Nos últimos anos o interesse pelo estudo da Terra Preta de Índio (TPI) tem aumentado em razão das suas características únicas em relação aos solos normalmente encontrados na região, como sua maior fertilidade natural. Diversos estudos relatam que a presença do chamado carbono pirogênico na composição das TPIs é a responsável por esta superioridade, entretanto ainda não se sabe se este afeta as propriedades físicas dos solos de TPI. Esta pesquisa tem como objetivo comparar o comportamento de propriedades físico-hídricas de solos antrópicos (Terra Preta de Índio) com um solo adjacente por meio da determinação de suas propriedades físicas, e verificar a distribuição do carbono pirogênico entre os diferentes compartimentos da matéria orgânica em solos de TPI e adjacentes. Para este estudo foram coletadas amostras indeformadas em anéis volumétricos e blocos em uma área de TPI e adjacente. As áreas estão localizadas na Floresta Nacional de Caxiuanã, estado do Pará. As propriedades físicas analisadas foram textura, porosidade total, macro e microporosidade, curva de retenção da água no solo, condutividade hidráulica saturada, permeabilidade do solo ao ar e estabilidade de agregados. Para verificar o comportamento da matéria orgânica foi realizado o fracionamento físico, onde foram analisados a distribuição do carbono total e pirogênico nas diferentes frações da matéria orgânica. Verificou-se diferença nas duas áreas quanto às propriedades físicas porosidade total, macro e microporosidade, condutividade hidráulica do solo (Ksat), permeabilidade do solo ao ar (Ka), e retenção de água no solo, entretanto não foi possível verificar diferenças na estabilidade de agregados entre as duas áreas. A distribuição da matéria orgânica nas diferentes frações do solo foi distinta nas duas áreas, onde verificou-se que na área de TPI o C no solo foi predominante na fração macroagregados, enquanto que na área adjacente o carbono se localizou em maior quantidade na fração microagregados. Os valores de carbono pirogênico foram maiores na área de TPI do que na área adjacente, demostrando que a matéria orgânica das TPIs apresenta uma composição diferenciada, modificando o comportamento das propriedades físicas dos solos. / In recent years the interest in the study of Terra Preta de Indio or Amazonian Dark Earths (TPI) has increased, especially because of its unique characteristics when related to typical soils of the region, as its higher natural fertility. Several studies have reported that the presence of so-called pyrogenic carbon in its composition is responsible for this superiority, however it is not known if it affects the physical properties of TPI soils. This research aims to compare the behavior of physical and hydraulic properties of anthropic soils (Terra Preta de Indio) to an adjacent soil by determining its physical properties, and evaluating the distribution of the pyrogenic carbon between the different compartments of organic matter for both soils. For this study, undisturbed soil samples were collected in volumetric cylinders and blocks from a TPI and adjacent area. The areas are located in Caxiuanã National Forest, state of Pará, Brazil. The analyzed physical properties were texture, porosity, macro and microporosity, soil water retention curve, soil saturated hydraulic conductivity, soil permeability to air and aggregate stability. A physical fractionation was performed to verify the behavior of organic matter, which analyzed the distribution of the total and pyrogenic carbon in the different fractions of organic matter. There were difference in the two areas regarding the physical properties as total porosity, macro and microporosity, soil hydraulic conductivity (Ksat), air permeability to soil (Ka), and soil water retention, however it was not possible to see differences in stability aggregates between the two areas. The distribution of organic matter in different soil fractions was different in the two areas, where it was found that in the TPI area, soil carbon was prevalent in the macroaggregates fraction, while the adjacent area had larger amounts in the microaggregates fraction. The values for pyrogenic carbon were higher in the TPI area, showing that the organic matter of TPIs has a different composition which modifies the behavior of physical properties in the soil.

