104 results match your criteria: "Thünen Institute of Climate-Smart Agriculture[Affiliation]"

Rewetted bogs with high water levels (WL) and mire-specific vegetation are crucial carbon (C) sinks, but their function might be threatened by tree encroachment, a phenomenon widespread in the northern hemisphere that often coincides with low WL. This might impact C cycling both at the ecosystem and microform scale in multiple ways, but so far, data are lacking. We established two sites in the same former peat extraction area, one showing permanently high WL and mire-specific vegetation (open site, OS), while the other one has more fluctuating WL and a dense birch ( Ehrh.

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Soil monitoring requires accurate and spatially explicit information on soil organic carbon (SOC) trends and changes over time. Spatiotemporal SOC models based on Earth Observation (EO) satellite data can support large-scale SOC monitoring but often lack sufficient temporal validation based on long-term soil data. In this study, we used repeated SOC samples from 1986 to 2022 and a time series of multispectral bare soil observations (Landsat and Sentinel-2) to model high-resolution cropland SOC trends for almost four decades.

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Urease and nitrification inhibitors can reduce ammonia and greenhouse gas emissions from fertilizers and manure but their effectiveness depends on the conditions under which they are used. Consequently, it is essential for the credibility of emission reductions reported in regulatory emission inventories that their effectiveness is assessed under real-world conditions and not just in the laboratory. Here, we specify the criteria we consider necessary before the effects of inhibitors are included in regulatory emission inventories.

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Successful NH abatement policies and regulations in German agriculture.

Sci Total Environ

December 2024

Precision Agriculture Lab, School of Life Sciences, Technical University of Munich, D-85354 Freising, Germany.

Anthropogenic ammonia (NH) emissions, of which about 95 % are from agriculture, have led to environmental pollution, resulting in tremendous damage to human health and ecosystems. Thus, the NEC Directive 2016/2284/EU sets national reduction targets for NH emissions in individual EU countries. To implement the NEC Directive for NH emission targets, Germany amended the Fertilizer Application Ordinance in 2017 and 2020 (DüV_amended) and set the air pollution control regulation, Technical Instructions on Air Quality Control (TA_Luft).

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Adaptive traits of clade ammonia-oxidizing archaea.

mBio

November 2024

Interdisciplinary Graduate Program in Advance Convergence Technology and Science, Jeju National University, Jeju, South Korea.

Article Synopsis
  • Nitrification, a crucial part of the nitrogen cycle, is mainly driven by ammonia-oxidizing microorganisms, particularly ammonia-oxidizing archaea (AOA), which have unique traits influencing their adaptations.
  • The study conducted comparative genomics on 39 AOA genomes, revealing the absence of typical ammonium transporters, suggesting distinctive physiological traits for AOA compared to other nitrifiers.
  • Findings indicate that AOA may utilize a different outer cell structure, providing insights into their ecological roles and adaptations in terrestrial ecosystems, and highlighting their significance in nitrogen cycling and environmental impacts like eutrophication and greenhouse gas emissions.
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Article Synopsis
  • Denitrification is an essential process in soil nitrogen cycling that primarily occurs in microbial hotspots around particulate organic matter (POM), affecting greenhouse gas emissions like dinitrogen and nitrous oxide.
  • To accurately predict these emissions, it's crucial to quantify the distribution of POM, as it influences local oxygen balance and microbial activity in soils.
  • Findings indicate that both proximal and distal POM contribute to greenhouse gas emissions, with distal POM significantly driving denitrification rates, particularly in grasslands, highlighting the intricate relationship between soil structure, organic carbon supply, and microbial activity.
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Article Synopsis
  • - Erosion-induced topsoil dilution negatively affects soil health and crop productivity, particularly in biogeochemical cycling of nutrients like nitrogen (N) and carbon (C) in agricultural systems.
  • - The study examined how soil type, topsoil dilution, and the form of N fertilizer (mineral vs. organic) influence N cycling, using canola plants in a pot experiment with different soil types.
  • - Findings showed that while topsoil dilution did not significantly impact N cycling in the plant-soil systems, the choice of fertilizer and soil type played key roles in N recovery and utilization, suggesting a need for careful management practices in agriculture.
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Soil organic carbon (SOC) accrual, and particularly the formation of fine fraction carbon (OC), has a large potential to act as sink for atmospheric CO. For reliable estimates of this potential and efficient policy advice, the major limiting factors for OC accrual need to be understood. The upper boundary of the correlation between fine mineral particles (silt + clay) and OC is widely used to estimate the maximum mineralogical capacity of soils to store OC, suggesting that mineral surfaces get C saturated.

