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Separation of ‘Autotrophic’ and ‘Heterotrophic’ Respiration in an Oak-Grass Savanna and their Link with Canopy Photosynthesis. Dennis Baldocchi, Jianwu Tang & Liukang Xu. Biometeorology Lab Dept Environmental Science, Policy and Mgt University of California, Berkeley.
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Separation of ‘Autotrophic’ and ‘Heterotrophic’ Respiration in an Oak-Grass Savanna and their Link with Canopy Photosynthesis Dennis Baldocchi, Jianwu Tang & Liukang Xu Biometeorology Lab Dept Environmental Science, Policy and Mgt University of California, Berkeley CarboEurope, Crete, 2006
Outline • Introduction • Quantifying Roles of Lags, Pulses and Switches • Objectives • Methods • Site Description • Continuous Soil CO2 Measurements • Flux-gradient measurements • Results and Discussion • Responses to temperature, rain pulses and photosynthetic activity • Test with Eddy Covariance
Partitioning Soil Respiration: Principles Kuyzakov 2006
Girdling Experiment Hogberg et al. 2000, Nature
Experimental Treatments Under a Tree: ~Ra+Rh Open Grassland: ~Rh (summer)
Continuous Soil Respiration with soil CO2 Sensors [CO2] must be corrected for temperature
Theory/Equations Moldrup et al. 1999 Fcp: fraction silt and sand; b: constant; f:porosity; e: air-filled pore space
Validation with Chambers Baldocchi et al. JGR Biogeoscience, 2006
Validation with EC Baldocchi et al. JGR Biogeoscience, 2006
What Happens After Rain? • Microbial Stimulation • It occurs for 4 days, until the soil dries • Evacuation of Pores • cannot be sustained for several days
Effects of temperature, soil moisture, rain and photosynthesis on CO2 Efflux Baldocchi et al. JGR Biogeoscience, 2006
When Does Root Respiration Initiate?: Prior, Coincident or After the Start of Photosynthesis Canopy Ps starts ~d80 Rauto starts ~d100
Temperature:hysteresis and lags Tang et al GCB 2005
Why?:Respiration Lags Photosynthesis, v1:Hourly Scale Tang et al GCB 2005
Continuous Measurements Enable Use of Inverse Fourier Transforms to Quantify Lag Times Tang et al GCB 2005
Respiration Lags Photosynthesis, v2:Daily Scale Tang et al GCB 2005
Conclusions • Profile systems with soil CO2 sensors can be used to measure soil respiration with confidence • Natural gradients can be used to separate effects of autotrophic and heterotrophic respiration • Recent photosynthate is translocated to the soil and stimulates soil respiration • This causes a decoupling between soil respiration and soil temperature • Soil respiration under active trees is much greater than under dead grass
Biometeorology Team Liukang Xu Jianwu Tang Ted Hehn Funding: US DOE/TCP; WESTGEC/NIGEC; Kearney Soil Science Found.,Ca Ag Expt Station, AmeriFlux