2008 Joint Annual Meeting (5-9 Oct. 2008): Nitrate in Soils Capped by Desert Pavement, Mojave Desert, California

58-1 Nitrate in Soils Capped by Desert Pavement, Mojave Desert, California



Monday, 6 October 2008
George R. Brown Convention Center, Exhibit Hall E
Robert Graham, Soil & Water Sciences Program, University of California, Department of Environmental Sciences, Riverside, CA 92521-0424, Christopher Amrhein, Environmental Sciences, University of California, Riverside, 900 University Ave, Riverside, CA 92521 and Yvonne A. Wood, Cooperative Extension, University of California, 2665 Highland Drive, Bishop, CA 93514-3023
We have found exceptionally high nitrate levels (up to 12,750 kg/ha) at shallow depths (?1 m) in soils mantled by desert pavement. Nearby soils without desert pavement had nitrate contents that were one to two orders of magnitude lower. The soil conditions coincident with desert pavement (i.e., stability, antiquity, and virtually no leaching) favor the retention and accumulation of nitrate delivered by atmospheric deposition or fixed in situ. The nitrate stored in soils under desert pavement is a previously unrecognized pool of nitrogen with the potential to increase the global nitrogen inventory for near-surface desert soils to five times the previous estimates. Its near-surface occurrence makes this labile nitrogen pool particularly susceptible to mobilization by climate change or human disturbance, risking contamination of surface and ground waters.