Changes in soil properties, microbial biomass, and fluxes of C and N in soil following post-agricultural grassland restoration
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Temporal dynamics of soil properties were examined in a restoration chronosequence.

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Bulk density and available N and P declined to new steady state levels.

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Microbial C and N pools increased 5-fold during the 3.5 decades of restoration,

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In situ soil COb>2b> efflux increased to equilibrium within the 35-year chronosequence.

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Recovery of total C and N stocks are predicted to take approximately 350 years.

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