Food production security and resiliency require combination of agricultural management practices that are environmentally friendly and economically viable. Cover crops and tillage are two typical management practices that influence corn (Zea mays L.) and soybean (Glycine max L.) production in Illinois and the Midwest, USA. Finding practices that could potentially reduce nitrous oxide (N2O) emissions and sequester carbon (C) in the soil can improve agricultural resiliency to climate change. Generally, shifting from reduced tillage (RT) to no-till (NT) improves soil structure and decreases C emissions or sequesters soil C but might increase N2O emissions. Including a legume cover crop such as hairy vetch (Vicia villosa L.) before corn is preferred to winter cereal cover crops (WCCCs) to avoid yield penalty in corn and ensure high grain production. Winter cereal cover crops such as winter cereal rye (Secale cereale) (WCR) could potentially decrease soil N2O emissions during fallow period by capturing residual N and reducing soil moisture. These conditions could change in soils with legacy tillage (RT vs. NT) effects due to changes in soil physical, chemical, and biological over time. We utilized a medium-term (six-year-old) trial to test several hypotheses. We hypothesized that RT increases the soil temperature, accelerates soil organic matter mineralization, and especially in combination with hairy vetch could increase soil N in the soil leading to increased corn grain yield and N2O emission (Chapter 1). We also hypothesized that WCR takes up residual N after harvesting corn, decrease soil N, use soil moisture, and therefore, could decrease soil N2O emission (Chapter 2). For study 1 (Chapter 1), our objective was to evaluate the influence of cover crop (hairy vetch) vs. a no CC control and tillage systems (RT vs. NT) on (i) corn yield, N uptake, removal, and N balance; (ii) N2O emissions during corn season; (iii) yield scaled N2O emissions on a long-term (eight years) tillage × cover cropping system during the corn growing season in 2019 and 2021. We also analyzed factors that influence N2O emissions via principal component analysis in corn season. In corn growing seasons, we found that corn grain yield was higher in RT than NT reflecting on more N in the soil in RT than NT. Hairy vetch increased corn grain yield, soil N, and N2O-N indicating increased corn grain yield by hairy vetch N contribution let to higher N loss. Yield-scaled N2O-N emissions in NT-2019 (3696.4 g N2O-N Mg-1) were twofold higher than RT-2019 (1872.7 g N2O-N Mg-1) and almost fourfold higher than NT-2021 and RT-2021 indicating in a wet year like 2019, yield-scaled N2O-N emissions were higher in NT than RT. Principal component analysis indicated N2O-N fluxes were less driven by soil N and more by environmental conditions and N balances reflecting on N application at planting in this trial. . The objectives for chapter 2 were to evaluate the legacy effect of tillage (RT vs. NT) and cover crops (WCR vs. a no cover crop control) on soil nitrate-N (NO3-N), volumetric water content (VWC), temperature, and N2O emission trends during a fallow period after corn in a six-yr trial. In spring 2020 we also estimated WCR biomass and N uptake as affected by tillage practices and compared WCR biomass to weeds in the no cover crop treatment. In rye growing season, winter cereal rye biomass was 55% higher than weeds in the fallow treatment. A linear positive relation between WCR biomass and N uptake (R2= 0.93) and C accumulation (R2 = 0.99) indicates WCR captures more N and adds more C inputs than weeds. Winter cereal rye biomass was also higher in RT than NT reflecting on higher soil temperature and N availability in RT than NT. Soil VWC was lower in WCR plots and there was a negative linear relation between days of the year (DOY) and VWC (R2 = 0.6). Despite all these differences, soil N2O-N values were mainly less than 5 g N2O-N ha-1d-1 in all sampling dates regardless of tillage or cover crop treatment. We conclude that in poorly drained Alfisols with claypan and fragipans, NT is not an effective strategy to decrease N2O-N fluxes. Hairy vetch benefits corn grain yield and supplement N but that increases N loss through N2O-N emissions. We concluded that we should focus on decreasing N2O emissions early in corn season since majority of N is lost during that time sometimes 300 times higher than those reported during the WCR phase. Some changes in management practices that could reduce N2O losses are shifting from upfront N application to sidedress N management, terminating hairy vetch at or even after corn planting, and combine these efforts with enhanced efficiency fertilizers that control nitrification and denitrification.

