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首页> 外文期刊>Agricultural and Forest Meteorology >CO sub(2)/heat fluxes in rice fields: Comparative assessment of flooded and non-flooded fields in the Philippines
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CO sub(2)/heat fluxes in rice fields: Comparative assessment of flooded and non-flooded fields in the Philippines

机译:稻田中CO sub(2)/热通量:菲律宾水淹和非水淹田的比较评估

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摘要

The seasonal fluxes of heat, moisture and CO sub(2) were investigated under two different rice environments: flooded and aerobic soil conditions, using the eddy covariance technique during 2008 dry season. The fluxes were correlated with the microclimate prevalent in each location. This study was intended to monitor the environmental impact, in terms of C budget and heat exchange, of shifting from lowland rice production to aerobic rice cultivation as an alternative to maintain crop productivity under water scarcity. The aerobic rice fields had higher sensible heat flux (H) and lower latent heat flux (LE) compared to flooded fields. On seasonal average, aerobic rice fields had 48% more sensible heat flux while flooded rice fields had 20% more latent heat flux. Consequently, the aerobic rice fields had significantly higher Bowen ratio (0.25) than flooded fields (0.14), indicating that a larger proportion of the available net radiation was used for sensible heat transfer or for warming the surrounding air. The total C budget integrated over the cropping period showed that the net ecosystem exchange (NEE) in flooded rice fields was about three times higher than in aerobic fields while gross primary production (GPP) and ecosystem respiration (R sub(e)) were 1.5 and 1.2 times higher, respectively. The high GPP of flooded rice ecosystem was evident because the photosynthetic capacity of lowland rice is naturally large. The R sub(e) of flooded rice fields was also relatively high because it was enhanced by the high photosynthetic activities of lowland rice as manifested by larger above-ground plant biomass. The NEE, GPP, and R sub(e) values for flooded rice fields were -258, 778, and 521gCm super(-) super(2), respectively. For aerobic rice fields, values were -85, 515, and 430gCm super(-) super(2) for NEE, GPP, and R sub(e), respectively. The ratio of R sub(e)/GPP in flooded fields was 0.67 while it was 0.83 for aerobic rice fields. This short-term data showed significant differences in C budget and heat exchange between flooded and aerobic rice ecosystems. Further investigation is needed to clarify seasonal and inter-annual variations in microclimate, carbon and water budget of different rice production systems.
机译:在2008年旱季期间,使用涡度协方差技术研究了两种不同的水稻环境(淹水和好氧土壤条件)下的热量,水分和CO sub(2)的季节性通量。通量与每个位置普遍存在的微气候相关。这项研究旨在监测碳预算和热交换方面的环境影响,即从低地水稻生产向需氧水稻种植转移,以在缺水的情况下维持作物生产力。与淹水田相比,好氧稻田具有较高的显热通量(H)和较低的潜热通量(LE)。平均而言,好氧稻田的感热通量增加48%,而淹水稻田的潜热通量增加20%。因此,好氧稻田的鲍恩比(0.25)明显高于淹水田(0.14),这表明较大的可用净辐射量用于显热传递或加热周围的空气。整个种植期的碳预算总额表明,淹水稻田的净生态系统交换量(NEE)是有氧田地的三倍,而初级生产总值(GPP)和生态系统呼吸(R sub(e))为1.5和分别高1.2倍。水稻泛滥的生态系统具有较高的GPP,这很明显,因为低地水稻的光合作用能力自然很高。淹水稻田的R sub(e)也相对较高,因为低地稻的高光合作用增强了Rsub(e),这表现为地上植物生物量较大。淹水稻田的NEE,GPP和R sub(e)值分别为-258、778和521gCm super(-)super(2)。对于有氧稻田,NEE,GPP和R sub(e)的值分别为-85、515和430gCm super(-)super(2)。淹水田中R sub(e)/ GPP的比率为0.67,而好氧稻田中的比率为0.83。这项短期数据表明,淹水和好氧水稻生态系统之间的碳平衡和热交换存在显着差异。需要进一步调查以弄清不同水稻生产系统的小气候,碳和水预算的季节性和年度间变化。

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