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首页> 外文期刊>Soil and Water Research >Methane production potential of soil profile in organic paddy field
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Methane production potential of soil profile in organic paddy field

机译:有机稻田土壤剖面甲烷生产潜力

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The use of organic fertilizers in the organic paddy/rice field can increase methane (CH 4 ) production, which leads to environmental problems. In this study, we aimed to determine the CH 4 production potential (CH 4 -PP) by a soil profile from samples using flood incubation. Soil properties (chemical, physical, and biological) were analyzed from soil samples of three different paddy farming systems (organic, semi-organic, and conventional), whilst soil from teak forest was used as the control. A significant relationship was determined between soil properties and CH 4 -PP. The average amount of CH 4 -PP in the organic rice field profile was the highest among all the samples (1.36 μg CH 4 /kg soil/day). However, the CH 4 oxidation potential (CH 4 -OP) is high as well, as this was a chance of mitigation options should focus on increasing the methanotrophic activity which might reduce CH 4 emissions to the atmosphere. The factor most influencing CH 4 -PP is soil C-organic (C org ). C org and CH 4 -PP?of the top soil of organic rice fields were 2.09% and 1.81 μg CH 4 /kg soil/day, respectively. As a consequence, here the mitigation options require more efforts than in the other farming systems. Soil with various amounts of C org reached a maximum point of CH 4 -PP at various time after incubation (20, 15, and 10 days for the highest, medium, and the lowest amounts of C org , respectively). A high amount of C org provided enough C substrate for producing a higher amount of CH 4 and reaching its longer peak production than the low amount of C org . These findings also provide guidance that mitigation option reduces CH 4 emissions from organic rice fields and leads to drainage every10–20 days before reaching the maximum CH 4 -PP.
机译:在有机稻田/水稻田中使用有机肥料会增加甲烷(CH 4 )的产量,从而导致环境问题。在这项研究中,我们旨在通过洪水孵育通过土壤剖面确定CH 4 的生产潜力(CH 4 -PP)。从三种不同稻田耕作系统(有机,半有机和常规)的土壤样品中分析了土壤特性(化学,物理和生物学),而柚木林的土壤用作对照。土壤性质与CH 4 -PP之间存在显着关系。在所有样品中,有机稻田剖面中CH 4 -PP的平均含量最高(1.36μgCH 4 / kg土壤/天)。但是,CH 4 的氧化电位(CH 4 -OP)也很高,因为这是一个缓解措施,应着重于提高甲烷营养活性,这可能会降低CH 4 排放到大气中。影响CH 4 -PP的最主要因素是土壤C-有机(C org )。有机稻田表层土壤C org 和CH 4 -PP?/ kg土壤/天分别为2.09%和1.81μgCH 4 / kg , 分别。结果,与其他耕种系统相比,此处的缓解措施需要更多的努力。孵育后不同时间(最高,中值和最高值分别为20、15和10天),具有各种C org 的土壤在CH 4 -PP的最高点。分别为C org 的最低数量)。大量的C org 提供了足够的C底物,以产生比少量的C org更高的CH 4 并达到更长的峰值产生。子>。这些发现还为减缓选择减少有机稻田CH 4 的排放并在达到最大CH 4 -PP之前每10–20天引流提供了指导。

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