Chin J Plant Ecol ›› 2008, Vol. 32 ›› Issue (5): 1041-1051.DOI: 10.3773/j.issn.1005-264x.2008.05.009

Special Issue: 碳水能量通量

• Original article • Previous Articles     Next Articles

DROUGHT EFFECTS ON CARBON EXCHANGE IN A SUBTROPICAL CONIFEROUS PLANTATION IN CHINA

GU Feng-Xue1, YU Gui-Rui2,*(), WEN Xue-Fa2, TAO Bo2, LI Ke-Rang2, LIU Yun-Fen2   

  1. 1Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences, Key Laboratory of Agro-Environment & Climate Change, Ministry of Agriculture, Beijing 100081, China
    2Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
  • Received:2007-12-06 Accepted:2008-02-25 Online:2008-12-06 Published:2008-09-30
  • Contact: YU Gui-Rui

Abstract:

Aims Drought effects on terrestrial ecosystems are a key issue in global change research. This study was designed to 1) analyze effects of drought on carbon exchange in a subtropical coniferous plantation; 2) elucidate the sensitivity of carbon exchange to different degree of water deficit and the critical values when the ecosystem converts from carbon sink to source and 3) investigate the main factors that control ecosystem carbon exchange when drought occurs.

Methods The CEVSA2 model, which incorporated several significant modifications based on the CEVSA process-based ecosystem model and has been tested by using eddy covariance observation in different forest ecosystems, was parameterized by using site-specific ecophysiological measurements. Drought scenarios were designed to analyze effects on annual carbon budget and to elucidate the main control factors.

Important findings Drought decreases ecosystem production and carbon exchange significantly. Compared with simulation of no drought effect scenario, the droughts in 2003 and 2004 decrease annual net ecosystem production (NEP) by 63% and 47%, respectively. Ecosystem photosynthesis and respiration respond to drought differently, and the more rapid decrease of gross ecosystem production (GEP) than ecosystem respiration (Re) lead to the decrease of NEP when drought occurs. As daily average vapor pressure deficit (VPD) rises above 1.5 kPa, GEP, Re and NEP begin to decrease; When VPD rises above 2.5 kPa and relative soil water content (RSW; soil water content/saturated soil water content) decreases below 40%, the ecosystem converts from a carbon sink to source. Soil water deficit, which is the main factor controlling the ecosystem carbon exchange, accounts for 46% to the decrease of total annual NEP in 2003 and 2004, and atmospheric drought accounts for only 4%.

Key words: CEVSA2 model, drought effect, carbon exchange, subtropical coniferous plantation, eddy covariance