This doctoral research provides an advanced molecular approach for the investigation of microbial structure and function in response to operational conditions of biological nitrogen removal (BNR) processes, including those leading to direct production of a major greenhouse gas, nitrous oxide (N₂O). The wastewater treatment sector is estimated to account with 3% of total anthropogenic N₂O emissions. Nevertheless, the contribution from wastewater treatment plants (WWTPs) is considered underestimated due to several limitations on the estimation methodology approach suggested by the Intergovernmental Panel on Climate Change (IPCC). Although for the past years efforts have been made to characterize the production of N₂O from these systems, there are still several limitations on fundamental knowledge and operational applications. Those include lack of information of N₂O production pathways associated with control of aeration, supplemental organic carbon sources and adaptation of the microbial community to the repeated operational conditions, among others. The components of this thesis, lab-scale investigations and full-scale monitoring of N₂O production pathways and emissions in conjunction with meta-omics approach, have a combined role in addressing such limitations. Lab-scale experiments imposing short-term anoxic-aerobic cycling on partial- and full-nitrification based processes were conducted to investigate the microbial response to N₂O production. Interestingly, it was determined that full-nitrification systems could be a higher contributor to N₂O production and emissions than partial-nitrification. While it has been reported in the literature a higher contribution from the latter when the microbial community is not subjected to oxygen cycling conditions. Following the knowledge obtained with a single anoxic-aerobic cycle imposed to nitrifying communities, long-term adaptation of the microbial community to continued anoxic-aerobic cycling and its impact on N₂O production were investigated through a meta-omics approach. Long-term studies are particularly significant regarding engineered systems, where the microorganisms are continually subjected to cycling conditions again and again. A microbial adaptation at the RNA level was identified on both autotroph and heterotroph organisms. The transcripts of the metabolic pathways related to NO and N₂O production (nir, nor) and consumption (nor, nos) were initially induced followed by a gradual decline, leading to a parallel reduction in gaseous emissions over time. Other pathways not typically interrogated in conjunction with the nitrogen metabolism, such as electron transport chain and carbon fixation were also investigated and revealed a mechanism to overcome the imbalance in electron flow and generation of proton motive force (increased transcription of terminal oxidase genes, cco and cox) to uphold carbon fixation during continued cycling. The second part of this thesis focuses on full-scale WWTPs, where it is crucial to determine specific nuances of the systems’ dynamics and of the different types of treatment that may contribute to increased production and emissions of N₂O. For that purpose, two distinct BNR systems not usually considered and studied in terms of N₂O production and emissions were chosen. First, a separate centrate treatment (SCT) process employing glycerol as the supplemental carbon source was monitored. Significantly, this system was found to have one of the highest levels of N₂O production and emission report thus far. Glycerol revealed to foster a microbial community (i.e. Burkholderiales, Rhodobacterales and Sphingomonadales) that stores internal carbon and promote partial denitrification, leading to accumulation of nitrite and N₂O [7-11]. Second, both fixed- and moving-bed biofilm BNR systems were investigated. The overall N₂O emission fractions for the Integrated Fixed-Film Activated Sludge (IFAS)(0.09 – 1.1% infl-TKN) and denitrification filters (0.11 – 1.4% infl-TN) were similar to the reported emissions from suspended growth activated sludge systems [4-6]. For the IFAS system, aqueous and gaseous N₂O profiles paralleled the diurnal variability on influent nitrogen load. The production of N₂O was significantly correlated with ammonia concentration (p<0.05, r=0.91), suggesting the production through hydroxylamine oxidation pathway. Denitrification filters displayed a very peculiar pattern on N₂O emissions associated with intermittent operational cycles (i.e. nitrogen release cycle and backwash). These intrinsic operations of the denitrification filters contributed to transient oxygen conditions and nearly the entire N₂O emissions through gaseous stripping and production by inhibition of denitrification. Similarly to suspended growth systems, process design and operations demonstrated to also play an important role in N₂O emissions from attached growth processes. Finally, aeration strategies for energy efficient conventional nitrification based on the microbial community development and its associated performance was investigated in lab-scale. It was demonstrated that using the same air supply rate, continuous and intermittent aeration resulted in completely different microbial structure. Consequently, distinct kinetics and nitrification performance were observed. The aeration rate could be minimized (resulting in reduction in energy consumption) for high ammonia removal efficiency and lower N₂O emissions, as long as the process is designed accordingly to the microbial ecology developed in such conditions. In sum, the microbial structure, function and connection of metabolic pathways of complex engineered microbial communities as applicable to BNR systems and its operations were investigated in detail. From an engineering perspective, this dissertation provides an advancement on the molecular approach to characterize structure and function of microbial responses to engineered operations beyond the business-as-usual target genes, which can eventually result in better design and control of engineered BNR processes. This study offers more than an improved scientific understanding of the complex microbial environment and direct engineering applications. It connects sanitation with water quality and the greenhouse gas effect by prioritizing concurrent enhanced biological nitrogen removal and mitigation of N₂O production and emission. Ultimately the implications of the result presented herein can provide economical, environmental, health benefits for the society.