The solid product of pyrolysis, called \"biochar\" (BC) in the context of improving soil properties as part of agronomic or environmental management, also got into focus as a climate mitigation strategy. The researcher investigated the effects of BC on soil attributes, nitrogen (N) use and GHG emissions. In Chapter 1 the origin of BC was commented. In Chapter 2, BC from sugarcane straw was characterized, and its priming on native SC was evaluated with the treatments: (T1) Soil; (T2) BC; (T3) Soil + BC 10 Mg ha-1; (T4) Soil + BC 20 Mg ha-1; and (T5) Soil + BC 50 Mg ha-1. In Chapter 3, it was evaluated the combination of BC, filter cake (F) and vinasse (V), in relation to soil attributes and carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) emissions. The treatments were: (T1) Soil + FC + V; (T2) Soil + FC + V + BC 10 Mg ha-1; (T3) Soil + FC + V + BC 20 Mg ha-1; and (T4) Soil + FC + V + BC 50 Mg ha-1. In Chapter 4, the nitrogen (N) use efficiency was investigated in a pot trial under wheat using NH4[15N]O3 and rates of BC, with the treatments: (T1) Soil, with N, no BC; (T2) Soil, with N, BC 10 Mg ha-1; (T3) Soil, with N, BC 20 Mg ha-1; and (T4) Soil, with N, BC 50 Mg ha-1. BC had C and N contents higher compared to the feedstock. Total K, Mg and P also increased. The lowest CO2 fluxes were for BC, and CO2 from soil and soil + BC did not differ. The highest CO2 - C4 was in the first day, and there were no differences in the CO2 - C3. The BC presents characteristics to improve soil attributes. BC stability is an opportunity to reduce CO2 emissions. In Chapter 3, soil pH, P and base contents increased and Al3+ decreased with BC to sandy soil. Impacts of BC on the CEC were higher in sandy soil. Mineral N decreased with BC. Cumulative CO2 in T1 were higher in sandy and clayey soils than the control. T2 and T3 in sandy soil increased CO2 emissions, but T4 did not differ from T1. BC reduced N2O emissions from sandy and clayey soils relative to T1. BC with FC and V affected pH, CEC, P and base contents. However, those effects were higher in sandy soil. The BC supressed N2O from V and FC. In Chapter 4, BC decreased N2O from N fertilization compared to only N fertilizer. T4 had higher tillering and grain yield. Also, T2 to T4 had higher 100-grain weight and shoot. T3 and T4 had the highest N in grains. The application of BC to soil improves N availability and use efficiency, enhances grain yields and reduces N2O from N fertilization. This study opened encouraging perspectives to the evaluation of sugarcane straw BC to improve soil quality and mitigate GHG emissions. / O produto sólido da pirólise, denominado \"biochar\" (BC) no contexto da melhoria nos atributos do solo como parte do manejo agrícola e ambiental, também tem se destacado na mitigação das mudanças climáticas. O pesquisador investigou os efeitos do BC nos atributos do solo, uso do nitrogênio (N) e emissões de GEE. No Cap. 1 comentou-se a origem do BC. No Cap. 2, caracterizou-se o BC de palha de cana-de-açúcar e avaliou-se o potencial de decomposição do C do solo, com os tratamentos: (T1) Solo; (T2) BC; (T3) Solo + BC 10 Mg ha-1; (T4) Solo + BC 20 Mg ha-1 (T4); e (T5) Solo + BC 50 Mg ha-1. No Cap. 3, avaliou-se a combinação BC, torta de filtro (TF) e vinhaça (V) em atributos do solo e fluxos de dióxido de carbono (CO2), metano (CH4) e óxido nitroso (N2O) nos tratamentos: (T1) Solo + TF + V; (T2) Solo + TF + V + BC 10 Mg ha-1; (T3) Solo + TF + V + BC 20 Mg ha-1; e (T4) Solo + TF + V + BC 50 Mg ha-1. No Cap. 4 investigou-se a eficiência de uso do N num experimento em vasos com trigo usando NH4 [15N]O3 e doses de BC, com os tratamentos: (T1) Solo, com N, sem BC; (T2) Solo, com N, BC 10 Mg ha-1; (T3) Solo, com N, BC 20 Mg ha-1; e (T4) Solo, com N, BC 50 Mg ha-1. Os teores de C e N do BC foram maiores comparado à biomassa. K, Mg e P totais também aumentaram. Os menores fluxos de CO2 foram do BC. O CO2 do solo e solo + BC não diferiram. Observou-se maior CO2 - C4 no primeiro dia de incubação, porém sem diferenças no CO2 - C3. O BC apresenta características para melhorar atributos do solo e reduzir as emissões de CO2. No Cap. 3, pH, P e bases aumentaram e o Al3+ diminuíu com o BC. Os impactos do BC na CTC foram maiores em solo arenoso. O N mineral diminuíu com o BC. O CO2 acumulado no T1 foi maior nos solos arenoso e argiloso comparado ao controle. O T2 e T3 aumentaram o CO2 acumulado do arenoso relativo ao T1, enquanto T4 e T1 não diferiram. O BC reduziu as emissões de N2O pelos solos arenoso e argiloso comparado ao T1. O BC combinado à TF e V afetaram pH, CTC, P e bases do solo arenoso. O BC suprimiu o N2O de solos com V e TF. No Cap. 4, o BC diminuíu as emissões de N2O comparado ao fertilizante N apenas. T4 teve rendimento de grãos superior ao T1. T2 a T4 apresentaram maior peso de 100 grãos e biomassa aérea. T3 e T4 tiveram maior N em grãos. O BC melhora o uso do N, a produção de grãos e reduz o N2O de fertilizante N, abrindo perspectivas para a avaliação do BC de palha de cana-de-açúcar na melhoria da qualidade do solo e mitigar das emissões de GEE.

