title: Plant diversity, CO2, and N influence inorganic and organic N leaching in grasslands.
abstract: In nitrogen (N)-limited systems, the potential to sequester carbon depends on the balance between N inputs and losses as well as on how efficiently N is used, yet little is known about responses of these processes to changes in plant species richness, atmospheric CO2 concentration ([CO2]), and N deposition. We examined how plant species richness (1 or 16 species), elevated [CO2] (ambient or 560 ppm), and inorganic N addition (0 or 4 g x m(-2) x yr(-1)) affected ecosystem N losses, specifically leaching of dissolved inorganic N (DIN) and organic N (DON) in a grassland field experiment in Minnesota, USA. We observed greater DIN leaching below 60 cm soil depth in the monoculture plots (on average 1.8 and 3.1 g N x m(-2) x yr(-1) for ambient N and N-fertilized plots respectively) than in the 16-species plots (0.2 g N x m(-2) x yr(-1) for both ambient N and N-fertilized plots), particularly when inorganic N was added. Most likely, loss of complementary resource use and reduced biological N demand in the monoculture plots caused the increase in DIN leaching relative to the high-diversity plots. Elevated [CO2] reduced DIN concentrations under conditions when DIN concentrations were high (i.e., in N-fertilized and monoculture plots). Contrary to the results for DIN, DON leaching was greater in the 16-species plots than in the monoculture plots (on average 0.4 g N x m(-2) x yr(-1) in 16-species plots and 0.2 g N x m(-2) x yr(-1) in monoculture plots). In fact, DON dominated N leaching in the 16-species plots (64% of total N leaching as DON), suggesting that, even with high biological demand for N, substantial amounts of N can be lost as DON. We found no significant main effects of elevated [CO2] on DIN or DON leaching; however, elevated [CO2] reduced the positive effect of inorganic N addition on DON leaching, especially during the second year of observation. Our results suggest that plant species richness, elevated [CO2], and N deposition alter DIN loss primarily through changes in biological N demand. DON losses can be as large as DIN loss but are more sensitive to organic matter production and turnover.
authors.affiliation: Department of Ecology, Evolution and Behavior, University of Minnesota, St. Paul, Minnesota 55108, USA. fadijkstra@yahoo.com
authors.forename: Feike A
authors.initials: FA
authors.lastname: Dijkstra
authors.forename: Jason B
authors.initials: JB
authors.lastname: West
authors.forename: Sarah E
authors.initials: SE
authors.lastname: Hobbie
authors.forename: Peter B
authors.initials: PB
authors.lastname: Reich
authors.forename: Jared
authors.initials: J
authors.lastname: Trost
mesh_terms: D044822:Biodiversity; D002245:Carbon Dioxide; D009584:Nitrogen; D010944:Plants / Q000378:metabolism*; D006109:Poaceae; D012987:Soil / Q000032:analysis*
chemical_list: D012987:Soil; D002245:Carbon Dioxide; D009584:Nitrogen