Master of Science / Department of Agronomy / Charles W. Rice / Agricultural lands receiving N inputs are considered the primary source of N2O, a potent greenhouse gas. N fertilizer management has shown variable effects on both N2O losses and corn grain yield. The objectives of this study were to assess the impact of N source and placement on N2O emissions, fertilizer-induced emission factor (FIEF), corn grain yield, yield-scaled N2O emissions (YSNE) and N fertilizer recovery efficiency (NFRE). The experiment was conducted from 2013 through 2014 at the Agronomy North Farm located at Kansas State University, Manhattan, KS. The soil was a moderately well-drained Kennebec silt loam. The treatments were broadcast urea (BC-Urea), broadcast urea ammonium nitrate (UAN) (BC-UAN), broadcast coated urea (BC-CU), surface-band UAN (SB-UAN), subsurface-band UAN (SSB-UAN), subsurface-band UAN + nitrification inhibitor (SSB-UAN+I) and a 0 N control. In 2013, SSB- UAN emitted significantly more N2O (2.4 kg N2O-N ha-1), whereas control (0.3 kg ha-1) and BC- UAN (0.6 kg ha-1) emitted the least. In 2014, most treatments emitted between 3.3 and 2.5 kg N2O-N ha-1. Only SSB-UAN+I (1.03 kg ha-1) and control (0.26 kg ha-1) were significantly lower. The use of a nitrification inhibitor decreased N2O emissions by 62% and 55% in 2013 and 2014, respectively. BC treatments had cumulative emissions significantly higher in 2014 compared to 2013. Only SSB-UAN+I had a significantly lower FIEF (0.4%), and 2013 FIEF (0.68%) was significantly lower than that of 2014 (1.38%). In 2013, banded treatments had significantly higher grain yields (from 9.1 to 10.5 Mg ha-1), whereas in 2014 fewer differences among N treatments were observed, ranging from 7.2 to 8.6 Mg ha-1. Banded treatments had significantly lower grain yields in 2014 compared to 2013. Only BC-UAN and SSB-UAN+I had significantly lower YSNE, and 2013 had lower YSNE than 2014. In 2013, SSB-UAN had the greatest NFRE, whereas BC treatments had the lowest. In 2014, N treatments did not differ in NFRE. SSB-UAN and SSB-UAN+I had significantly lower NFRE values in 2014 compared to 2013. Fertilizer source and placement have the potential to mitigate N2O emissions and promote high yields and NFRE in corn, however, the response is dependent on the rainfall pattern after fertilizer application. The option of banding UAN without any additive promoted higher N2O losses on a year when precipitation was well distributed, but also enhanced grain yield and NFRE. On the other hand, under the same precipitation conditions, broadcasting N fertilizer promoted lower N2O losses, grain yield and NFRE, but those were all improved in a wet year. Therefore, the subsurface band placement would be the best option under a normal year, whereas broadcasting fertilizer would be the best option under a wetter year. Further, the use of NI with subsurface band UAN provides the most sustainable option, since the NI decreased N2O losses compared to UAN alone in both years. Further research should evaluate N source and placement combinations under different environments in order to better understand how they impact crop performance and the negative environmental aspects of N fertilization. It is important to test those treatments under different precipitation scenarios and look for trends that indicate the best N management option at the local level.

