SSSAJ Journal of Natural Resources and Life Sciences Education
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Fig. 1. Soil mineral N in the Brady sandy loam, Fox loamy sand, Conestogo loam, Perth silt loam, and Brookston clay loam after the 1-mo incubation as affected by water-filled pore space, relative compaction, and legume treatments. The dashed line represents the initial mineral N levels in the soil.





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