The Exchange of Soil Nitrite and Atmospheric HONO: A Missing Process in the Nitrogen Cycle and Atmospheric Chemistry

Author(s):  
Hang Su ◽  
Yafang Cheng ◽  
Ulrich Pöschl
2016 ◽  
Author(s):  
Nathan J. Chellman ◽  
Meredith G. Hastings ◽  
Joseph R. McConnell

Abstract. Nitrogen oxides (NOx = NO + NO2) have an important impact on the atmosphere and biosphere through controls on oxidant concentrations and the formation of nitric acid (e.g. acid rain). Anthropogenic emissions from fossil fuel combustion, land use change, and agriculture have altered the global nitrogen cycle since the beginning of the Industrial Revolution but contributions from specific sources are difficult to quantify, hindering understanding of changes to the natural environment and design of effective mitigation strategies. Ice core records reveal changes in the nitrogen cycle over time in connection to climate, atmospheric chemistry, and the biosphere. Here we use a seasonally resolved ice core record of the nitrogen isotopic composition of nitrate (δ15N–NO3−), together with a broad suite of highly resolved (> 22 samples y−1) elemental and chemical tracers, to investigate sources of nitrate deposited in central Greenland from 1760 CE to present. A marked negative trend in δ15N–NO3− since ~ 1940 CE paralleled a nearly three-fold increase in nitrate concentration. Based on correlated increases in tracer concentrations, independent emission estimates of oil burning, and an isotope mixing model, North American oil combustion likely was the primary driver of recent changes in the nitrogen cycle recorded in Greenland.


2015 ◽  
Vol 112 (50) ◽  
pp. 15384-15389 ◽  
Author(s):  
Bettina Weber ◽  
Dianming Wu ◽  
Alexandra Tamm ◽  
Nina Ruckteschler ◽  
Emilio Rodríguez-Caballero ◽  
...  

Reactive nitrogen species have a strong influence on atmospheric chemistry and climate, tightly coupling the Earth’s nitrogen cycle with microbial activity in the biosphere. Their sources, however, are not well constrained, especially in dryland regions accounting for a major fraction of the global land surface. Here, we show that biological soil crusts (biocrusts) are emitters of nitric oxide (NO) and nitrous acid (HONO). Largest fluxes are obtained by dark cyanobacteria-dominated biocrusts, being ∼20 times higher than those of neighboring uncrusted soils. Based on laboratory, field, and satellite measurement data, we obtain a best estimate of ∼1.7 Tg per year for the global emission of reactive nitrogen from biocrusts (1.1 Tg a−1of NO-N and 0.6 Tg a−1of HONO-N), corresponding to ∼20% of global nitrogen oxide emissions from soils under natural vegetation. On continental scales, emissions are highest in Africa and South America and lowest in Europe. Our results suggest that dryland emissions of reactive nitrogen are largely driven by biocrusts rather than the underlying soil. They help to explain enigmatic discrepancies between measurement and modeling approaches of global reactive nitrogen emissions. As the emissions of biocrusts strongly depend on precipitation events, climate change affecting the distribution and frequency of precipitation may have a strong impact on terrestrial emissions of reactive nitrogen and related climate feedback effects. Because biocrusts also account for a large fraction of global terrestrial biological nitrogen fixation, their impacts should be further quantified and included in regional and global models of air chemistry, biogeochemistry, and climate.


2021 ◽  
Author(s):  
Pierre-Francois Coheur ◽  
Pieternel Levelt ◽  
Lieven Clarisse ◽  
Martin Van Damme ◽  
Henk Eskes ◽  
...  

<p>The nitrogen cycle has been heavily perturbed due to ever growing agriculture, industry, transport and domestic production. It is believed that we now have reached a point where the nitrogen biochemical flow has exceeded its planetary boundary for a safe operating zone. This goes together with a cascade of impacts on human health and ecosystems. To better understand and address these impacts, there is a critical need to quantify the global nitrogen cycle and monitor its perturbations on all scales, down to the urban or agricultural source.</p><p>The Nitrosat concept, which was proposed most recently in the framework of ESA’s Earth Explorer 11 call, has for overarching objective to simultaneously identify the emission contributions of NH<sub>3 </sub>and NO<sub>2</sub> from farming activities, industrial complexes, transport, fires and urban areas. The specific Nitrosat science goals are to:</p><ul><li>Quantify the emissions of NH<sub>3</sub> and NO<sub>2</sub> on the landscape scales, to expose individual sources and characterize the temporal patterns of their emissions.</li> <li>Quantify the relative contribution of agriculture, in its diversity of sectors and practices, to the total emissions of reactive nitrogen.</li> <li>Quantify the contribution of reactive nitrogen to air pollution and its impact on human health.</li> <li>Constrain the atmospheric dispersion and surface deposition of reactive nitrogen and its impacts on ecosystems and climate; and contribute to monitoring policy progress to reduce nitrogen deposition in Natura 2000 areas in Europe.</li> <li>Reduce uncertainties in the contribution of reactive nitrogen to climate forcing, atmospheric chemistry and interactions between biogeochemical cycles.</li> </ul><p>To achieve these objectives, Nitrosat would consist of an infrared Imaging Fourier Transform Spectrometer and a Visible Imaging Pushbroom Spectrometer. These imaging spectrometers will measure NH<sub>3</sub> and NO<sub>2</sub> (respectively) at 500 m, which is the required spatial scale to differentiate, identify and quantify the main point and area sources in a single satellite overpass. Source regions would be probed from once a week to once a month to reveal the seasonal patterns. Combined with air quality models, assimilation and inverse modelling, these measurements would allow assessing the processes that are relevant for the human disruption of the nitrogen cycle and their resulting effects, in much more detail than what will be achieved with the satellite missions that are planned in the next decade. In this way, Nitrosat would enable informed evaluations of future policies on nitrogen emission control.</p>


2012 ◽  
Vol 36 (10) ◽  
pp. 1572 ◽  
Author(s):  
Luo-qin FU ◽  
Jian-dong SUN ◽  
Bin DENG ◽  
Quan LIANG ◽  
Xiao-ping ZHANG ◽  
...  

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