Nas últimas décadas as mudanças climáticas foram evidenciadas pelo aumento da temperatura global, diminuição dos estoques de carbono terrestres, associados ao aumento nas emissões de gases de efeito estufa (GEE). A floresta Amazônica é o maior bioma tropical do mundo e desenvolve serviços ambientais estratégicos no planeta. Entretanto, há mais de duas décadas que o desmatamento na Amazônia impulsiona as emissões globais de GEE, diminuindo o armazenamento de carbono do solo com alterações na dinâmica nas populações microbianas e nos ciclos biogeoquimicos pela mudança de uso da terra. O objetivo desse estudo foi avaliar as alterações temporais dos atributos químicos do solo, quantificar as emissões de CO2, CH4 e N2O e verificar as alterações na estrutura bacteriana do solo após o corte e queima de vegetação nativa na Amazônia. O estudo foi desenvolvido em área de vegetação nativa no norte do estado de Rondônia, região sul da Amazônia no Brasil. A área de estudo consistiu-se de quatro hectares, onde foi realizado o corte e queima em 2,25 hectares. Foram realizadas amostragens para avaliação da fertilidade do solo e estoques de carbono (C) e nitrogenio (N) nas profundidades de 0-5, 5-10, 10-15, 15-20, 20-30, 30-40, 40-50, 50-60, 60-80 e 80-100 cm. As coletas foram realizadas em vegetação nativa e aos 2, 30, 60, 90, 120, 240 e 365 dias após corte e queima. Foram determinados os atributos pH, Al, H+Al, Ca, Mg, K, P, C, N e calculados os valores de soma de bases, CTC, V % e m %. As coletas para quantificar as emissões dos GEE foram realizadas simultaneamente na área de vegetação nativa e no hectare central da área de corte e queima aos 19, 31, 48, 61 e 81 dias após corte e 2 , 4, 6, 8, 15, 31, 45, 61, 88, 122, 153, 180, 240 e 350 dias após queima, com amostragens aos 0, 20, 40 e 60 minutos. Os atributos microbiológicos do solo foram avaliados pela técnica de T-RFLP com amostragens realizadas simultaneas nas duas áreas, aos 32 e 62 dias após o corte e aos 2, 15, 30, 45, 60, 90, 120, e 360 dias após queima da biomassa vegetal. Foi verificado rápido aumento da fertilidade do solo e diminuição da acidez e teores de Al+3 após a queima, entretanto esse efeito foi pouco persistente, retornando ao status inicial do solo após um ano. Houve redução de 30 % nos estoques de C e N do solo no final do estudo, evidenciando os efeitos deletérios da mudança do uso da terra nos atributos químicos do solo. Foi registrado redução de 50 % das emissões de CO2 equivalente após o corte, comparada à vegetação nativa e reduções nas emissões de GEE de 35 % após um ano de estudo. Verificou-se na camada superficial, alterações significativas na estrutura da comunidade bacateriana do solo em decorrência do impacto do fogo e das alterações nos atributos químicos em função da deposição superficial de cinzas no solo, entretanto não foi verificada alterações significativa nas camadas abaixo de 5 cm. Este estudo forneceu importantes informações para o entendimento dos impactos e as alterações causadas pelo processo de conversão florestal tropical pelo corte e queima de vegetação nativa na Amazônia. / In recent decades, climate change has been evidenced by the increase in global temperature and the decrease in terrestrial carbon stocks, associated with an increase in greenhouse gas (GHG) emissions. The Amazon rainforest is the largest tropical biome in the world and develops strategic environmental services on the planet. However, for more than two decades, deforestation in Amazon has driven global GHG emissions, reducing soil carbon storage with changes in microbial populations dynamics and in biogeochemical cycles due to land use change. The objective of this study was to evaluate the temporal alterations of soil chemical attributes, quantify CO2, CH4 and N2O emissions and verify changes in soil bacterial structure, due to the slash and burn of the native vegetation in Amazon. The study was developed in an area of native vegetation in the north of Rondônia state, southern region of Amazon in Brazil. The study area consisted of 4 