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Variations of carbon dioxide exchange in paddy field ecosystem under water-saving irrigation in Southeast China

机译:东南节水灌溉下稻田生态系统中二氧化碳交换的变化

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Based on the results of continuous flux measurements in the Taihu Lake Region of China, the carbon dioxide (CO2) exchange of paddy fields under water-saving irrigation and its influence factors were analyzed. The net ecosystem exchange of CO2 (NEE) were negative during the daytime and positive at night, and the minimum value appeared around noon. The peak CO2 uptake in the flourishing period was approximately 1.5 times the values observed in the tillering and ripening stages. Frequent alternation of wetting and drying in paddy fields with water-saving irrigation resulted in larger NEE for the typical day before soil rewatering than that for the day after soil rewatering in the early growth stage. These alterations had a minimal effect on diurnal variation of NEE in the late rice growth stage. The average NEE for the typical days after soil rewatering in July and August were 2.30 and 1.38 times that before soil rewatering, respectively. CO2 exchange in paddy field ecosystem under water-saving irrigation displayed seasonal variation with the change of rice plant growth. The total ecosystem respiration (Re.), NEE and gross primary productivity (GPP) were 1996.88, -1284.15 and 3281.03 g m(-2), respectively, throughout the growth stage. These results showed that the paddy field ecosystem under water-saving irrigation was a sink for atmospheric CO2. Frequent alternation of wetting and drying processes increased the ecosystem reparation of paddy fields under water-saving irrigation and produced smaller net CO2 absorption compared to that of flooding irrigation. The net CO2 absorption because of plant photosynthesis during the daytime and the net CO2 release at night measured by static transparent chamber method were larger than those measured by eddy covariance method (P 0.05). The nighttime respiration of paddy field ecosystem under water-saving irrigation increased exponentially with temperature. Additionally, a larger temperature sensitivity coefficient (Q(10)) was observed for paddy fields under water-saving irrigation compared to that under flooding irrigation. The photosynthetic photon flux density (PPFD) was the most important factor for regulating daytime GPP. And the light saturation point during the heading-flowering and milk stages of paddy field ecosystem with water-saving irrigation (1500 mu mol m(-2) s(-1)) was higher than that of fields with flooding irrigation in previous studies. A significant positive correlation was found between the leaf area index (LAI) and the daily GPP. ((C)) 2015 Elsevier B.V. All rights reserved.
机译:基于中国太湖地区的连续通量测量结果,分析了节水灌溉下稻田的二氧化碳交换及其影响因素。白天生态系统净CO2交换量(NEE)为负,晚上为正,最小值在中午左右出现。在旺盛时期吸收的最高CO2约为分ing和成熟阶段观察到的值的1.5倍。在节水灌溉下,稻田经常发生湿润和干燥交替变化的情况,因此,在土壤复水之前的典型一天的NEE比生长初期土壤复水后的更大。这些改变对水稻生育后期的NEE日变化影响很小。 7月和8月土壤复水后典型日子的平均NEE分别是土壤复水前的2.30和1.38倍。节水灌溉下稻田生态系统中的CO 2交换随水稻生长变化而呈现季节变化。在整个生长阶段,总生态系统呼吸(Re。),NEE和总初级生产力(GPP)分别为1996.88,-1284.15和3281.03 g m(-2)。这些结果表明,节水灌溉下的稻田生态系统是大气中CO2的汇。与节水灌溉相比,频繁进行的干湿交替改变增加了节水灌溉下稻田的生态系统修复,并产生了较小的净二氧化碳吸收量。静态透明室法测得的白天植物光合作用引起的净CO2吸收量和夜间的净CO2释放量大于涡动协方差法测得的净CO2吸收量(P <0.05)。节水灌溉下稻田生态系统夜间呼吸作用随温度呈指数增加。此外,与节水灌溉相比,节水灌溉稻田的温度敏感性系数(Q(10))更大。光合光子通量密度(PPFD)是调节白天GPP的最重要因素。节水灌溉(1500μmol m(-2)s(-1))在稻田生态系统抽穗开花和抽乳期的光饱和点高于以往研究中的水淹灌溉。在叶面积指数(LAI)和每日GPP之间发现了显着的正相关。 ((C))2015 Elsevier B.V.保留所有权利。

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