301-5 Carbon Dynamics of Agroforest Systems in the Lower Mississippi Alluvial Valley.

Poster Number 2026

See more from this Division: S07 Forest, Range & Wildland Soils
See more from this Session: Soil Carbon, Nutrients, and Greenhouse Gases From Managed Forest and Range Systems
Tuesday, October 23, 2012
Duke Energy Convention Center, Exhibit Hall AB, Level 1
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Kristin M. McElligott, Arkansas Forest Resources Center, University of Arkansas Division of Agriculture, Monticello, AR, Hal Liechty, School of Forest Resources, University of Arkansas at Monticello, Monticello, AR, Kristofor R. Brye, Crop, Soil and Environmental Sciences, University of Arkansas, Fayetteville, AR and Michael Blazier, Louisiana State University AgCenter, Homer, LA
Poster Presentation
  • McElligottSSSA2012final.pdf (1.5 MB)
  • Agroforest management systems that integrate switchgrass and trees have the potential to yield high cellulosic biomass production along with a suite of other ecosystem services.  When managed as biofuel feedstocks, switchgrass (Panicum virgatum L.) and eastern cottonwood (Populus deltoides L.) have high potential for sequestering carbon (C) due to their high growth rates, minimal resource requirements, and ability to grow on marginal lands.  In 2009, we established a long-term agroforest study at three locations in the Lower Mississippi Alluvial Valley in order to compare C flux and sequestration rates associated with switchgrass, and eastern cottonwood relative to those in conventional row cropping systems (i.e., soybean-sorghum rotation) grown on marginal soils.  The three years since establishment, we have quantified net total above- and below-ground biomass C, seasonal soil CO2 flux, as well as C, N, and labile C in soil.  In the third year, aboveground biomass production of the switchgrass and cottonwood was as great as 7.20 and 3.23 dry tons/acre, respectively—each considerably higher than the conventional soybean row crop (1.8 dry tons/acre).  Spring CO2 flux rates were greater in the conventional row and switchgrass crops than in the cottonwood, suggesting that cottonwood systems may be better able to lower soil CO2 emissions.  An assessment of these cropping systems on plant-soil carbon dynamics will be presented as a synthesis of spring and summer 2012 soil CO2 flux rates and their relation to soil and biomass C, and nitrogen pools to better understand the long-term impact of these cropping systems on ecosystem services.
    See more from this Division: S07 Forest, Range & Wildland Soils
    See more from this Session: Soil Carbon, Nutrients, and Greenhouse Gases From Managed Forest and Range Systems