A Terra Preta Antropogênica (TPA) tem essa denominação porque é encontrada em sítios arqueológicos, onde viveram grupos pré-históricos e é considerada um dos solos mais férteis do mundo. Nela é encontrada grande quantidade de material deixado por grupos indígenas como fragmentos cerâmicos, artefatos líticos, e especialmente carvão pirogênico. Estudos realizados com o carvão pirogênico verificaram que ele aumenta a capacidade de trocas catiônicas nesses solos. Por meio de microscopia de fluorencência, foi observada a presença de microrganismos habitando esse carvão, no entanto, não se sabe quais seriam. Devido à falta de informações sobre a diversidade bacteriana nessas estruturas, este trabalho estudou a diversidade bacteriana em amostras de carvão pirogênico de solos TPA coletadas nos sítios Lagoa Balbina (Amazônia Central- Amazonas) e Mina I (Amazônia Oriental - Pará), através de técnicas moleculares independentes de cultivo. O estudo visou também comparar essa diversidade com a encontrada no solo de onde carvão foi isolado. As estruturas de carvão foram separadas fisicamente dos solos e seu DNA genômico total extraído e usado como molde em reação de PCR utilizando oligonucleotídeos do gene 16S rRNA para o Domínio Bacteria. O produto da PCR foi clonado em vetor e os clones foram sequenciados e comparados com o banco de dados de 16S rRNA do RDPX. Com a construção das bibliotecas de clones do gene 16S rRNA a partir das amostras de carvão pirogênico observou-se que existe maior número de bactérias desconhecidas no carvão pirogênico do que no solo onde ele foi isolado. Acidobacteria foi o filo predominante nas bibliotecas de carvão pirogênico das duas localidades de estudo, assim como na biblioteca do solo do sítio Mina I. Já na biblioteca do solo do sítio Lagoa Balbina houve predominância do filo Firmicutes. Por meio do método de rarefação foi possível constatar uma menor riqueza de UTOs nas comunidades bacterianas presentes nas estruturas de carvão pirogênico quando comparado à riqueza de UTOs das comunidades bacterianas cujo habitat é o solo. Mas quando se compara a riqueza de UTOs entre as estruturas de carvão isoladas das duas localidades, observa-se que a riqueza é maior no sítio Mina I. Os valores obtidos com os índices de diversidade revelaram menor diversidade de UTOs nas bibliotecas obtidas para o carvão pirogênico das duas regiões estudadas se comparado dos valores para as bibliotecas obtidas do solo da mesma região. Os valores obtidos com os métodos não paramétricos revelaram maior riqueza de UTOs para as bibliotecas do carvão do sítio Mina I e solo TPA do sítio Balbina. A análise da PCA revelou que as bibliotecas do sítio Balbina mostraram-se altamente similares. Em adição, a análise com S-Libshuff, verificou que todas as bibliotecas comparadas são significativamente diferentes quanto à composição das comunidades bacterianas. O carvão pirogênico não é uma estrutura inerte, pois é capaz de ser habitado por diferentes bactérias e a sua estrutura da comunidade bacteriana é diferente daquela de onde ele foi segregado / Anthropogenic Dark Earth (ADE) has this denomination because it is found at archeological sites, where prehistoric groups lived, and it is considered one of the most fertile soils of the world. In this soil a great amount of material left by indigenous groups was found as ceramic fragments, lithic workmanships, and especially pyrogenic black carbon. Studies accomplished with the pyrogenic black carbon verified that it increases the capacity of cationic changes in soils. Through fluorescence microscopy, the presence of microorganisms was observed inhabiting that black carbon, however, this community is still unknown,due to the lack of information about the bacterial diversity in those structures.This work studied the bacterial diversity in samples of pyrogenic black carbon of ADE soils, collected at the sites Lagoa Balbina (Central Amazon) and Mina I (Oriental Amazon), through molecular techniques independent of cultivation. The study also sought to compare that diversity with the one of the soil where black carbon was isolated. The