Procedursmärta är den vanligaste orsaken till smärta hos barn i sjukvården. Dagligen genomförs diagnostiska och terapeutiska procedurer på barn, som både är skrämmande och smärtsamma. Barn som upplever otillräcklig smärtlindring under medicinska procedurer har en högre nivå av rädsla och ångest inför framtida procedurer, de reagerar dessutom kraftigare på akut smärta. Att låta barn inhalera en blandning av lustgas och syrgas ger både en smärtlindring och sedering. Stor fördel är att lustgas är enkel att administrera, har en kort anslagstid och effekten avklingar snabbt när inhalationen avslutas, och ger få biverkningar. Syftet med litteraturstudien var att beskriva effekten av lustgas i samband med att barn utsätts för smärtsamma procedurer inom hälso- och sjukvården. En litteraturstudie utfördes där tio vetenskapliga studier grundlade resultetet. Vid bearbetningen identifierades tre olika teman, dessa var; Lustgas och smärta, Lustgas och biverkningar, Lustgas och fasta. I resultatet framkom att lustgassedering är en effektiv och säker metod för att uppnå smärtlindring och sedering under mindre, men smärtsamma medicinska procedurer, med få biverkningar. Allt fler barn sederas med lustgas vid olika medicinska procedurer av icke anestesiutbildade sjuksköterskor. En konklusion av resultatet var, för att sjuksköterskan ska kunna möta kraven måste systematisk utbildning och träning finnas och tydliga guidelines utarbetas och vara förankrad hos all personal. Detta måste prioriteras, förbättras och kontinuerligt uppdateras.

Nitrous oxide (N2O) is a widely used anesthetic adjunct in dentistry and medicine that is also commonly abused. N2O alters the function of several receptors in vitro and ex vivo, however, the receptors systems underlying its abuse-related intoxicating effects are poorly understood. The goals of this dissertation were to (1) establish N2O as a discriminative stimulus, (2) characterize the temporal properties of the discriminative stimulus, (3) determine the degree of similarity between N2O and other inhalants and (4) explore the neurochemical effects responsible for the stimulus properties of N2O. Twenty-four mice were trained to discriminate 10 minutes exposure to 60% N2O+40% O2 from 100% O2 in daily 5 minute food-reinforced operant sessions. Mice acquired the discrimination in a mean of 38 sessions. N2O produced concentration-dependent full substitution for itself. Full substitution required 7 minutes of N2O exposure but the offset of stimulus effects following cessation of N2O exposure were more rapid. Varying degrees of partial substitution for N2O were engendered by abused vapors and vapor anesthetics. The aromatic hydrocarbon toluene produced the most robust substitution for N2O. One or more toluene concentrations produced full substitution for N2O in 7 of 8 subjects, suggesting that these two abused inhalants share common neurochemical mechanisms. The NMDA receptor open channel blockers (+)-MK-801, ketamine and memantine produced dose-dependent partial substitution for N2O. A competitive NMDA antagonist and NMDA glycine site antagonist did not substitute for N2O. Pretreatment with (+)-MK-801 as well as ethanol produced dose-dependent leftward shifts in the N2O concentration effect curve further suggesting some overlap in their mechanisms of action. GABAA agonists and positive allosteric modulators, opioid agonists, serotonergic agonists, nicotine, a nNOS inhibitor and the psychomotor stimulant amphetamine all failed to appreciably substitute for N2O and/or failed to alter the N2O concentration effect curve when administered prior to N2O exposure. No drug tested produced greater than 80% mean N2O-lever selection leaving open the possibility of other neurochemical contributors to the stimulus effects of N2O.

