Changes in N cycling in the rhizosphere of canola lead to decreased N requirements in a following wheat crop.

Cathryn A O’Sullivan1, Elliott G Duncan2, Kelley Whisson1, Karen Treble1, Margaret M Roper1, Mark B Peoples3.

1 CSIRO Agriculture, Private Bag 5, Wembley, WA 6913, Australia.

2 Future Industries Institute, University of South Australia, Mawson Lakes Campus, Mawson Lakes, SA 5095, Australia.

3 CSIRO Agriculture, Clunies Ross St, Black Mountain, ACT 2601, Australia.

Abstract

Growing canola in rotations is known to increase the yield of following cereal crops. In addition to providing a disease break and better weed management, it has been suggested that following crops have lower N fertiliser requirements. The aim of this study was to confirm the lower N requirement of wheat following canola and to postulate possible mechanisms to explain this effect.

In a field study, wheat was grown under several N fertiliser levels in paddocks where either canola or wheat/pasture were grown in the previous year. In parallel, laboratory and glasshouse studies were used to examine the impact of canola  on nitrification, N mineralisation and N immobilisation rates.

Two seasons of field data in Wongan Hills, WA, and one season in Merredin, WA, showed that wheat had a lower N fertiliser requirement following canola than a wheat or pasture rotation.  In the laboratory, nitrification rates were significantly lower in the rhizosphere of canola cv. Hyola 404RR than wheat cv. Janz, while N immobilisation and remobilisation rates were significantly higher.

To explain this we hypothesise that decreased nitrification rates conserve N as NH4+ during the canola season leading to increased N immobilisation rates and an elevated organic N pool that is likely to be stored over hot and dry summers in the WA region.  this organic N pool can be remobilised providing an alternative N source for the following crop. Further study is needed to fully explore this concept.

Tackling climate change in agriculture- key mechanisms in GHG mitigation

Adrian Leip, Gema Carmona-Garcia, Simone Rossi

1 European Commission, Joint Research Centre, Institute for Environment and Sustainability, Via Fermi 2749, TP 266/040

I-21027 ISPRA (VA), Italy, https://ec.europa.eu/jrc/en, adrian.leip@jrc.ec.europa.eu

Abstract

We assessed the question of side effects and of the accountability of mitigation measures in the Agriculture, Forestry, and Other Land Uses (AFOLU) sector in national greenhouse gas inventories, proposing a novel classification system of available mitigation measures on the basis of ‘mitigation strategies’ and ‘mitigation mechanisms’. While the first differentiates measures which require collection of data from those for which specific emission factors or parameters need to be developed, the second groups mitigation measures according to the ‘term’ that is exploited to achieve emission reductions. We find that current IPCC methodologies provide a good basis to account for the majority of mitigation measures. Most of them will be reflected in national greenhouse gas inventories if default tier 1 approaches or (in some cases) national level tier 2 approaches are used (according to IPCC terminology). Efforts should be concentrated on improving data availability especially about management options, which is often the major obstacle in accounting for the effect of mitigation efforts. Examples include mitigation measures focusing on the improvement of feed intake of animals, or actions aimed at incrementing the soil organic carbon stock in agricultural soils through appropriate management practices. We conclude that simple farm level tools may have a good potential in collecting the data required, and offer the opportunity of full flexibility for the farmers to select concrete farm practice changes and monitor their performance.

Validation of ammonia satellite retrievals with ground-based FTIR

Enrico Dammers1, M. Palm2, Martin Van Damme3, Mark W. Shephard4, Lieven Clarisse3, Karen E. Cady-Pereira5, Simon Whitburn3, Pierre Francois Coheur3, M.Schaap6 and Jan Willem Erisman1,7

1 Cluster Earth and Climate, Department of Earth Sciences, Vrije Universiteit Amsterdam, Amsterdam, the Netherlands. E.Dammers@vu.nl

2 Institut für Umweltphysik, University of Bremen, Bremen, Germany

3 Spectroscopie de l’Atmosphère, Service de Chimie Quantique et Photophysique, Université Libre de Bruxelles (ULB), Brussels, Belgium