hectares, where it was cut and burned in 2.25 hectares. Samples were collected to evaluate soil fertility and carbon (C) and nitrogen (N) stocks at the depths of 0-5, 5-10, 10-15, 15-20, 20-30, 30-40, 40- 50, 50-60, 60-80 and 80-100 cm. These samples were collected in native vegetation at 2, 30, 60, 90, 120, 240 and 365 days after cutting and burning. The attributes pH, Al, H + Al, Ca, Mg, K, P, C, N were determined and the values of base sum, CEC, base saturation and aluminum saturation were calculated. The samples to quantify GHG emissions were carried out simultaneously in the native vegetation area and in the central hectare of the cutting and burning area at 19, 31, 48, 61 and 81 days after cutting and 2, 4, 6, 8, 15, 31, 45, 61, 88, 122, 153, 180, 240 and 350 days after burning, with samples at 0, 20, 40 and 60 minutes. The microbiological attributes of the soil were evaluated by T-RFLP technique with simultaneous samplings in the two areas, at 32 and 62 days after cutting and at 2, 15, 30, 45, 60, 90, 120, and 360 days after plant biomass burning. A rapid increase in soil fertility and a decrease in acidity and Al+3 contents after burning were verified, however this effect was not persistent, returning to the initial soil status after one year. There was a 30 % reduction in soil C and N stocks at the end of the study, evidencing the deleterious effects of land use change on soil chemical attributes. Also, a 50 % reduction in CO2 emissions after cutting, compared to native vegetation and, a 35 % reduction in GHG emissions after one year of study, were observed. We verified in the surface layer, significant alterations in the soil bacteria structure due to the fire impact and the changes in the chemical attributes, such as surface deposition of ashes. However, we did not verified significant changes in the layers lower than 5 cm. Our study provided important information for understanding the impacts and changes of the tropical forest conversion process by slash and burning native vegetation in Amazon.

Nas últimas décadas as mudanças climáticas foram evidenciadas pelo aumento da temperatura global, diminuição dos estoques de carbono terrestres, associados ao aumento nas emissões de gases de efeito estufa (GEE). A floresta Amazônica é o maior bioma tropical do mundo e desenvolve serviços ambientais estratégicos no planeta. Entretanto, há mais de duas décadas que o desmatamento na Amazônia impulsiona as emissões globais de GEE, diminuindo o armazenamento de carbono do solo com alterações na dinâmica nas populações microbianas e nos ciclos biogeoquimicos pela mudança de uso da terra. O objetivo desse estudo foi avaliar as alterações temporais dos atributos químicos do solo, quantificar as emissões de CO2, CH4 e N2O e verificar as alterações na estrutura bacteriana do solo após o corte e queima de vegetação nativa na Amazônia. O estudo foi desenvolvido em área de vegetação nativa no norte do estado de Rondônia, região sul da Amazônia no Brasil. A área de estudo consistiu-se de quatro hectares, onde foi realizado o corte e queima em 2,25 hectares. Foram realizadas amostragens para avaliação da fertilidade do solo e estoques de carbono (C) e nitrogenio (N) nas profundidades de 0-5, 5-10, 10-15, 15-20, 20-30, 30-40, 40-50, 50-60, 60-80 e 80-100 cm. As coletas foram realizadas em vegetação nativa e aos 2, 30, 60, 90, 120, 240 e 365 dias após corte e queima. Foram determinados os atributos pH, Al, H+Al, Ca, Mg, K, P, C, N e calculados os valores de soma de bases, CTC, V % e m %. As coletas para quantificar as emissões dos GEE foram realizadas simultaneamente na área de vegetação nativa e no hectare central da área de corte e queima aos 19, 31, 48, 61 e 81 dias após corte e 2 , 4, 6, 8, 15, 31, 45, 61, 88, 122, 153, 180, 240 e 350 dias após queima, com amostragens aos 0, 20, 40 e 60 minutos. Os atributos microbiológicos do solo foram avaliados pela técnica de T-RFLP com amostragens realizadas simultaneas nas duas áreas, aos 32 e 62 dias após o corte e aos 2, 15, 30, 45, 60, 90, 120, e 360 dias após queima da