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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Humus--Mathematical models--Evaluation--Congresses. ; Electronic books.
    Description / Table of Contents: Proceedings of the NATA Advanced Research Workshop "Evaluation of Soil Organic Matter Models Using Existing Long-Term Datasets", held at IACR-Rothamsted, Harpenden, UK, May 21-26, 1995.
    Type of Medium: Online Resource
    Pages: 1 online resource (424 pages)
    Edition: 1st ed.
    ISBN: 9783642610943
    Series Statement: Nato asi Subseries I: Series ; v.38
    DDC: 631.4/17
    Language: English
    Note: Intro -- Evaluation of Soil Organic Matter Models -- Copyright -- PREFACE -- WORKSHOP PARTICIPANTS -- CONTENTS -- PLENARY PAPERS -- Why evaluate soil organic matter models? -- The Contribution of the Soil Organic Matter Network (SOMNET) to GCTE -- Why Site Networks? -- The North American Site Network -- The Australian Site Network -- Long-term data sets from Germany and Eastern Europe -- Establishing a European GCTE Soil Organic Matter Network (SOMNET) -- Interpretation Difficulties with Long-Term Experiments -- Review and Classification of Ten Soil Organic Matter (SOM) Models -- Ecosystem model comparisons: science or fantasy world? -- Matching Measurable Soil Organic Matter Fractions with Conceptual Pools in Simulation Models of Carbon Turnover: Revision of Model Structure -- ¹Modeling the Measurable or Measuring the Modelable: A Hierarchical Approach to Isolating Meaningful Soil Organic Matter Fractionations -- Quantitative methods to evaluate and compare Soil Organic Matter (SOM) Models -- Soil Organic Matter Models and Global Estimates of Soil Organic Carbon -- SOIL ORGANIC MATTER MODELS -- The Soil Submodel of the ITE (Edinburgh) Forest and Hurley Pasture Models -- SOMM - a model of soil organic matter and nitrogen dynamics in terrestrial ecosystems -- RothC-26.3 - A Model for the turnover of carbon in soil -- Modelling approaches of soil organic matter turnover within the CANDY system -- Organic matter dynamics simulated with the 'Verberne'-model -- The DNDC Model -- Description of the model NCSOIL -- Simulating soil carbon and nitrogen dynamics with the soil-plant-atmosphere system model DAISY -- The CENTURY model -- LONG-TERM EXPERIMENTS WITH SOIL ORGANIC MATTER MEASUREMENTS -- Soil organic matter dynamics in Sanborn Field (North America) -- The Askov Long-Term Experiments on Animal Manure and Mineral Fertilizers. , The Tamworth Legume/Cereal Rotation -- Long-term fertilization trials in Hungary -- Essai permanent plots, Gembloux -- The Waite Pennanent Rotation Trial -- Woodslee Tile Runoff Experiment: Fertilization Effects on Soil Organic Matter -- Effect of Farm Yard Manure and Fertilizer Nitrogen in Pearl millet-Wheat cropping Sequence -- The Breton Classical Plots -- Long-term field experiment Praha - Ruzyně, Czech Republic -- The Static Experiment Bad Lauchstädt, Germany -- The Park Grass Experiment, 1856-1995 -- Geescroft Wilderness, 1883-1995 -- ¹Long-term Residue Management Experiment: Pendleton, Oregon USA -- Carbon Changes During the Growth of Loblolly Pine on Formerly Cultivated Soil: The Calhoun Experimental Forest, U.S.A. -- Soil Organic Matter Dynamics in the North American Corn Belt: The Arlington Plots -- Soil Evolution Under Dry Meadows in a Boreal climate: The Moscow Dry Meadow Experimental Site -- INDEX.
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  • 2
    Online Resource
    Online Resource
    Oxford :Taylor & Francis Group,
    Keywords: Atmospheric methane - Environmental aspects. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (270 pages)
    Edition: 1st ed.
    ISBN: 9781849775090
    DDC: 551.6
    Language: English
    Note: Cover -- Title -- Copyright -- Contents -- 1 Methane Sources and the Global Methane Budget -- 2 The Microbiology of Methanogenesis -- 3 Wetlands -- 4 Geological Methane -- 5 Termites -- 6 Vegetation -- 7 Biomass Burning -- 8 Rice Cultivation -- 9 Ruminants -- 10 Wastewater and Manure -- 11 Landfills -- 12 Fossil Energy and Ventilation Air Methane -- 13 Options for Methane Control -- 14 Summary -- Contributors -- Acronyms and Abbreviations -- Index.