4 Environment Canada, Toronto, Ontario, Canada

5 Atmospheric and Environmental Research (AER), Lexington, Massachusetts, USA

6 TNO, Climate Air Sustainability, Utrecht, the Netherlands

7 Louis Bolk Institute, Driebergen, the Netherlands

Abstract

Global emissions of reactive nitrogen have increased due to human activities and are estimated to be a factor four larger than pre-industrial levels. Concentration levels of NOx are declining, but ammonia (NH3) levels are increasing globally. At its current concentrations NH3 poses a large threat to both the environment and human health. Still relatively little is known about the total budget as well as the global distribution. Surface observations are sparsely available, mostly for north-western Europe, the United States and China, and are limited by the high costs and poor spatial and temporal resolution. The lifetime of atmospheric NH3 is short, in the range of several hours to a few days and the existing surface measurements are not sufficient to estimate global concentrations. Space-based InfraRed-sounders such as the Infrared Atmospheric Sounding Interferometer (IASI) and the Cross-track Infrared Sounder (CrIS) enable global observations of atmospheric NH3 which can overcome the limitations of existing surface observations. One challenge with satellite NH3 retrievals is that they are complex and require extensive validation. Presently only a limited number of satellite NH3 validation campaigns have been performed with limited spatial, vertical and temporal coverage. In this study we demonstrate the use of a recently developed retrieval methodology for ground-based Fourier Transform Infrared Spectroscopy (FTIR) instruments to obtain vertical concentration profiles of NH3. We will use the retrieved profiles from eight stations with a range of NH3 pollution levels to validate satellite NH3 products.

Process-based modelling of NH3 exchange over a grazed field

Andrea Móring1,2, Massimo Vieno2, Ruth M. Doherty3, Celia Milford4,5, Eiko Nemitz2, Marsailidh M. Twigg2, Mark A. Sutton2

1 University of Edinburgh, High School Yards, Edinburgh, United Kingdom, EH8 9XP, andrea.moring@ed.ac.uk
2 Centre for Ecology & Hydrology, Bush Estate, Penicuik, United Kingdom, EH26 0QB
3 University of Edinburgh, The King’s Buildings, Alexander Crum Brown Road, Edinburgh, United Kingdom, EH9 3FF
4
Associate Unit CSIC University of Huelva ”Atmospheric Pollution”, CIQSO, University of Huelva, Huelva, Spain, E21071

5 Izaña Atmospheric Research Center, AEMET, Joint Research Unit to CSIC “Studies on Atmospheric Pollution”, Santa Cruz de Tenerife, Spain

Abstract

In this study a process-based ammonia (NH3) exchange model for a grazed field has been described and evaluated. The presented model is based on a patch-scale NH3 exchange model, GAG (Generation of Ammonia from Grazing), which has been here extended to the field scale. GAG accounts for the total ammoniacal nitrogen and water content of the soil as well as the soil pH under a single urine patch. The new, field scale model combined multiple runs of the patch-scale model including both urine-affected and unaffected areas. The field-scale model was tested over two modelling periods, using NH3 flux measurements taken at an intensively managed grassland, Easter Bush, UK. The model represented well the observed fluxes. It was found that the temporal evolution of the NH3 exchange flux was dominated by the NH3 emission from the urine patches. The results also showed that the evolution of NH3 emission from urine patches deposited in different time steps could be substantially different: in some cases the first high NH3 emission peak occurred a day or two days after the deposition of the given urine patch. Furthermore, according to our findings, NH3 fluxes over the field in a given day could be considerably affected by the NH3 emission from urine patches deposited several days earlier. The approach is designed to provide a balance between simplicity and process representation to allow it to be ultimately applied in regional scale atmospheric emission, transport and deposition modelling.

Nitrous oxide’s ozone destructiveness under different climate scenarios

David R. Kanter1,2, Sonali P. McDermid1,3, Larissa Nazarenko3

1Department of Environmental Studies, New York University, 285 Mercer Street, New York, NY, 10003, USA

2Agriculture and Food Security Center, Columbia University, 61 Route 9w, Palisades, NY, 10964, USA

3NASA Goddard Institute for Space Sciences, 2880 Broadway, New York, NY, 10025, USA

Abstract

Nitrous oxide (N2O) is an important greenhouse gas and ozone depleting substance as well as a key component of the nitrogen cascade. While emissions scenarios indicating the range of N2O’s potential future contributions to radiative forcing are widely available, the impact of these emissions scenarios on future stratospheric ozone depletion is less clear. This is because N2O’s ozone destructiveness is partially dependent on tropospheric warming, which affects ozone depletion rates in the stratosphere. Consequently, in order to understand the possible range of stratospheric ozone depletion that N2O could cause over the 21st century, it is important to decouple the greenhouse gas emissions scenarios and compare different emissions trajectories for individual substances (e.g. business-as-usual carbon dioxide (CO2) emissions versus low emissions of N2O). This study is the first to follow such an approach, running a series of experiments using the NASA Goddard Institute for Space Sciences ModelE2 atmospheric sub-model. We anticipate our results to show that stratospheric ozone depletion will be highest in a scenario where CO2 emissions reductions are prioritized over N2O reductions, as this would constrain ozone recovery while doing little to limit stratospheric NOx levels (the breakdown product of N2O that destroys stratospheric ozone). This could not only delay the recovery of the stratospheric ozone layer, but might also prevent a return to pre-1980 global average ozone concentrations, a key goal of the international ozone regime. Accordingly, we think this will highlight the importance of reducing emissions of all major greenhouse gas emissions, including N2O, and not just a singular policy focus on CO2.

