대기 중 CO2 변화에 따른 토양 CO2 방출량 변화 (DYNAMICS OF SOIL CO2 EFFLUX UNDER VARYING ATMOSPHERIC CO2 CONCENTRATIONS) Dohyoung Kim Duke University July 19 2016 OUTLINE Introduction Materials and methods Dynamics of soil CO2 efflux Changes in carbon assimilation Conclusion INTRODUCTION 407.42 ppm (Apr. 2016) Mean CO2 growth rate: 2 ppm/yr (2001-2010) FREE AIR CO2 ENRICHMENT (FACE) Overcome temporal and spatial limits of chamber experiments Allow investigation of undisturbed ecosystems Not modifying plant’s interaction with light, temperature, wind, precipitation, and other biological factors Allow integrated measurement of many processes Allow to study plants with extended period and space © Brookhaven National Laboratory INTRODUCTION PLANTS’ GENERAL RESPONSES Increase of Photosynthesis Leaf area Tree growth Soil moisture Soil respiration Fine-root biomass Decrease of Stomatal conductance Transpiration INTRODUCTION OBJECTIVES 1. To assess whether the termination of eCO2 alters the soil CO2 efflux in previously eCO2 plots 2. To isolate the processes influencing the amount of CO2 returning to the atmosphere from the forest floor-soil system © 2010 State of California INTRODUCTION weeks to months days to weeks Rhizosphere microorganisms exudation FCO2 respiration Atmospheric CO2 Mycorrhizal fungi Root photosynthesis allocation necromass Labile SOM Soil microorganisms decomposition months to years Recalcitrant SOM decades to centuries Leaf MATERIALS AND METHODS SITE DESCRIPTION Duke FACE site Tree age: ~30 years Dominant species Loblolly pine (Pinus taeda) Major understory Sweetgum (Liquidambar styraciflua) Winged elm (Ulmus alata) Red maple (Acer rubrum) MATERIALS AND METHODS SITE HISTORY 1983 3-yr-old seedlings were planted 1994-1995 Prototype experiment 2005-2012 N fertilization (11.2 g N m-2 yr-1) 1996 FACE started (+200 ppm) 2010-2011 Final harvest 2010 FACE ended 2011-2012 Relaxation period MATERIALS AND METHODS MANIPULATION OF CO2 CONCENTRATION Short-term late Aug. to early Oct. 5-day intervals five CO2 levels (A, +100, +150, +200, +300) two moisture conditions (REW = 0.03, 0.78) Long-term terminated on Oct. 31, 2010 monitored for two years (Tor-ngern et al., 2014) MATERIALS AND METHODS AUTOMATED CARBON EFFLUX SYSTEM (ACES) chamber-based multiport 11 chambers per plot switched between two fixed locations once a week MATERIALS AND METHODS AUTOMATED CARBON EFFLUX SYSTEM (ACES) Measurement: 10 minutes per chamber mean of last 3 minutes was used more than half available data per day per chamber Missing data unstable air flow or CO2 concentration air flow or CO2 concentration out of specific range abnormal soil CO2 effluxes periodic maintenance and recalibration occasional power outage failure of gas analyzer and tubing MATERIALS AND METHODS BAYESIAN STATE-SPACE MODEL Ft-1 Ft Ft+1 Data model Rt-1 Rt Rt+1 Process model Xt-1 τ2 Xt σ2 Xt+1 β Parameter model p (s 2 , t 2 , R, b | F ) µ N ( Ft | Rt , t 2 ) N ( Rt | Xt , s 2 ) IG (t 2 | t1, t2 ) IG (s 2 | s1, s2 ) N ( b | b0 ,Vb ) RESULTS HYPOTHESES Will soil CO2 efflux change with short- and longterm manipulation of CO2 concentration? H1: Effect of five-day CO2 changes will be reflected in changes of soil CO2 efflux (FCO2). H2: FCO2 will decline to that of aCO2 within ~3 months and remain at the level for the following two years. RESULTS MODEL PERFORMANCE RESULTS DAILY MEAN VALUES RESULTS SHORT-TERM MANIPULATION RESULTS ANNUAL INTEGRATED FCO2 RESULTS RESPONSE RATIO ~5 weeks after ~35% RESULTS RESPONSE RATIO RESULTS MONTHLY LEAF AREA AND FCO2 CHANGES IN CARBON ASSIMILATION Elevated CO2 photosynthesis A = GS × ca(1-ci/ca) Root allocation Leaf CHANGES IN CARBON ASSIMILATION Will stomatal conductance respond to termination of long-term CO2 enrichment? STOMATAL CONDUCTANCE Responses to eCO2 Direct: increase in ci stomatal closure Indirect: structural changes RESULTS Lower growing season T in 2009 Growing season M was lowest in 2010 and highest in 2012 RESULTS CHANGES IN LEAF AREA Leaf area returned to ambient level +22% +9% +40% RESULTS MONTHLY MEAN GS GS of pine in previously eCO2 increased Response of GS of sweetgum were not particularly faster than pine 0.69 1.12 0.94 0.84 0.74 0.97 0.64 1.11 RESULTS MONTHLY TRANSPIRATION Canopy transpiration in previously eCO2 maintained RESULTS CANOPY CONDUCTANCE RESULTS MONTHLY C UPTAKE AND FCO2 CNPI = GC × [CO2] ratio (canopy net photosynthesis index) CONCLUSION
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