@article {KNZ001949,
	title = {Changes in potential nitrous oxide efflux during grassland restoration},
	journal = {Journal of Environmental Quality},
	volume = {48},
	year = {2019},
	pages = {1913-1917},
	abstract = {<p>14 Nitrous oxide efflux from soil is an important ecological process in terms of global climate 15 impacts, stratospheric chemistry, and soil fertility. The effects of grassland restoration on nitrous 16 oxide (N 2 O) efflux in formerly cultivated agricultural soils are not well known. Restoration 17 changes the storage and availability of soil C and N, with potential consequences for N 2 O efflux. 18 We examined changes in potential N 2 O efflux across a 35-year chronosequence of grassland 19 restorations, using lab incubations at moisture levels that maximized N 2 O emissions, to quantify 20 the relationship between N 2 O efflux and soil properties known to change predictably during 21 grassland restoration. We found that restoring cultivated agricultural land to grassland rapidly 22 decreased N 2 O efflux from soils, though native prairie had a potential N 2 O efflux higher than the 23 agricultural land. The oldest restoration had N 2 O efflux 50 times lower than native prairie. 24 Changes in N 2 O efflux were more strongly correlated with N mineralization than C.</p>},
	keywords = {LTER-KNZ},
	author = {Scott, D.A. and Rosenzweig, S.T. and S.G. Baer and John M. Blair}
}
@article {KNZ001752,
	title = {Changes in soil properties, microbial biomass, and fluxes of C and N in soil following post-agricultural grassland restoration},
	journal = {Applied Soil Ecology},
	volume = {100},
	year = {2016},
	pages = {186 - 194},
	abstract = {<p>Understanding the dynamics of soil C and N pools and fluxes following grassland restoration in formerly cultivated soils is needed to assess the capacity of this land-use change to return soil properties and function to pre-disturbance conditions. We examined changes in physical (bulk density) and chemical (pH, available P and N, and total stocks of C and N) properties, microbial biomass C and N, and transformation rates of C and N in soil (0\&ndash;10 cm depth) across a 35-year chronosequence of prairie restorations and never-cultivated (native) prairie to evaluate the rate and extent to which sowing native perennial plants into formerly cultivated soils returns soil to steady state conditions. Bulk density, available P, and extractable inorganic N decreased exponentially across the chronosequence. Soil pH increased linearly across the chronosequence to exceed that in native prairie soil. Total C and N stocks in cultivated soil were \&lt;50\% that of native prairie, and increased at rates of 26.2 g C m\&minus;2 year\&minus;1 and 1.68 g N m\&minus;2 year\&minus;1 across the chronosequence. In the oldest restoration, total C and N stocks were 55\% and 41\% higher than the cultivated soil, respectively. Recovery of C and N stocks to levels comparable to native prairie soil was estimated to take 350 years. Microbial biomass C and N increased 5-fold. Potential C mineralization rate was comparable to native prairie soil following two decades of restoration, and exceeded native prairie in the 35-years restoration. In situ soil CO2 efflux reached equilibrium in \&lt;30 years. Potential net N mineralization rate, however, did not exhibit a directional change across the restoration chronosequence, but was lowest in the oldest restored grasslands. Thus, cessation of tillage and sowing native vegetation leads to rapid decreases in available N and P, and promotes rapid (decadal scale) recovery of labile soil organic matter pools, but recovery of total C and N pools requires several centuries. This study suggests that soil properties related to nutrient retention and regulation of nutrient availability can be reestablished within the first few decades of restoration, while C sequestration will continue on a longer time scale.</p>},
	keywords = {LTER-KNZ, Bulk density, chronosequence, soil respiration, SOM recovery, tallgrass prairie},
	issn = {09291393},
	doi = {10.1016/j.apsoil.2016.01.001},
	url = {https://www.sciencedirect.com/science/article/pii/S0929139316300014?via\%3Dihub},
	author = {Rosenzweig, S.T. and Carson, M.A. and S.G. Baer and John M. Blair}
}
