JEQ Journal of Natural Resources and Life Sciences Education
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Figure 1


Fig. 1. Seasonal mean CO2 evolution rates (a) and specific mineralization rates of soil organic carbon (RESPsp) (b) from no-tillage (NT) and conventional-tillage (CT) soils in DeKalb, Monmouth (from Yoo and Wander, 2006), and Perry, IL. If the letters above data from each location are not the same, then means were significantly different at P < 0.05.





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