Quantification of N2O emission pathways via a 15N tracing model

2014 ◽  
Vol 72 ◽  
pp. 44-54 ◽  
Author(s):  
Christoph Müller ◽  
Ronnie J. Laughlin ◽  
Oliver Spott ◽  
Tobias Rütting
2004 ◽  
Vol 36 (4) ◽  
pp. 619-632 ◽  
Author(s):  
Christoph Müller ◽  
R.J. Stevens ◽  
R.J. Laughlin

2005 ◽  
Vol 37 (5) ◽  
pp. 1007-1008 ◽  
Author(s):  
Christoph Müller ◽  
R. James Stevens ◽  
Ronald J. Laughlin

SOIL ◽  
2016 ◽  
Vol 2 (4) ◽  
pp. 601-614 ◽  
Author(s):  
Anne B. Jansen-Willems ◽  
Gary J. Lanigan ◽  
Timothy J. Clough ◽  
Louise C. Andresen ◽  
Christoph Müller

Abstract. Over the last century an increase in mean soil surface temperature has been observed, and it is predicted to increase further in the future. In order to evaluate the legacy effects of increased temperature on both nitrogen (N) transformation rates in the soil and nitrous oxide (N2O) emissions, an incubation experiment and modelling approaches were combined. Based on previous observations that gross N transformations in soils are affected by long-term elevated-temperature treatments we hypothesized that any associated effects on gaseous N emissions (e.g. N2O) can be confirmed by a change in the relative emission rates from various pathways. Soils were taken from a long-term in situ warming experiment on temperate permanent grassland. In this experiment the soil temperature was elevated by 0 (control), 1, 2 or 3 °C (four replicates per treatment) using IR (infrared) lamps over a period of 6 years. The soil was subsequently incubated under common conditions (20 °C and 50 % humidity) and labelled as NO315NH4 Gly, 15NO3NH4 Gly or NO3NH4 15N-Gly. Soil extractions and N2O emissions were analysed using a 15N tracing model and source-partitioning model. Both total inorganic N (NO3− + NH4+) and NO3− contents were higher in soil subjected to the +2 and +3 °C temperature elevations (pre- and post-incubation). Analyses of N transformations using a 15N tracing model showed that, following incubation, gross organic (but not inorganic) N transformation rates decreased in response to the prior soil warming treatment. This was also reflected in reduced N2O emissions associated with organic N oxidation and denitrification. Furthermore, a newly developed source-partitioning model showed the importance of oxidation of organic N as a source of N2O. In conclusion, long-term soil warming can cause a legacy effect which diminishes organic N turnover and the release of N2O from organic N and denitrification.


2005 ◽  
Vol 37 (5) ◽  
pp. 1003-1005 ◽  
Author(s):  
Jesper Luxhøi ◽  
Bruno Mary ◽  
Lars S. Jensen

2021 ◽  
Vol 320 ◽  
pp. 107557
Author(s):  
Huan Chen ◽  
Chengyan Zheng ◽  
Fu Chen ◽  
Yuqiang Qiao ◽  
Shizhou Du ◽  
...  
Keyword(s):  

2021 ◽  
pp. 1-10
Author(s):  
Shuqian Sun ◽  
Xiaohui Bi ◽  
Bin Yang ◽  
Weihong Zhang ◽  
Xinyu Zhang ◽  
...  
Keyword(s):  

2021 ◽  
Vol 13 (9) ◽  
pp. 4928
Author(s):  
Alicia Vanessa Jeffary ◽  
Osumanu Haruna Ahmed ◽  
Roland Kueh Jui Heng ◽  
Liza Nuriati Lim Kim Choo ◽  
Latifah Omar ◽  
...  

Farming systems on peat soils are novel, considering the complexities of these organic soil. Since peat soils effectively capture greenhouse gases in their natural state, cultivating peat soils with annual or perennial crops such as pineapples necessitates the monitoring of nitrous oxide (N2O) emissions, especially from cultivated peat lands, due to a lack of data on N2O emissions. An on-farm experiment was carried out to determine the movement of N2O in pineapple production on peat soil. Additionally, the experiment was carried out to determine if the peat soil temperature and the N2O emissions were related. The chamber method was used to capture the N2O fluxes daily (for dry and wet seasons) after which gas chromatography was used to determine N2O followed by expressing the emission of this gas in t ha−1 yr−1. The movement of N2O horizontally (832 t N2O ha−1 yr−1) during the dry period was higher than in the wet period (599 t N2O ha−1 yr−1) because of C and N substrate in the peat soil, in addition to the fertilizer used in fertilizing the pineapple plants. The vertical movement of N2O (44 t N2O ha−1 yr−1) was higher in the dry season relative to N2O emission (38 t N2O ha−1 yr−1) during the wet season because of nitrification and denitrification of N fertilizer. The peat soil temperature did not affect the direction (horizontal and vertical) of the N2O emission, suggesting that these factors are not related. Therefore, it can be concluded that N2O movement in peat soils under pineapple cultivation on peat lands occurs horizontally and vertically, regardless of season, and there is a need to ensure minimum tilling of the cultivated peat soils to prevent them from being an N2O source instead of an N2O sink.


Sign in / Sign up

Export Citation Format

Share Document