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首页> 外文期刊>Agricultural and Forest Meteorology >Long term observations of carbon dioxide exchange over cultivated savanna under a Sudanian climate in Benin (West Africa)
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Long term observations of carbon dioxide exchange over cultivated savanna under a Sudanian climate in Benin (West Africa)

机译:在贝宁(西非)的苏丹气候下,在人工稀树草原上进行二氧化碳交换的长期观测

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Turbulent CO2 exchanges between a cultivated Sudanian savanna and the atmosphere were measured during 29 months (August 2007-December 2009) by an eddy-covariance system in North-Western Benin, West Africa. The site (Lat 9.74 degrees N, Long 1.60 degrees E, Alt: 449 m) is the one of three sites fitted out by the international AMMA-CATCH program. The flux station footprint area is mainly composed of herbs and crops with some sparse trees and shrubs. Fluxes data were completed by an inventory of dominating species around the tower and the meteorological measurements. Flux response to climatic and edaphic factors was studied. Water was found the main controlling factor of ecosystem dynamics: much larger uptake was found in wet than dry season. During wet season, a very clear answer of net CO2 fluxes to photosynthetic photon fluxes density (PPFD) was observed. A low limitation in response to saturation deficit and soil water variability was however observed. The total ecosystem respiration (TER) was found highly dependent on soil moisture below 0.1 m(3) m(-3), but saturates above this threshold. The average annual carbon sequestration was 232 +/- 27 gC m(-2) with its inter-annual variability mainly controlled by TER. Finally, the ecosystem appeared more efficient during morning and wet season than during afternoon and dry period
机译:在西非贝宁西北部的涡旋协方差系统测量了29个月(2007年8月至2009年12月)中苏丹人工稀树草原与大气之间的湍流CO2交换。该站点(北纬9.74度,东经1.60度,高度:449 m)是国际AMMA-CATCH计划选出的三个站点之一。通量站的足迹区域主要由草药和农作物组成,并有一些稀疏的树木和灌木丛。通量数据由塔周围主要物种的清单和气象测量数据完成。研究了对气候和水文因素的通量响应。人们发现水是生态系统动力学的主要控制因素:在潮湿季节比干旱季节吸收的水分要多得多。在雨季,观察到净CO2通量对光合光子通量密度(PPFD)的明确回答。然而,观察到对饱和度不足和土壤水分变异性的低限制。发现总的生态系统呼吸(TER)高度依赖于0.1 m(3)m(-3)以下的土壤水分,但高于该阈值时饱和。年平均碳固存量为232 +/- 27 gC m(-2),其年间变化主要由TER控制。最后,早午和湿季的生态系统似乎比午后和干旱的时期更有效率

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