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Converting natural vegetation for agriculture has resulted in the loss of approximately 5% of the current global terrestrial soil organic carbon (SOC) stock to the atmosphere. Increasing the agricultural area under grassland may reverse some of these losses, but the effectiveness of such a strategy is limited by how quickly SOC recovers after conversion from cropland. Using soil data and extensive land-use histories gathered during the national German agricultural soil inventory, this study aims to answer three questions regarding agricultural land-use change (LUC): (i) how do SOC stocks change with depth following LUC; (ii) how long does it take to reach SOC equilibrium after LUC; and (iii) what is the legacy effect of historic LUC on present day SOC dynamics? By using a novel approach that substitutes space for time and accounts for differences in site properties using propensity score balancing, we determined that sites that were converted from cropland to grassland reached a SOC equilibrium level 47.

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Article Synopsis
  • Carbon-rich peat soils used for agriculture have lost significant carbon due to drainage, but wet crop cultivation, especially rice, could help reduce CO and NO emissions while maintaining agricultural production.
  • Water table and soil management strategies can affect methane emissions from rice cultivation and influence how rice plants distribute their biomass.
  • The study found that lower water tables and the addition of mineral soil reduced belowground biomass and methane emissions, suggesting that managing these factors could be a viable strategy for lowering methane emissions in wet rice cultivation.
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Encroachment of vascular plants (VP) in temperate raised bogs, as a consequence of altered hydrological conditions and nutrient input, is widely observed. Effects of such vegetation shift on water and carbon cycles are, however, largely unknown and identification of responsible plant physiological traits is challenging. Process-based modelling offers the opportunity of gaining insights into ecosystem functioning beyond observations, and to infer decisive trait shifts of plant functional groups.

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Nitrogen is an essential nutrient in the environment that exists in multiple oxidation states in nature. Numerous microbial processes are involved in its transformation. Knowledge about very complex N cycling has been growing rapidly in recent years, with new information about associated isotope effects and about the microbes involved in particular processes.

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Significance of phosphorus deficiency for the mitigation of mercury toxicity in the Robinia pseudoacacia L.- rhizobia symbiotic association.

J Hazard Mater

April 2024

Center of Molecular Ecophysiology (CMEP), College of Resources and Environment, Southwest University No. 2, Tiansheng Road, Beibei District, 400715 Chongqing, China.

Article Synopsis
  • Nitrogen-fixing legumes can help remediate Mercury-contaminated soil, but their effectiveness is influenced by phosphorus availability for nodule formation.
  • A study on two Robinia pseudoacacia L. strains from different climates revealed that phosphorus deficiency reduces toxicity from Mercury at the molecular level, benefiting plant health and nutrient use.
  • Rhizobia inoculation enhanced plant resilience against Mercury and phosphorus deficiency, with one strain showing better nodulation and biomass, making it a promising candidate for future phytoremediation efforts in phosphorus-poor environments.
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This study investigated the influence of vegetation and microforms on methane (CH) balances of a rewetted bog in north-west Germany. The two study sites are in close proximity on the same former peat extraction area, one dominated by Sphagnum-mosses and the other one by a dense Betula pubescens stand with a high Eriophorum vaginatum cover. The contribution of microforms (hummocks/hollows) to CH emissions and the effect of Betula encroachment has been studied.