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  • 3
    Online Resource
    Online Resource
    Cambridge :Royal Society of Chemistry,
    Keywords: Agricultural innovations. ; Electronic books.
    Description / Table of Contents: This comprehensive volume examines the environmental impact made by agriculture in the 21st Century, looking forward to the future with the lessons of the past.
    Type of Medium: Online Resource
    Pages: 1 online resource (193 pages)
    Edition: 1st ed.
    ISBN: 9781849734974
    Series Statement: ISSN ; v.34
    DDC: 333.7614
    Language: English
    Note: Intro -- Environmental Impacts of Modern Agriculture -- Contents -- Editors -- List of Contributors -- Modern Agriculture and Implications for Land Use and Management -- 1 Introduction and Overview -- 2 Agricultural Systems -- 3 Global and Regional Issues -- 3.1 Demand Side Factors -- 3.2 Supply Side Factors -- 4 Agricultural Land and the Role of Science and Technology -- 5 Case Study: UK Agriculture and Land Use -- 5.1 Trends in UK Agriculture -- 5.1.1 Agriculture's Contribution to UK Economy -- 5.1.2 Agricultural Land Use -- 5.1.3 Farm Size -- 5.1.4 Farm Yields -- 5.1.5 Agricultural Commodity Prices -- 5.1.6 UK Farm Incomes -- 5.1.7 Productivity of UK Farms -- 5.1.8 Demand for Food in the UK -- 5.1.9 Food Self-sufficiency and Food Security -- 6 Agriculture and Environment -- 7 Agriculture and Ecosystem Services -- 8 Agriculture and Climate Change -- 9 Agriculture and Energy -- 10 Future Prospects for Land Use in the UK -- 10.1 Scope to Release Land from Agricultural Production -- et al., 2005). -- 10.2 Technology Change and Land Use -- 11 Implications for Policy -- References -- Impacts of Agriculture upon Soil Quality -- 1 Introduction to Soil Quality -- 2 Soil Organic Matter Decline -- 3 Soil Compaction -- 4 Soil Erosion -- 5 Soil Biodiversity -- 6 Soil Contamination -- 6.1 Nutrients -- 6.2 Heavy Metals -- 6.3 Organic Pollutants -- 7 Soil Sealing -- 8 Soil Salinisation -- 9 Conclusions -- References -- Impacts of Agriculture upon Greenhouse Gas Budgets -- 1 Introduction -- 2 Current Agricultural Sources of Nitrous Oxide, Methane and Carbon Dioxide -- 2.1 Nitrous Oxide -- 2.2 Methane -- 2.3 Carbon Dioxide -- 3 International Reporting of Greenhouse Gas Emissions -- 3.1 Indirect Emissions - Is there a Gap between Top-down and Bottom-up Global Budgets? -- 4 Future Mitigation Strategies -- 4.1 Nitrous Oxide. , 4.1.1 Optimising Nitrogen Use by Crop Plants -- 4.1.2 Optimising Nitrogen Use by Livestock -- 4.1.3 Inhibitors -- 4.1.4 Soil Management and Tillage -- 4.1.5 Land Use Change -- 4.2 Methane -- 4.2.1 Methane from Ruminant Livestock -- 4.2.2 Dietary Opportunities -- 4.2.3 Avoiding Inefficiencies -- 4.2.4 Livestock Reduction or Replacements -- 4.2.5 Methane from Wetland Rice -- 4.3 Carbon Dioxide -- 4.4 Greenhouse Gas Mitigation Potential: Combined Effects of all Gases -- 4.5 The Economics of Mitigation -- 5 Conclusions -- References -- Impacts of Agriculture on Water-borne Pathogens -- 1 Introduction -- 2 Policy Developments -- 3 Microbial Dynamics -- 3.1 Pathogens, Indicators and Health Risk -- 3.2 Catchment Microbial Flux -- 3.3 Flux Attenuation and Mitigation of Resource Impacts -- 4 Conclusions -- References -- Pesticides in Modern Agriculture -- 1 Introduction -- 2 The Traditional Context of the Agricultural Uses of Pesticides -- 3 The Changing Nature of Pesticide Use from Earliest Agricultural Times to the Present Day -- 4 Risks to Human Health from Pesticide Use in Agriculture -- 5 Pesticide Use in Current Agricultural Systems - A Changing and Challenging Context -- 6 Future Pesticide Use and Approaches to their Regulation and Management -- References -- Balancing the Environmental Consequences of Agriculture with the Need for Food Security -- 1 Preamble -- 1.1 The Need for Food Security -- 1.2 The Importance of Environmental Sustainability and a Role for the UK -- 2 Agriculture's Environmental Impact and a Summary of the Issues -- 2.1 Some Terminology -- 2.2 Man-managed and Natural Ecosystems - Competition for Photosynthate -- 2.3 The Application of Science - Manipulating Genotype and Environment -- 2.4 Impacts from Fossil-fuel Use -- 2.5 Reactive Nitrogen -- 2.6 Water - Excess and Shortage -- 2.7 Contaminants and Pollutants. , 2.8 Avoiding Negative Environmental Consequences of Agricultural Practice - A Summary -- 3 Sustainable Intensi cation -- 3.1 Global Land Use -- 3.2 Anthromes and Anthropogenic Ecosystem Processes -- 3.3 Examples of Sustainable Intensi cation -- 3.4 Management of Biodiversity: Land Sharing or Land Sparing? -- 4 Land Use, Resource Management and Deliverables from Land -- 4.1 Understanding Interactions and Trade-offs -- 4.2 Units of Accounting -- 4.3 Some Examples of Trade-offs -- 5 A Systems-based Approach to GHG Balance -- 5.1 Agriculture as Part of the Problem and Part of the Solution -- 5.2 Fossil Fuel Substitution, Carbon Capture and Storage, Food Imports and the Cost of Valued Landscapes -- 6 Conclusions -- References -- Positive and Negative Impacts of Agricultural Production of Liquid Biofuels -- 1 Introduction -- 2 Agricultural Production as Part of Biofuel Life Cycles and Life Cycle Assessment -- 3 Energy -- 3.1 Solar Energy Conversion Efficiency of Current Agricultural Crop-based Liquid Biofuels -- 3.2 Replacement of Fossil Fuels -- 3.3 Energetic Return on Investment (EROI) -- 4 Water Footprints of Current Agricultural Crop-based Liquid Biofuels -- 5 Life Cycle Greenhouse Gas Emissions and the Carbon Debt of Current Agricultural Crop-based Liquid Biofuels -- 6 Life Cycle Emissions of Pollutants Linked to Current Agricultural Crop-based Liquid Biofuels -- 7 Impact of Agricultural Crop-based Liquid Biofuels on Natural Ecosystems and Biodiversity -- 8 Effect of Current Agricultural Crop-based Liquid Biofuels on Food Prices and Hunger -- 9 Liquid Biofuels from Crop Residues -- 10 Conclusions -- References -- Subject Index.
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  • 4
    Publication Date: 2019-04-01
    Keywords: ddc:300
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
    Type: bookpart , doc-type:bookPart
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  • 5
    Publication Date: 2024-01-12
    Description: Knowledge of the spatial distribution of the fluxes of greenhouse gases (GHGs) and their temporal variability as well as flux attribution to natural and anthropogenic processes is essential to monitoring the progress in mitigating anthropogenic emissions under the Paris Agreement and to inform its global stocktake. This study provides a consolidated synthesis of CH4 and N2O emissions using bottom-up (BU) and top-down (TD) approaches for the European Union and UK (EU27 + UK) and updates earlier syntheses (Petrescu et al., 2020, 2021). The work integrates updated emission inventory data, process-based model results, data-driven sector model results and inverse modeling estimates, and it extends the previous period of 1990–2017 to 2019. BU and TD products are compared with European national greenhouse gas inventories (NGHGIs) reported by parties under the United Nations Framework Convention on Climate Change (UNFCCC) in 2021. Uncertainties in NGHGIs, as reported to the UNFCCC by the EU and its member states, are also included in the synthesis. Variations in estimates produced with other methods, such as atmospheric inversion models (TD) or spatially disaggregated inventory datasets (BU), arise from diverse sources including within-model uncertainty related to parameterization as well as structural differences between models. By comparing NGHGIs with other approaches, the activities included are a key source of bias between estimates, e.g., anthropogenic and natural fluxes, which in atmospheric inversions are sensitive to the prior geospatial distribution of emissions. For CH4 emissions, over the updated 2015–2019 period, which covers a sufficiently robust number of overlapping estimates, and most importantly the NGHGIs, the anthropogenic BU approaches are directly comparable, accounting for mean emissions of 20.5 Tg CH4 yr−1 (EDGARv6.0, last year 2018) and 18.4 Tg CH4 yr−1 (GAINS, last year 2015), close to the NGHGI estimates of 17.5±2.1 Tg CH4 yr−1. TD inversion estimates give higher emission estimates, as they also detect natural emissions. Over the same period, high-resolution regional TD inversions report a mean emission of 34 Tg CH4 yr−1. Coarser-resolution global-scale TD inversions result in emission estimates of 23 and 24 Tg CH4 yr−1 inferred from GOSAT and surface (SURF) network atmospheric measurements, respectively. The magnitude of natural peatland and mineral soil emissions from the JSBACH–HIMMELI model, natural rivers, lake and reservoir emissions, geological sources, and biomass burning together could account for the gap between NGHGI and inversions and account for 8 Tg CH4 yr−1. For N2O emissions, over the 2015–2019 period, both BU products (EDGARv6.0 and GAINS) report a mean value of anthropogenic emissions of 0.9 Tg N2O yr−1, close to the NGHGI data (0.8±55 % Tg N2O yr−1). Over the same period, the mean of TD global and regional inversions was 1.4 Tg N2O yr−1 (excluding TOMCAT, which reported no data). The TD and BU comparison method defined in this study can be operationalized for future annual updates for the calculation of CH4 and N2O budgets at the national and EU27 + UK scales. Future