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洱海湖滨农田生态系统的碳收支评估

Carbon budget assessment of lakeside farmland ecosystem in Erhai Lake

  • 摘要: 在洱海湖滨农田生态系统应用涡动相关技术开展水稻和蚕豆生长季CO2通量的长期观测(2007—2012年),明确了两种作物轮作条件下农田生态系统的CO2通量变化特征和生态系统的源/汇功能。结果表明:(1)洱海湖滨农田在水稻和蚕豆两种不同下垫面时的气候条件差异较大。在水稻生长季,有较高的气温(Ta)和相对湿度(RH),饱和水汽压差(VPD)呈现先下降后平稳的趋势,太阳总辐射(Rg)波动较明显,风速(WS)和摩擦速度(ustar)呈弱的下降趋势;在蚕豆生长季,Ta呈现先下降再上升的趋势,RH表现为逐渐下降,而VPD和Rg呈上升趋势,WS和ustar呈现先上升后下降的趋势。(2)洱海湖滨农田生态系统CO2通量具有明显的日变化和季节变化特征,在日尺度表现为“U”型的日变化特征,在季节尺度表现为单峰双谷“W”型的变化特征。在水稻生长季,CO2通量的峰值出现在拔节和抽穗期;在蚕豆生长季,CO2通量的峰值出现在结荚至鼓粒期。(3)日尺度上,洱海湖滨农田生态系统CO2通量变化的主要控制因子是RH,而小时尺度上是Rg。(4)水稻-蚕豆农田生态系统总体表现为碳汇。水稻生长季净碳交换为503.8 gC.m-2,总初级生产力为866.6 gC.m-2蚕豆生长季净碳交换为143.5 gC.m-2,总初级生产力为716.2 gC.m-2,水稻生长季的固碳能力约为蚕豆的3.5倍。

     

    Abstract: A long-term observation (2007-2012) of CO2 fluxes during the rice and broad bean growing seasons was conducted in the Erhai Lake riparian farmland ecosystem using eddy covariance techniques. The study clarified the characteristics of CO2 flux changes and the source/sink function of the farmland ecosystem under the condition of crop rotation of the two crops. The results showed that: (1) The climatic conditions of the lakeside farmland in Erhai Lake are quite different when rice and broad bean are different underlying surfaces. In the rice growing season, the temperature (Ta) and relative humidity (RH) were relatively high, the saturated water vapor pressure difference (VPD) showed a trend of first decreasing and then stabilizing, the total solar radiation (Rg) fluctuated significantly, and the wind speed (WS) and friction velocity (ustar) showed a weak downward trend. In the growing season of broad bean, Ta showed a trend of first decreasing and then increasing, RH showed a gradual decrease, while VPD and Rg showed an upward trend, and WS and ustar showed a trend of first increasing and then decreasing. (2) The CO2 fluxes in the Erhai Lake riparian farmland ecosystem showed obvious diurnal and seasonal variation characteristics, showing a "U"-shaped diurnal variation pattern and a single-peak double-trough "W"-shaped seasonal variation pattern. During the rice growing season, the peak of CO2 fluxes occurred during the jointing and heading stages; during the broad bean growing season, the peak of CO2 fluxes occurred from podding to seed filling. (3) On the daily scale, the main controlling factor for the change of CO2 fluxes in the Erhai Lake riparian farmland ecosystem was RH, while on the hourly scale, it was Rg. (4) The rice-broad bean farmland ecosystem generally showed carbon sink characteristics. The net carbon exchange during the rice growing season was 503.8 gC.m-2, and the gross primary productivity was 866.6 gC.m-2; the net carbon exchange during the broad bean growing season was 143.5 gC.m-2, and the gross primary productivity was 716.2 gC.m-2. The carbon sequestration capacity of the rice growing season was about 3.5 times that of the broad bean growing season.

     

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