biomassa vegetal. Foi verificado rápido aumento da fertilidade do solo e diminuição da acidez e teores de Al+3 após a queima, entretanto esse efeito foi pouco persistente, retornando ao status inicial do solo após um ano. Houve redução de 30 % nos estoques de C e N do solo no final do estudo, evidenciando os efeitos deletérios da mudança do uso da terra nos atributos químicos do solo. Foi registrado redução de 50 % das emissões de CO2 equivalente após o corte, comparada à vegetação nativa e reduções nas emissões de GEE de 35 % após um ano de estudo. Verificou-se na camada superficial, alterações significativas na estrutura da comunidade bacateriana do solo em decorrência do impacto do fogo e das alterações nos atributos químicos em função da deposição superficial de cinzas no solo, entretanto não foi verificada alterações significativa nas camadas abaixo de 5 cm. Este estudo forneceu importantes informações para o entendimento dos impactos e as alterações causadas pelo processo de conversão florestal tropical pelo corte e queima de vegetação nativa na Amazônia. / In recent decades, climate change has been evidenced by the increase in global temperature and the decrease in terrestrial carbon stocks, associated with an increase in greenhouse gas (GHG) emissions. The Amazon rainforest is the largest tropical biome in the world and develops strategic environmental services on the planet. However, for more than two decades, deforestation in Amazon has driven global GHG emissions, reducing soil carbon storage with changes in microbial populations dynamics and in biogeochemical cycles due to land use change. The objective of this study was to evaluate the temporal alterations of soil chemical attributes, quantify CO2, CH4 and N2O emissions and verify changes in soil bacterial structure, due to the slash and burn of the native vegetation in Amazon. The study was developed in an area of native vegetation in the north of Rondônia state, southern region of Amazon in Brazil. The study area consisted of 4 hectares, where it was cut and burned in 2.25 hectares. Samples were collected to evaluate soil fertility and carbon (C) and nitrogen (N) stocks at the depths of 0-5, 5-10, 10-15, 15-20, 20-30, 30-40, 40- 50, 50-60, 60-80 and 80-100 cm. These samples were collected in native vegetation at 2, 30, 60, 90, 120, 240 and 365 days after cutting and burning. The attributes pH, Al, H + Al, Ca, Mg, K, P, C, N were determined and the values of base sum, CEC, base saturation and aluminum saturation were calculated. The samples to quantify GHG emissions were carried out simultaneously in the native vegetation area and in the central hectare of the cutting and burning area at 19, 31, 48, 61 and 81 days after cutting and 2, 4, 6, 8, 15, 31, 45, 61, 88, 122, 153, 180, 240 and 350 days after burning, with samples at 0, 20, 40 and 60 minutes. The microbiological attributes of the soil were evaluated by T-RFLP technique with simultaneous samplings in the two areas, at 32 and 62 days after cutting and at 2, 15, 30, 45, 60, 90, 120, and 360 days after plant biomass burning. A rapid increase in soil fertility and a decrease in acidity and Al+3 contents after burning were verified, however this effect was not persistent, returning to the initial soil status after one year. There was a 30 % reduction in soil C and N stocks at the end of the study, evidencing the deleterious effects of land use change on soil chemical attributes. Also, a 50 % reduction in CO2 emissions after cutting, compared to native vegetation and, a 35 % reduction in GHG emissions after one year of study, were observed. We verified in the surface layer, significant alterations in the soil bacteria structure due to the fire impact and the changes in the chemical attributes, such as surface deposition of ashes. However, we did not verified significant changes in the layers lower than 5 cm. Our study provided important information for understanding the impacts and changes of the tropical forest conversion process by slash and burning native vegetation in Amazon.

