Long-term reduction in nitrogen and proton inputs did not affect atmospheric methane uptake and nitrous oxide emission from a German spruce forest soil

2002 ◽  
Vol 34 (11) ◽  
pp. 1815-1819 ◽  
Author(s):  
W. Borken ◽  
F. Beese ◽  
R. Brumme ◽  
N. Lamersdorf
2018 ◽  
Vol 115 (34) ◽  
pp. 8587-8590 ◽  
Author(s):  
Xiangyin Ni ◽  
Peter M. Groffman

Forest soils are a sink for atmospheric methane (CH4) and play an important role in modulating the global CH4 budget. However, whether CH4 uptake by forest soils is affected by global environmental change is unknown. We measured soil to atmosphere net CH4 fluxes in temperate forests at two long-term ecological research sites in the northeastern United States from the late 1990s to the mid-2010s. We found that annual soil CH4 uptake decreased by 62% and 53% in urban and rural forests in Baltimore, Maryland and by 74% and 89% in calcium-fertilized and reference forests at Hubbard Brook, New Hampshire over this period. This decrease occurred despite marked declines in nitrogen deposition and increases in atmospheric CH4 concentration and temperature, which should lead to increases in CH4 uptake. This decrease in soil CH4 uptake appears to be driven by increases in precipitation and soil hydrological flux. Furthermore, an analysis of CH4 uptake around the globe showed that CH4 uptake in forest soils has decreased by an average of 77% from 1988 to 2015, particularly in forests located from 0 to 60 °N latitude where precipitation has been increasing. We conclude that the soil CH4 sink may be declining and overestimated in several regions across the globe.


2007 ◽  
Vol 53 (5) ◽  
pp. 678-691 ◽  
Author(s):  
Tomoaki Morishita ◽  
Tadashi Sakata ◽  
Masamichi Takahashi ◽  
Shigehiro Ishizuka ◽  
Takeo Mizoguchi ◽  
...  

2014 ◽  
Vol 34 (17) ◽  
Author(s):  
方华军 FANG Huajun ◽  
程淑兰 CHENG Shulan ◽  
于贵瑞 YU Guirui ◽  
王永生 WANG Yongsheng ◽  
徐敏杰 XU Minjie ◽  
...  

1997 ◽  
Vol 77 (4) ◽  
pp. 565-570 ◽  
Author(s):  
Verlan L. Cochran ◽  
Elena B. Sparrow ◽  
Sharon F. Schlentner ◽  
Charles W. Knight

Methane and nitrous oxide are important radiatively active gases that are influenced by agricultural practices. This study assesses long-term tillage, crop residue management, and N fertilization rates on the flux of these two gases at a high latitude site representing the northern fringe of large-scale agriculture. Cumulative methane uptake for the summer was higher from no-tillage plots than tilled plots. This was associated with lower soil water contents with tillage. Thus, the reduction in CH4 uptake was attributed to water stress on methane oxidizers. At planting, soil water contents were near field capacity, and the no-till plots had the lowest uptake which was attributed to restricted diffusion of methane to active sites. A similar pattern of methane uptake to soil water content was found with the residue management treatments. Removing the straw lowered the soil water content and for most of the season methane uptake was also lower than where the straw had been left on the plots. Nitrogen fertilizer rate had little effect on methane uptake over the summer, but high N rates lowered consumption during the time of active nitrification early in the season. This corresponded to the time of maximum efflux of nitrous oxide. Nitrous oxide efflux was greatest at the high N rate where straw was retained on the plots. Key words: Methane, nitrous oxide, nitrification, denitrification, barley


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