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Measuring the rhizodeposition of carbon by rice: an approach based on carbon flux observations

机译:用稻米测量碳的无溶解沉积:一种基于碳通量观测的方法

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Rhizodeposition is an important component of carbon cycling in terrestrial ecosystems. However, there remains tremendous uncertainty in its quantification due to the methodological limitations. In the present study, we propose a method to evaluate the rhizodeposition by plants by observing carbon flux. We investigated the ecosystem CO2 flux variability and calculated the rhizodeposition of carbon by the rice rhizosphere, by using the carbon flux, meteorological data, and biomass observation from 2003 to 2011 at the Taoyuan Agro-ecological Experimental Station, a representative subtropical paddy ecosystem. Our data indicated that the process of rhizodeposition is the major reason for the discrepancy between the biomass and net primary productivity of the paddy ecosystem under intensive human interference. Both the amount and ratio of rhizodeposition of carbon in this paddy ecosystem were assessed; this provides important theoretical and methodological support for further investigating rhizodeposition by rice under field conditions. The rhizodeposition amount in the growing season of early rice, late rice, and for the entire planting period was 0.52-2.56, 0.74-3.75, and 1.61-5.24 t ha(-1), respectively, with the corresponding mean (+/- SD) rhizodeposition ratios of 23.16 +/- 8.87%, 28.16 +/- 12.94%, and 27.00 +/- 9.3%. This method enabled us to calculate rhizodeposition under in situ conditions, and the results showed that the growing season of late rice was the primary period for rhizodeposition in rice ecosystem.
机译:罗唑是陆地生态系统中碳循环的重要组成部分。然而,由于方法论限制,仍然存在巨大的不确定性。在本研究中,我们提出了一种通过观察碳通量来评估植物的无状沉积的方法。我们调查了生态系统CO2助焊剂变异性,并计算了水稻根际的碳的无溶解沉积,通过使用2003年至2011年在桃园农业生态实验站,代表亚热带稻草生态系统。我们的数据表明,Rhizodeposition的过程是在密集的人类干扰下稻田生态系统的生物量和净初级生产力之间差异的主要原因。评估了该稻田生态系统中碳的碳的量和比例均进行评估;这提供了在现场条件下进一步研究水稻的无状沉积的重要理论和方法支持。早稻,晚稻和整个种植时期生长季节的rhizodeposition含量分别为0.52-2.56,0.74-3.75和1.61-5.24 t ha(-1),相应的平均值(+/- SD)RhizoDeposition比例为23.16 +/- 8.87%,28.16 +/- 12.94%和27.00 +/- 9.3%。该方法使我们能够在原位条件下计算无状泡,结果表明,晚稻的生长季节是水稻生态系统中的酸石溶剂的主要时期。

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