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Environmental Factors Controlling Soil Respiration in Three Semiarid Ecosystems

Richard T. Conanta, Jeffrey M. Klopatekb,c and Carole C. Klopatekb,c

a Natural Resource Ecology Lab., Colorado State Univ., Fort Collins, CO 80523-1499 USA
b Dep. of Botany, Arizona State Univ., Tempe, AZ 85287-1601 USA
c USDA Forest Service, c/o Dep. of Microbiology, Arizona State Univ., Tempe, AZ 85287-2701 USA



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Fig. 1 Summary of experimental design showing all mesocosms incubated at each site. Mesocosm types indicate the site of origin and cover type. Four replicates of each mesocosm type are shown

 


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Fig. 2 Seasonal pattern of soil moisture for the three PJ mesocosm types incubated at each of the three incubation sites (DS, desert scrub; PJ, pinyon–juniper; PP, ponderosa pine). Values are the average of four replicate measurements (±95% confidence intervals)

 


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Fig. 3 Seasonal pattern of soil respiration for the three PJ mesocosm types incubated at each of the three incubation sites (DS, desert scrub; PJ, pinyon–juniper; PP, ponderosa pine). Values are the average of four replicate measurements (±95% confidence intervals)

 


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Fig. 4 Average soil respiration (±95% confidence intervals) for six mesocosm types at the desert scrub (DS), pinyon–juniper woodland (PJ), and ponderosa pine forest (PP) Sites. Soil respiration values are normalized per unit C in each mesocosm (including soil, litter, and duff). Names of mesocosms indicate the site of origin and cover type (interspace [i], juniper canopy [j], pinyon canopy [p], or ponderosa canopy [pp])

 





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