How do NH3 emissions relate to nitrogen use efficiency of livestock production?

Groenestein, C.M.1, Hutchings, N.J.2 , Haenel, H.D.3, Amon, B.4, Menzi, H.5, Mikkelsen, M.H.6, Misselbrook, T.H.7, van Bruggen, C.8, Kupper, T.9, Webb, J.10

1 Wageningen UR Livestock Research, De Elst 1, 6708 WD Wageningen, www.wageningenur.nl/en/livestockresearch, karin.groenestein@wur.nl

2 Dept. of Agroecology, Aarhus University, Research Centre Foulum, 8830 Tjele, Denmark

3 Thünen Institute of Climate-Smart Agriculture (TI-AK), Bundesallee 50,38116 Braunschweig, Germany

4 Leibniz Institute for Agricultural Engineering, Max-Eyth-Allee 100, 14469 Potsdam, Germany

5 Agroscope, Inst. For Livestock Sciences, P.O. Box 64, CH-1725 Posieux, Switzerland

6 Dept. of Environmental Science, Frederiksborgvej 399, 4000 Roskilde, Denmark

7 Sustainable Soils and Grassland Systems, Rothamsted Research, North Wyke, Devon, UK, EX20 2SB

8 Organisation, address, city, state, postcode, website, Email

9 Bern University of Applied Sciences, School of Agricultural, Forest and Food Sciences Laenggasse 85 CH-3052 Zollikofen

10 Ricardo Ltd, Gemini Building, Harwell, UK. OX11

Abstract

Ammonia (NH3) emissions from livestock production systems can be substantial but difficult to measure. Here we explore the relationship between NH3 emissions, the emission intensity (NH3-N emitted/product N) and the more easily measured feed Nitrogen Use Efficiency (NUE). Using a conceptual model, we find that the relationship between emission intensity and NUE is equivalent to that between NH3-N emission and feed N intake. Furthermore, there is a linear relationship between the two, with a slope that is dependent on characteristics of the animal and its feed, and the manure management system. This is illustrated using data taken from the emission inventories of six European countries, which found a linear relationship, with much variation within a commodity type. Using the same data, we show how the effects of animal and feed characteristics can be separated from those of the manure management system.

Increased influence of nitrogen limitation on CO2 emissions from historical and future land use and land-use change

Atul K Jain1, Prasanth Meiyappan1 and Joanna I House2

1Department of Atmospheric Sciences, University of Illinois, Urbana, IL 61801, USA

2Department of Geography, Cabot Institute, University of Bristol, Bristol, BS8 1SS, UK

Abstract

We estimate the impacts of nitrogen limitation on the CO2 emissions from land use and land-use change (LULUC), including wood harvest, for the period 1900-2100. We use a land-surface model that includes a fully coupled carbon and nitrogen cycle, and accounts for forest regrowth processes following agricultural abandonment and wood harvest. Future projections are based on the four Representation Concentration Pathways used in the IPCC Fifth Assessment Report. Results show that excluding nitrogen limitation will underestimate global LULUC emissions by 34-52 PgC (20-30%) during the 20th century and by 128-187 PgC (90-150%) during the 21st century. The underestimation increases with time because: (1) Projected annual wood harvest rates from forests summed over the 21st century are 380-1080% higher compared to those of the 20th century, resulting in more regrowing secondary forests, (2) Nitrogen limitation reduces the CO2 fertilization effect on net primary production of regrowing secondary forests following wood harvest and agricultural abandonment, and (3) Nitrogen limitation effect is aggravated by the gradual loss of soil nitrogen from LULUC disturbance. Our study implies that: (1) Nitrogen limitation of CO2 uptake is substantial and sensitive to nitrogen inputs, (2) If LULUC emissions are larger than previously estimated in studies without nitrogen limitation, then meeting the same climate mitigation target would require an equivalent additional reduction of fossil fuel emissions, and (3) The effectiveness of land-based mitigation strategies will critically depend on the interactions between nutrient limitations and secondary forests resulting from LULUC.

