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气体捕集和微生物 NO 还原减少了生物炭改良砂壤土中 NO 的排放。

Gas entrapment and microbial NO reduction reduce NO emissions from a biochar-amended sandy clay loam soil.

机构信息

Geomicrobiology &Microbial Ecology, Center for Applied Geosciences, University of Tuebingen, Tuebingen, Germany.

Fertilization and Soil Matter Dynamics, Institute of Crop Science, University of Hohenheim, Stuttgart, Germany.

出版信息

Sci Rep. 2016 Dec 23;6:39574. doi: 10.1038/srep39574.

Abstract

Nitrous oxide (NO) is a potent greenhouse gas that is produced during microbial nitrogen transformation processes such as nitrification and denitrification. Soils represent the largest sources of NO emissions with nitrogen fertilizer application being the main driver of rising atmospheric NO concentrations. Soil biochar amendment has been proposed as a promising tool to mitigate NO emissions from soils. However, the underlying processes that cause NO emission suppression in biochar-amended soils are still poorly understood. We set up microcosm experiments with fertilized, wet soil in which we used N tracing techniques and quantitative polymerase chain reaction (qPCR) to investigate the impact of biochar on mineral and gaseous nitrogen dynamics and denitrification-specific functional marker gene abundance and expression. In accordance with previous studies our results showed that biochar addition can lead to a significant decrease in NO emissions. Furthermore, we determined significantly higher quantities of soil-entrapped NO and N in biochar microcosms and a biochar-induced increase in typical and atypical nosZ transcript copy numbers. Our findings suggest that biochar-induced NO emission mitigation is based on the entrapment of NO in water-saturated pores of the soil matrix and concurrent stimulation of microbial NO reduction resulting in an overall decrease of the NO/(NO + N) ratio.

摘要

一氧化二氮(NO)是一种强效温室气体,在硝化和反硝化等微生物氮转化过程中产生。土壤是一氧化二氮排放的最大来源,而氮肥的应用是导致大气中一氧化二氮浓度上升的主要驱动因素。土壤生物炭的添加被提议作为一种减少土壤一氧化二氮排放的有前途的工具。然而,生物炭添加土壤中抑制一氧化二氮排放的潜在过程仍未得到很好的理解。我们在施肥的湿润土壤中进行了微宇宙实验,在这些实验中我们使用氮示踪技术和定量聚合酶链反应(qPCR)来研究生物炭对矿物和气态氮动态以及反硝化特定功能标记基因丰度和表达的影响。与之前的研究一致,我们的结果表明,生物炭的添加可以导致一氧化二氮排放的显著减少。此外,我们还确定了生物炭微宇宙中土壤固持的 NO 和 N 的数量明显增加,以及生物炭诱导的典型和非典型 nosZ 转录本拷贝数增加。我们的研究结果表明,生物炭诱导的一氧化二氮排放减少是基于土壤基质水饱和孔隙中 NO 的固持以及对微生物 NO 还原的同时刺激,从而导致一氧化二氮/(NO + N)比值总体下降。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/98fc/5180216/ca403436ada4/srep39574-f1.jpg

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