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95 Carbon dioxide efflux from stems and soil during a cottonwood dry-down experiment under low and high atmospheric CO2. Johnsen, Kurt1, Butnor, John1, Maier, Chris1, Murthy, Rameesh2, 1 2 ABSTRACT- Cottonwood (Populus deltoides) trees, located in Biosphere 2 (Oracle, AZ), grew from cut stumps from April 15, 2000. Trees were grown in two compartments under low (430 ppm) or high (1200 ppm) atmospheric CO2. Beginning in November 2000, the trees were subjected to increased water stress via step-wise increases in soil and atmospheric drought. During the dry-down, a sub-set of trees was continuously measured for both stem and soil CO2 efflux; soil chambers were placed at the base of the tree and between rows. There was high among-location variation in soil CO2 efflux that precluded response surface analyses; however, over the course of the dry-down, soil CO2 efflux rates declined by 14% and 39% under low and high atmospheric CO2, respectively. The greater reduction under elevated CO2 was due to a more rapid and severe dry-down of the soil due to greater leaf areas in the high atmospheric CO2 stands. Despite the high among-location variation, both tree position and treatment effects were strong. Under low atmospheric CO2, soil CO2 efflux at the base of the trees averaged 5.03 mmol CO2 m2 s-1 while inter-row CO2 efflux was 3.94 mmol CO2 m2 s-1. Values in the high CO2 compartment were 7.27 (tree-base) and 6.91 mmol CO2 m2 s-1 (inter-row). Thus, an increase in atmospheric CO2 of 300% was associated with an increase in soil CO2 efflux of 68%. KEY WORDS: Populus deltoides , drought, respiration |