structures of black carbon were separate physically from the soils and total genomic DNA was extracted and used as template in a PCR reaction, using primers of the 16S rRNA gene for the Bacteria Domain. The PCR product was used for construction of clone libraries and the clones were sequenced and compared with the 16S rRNA of RDPX database. The 16S rRNA gene clone libraries from the samples of pyrogenic black carbon, it shown that is a larger number of unknown bacteria in the black carbon than in the soil where it was isolated. Acidobacteria was the predominant phylum in the pyrogenic black carbon libraries from the both studied places, as well as in the soil library from Mina I site. However in the library Lagoa Balbina site there was predominance of the phylum Firmicutes. Through the rarefaction method it was possible to verify a smaller richness of OTUs in the bacterial communities presents in the pyrogenic black carbon structures when compared to the OTUs richness of the bacterial soil communities.But, when the OTUs richness is compared among the isolated structures of pyrogenic black carbon of the two places, it is observed that the richness is higher in the Mina I site. The values from diversity indexes revealed smaller diversity of OTUs in the pyrogenic black carbon libraries when compared with the soil libraries for the two studied areas. The obtained values with the nonparametric methods revealed larger OTUs richness in the black carbon library of Mina I site and in the ADE soil library of the Balbina site. The PCA analysis showed that the libraries of the site Balbina site were highly similar. In addition, the analysis with S-Libshuff verified that all of the compared libraries were significantly different in bacterial communities composition. The pyrogenic black carbon is not an inert structure, once it is capable of being inhabited by different bacteria, and its bacterial community structure is different from that one where is was segregated

Nos últimos anos o interesse pelo estudo da Terra Preta de Índio (TPI) tem aumentado em razão das suas características únicas em relação aos solos normalmente encontrados na região, como sua maior fertilidade natural. Diversos estudos relatam que a presença do chamado carbono pirogênico na composição das TPIs é a responsável por esta superioridade, entretanto ainda não se sabe se este afeta as propriedades físicas dos solos de TPI. Esta pesquisa tem como objetivo comparar o comportamento de propriedades físico-hídricas de solos antrópicos (Terra Preta de Índio) com um solo adjacente por meio da determinação de suas propriedades físicas, e verificar a distribuição do carbono pirogênico entre os diferentes compartimentos da matéria orgânica em solos de TPI e adjacentes. Para este estudo foram coletadas amostras indeformadas em anéis volumétricos e blocos em uma área de TPI e adjacente. As áreas estão localizadas na Floresta Nacional de Caxiuanã, estado do Pará. As propriedades físicas analisadas foram textura, porosidade total, macro e microporosidade, curva de retenção da água no solo, condutividade hidráulica saturada, permeabilidade do solo ao ar e estabilidade de agregados. Para verificar o comportamento da matéria orgânica foi realizado o fracionamento físico, onde foram analisados a distribuição do carbono total e pirogênico nas diferentes frações da matéria orgânica. Verificou-se diferença nas duas áreas quanto às propriedades físicas porosidade total, macro e microporosidade, condutividade hidráulica do solo (Ksat), permeabilidade do solo ao ar (Ka), e retenção de água no solo, entretanto não foi possível verificar diferenças na estabilidade de agregados entre as duas áreas. A distribuição da matéria orgânica nas diferentes frações do solo foi distinta nas duas áreas, onde verificou-se que na área de TPI o C no solo foi predominante na fração macroagregados, enquanto que na área adjacente o carbono se localizou em maior quantidade na fração microagregados. Os valores de carbono pirogênico foram maiores na área de TPI do que na área adjacente, demostrando que a matéria orgânica das TPIs apresenta