La fertilité de terres agricoles dépend en large partie du recyclage des nutriments dans le sol. Généralement, ce recyclage est effectué en grande partie par les communautés bactériennes du sol. On assume donc souvent que la diversité bactérienne du sol peut constituer un indicateur de sa santé/fertilité. Cependant, certaines pratiques agricoles conventionnelles nuisent à la diversité bactérienne du sol. Parmi ces pratiques, le labourage et les applications d’intrants chimiques tels que les pesticides, les antibiotiques et les engrais influencent négativement la diversité microbienne. Par conséquent, des recherches actives sont menées pour développer des façons de rétablir la diversité microbienne dans les sols en agriculture conventionnelle. Plusieurs alternatives biologiques ont été développées au fil des ans, aboutissant à des produits commerciaux en tant que des biostimulants incluant des substances d’origines biologiques, des microorganismes ou la combinaison des deux. Entre autres, le thé de compost a été développé et suggéré comme étant un produit riche en microorganismes bénéfiques, ayant les capacités d’améliorer les cultures et la durabilité des systèmes agricoles biologiques. Cependant, sa performance et son application à grande échelle dans les systèmes de production conventionnelle demeurent peu étudiées. L’objectif de ce mémoire et d’évaluer l'effet du thé de compost sur l'abondance, la diversité et la structure des communautés bactériennes du sol et les rendements, dans un essai en champs de la production du soja dans un système conventionnel de monoculture. Dans un champ d’environ trois hectares est subdivisé en six blocs, chacun contenait deux parcelles: l'une a été traitée par le thé de compost frais et l'autre a été utilisé comme témoin avec thé de compost stérilisé à la chaleur pour tuer les microorganismes. Notre hypothèse est que le thé de compost frais améliore la croissance du soja et son rendement avec l’apport de microorganismes bénéfiques et l’enrichissement des communautés bactériennes des sols. Le séquençage à haut débit de l’ADN ribosomique 16S bactérien extrait de différents échantillons (thé de compost, sol traité et sol témoin), associé aux analyses bio-informatiques et statistiques, a démontré que le traitement du thé de compost frais n'a pas influencé de manière significative les communautés bactériennes, ni par des changements dans la diversité alpha, ni dans la structure de la communauté de celles-ci. De plus, les résultats des analyses de croissance des plantes et de rendement ont eu aucun effet significatif du thé de compost frais sur la biomasse végétative des plantes ou le poids des graines de soja. Nos résultats de recherche indiquent que le thé de compost frais utilisé dans notre expérience n’a pas modifié les communautés bactériennes des sols traités et n’a pas influencé la croissance des plantes ni le rendement en grain. Notre hypothèse n’est pas supportée par ces résultats qui suggèrent que les bénéfices relatifs à l’application du thé de compost frais ne sont pas dus aux microorganismes vivants mais plutôt à un apport potentiel des nutriments. L’absence d'effets positifs dans notre étude pourrait être attribué spécifiquement à notre conception expérimentale, au thé de compost utilisé, ou à la dose ou la fréquence d'application de celui-ci. D’autres expériences sont nécessaires afin de tirer des conclusions robustes quant à l’effet et la performance du thé de compost sur des cultures conventionnelles. / The fertility of agricultural lands largely depends on the recycling of nutrients in the soil. Usually, this recycling is carried out largely by bacterial communities in the soil, that their diversity is an important indicator of the health and fertility of agricultural soils. However, some agricultural practices, especially in conventional production systems, harm the essential functions of these soil bacterial communities. Among these practices, tillage and the applications of chemical inputs such as pesticides, antibiotics and fertilizers negatively influence the diversity and structures of microbial communities. As a result, the abundance and diversity of these beneficial microorganisms and the potential services they provide decrease in these soils. Several biological alternatives have been developed over the years, resulting in commercial products as biostimulants including substances of biological origin, microorganisms or a combination of the two. Among others, compost tea has been developed and suggested as a product rich in beneficial microorganisms, with the capacity to improve crops and the sustainability of organic farming systems. However, its performance and large-scale application in conventional production systems remains little studied. The objective of this master’s thesis is to assess the effect of fresh compost tea on the abundance, diversity and structure of soil bacterial communities and yields, in a field trial of soybean production in a conventional system of monoculture. In a field of about three hectares is subdivided into six blocks, each one contained two plots: one was treated with fresh compost tea and the other was used as a control with heat sterilized compost tea to kill microorganisms. Our hypothesis is that fresh compost tea improves soybean growth and yield with the addition of beneficial microorganisms and the enrichment of bacterial communities in soils. High throughput sequencing of bacterial 16S ribosomal DNA extracted from different samples (compost tea, treated soil and control soil), combined with bioinformatics and statistical analyzes, demonstrated that processing of compost tea did not significantly influenced bacterial communities, neither by changes in alpha diversity nor in their community structure. In addition, the results of plant growth and yield analyzes had no significant effect of fresh compost tea on plant vegetative biomass or soybean weight. Our research results indicate that the fresh compost tea used in our experiment did not change the bacterial population in the treated soils and it did not show a significant effect on either plant growth or yield. Our hypothesis is not supported by these results which suggest that the relative benefits of the application of compost tea are not due to living microorganisms but rather to a potential supply of nutrients. The lack of positive effects in our study could be attributed specifically to our experimental design, the compost tea used, or the dose or frequency of its application. More experiments are needed in order to draw robust conclusions about the effect and performance of compost tea on conventional crops.