Doctor of Philosophy / Department of Agronomy / Charles W. Rice / Nitrogen is critical for plant growth and is a major cost of inputs in production agriculture. Too much nitrogen (N) is also an environmental concern. Agricultural soils account for 85% of anthropogenic N₂O which is a major greenhouse gas. Management strategies for N fertilization and tillage are necessary for enhancing N use efficiency and reducing negative impacts of N to the environment. The different management practices induce changes in substrate availability for microbial activity that may result in increasing or reducing net N₂O emitted from soils. The objectives of this research were to (1) integrate results from field studies to evaluate the effect of different management strategies on N₂O emissions using a meta-analysis, (2) quantify N₂O-N emissions under no-tillage (NT) and tilled (T) agricultural systems and the effect of different N source and placements, (3) perform sensitivity analysis, calibration and validation of the Denitrification Decomposition (DNDC) model for N₂O emissions, and (4) analyze future scenarios of precipitation and temperature to evaluate the potential effects of climate change on N₂O emissions from agro-ecosystems in Kansas. Based on the meta-analysis there was no significant effect of broadcast and banded N placement. Synthetic N fertilizer usually had higher N₂O emission than organic N fertilizer. Crops with high N inputs as well as clay soils had higher N₂O fluxes. No-till and conventional till did not have significant differences regarding N₂O emissions. In the field study, N₂O-N emissions were not significantly different between tillage systems and N source. The banded N application generally had higher emissions than broadcasted N. Slow release N fertilizer as well as split N applications reduced N₂O flux without affecting yield. Simulations of N₂O emissions were more sensitive to changes in soil parameters such as pH, soil organic carbon (SOC), field capacity (FIELD) and bulk density (BD), with pH and SOC as the most sensitive parameters. The N₂O simulations performed using Denitrification Decomposition model on till (Urea) had higher model efficiency followed by no-till (compost), no-till (urea) and till (compost). At the regional level, changes in climate (precipitation and temperature) increased N₂O emission from agricultural soils in Kansas. The conversion from T to NT reduced N₂O emissions in crops under present conditions as well as under future climatic conditions.

Seagrass meadows may play a substantial role in climate change mitigation as they are capable to sequester and store substantial amounts of anthropogenic carbon in plant biomass and, more importantly, in their underlying sediments. In this PhD thesis, the carbon-burial potential was assessed by quantifying the amount of organic carbon stored in different seagrass meadows, each dominated by one of the four major seagrass species in the Western Indian Ocean region. Impacts of anthropogenic disturbances on biomass carbon allocation, greenhouse gas emission (methane and nitrous oxide) and production of sulphide were investigated in Chwaka Bay, Zanzibar. The findings showed that east African seagrass meadows generally have high carbon sink capacity. The storage of sedimentary organic carbon, however, varied among seagrass habitats and across sites, and was up to five-fold higher in seagrass sediment to those of nearby unvegetated sediments. Seagrass meadows in eutrophicated sites had higher sedimentary organic carbon content, and substantially higher emission rates of nitrous oxides and methane, compared to more pristine meadows. Disturbances in terms of shading and simulated grazing of seagrass affected several processes, with major decreases in seagrass primary productivity, net community production and biomass carbon, in turn influencing seagrass carbon sequestration as well as stimulating anaerobic microbial processes. In addition, production of sulphide in the sediment and methane emissions from the sediment surface increased significantly when disturbed. At present, seagrass meadows in the Western Indian Ocean have high carbon sink capacity. This important ecosystem service is, however, highly threatened due to regional anthropogenic pressure, which may change the role of blue carbon rich habitats, such as seagrass meadows, from being a sink to a source of greenhouse gases. / <p>At the time of the doctoral defense, the following papers were unpublished and had a status as follows: Paper 1: Manuscript. Paper 2: Manuscript. Paper 4: Manuscript. Paper 5: Manuscript.</p>

Le cycle océanique de l'azote est à l'origine de deux rétro-actions climatiques au sein du système terre. D'unepart, il participe au contrôle du réservoir d'azote fixé disponible au développement du phytoplancton et à lamodulation de la pompe biologique, un des mécanismes de séquestration du carbone anthropique. D'autre part,le cycle de l'azote produit un gaz à effet de serre et destructuer d'ozone, le protoxyde d'azote (N2O). L'évolutionfuture du cycle de l'azote sous l'influence du rechauffement climatique, de la déoxygénation et de l'acidificationdes océans reste une question ouverte. Les processus tels que la fixation d'azote, la dénitrification et laproduction de protoxyde d'azote seront modifiés sous l'influence conjuguée des ces trois stresseurs. Cesinteractions peuvent être évaluées grâce aux modèles globaux de biogéochimie marine. Nous utilisons NEMOPISCESet l'ensemble des modèles CMIP5 pour projeter les modifications des taux de fixation d'azote, denitrification, de production et des flux air-mer de N2O à l'horizon de 2100 en réponse au scénario 'business-asusual'.Les effets liés à l'action combinée du rechauffement climatique et de l'acidification des océans sur leréservoir d'azote fixé, la production primaire et la rétro-action sur le bilan radiatif sont également évalués danscette thèse.! / The marine nitrogen cycle is responsible for two climate feedbacks in the Earth System. Firstly, it modulates thefixed nitrogen pool available for phytoplankton growth and hence it modulates in part the strength of thebiological pump, one of the mechanisms contributing to the oceanic uptake of anthropogenic CO2. Secondly, thenitrogen cycle produces a powerful greenhouse gas and ozone (O3) depletion agent called nitrous oxide (N2O).Future changes of the nitrogen cycle in response to global warming, ocean deoxygenation and oceanacidification are largely unknown. Processes such as N2-fixation, nitrification, denitrification and N2Oproduction will experience changes under the simultaneous effect of these three stressors. Global oceanbiogeochemical models allow us to study such interactions. Using NEMO-PISCES and the CMIP5 modelensemble we project changes in year 2100 under the business-as-usual high CO2 emissions scenario in globalscale N2-fixation rates, nitrification rates, N2O production and N2O sea-to-air fluxes adding CO2 sensitivefunctions into the model parameterizations. Second order effects due to the combination of global warming intandem with ocean acidification on the fixed nitrogen pool, primary productivity and N2O radiative forcingfeedbacks are also evaluated in this thesis.