uma composição diferenciada, modificando o comportamento das propriedades físicas dos solos. / In recent years the interest in the study of Terra Preta de Indio or Amazonian Dark Earths (TPI) has increased, especially because of its unique characteristics when related to typical soils of the region, as its higher natural fertility. Several studies have reported that the presence of so-called pyrogenic carbon in its composition is responsible for this superiority, however it is not known if it affects the physical properties of TPI soils. This research aims to compare the behavior of physical and hydraulic properties of anthropic soils (Terra Preta de Indio) to an adjacent soil by determining its physical properties, and evaluating the distribution of the pyrogenic carbon between the different compartments of organic matter for both soils. For this study, undisturbed soil samples were collected in volumetric cylinders and blocks from a TPI and adjacent area. The areas are located in Caxiuanã National Forest, state of Pará, Brazil. The analyzed physical properties were texture, porosity, macro and microporosity, soil water retention curve, soil saturated hydraulic conductivity, soil permeability to air and aggregate stability. A physical fractionation was performed to verify the behavior of organic matter, which analyzed the distribution of the total and pyrogenic carbon in the different fractions of organic matter. There were difference in the two areas regarding the physical properties as total porosity, macro and microporosity, soil hydraulic conductivity (Ksat), air permeability to soil (Ka), and soil water retention, however it was not possible to see differences in stability aggregates between the two areas. The distribution of organic matter in different soil fractions was different in the two areas, where it was found that in the TPI area, soil carbon was prevalent in the macroaggregates fraction, while the adjacent area had larger amounts in the microaggregates fraction. The values for pyrogenic carbon were higher in the TPI area, showing that the organic matter of TPIs has a different composition which modifies the behavior of physical properties in the soil.

The solid product of pyrolysis, called \"biochar\" (BC) in the context of improving soil properties as part of agronomic or environmental management, also got into focus as a climate mitigation strategy. The researcher investigated the effects of BC on soil attributes, nitrogen (N) use and GHG emissions. In Chapter 1 the origin of BC was commented. In Chapter 2, BC from sugarcane straw was characterized, and its priming on native SC was evaluated with the treatments: (T1) Soil; (T2) BC; (T3) Soil + BC 10 Mg ha-1; (T4) Soil + BC 20 Mg ha-1; and (T5) Soil + BC 50 Mg ha-1. In Chapter 3, it was evaluated the combination of BC, filter cake (F) and vinasse (V), in relation to soil attributes and carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) emissions. The treatments were: (T1) Soil + FC + V; (T2) Soil + FC + V + BC 10 Mg ha-1; (T3) Soil + FC + V + BC 20 Mg ha-1; and (T4) Soil + FC + V + BC 50 Mg ha-1. In Chapter 4, the nitrogen (N) use efficiency was investigated in a pot trial under wheat using NH4[15N]O3 and rates of BC, with the treatments: (T1) Soil, with N, no BC; (T2) Soil, with N, BC 10 Mg ha-1; (T3) Soil, with N, BC 20 Mg ha-1; and (T4) Soil, with N, BC 50 Mg ha-1. BC had C and N contents higher compared to the feedstock. Total K, Mg and P also increased. The lowest CO2 fluxes were for BC, and CO2 from soil and soil + BC did not differ. The highest CO2 - C4 was in the first day, and there were no differences in the CO2 - C3. The BC presents characteristics to improve soil attributes. BC stability is an opportunity to reduce CO2 emissions. In Chapter 3, soil pH, P and base contents increased and Al3+ decreased with BC to sandy soil. Impacts of BC on the CEC were higher in sandy soil. Mineral N decreased with BC. Cumulative CO2 in T1 were higher in sandy and clayey soils than the control. T2 and T3 in sandy soil increased CO2 emissions, but T4 did not differ from T1. BC