95-5
Soil Carbon Variation Along Ecological Trajectories Within the U.S.

Monday, November 4, 2013: 3:00 PM
Marriott Tampa Waterside, Florida Salon I-II, Second Level

Sabine Grunwald1, Alex McBratney2, Xiong Xiong3, Baijing Cao3, Larry T. West4, Skye Wills4, Terry D. Loecke5, Budiman Minasny6, Sebastian Campbell7, Risa Patarasuk8 and Chris Wade Ross9, (1)Soil & Water Sciences Department, University of Florida, Gainesville, FL
(2)Environmental Sciences, Faculty of Agrculture and Environment, The University of Sydney, Eveleigh, Australia
(3)University of Florida, Gainesville, FL
(4)USDA-NRCS, Lincoln, NE
(5)University of Nebraska - Lincoln, Lincoln, NE
(6)Department of Environmental Sciences, The University of Sydney, Eveleigh, Australia
(7)Department of Environmental Sciences, University of Sydney, Sydney, NSW, Australia
(8)Soil and Water Science Department, University of Florida, Gainesville, FL
(9)Soil and Water Science, University of Florida, Gainesville, FL
National assessment of soil carbon across the U.S. has been based on legacy data (Soil Survey Geographic Data – SSURGO and State Soil Geographic Data – STATSGO), which have become outdated due to global climate and land use changes, and human induced disturbances imposed on soil carbon dynamics in soil ecosystems. We present a new soil carbon stock assessment using recent extensive sampling (1 m depth) at several thousand sites in different soil and land use types. We assembled space-time sequences of environmental covariates covering the U.S. from various sources (remote sensing, such as the Moderate Resolution Imaging Spectroradiometer, MODIS; National Elevation Data; temperature and precipitation from PRISM project, etc.). The characterization of soil organic and inorganic carbon stocks along lithologic, pedogenic, topographic, biotic, and climatic trajectories provides new insight into causes and effects of soil carbon accretion. In the U.S. climate change has varied profoundly spatially and temporally over the past decades. Here we present the forcings of short- and long-term climatic change on the formation and distribution of soil organic carbon within different biomes and ecoregions in the U.S. The modeling of soil carbon variation within a spatially and temporally explicit modeling framework that incorporates environmental covariates offers a new perspective on the state of knowledge on soil carbon variation in a landscape stretching over diverse climatic zones (from semiarid to wet tropical) and biomes.
See more from this Division: ASA Section: Global Agronomy
See more from this Session: Symposium--The Soil-Crop Nexus Across Spatial and Temporal Scales (includes Global Digital Soil Map Graduate Student Competition)

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