O óxido nitroso (N2O) é o terceiro gás de efeito estufa natural mais importante no planeta Terra, suas emissões são provenientes, principalmente da atividade bacteriana em processos de nitrificação e desnitrificação. Este estudo foi desenvolvido com o objetivo de elucidar a contribuição da Bacia Amazônica nas emissões de N2O nos anos de 2010 e 2011. A quantificação do N2O foi realizada por meio da coleta do ar atmosférico utilizando aviões de pequeno porte que descreveram um perfil vertical da superfície até 4,4 km de altitude, em quatro locais, posicionados de tal forma na Bacia Amazônica, que possibilitasse um estudo que a representasse regionalmente. O fluxo de N2O foi estimado utilizando-se o método de integração de coluna que consiste na determinação da concentração deste gás, subtraído das concentrações de entrada do continente, levando-se em consideração o tempo que as massas de ar levaram da costa brasileira até o local de coleta. Foi determinada a emissão de N2O pela queima de biomassa, utilizando a razão CO:N2O, determinada nos perfis amostrados durante a estação de queima de biomassa. A Amazônia apresentou um caráter emissor para N2O, com uma emissão maior em 2010 de 3,84 TgN2O ano-1 e de 1,93 TgN2O ano-1 em 2011. Este comportamento provavelmente é resultante do efeito da temperatura mais elevada em 2010 do que 2011. / Nitrous oxide (N2O) is the third most important natural greenhouse gas on planet Earth, it emissions are provided, mainly from bacterial activity during process of nitrification and denitrification. This study was developed with the goal to elucidate the Amazon Basin contribution on N2O emissions during the years of 2010 and 2011. N2O quantification was performed by collecting atmospheric air using small aircraft that described a vertical profile from surface until 4,4 km of altitude, in four sites, positioned over the Amazon Basin so we could study it whole. The flux was estimated through column integration method, which consists in determine N2O subtracted from background concentrations and taking into account the time these air masses spent between the coast and the sampling sites. To determine N2O biomass burning contribution, the CO:N2O ratio was estimated at the dry season profiles. The Amazon presented an emission behavior for N2O, 3,84 TgN2O year-1 in 2010 and 1,93 TgN2O year-1 in 2011. This behavior is resulted by higher temperatures effects in 2010 than 2011.