comparability will be enhanced with further steps involving analysis at finer temporal resolutions and estimation of emissions over intra-annual timescales, which is of great importance for CH4 and N2O, and may help identify sector contributions to divergence between prior and posterior estimates at the annual and/or inter-annual scale. Even if currently comparison between CH4 and N2O inversion estimates and NGHGIs is highly uncertain because of the large spread in the inversion results, TD inversions inferred from atmospheric observations represent the most independent data against which inventory totals can be compared. With anticipated improvements in atmospheric modeling and observations, as well as modeling of natural fluxes, TD inversions may arguably emerge as the most powerful tool for verifying emission inventories for CH4, N2O and other GHGs.
    Description: Published
    Description: 1197–1268
    Description: OSA2: Evoluzione climatica: effetti e loro mitigazione
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 6
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: The current Intergovernmental Panel on Climate Change (IPCC) default methodology (tier 1) for calculating nitrous oxide (N2O) emissions from nitrogen applied to agricultural soils takes no account of either crop type or climatic conditions. As a result, the methodology omits factors that are crucial in determining current emissions, and has no mechanism to assess the potential impact of future climate and land-use change. Scotland is used as a case study to illustrate the development of a new methodology, which retains the simple structure of the IPCC tier 1 methodology, but incorporates crop- and climate-dependent emission factors (EFs). It also includes a factor to account for the effect of soil compaction because of trampling by grazing animals. These factors are based on recent field studies in Scotland and elsewhere in the UK. Under current conditions, the new methodology produces significantly higher estimates of annual N2O emissions than the IPCC default methodology, almost entirely because of the increased contribution of grazed pasture. Total emissions from applied fertilizer and N deposited by grazing animals are estimated at 10 662 t N2O-N yr−1 using the newly derived EFs, as opposed to 6 796 t N2O-N yr−1 using the IPCC default EFs. On a spatial basis, emission levels are closer to those calculated using field observations and detailed soil modelling than to estimates made using the IPCC default methodology. This can be illustrated by parts of the western Ayrshire basin, which have previously been calculated to emit 8–9 kg N2O-N ha−1 yr−1 and are estimated here as 6.25–8.75 kg N2O-N ha−1 yr−1, while the IPCC default methodology gives a maximum emission level of only 3.75 kg N2O-N ha−1 yr−1 for the whole area. The new methodology is also applied in conjunction with scenarios for future climate- and land-use patterns, to assess how these emissions may change in the future. The results suggest that by 2080, Scottish N2O emissions may increase by up to 14%, depending on the climate scenario, if fertilizer and land management practices remain unchanged. Reductions in agricultural land use, however, have the potential to mitigate these increases and, depending on the replacement land use, may even reduce emissions to below current levels.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science, Ltd
    Global change biology 4 (1998), S. 0 
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: In this paper we estimate the European potential for carbon mitigation of no-till farming using results from European tillage experiments. Our calculations suggest some potential in terms of (a) reduced agricultural fossil fuel emissions, and (b) increased soil carbon sequestration. We estimate that 100% conversion to no-till farming would be likely to sequester about 23 Tg C y–1 in the European Union or about 43 Tg C y–1 in the wider Europe (excluding the former Soviet Union). In addition, up to 3.2 Tg C y–1 could be saved in agricultural fossil fuel emissions. Compared to estimates of the potential for carbon sequestration of other carbon mitigation options, no-till agriculture shows nearly twice the potential of scenarios whereby soils are amended with organic materials. Our calculations suggest that 100% conversion to no-till agriculture in Europe could mitigate all fossil fuel-carbon emissions from agriculture in Europe. However, this is equivalent to only about 4.1% of total anthropogenic CO2-carbon produced annually in Europe (excluding the former Soviet Union) which in turn is equivalent to about 0.8% of global annual anthropogenic CO2-carbon emissions.