Newton-Bhabha Virtual Centre on Nitrogen Efficiency of Whole-cropping Systems for improved performance and resilience in agriculture (NEWS India-UK)

M.A. Sutton1, J. Drewer1, N. Raghuram2, D. Kumar3, A. Price4, J.U. Smith4, A. Bhatia3, D. Reay5, D. Subrahmanyam6, A. Ahmad7, U. Skiba1, U. Dragosits1, M. Vieno1, W.J. Bealey1, E. Carnell1, E. Roberts1, A. Stott8, S. Sohi5, A. Moring5, J. Hillier4, D.R. Nayak4, R. Prasana3, R. Singh3, C.N. Neeraja6, S.R. Voleti6, R.M. Kumar6, K. Surekha6, S. Hooda2, R. Babu6, N. Jain3, P. Pandey3, B. Ramakrishnan3, N. das Saha3, H. Pathak3

1 Centre for Ecology and Hydrology (CEH), Edinburgh Research Station, Bush Estate, Penicuik, EH26 0QB, Scotland, UK, www.ceh.ac.uk, juew@ceh.ac.uk

2 School of Biotechnology, Guru Gobind Singh Indraprastha University, Sector 16C, Dwarka, New Delhi-110078, India

3 ICAR-Indian Agricultural Research Institute, New Delhi 110012, India

4 University of Aberdeen, School of Biological Science, Rm G43 23 St Machar Drive, Aberdeen, AB24 3UU, Scotland, UK

5 University of Edinburgh, School of Geosciences, High School Yards, Edinburgh EH8 9XP, Scotland, UK

6 ICAR-Indian Institute of Rice Research, Rajendranagar, Hyderabad-500030, India

7 Department of Botany Aligarh Muslim University, Aligarh-202002, UP, India

8 Centre for Ecology and Hydrology (CEH), Lancaster Environment Centre, Library Avenue, Lancaster, LA1 4AP, UK

Abstract

NEWS India UK (Newton-Bhabha Virtual Centre on Nitrogen Efficiency of Whole-cropping Systems for improved performance and resilience in agriculture) is established to promote cooperation between the two countries that demonstrates innovative ways to improve agricultural nitrogen management, allowing increased and more resilient food production in India while reducing nitrogen losses to the environment. Here we present the structure of the Virtual Joint Centre including strategic and scientific goals and objectives as well as the activities planned to achieve these.

EQCom: an education and outreach simulation game for enhancing environmental quality in the commons

W.A. Hammac

USDA, Agriculture Research Service, National Soil Erosion Research Lab, 275 South Russell St., West Lafayette, Indiana, 47907, Ashley.Hammac@USDA.ARS.GOV

Abstract

EQCom is a simulation game for teaching the effects of conventional farming on natural resources and the social challenges involved in implementing solutions. Players are “farmers” who make a series of choices about farming practices, either conservation or conventional. Outcomes result based on those choices and they include aesthetic and economic consequences. Farmers and society prosper if farmers collectively implement conservation practices and protect common resources, but a farmer’s natural economic incentive is to make choices based on short-term private economics benefits instead of long-term private and public benefits. The natural progression in this game is for soil, air, and water resources to degrade and socio-eco-systems to suffer. Farmers will find over time that short-term economic gain must be sacrificed to achieve long-term sustainability and success. Farmers must regulate themselves or be regulated by government to succeed. This is a novel and exciting way to teach students, farmers, policy makers, and others about the complexity of conservation farming. Restoring environmental quality in the commons requires counter intuitive thinking, self-regulation, and consideration of public interest.

Effectiveness of two decades of policy measures to reduce ammonia emissions in the Netherlands

Roy Wichink Kruit1, Jan Aben1, Wilco de Vries1, Ferd Sauter1, Eric van der Swaluw1, Margreet van Zanten1, Addo van Pul1

1 National Institute for Public Health and the Environment (RIVM), Antonie van Leeuwenhoeklaan 9, 3721 MA Bilthoven, the Netherlands, www.rivm.nl, Roy.Wichink.Kruit@rivm.nl

Abstract

In this study, the effectiveness of two decades of policy measures to reduce ammonia emissions in the Netherlands is evaluated. It is shown that the ammonia concentration is more suitable for monitoring policy measures than the ammonium aerosol concentration or the wet deposition of NHx. This study shows that the decrease in ammonia emissions due to policy measures between 1990 and present did not result in a proportional decrease of the ammonia concentration in the air. The less effectively declining ammonia concentrations can largely be explained by the change in atmospheric chemical and meteorological conditions. The large decline in oxidized sulfur and nitrogen concentrations has led to reduced formation of sulfuric and nitric acid and consequently reduced formation of ammonium salts. In this way, relatively more ammonia remained in the atmosphere. Simultaneously, the absorbing surface became less acid, which resulted in less deposition of ammonia and more ammonia remaining in the atmosphere. Meteorology has a significant effect on the year-to-year variation in ammonia concentrations, but does not significantly affect the trend in the ammonia concentrations over the years. It is likely, however, that ammonia concentrations will increase due to climate change, e.g., dryer and warmer springs/summers.

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