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Combined application of biochar and nitrogen (N) fertilizer could offer opportunities to increase rice yield and reduce methane emissions from paddy fields. However, this strategy may increase nitrous oxide (NO) emissions, hence its interactive effects on GHG emissions, global warming potential (GWP) and GHG intensity (GHGI) remained poorly understood. We conducted a systematic review to i) evaluate the overall effects of combined application of biochar and N fertilizer rates on GHGs emissions, GWP, rice yield, and GHGI, ii) determine the quantities of biochar and N-fertilizer application that increase rice yield and reduce GHGs emissions and GHGI, and iii) examine the effects of biochar and different types of nitrogen fertilizers on rice yield, GHGs, GWP, and GHGI using data from 45 research articles and 183 paired observations.

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Livestock use in semi-arid South African ecosystems has not been extensively studied in relation to the Net Ecosystem Exchange (NEE) of carbon dioxide (CO). We present four years of measurements from twinned eddy-covariance towers in Nama-Karoo, South Africa, to investigate the carbon fluxes and the impact of grazing intensity on NEE. The design contrasted NEE at a long-term site grazed at recommended levels (LG) with a long-term heavily grazed (EG) site that had been rested for 10 years, and was monitored for two years after which intensive grazing was reintroduced for this experiment.

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The term carbon (C) sequestration has not just become a buzzword but is something of a siren's call to scientific communicators and media outlets. Carbon sequestration is the removal of C from the atmosphere and the storage, for example, in soil. It has the potential to partially compensate for anthropogenic greenhouse gas emissions and is, therefore, an important piece in the global climate change mitigation puzzle.

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Background And Aims: Understanding the fate and residence time of organic matter added to soils, and its effect on native soil organic carbon (SOC) mineralisation is key for developing efficient SOC sequestration strategies. Here, the effect of litter quality, particularly the carbon-to-nitrogen (C:N) ratio, on the dynamics of particulate (POC) and mineral-associated organic carbon (MAOC) were studied.

Methods: In a two-year incubation experiment, root litter samples of the C4-grass with four different C:N ratios ranging from 50 to 124 were added to a loamy agricultural topsoil.

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In recent decades, nanotechnology has been rapidly advancing in various fields of human activity, including veterinary medicine. The review presents up-to-date information on recent advancements in nanotechnology in the field and an overview of the types of nanoparticles used in veterinary medicine and animal husbandry, their characteristics, and their areas of application. Currently, a wide range of nanomaterials has been implemented into veterinary practice, including pharmaceuticals, diagnostic devices, feed additives, and vaccines.

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Monitoring of carbon-water fluxes at Eurasian meteorological stations using random forest and remote sensing.

Sci Data

September 2023

State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, Xinjiang, 830011, China.

Simulating the carbon-water fluxes at more widely distributed meteorological stations based on the sparsely and unevenly distributed eddy covariance flux stations is needed to accurately understand the carbon-water cycle of terrestrial ecosystems. We established a new framework consisting of machine learning, determination coefficient (R), Euclidean distance, and remote sensing (RS), to simulate the daily net ecosystem carbon dioxide exchange (NEE) and water flux (WF) of the Eurasian meteorological stations using a random forest model or/and RS. The daily NEE and WF datasets with RS-based information (NEE-RS and WF-RS) for 3774 and 4427 meteorological stations during 2002-2020 were produced, respectively.

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In this response to a letter to the editor, we provide evidence that the findings regarding a non-detectable limit of mineral-associated organic carbon as published in Begill et al. (2023) are robust. This is mainly done by showing that no methodological bias was present and that the main correlation was not driven by a few exceptional soils.

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Adopting land management practices that increase the stock of soil organic carbon (SOC) in croplands is widely promoted as a win-win strategy to enhance soil health and mitigate climate change. In this context, the definition of reference SOC content and stock values is needed to provide reliable targets to farmers, policymakers, and stakeholders. In this study, we used the LUCAS dataset to compare different methods for evaluating reference SOC content and stock values in European croplands topsoils (0-20 cm depth).

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Soil organic carbon (SOC) sequestration is a promising climate change mitigation option. In this context, the formation of the relatively long-lived mineral-associated organic carbon (MAOC) is key. To date, soils are considered to be limited in their ability to accumulate MAOC, mainly by the amount of clay and silt particles present.

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