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: The effect of liming on the flow of recently photosynthesized carbon to rhizosphere soil was studied using 13CO2 pulse labelling, in an upland grassland ecosystem in Scotland. The use of 13C enabled detection, in the field, of the effect of a 4-year liming period of selected soil plots on C allocation from plant biomass to soil, in comparison with unlimed plots. Photosynthetic rates and carbon turnover were higher in plants grown in limed soils than in those from unlimed plots. Higher δ13C‰ values were detected in shoots from limed plants than in those from unlimed plants in samples clipped within 15 days of the end of pulse labelling. Analysis of the aboveground plant production corresponding to the 4-year period of liming indicated that the standing biomass was higher in plots that received lime. Lower δ13C‰ values in limed roots compared with unlimed roots were found, whereas no significant difference was detected between soil samples. Extrapolation of our results indicated that more C has been lost through the soil than has been gained via photosynthetic assimilation because of pasture liming in Scotland during the period 1990–1998. However, the uncertainty associated with such extrapolation based on this single study is high and these estimates are provided only to set our findings in the broader context of national soil carbon emissions.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: Process-based models can be classified into: (a) terrestrial biogeochemical models (TBMs), which simulate fluxes of carbon, water and nitrogen coupled within terrestrial ecosystems, and (b) dynamic global vegetation models (DGVMs), which further couple these processes interactively with changes in slow ecosystem processes depending on resource competition, establishment, growth and mortality of different vegetation types. In this study, four models – RHESSys, GOTILWA+, LPJ-GUESS and ORCHIDEE – representing both modelling approaches were compared and evaluated against benchmarks provided by eddy-covariance measurements of carbon and water fluxes at 15 forest sites within the EUROFLUX project. Overall, model-measurement agreement varied greatly among sites. Both modelling approaches have somewhat different strengths, but there was no model among those tested that universally performed well on the two variables evaluated. Small biases and errors suggest that ORCHIDEE and GOTILWA+ performed better in simulating carbon fluxes while LPJ-GUESS and RHESSys did a better job in simulating water fluxes. In general, the models can be considered as useful tools for studies of climate change impacts on carbon and water cycling in forests. However, the various sources of variation among models simulations and between models simulations and observed data described in this study place some constraints on the results and to some extent reduce their reliability. For example, at most sites in the Mediterranean region all models generally performed poorly most likely because of problems in the representation of water stress effects on both carbon uptake by photosynthesis and carbon release by heterotrophic respiration (Rh).The use of flux data as a means of assessing key processes in models of this type is an important approach to improving model performance. Our results show that the models have value but that further model development is necessary with regard to the representation of the some of the key ecosystem processes.
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: Yearly, per-area carbon sequestration rates are used to estimate mitigation potentials by comparing types and areas of land management in 1990 and 2000 and projected to 2010, for the European Union (EU)-15 and for four country-level case studies for which data are available: UK, Sweden, Belgium and Finland. Because cropland area is decreasing in these countries (except for Belgium), and in most European countries there are no incentives in place to encourage soil carbon sequestration, carbon sequestration between 1990 and 2000 was small or negative in the EU-15 and all case study countries. Belgium has a slightly higher estimate for carbon sequestration than the other countries examined. This is at odds with previous reports of decreasing soil organic carbon stocks in Flanders. For all countries except Belgium, carbon sequestration is predicted to be negligible or negative by 2010, based on extrapolated trends, and is small even in Belgium. The only trend in agriculture that may be enhancing carbon stocks on croplands at present is organic farming, and the magnitude of this effect is highly uncertain.Previous studies have focused on the potential for carbon sequestration and have shown quite significant potential. This study, which examines the sequestration likely to occur by 2010, suggests that the potential will not be realized. Without incentives for carbon sequestration in the future, cropland carbon sequestration under Article 3.4 of the Kyoto Protocol will not be an option in EU-15.
    Type of Medium: Electronic Resource
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