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Monitoring of carbon dioxide and water vapour exchange over a young mixed forest plantation using eddy covariance technique

机译:使用涡度协方差技术监测年轻混交林中的二氧化碳和水蒸气交换

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Studies on CO2 and water vapour exchange in natural and man-made vegetation are necessary for quantifying their role in landscape-level carbon budget. The present study investigated variations in carbon and water vapour fluxes and monthly net ecosystem exchange (NEE) over a 9-year-old mixed forest plantation (Holoptelea integrifolia, Dalbergia sissoo, Acacia catechu and Albizia procera) in Terai Central Forest Division of Nainital district, Uttarakhand using January to September 2013 eddy covariance data. During leafless period (i.e. January), the plantation acted as a net carbon source (i.e. positive NEE) with daily mean release of 0.35 g C m(-2) day(-1), while from leaf onset to growing period (i.e. April to September), it acted as a sink (i.e. negative NEE) due to carbon uptake by an increasing number of leaves. The monthly mean daily NEE was noticed to be increasingly more negative in each subsequent month until September. The diurnal trend in NEE closely followed the variations in the intensity of photosynthetically active radiation. The diurnal NEE in all months was related to vapour pressure deficit with time-lag. Maximum daytime uptake (-29.5 mu mol m(-2) s(-1)) and night-time release of CO2 (8.2 mu mol m(-2) s-1) was observed in July. Monthly mean of daily NEE over plantation continuously increased from February and was highest (-5.74 g C m(-2) day(-1)) in September. Rectangular hyperbolic function provided reasonably good fit between NEE and PAR. Ecosystem parameters (alpha and P-max) of the light response curve also followed the canopy development trend.
机译:必须对自然和人造植被中的二氧化碳和水蒸气交换进行研究,以量化它们在景观水平碳预算中的作用。本研究调查了位于奈尼塔尔地区特赖中央森林分部的一个9年生混交林(Holoptelea integrifolia,Dalbergia sissoo,Acacia catechu和Albizia procera)的碳和水蒸气通量以及每月净生态系统交换(NEE)的变化。 ,Uttarakhand使用2013年1月至2013年9月的涡度协方差数据。在无叶时期(即一月),人工林作为净碳源(即正NEE),从叶生病到生长期(即四月),日平均释放量为0.35 g C m(-2)day(-1)。到9月),由于越来越多的叶子吸收了碳,它充当了一个汇(即NEE负值)。到9月为止,随后的每个月的平均每日NEE值都变得越来越负。 NEE的昼夜趋势紧随光合有效辐射强度的变化。所有月份的日均NEE值与时滞的蒸气压缺乏有关。 7月观察到最大的白天摄入量(-29.5μmolm(-2)s-1)和夜间释放的CO2(8.2μmolm(-2)s-1)。从2月开始,人工林的每日NEE的月平均数从2月份开始持续增加,并且在9月份最高(-5.74 g C m(-2)day(-1))。矩形双曲线函数在NEE和PAR之间提供了相当好的匹配度。光响应曲线的生态系统参数(α和P-max)也遵循冠层发展趋势。

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