As emissões de gases de efeito estufa (GEE) para atmosfera representam um dos principais desafios da população mundial atualmente. A pecuária contribui para as emissões antrópicas principalmente de metano (CH4) e óxido nitroso (N2O) à tmosfera. O Brasil possui o maior rebanho bovino comercial do mundo e assim, possui importante participação nas emissões destes gases. As emissões de CH4 são provenientes principalmente da fermentação entérica e da deposição de fezes nos solos sob pastagem,.as emissões de N2O são provenientes da urina. Os fatores de emissão utilizados para quantificar as emissões na pecuária foram desenvolvidos pelo Intergovernamental Panel of Climate Change baseados em pesquisas realizadas em regiões de clima temperado. Dessa maneira faz-se necessária a determinação de fatores específicos as condições tropicais brasileiras possibilitando exatidão na quantificação das emissões de GEE. O presente trabalho teve como objetivo quantificar as emissões de CH4 provenientes das fezes e de N2O provenientes da urina de bovinos de corte depositadas em solos sob pastagens, assim como verificar a interferência de diferentes manejos dos animais, fatores climáticos e fatores intrínsecos aos dejetos nestas emissões. A pesquisa foi desenvolvida em propriedade privada (Agropecuária Nova Vida, localizada em Ariquemes, RO), produtora de bovinos de corte em sistemas de manejo à pasto e emi-confinamento. As emissões de CH4 e N2O foram quantificadas nos dejetos provenientes dos animais à pasto e em semi-confinamento, em duas áreas experimentais: pasto sem e com cobertura protegendo as amostras da insolação direta e precipitação pluvial. Durante o período de coleta dos gases (10 dias) foram verificados variações na umidade, temperatura e teor de carbono nas fezes, umidade e teor de nitrogênio no solo com adição de urina em diferentes profundidades (0-3 cm, 3-6 cm, 6-10 cm, 10-15 cm, 15-20 cm). Adicionalmente, foram quantificadas as emissões de CH4 e N2O provenientes do solo sem deposição de dejetos, como tratamento testemunha. Com relação às variáveis climáticas, verificou-se interação significativa da umidade das fezes com a produção de CH4 no bolo fecal. A produção de N2O é extremamente variável, apresentando variação temporal e sazonal. O efeito da dieta na produção dos gases nos dejetos não pode ser avaliado devido a problemas metodológicos. Os fatores de emissão encontrados foram: 0,6 kg C-CH4 animal-1 ano -1 e 0,05 kg N-N2O kg N aplicado-1, para fezes e urina depositadas no solo, respectivamente. O balanço das emissões de GEE na propriedade foi calculado considerando todas as fontes de emissão de CH4 e N2O e o estoque de C nas pastagens. A emissão líquida determinada foi de 5.350 Mg C-equivalente na propriedade no ano de 2009. Limitações metodológicas proporcionaram a geração de resultados considerados parciais. Futuras pesquisas são sugeridas para que o conhecimento das emissões de CH4 provenientes das fezes e N2O da urina de bovinos em clima tropical seja consolidado / Global warming and greenhouse gases (GHG) emissions to the atmosphere represent one of the major challenges to modern society. Livestock production contributes mainly to methane (CH4) and nitrous oxide (N2O) emissions. Brazil has the largest commercial cattle herd in the world and accordingly contributes a significant amount to global emissions levels of these gases. Methane emissions are mainly from enteric fermentation and feces deposition on soils under pastures. Nitrous oxide emissions occur from urine deposition on soils under pastures. Emission factors that are used to quantify livestock emissions were defined by the Intergovernmental Panel on Climate Change and were developed based on studies conducted in temperate regions. However, it is necessary to determine specific emission factors that reflect the reality of Brazilian tropical conditions allowing accurate GHG emissions quantification. This study aims to quantify CH4 emissions from feces and N2O from urine of beef cattle deposited on soils under pastures. It also intends to verify the interference of different animal managements, weather and intrinsic manure factors on emissions levels. The research was conducted on a private property (Agropecuária Nova Vida) located in Ariquemes, RO. The Farms main activity is beef cattle production based on grazing and semi-confinement systems. Emissions of CH4 and N2O are quantified on two experimental areas: pasture without coverage and pastures with coverage protecting the samples from direct sunlight and rainfall. In addition to gases sampling (10 days) on feces moisture, temperature and carbon content are monitored. Moisture and nitrogen content in the soil with urine deposition are monitored at different depths (0-3 cm, 3-6 cm, 6-10 cm, 10-15 cm, 15-20 cm). Additionally, we have quantified CH4 and N2O emissions from soil without manure deposition as a control treatment. We have found statistically different emissions levels between soils with and without manure. Moisture on feces had a statistical significant effect on CH4 emissions from feces. Nitrous oxide production is extremely variable with temporal and seasonal variations. The effect of diet on gases production in manure is not evaluated due to methodological problems. The estimations for emission factors are: 0.6 kg CH4-C animal-1 year-1 and 0.05 kg N2O-N kg N-1 for feces and urine deposited in the soil, respectively. The GHG balance of the whole farm is calculated considering all sources of emission and the C stocks in pastures. The annual net emissions for the farm are determined as 5350 Mg C equivalent. Methodological limitations provided partial results. Future research is suggested to achieve better estimations on CH4 and N2O emissions from beef cattle feces and urine in tropical climate