reduced N2O emissions from sandy and clayey soils relative to T1. BC with FC and V affected pH, CEC, P and base contents. However, those effects were higher in sandy soil. The BC supressed N2O from V and FC. In Chapter 4, BC decreased N2O from N fertilization compared to only N fertilizer. T4 had higher tillering and grain yield. Also, T2 to T4 had higher 100-grain weight and shoot. T3 and T4 had the highest N in grains. The application of BC to soil improves N availability and use efficiency, enhances grain yields and reduces N2O from N fertilization. This study opened encouraging perspectives to the evaluation of sugarcane straw BC to improve soil quality and mitigate GHG emissions. / O produto sólido da pirólise, denominado \"biochar\" (BC) no contexto da melhoria nos atributos do solo como parte do manejo agrícola e ambiental, também tem se destacado na mitigação das mudanças climáticas. O pesquisador investigou os efeitos do BC nos atributos do solo, uso do nitrogênio (N) e emissões de GEE. No Cap. 1 comentou-se a origem do BC. No Cap. 2, caracterizou-se o BC de palha de cana-de-açúcar e avaliou-se o potencial de decomposição do C do solo, com os tratamentos: (T1) Solo; (T2) BC; (T3) Solo + BC 10 Mg ha-1; (T4) Solo + BC 20 Mg ha-1 (T4); e (T5) Solo + BC 50 Mg ha-1. No Cap. 3, avaliou-se a combinação BC, torta de filtro (TF) e vinhaça (V) em atributos do solo e fluxos de dióxido de carbono (CO2), metano (CH4) e óxido nitroso (N2O) nos tratamentos: (T1) Solo + TF + V; (T2) Solo + TF + V + BC 10 Mg ha-1; (T3) Solo + TF + V + BC 20 Mg ha-1; e (T4) Solo + TF + V + BC 50 Mg ha-1. No Cap. 4 investigou-se a eficiência de uso do N num experimento em vasos com trigo usando NH4 [15N]O3 e doses de BC, com os tratamentos: (T1) Solo, com N, sem BC; (T2) Solo, com N, BC 10 Mg ha-1; (T3) Solo, com N, BC 20 Mg ha-1; e (T4) Solo, com N, BC 50 Mg ha-1. Os teores de C e N do BC foram maiores comparado à biomassa. K, Mg e P totais também aumentaram. Os menores fluxos de CO2 foram do BC. O CO2 do solo e solo + BC não diferiram. Observou-se maior CO2 - C4 no primeiro dia de incubação, porém sem diferenças no CO2 - C3. O BC apresenta características para melhorar atributos do solo e reduzir as emissões de CO2. No Cap. 3, pH, P e bases aumentaram e o Al3+ diminuíu com o BC. Os impactos do BC na CTC foram maiores em solo arenoso. O N mineral diminuíu com o BC. O CO2 acumulado no T1 foi maior nos solos arenoso e argiloso comparado ao controle. O T2 e T3 aumentaram o CO2 acumulado do arenoso relativo ao T1, enquanto T4 e T1 não diferiram. O BC reduziu as emissões de N2O pelos solos arenoso e argiloso comparado ao T1. O BC combinado à TF e V afetaram pH, CTC, P e bases do solo arenoso. O BC suprimiu o N2O de solos com V e TF. No Cap. 4, o BC diminuíu as emissões de N2O comparado ao fertilizante N apenas. T4 teve rendimento de grãos superior ao T1. T2 a T4 apresentaram maior peso de 100 grãos e biomassa aérea. T3 e T4 tiveram maior N em grãos. O BC melhora o uso do N, a produção de grãos e reduz o N2O de fertilizante N, abrindo perspectivas para a avaliação do BC de palha de cana-de-açúcar na melhoria da qualidade do solo e mitigar das emissões de GEE.

Dynamic light scattering (DLS) is a method to size submicron particles by measuring their thermal motion (diffusion) in suspensions and emulsions. However, the validity of the Stokes-Einstein equation that relates the diffusion coefficient and the particle size is limited to spherical particles and very low concentrations. Within this thesis, DLS is used for the characterization of suspensions of pyrogenic silica which consists of fractal-like aggregates composed of sintered spherical primary particles. These structural features clearly complicate the understanding of DLS experiments and have been a severe obstacle to employing DLS as routine standard tool for the characterization of pyrogenic silica. The main objective of this thesis is therefore to evaluate the application of DLS in product development and quality assurance of pyrogenic silica industry, what essentially means to identify those structural properties of fractal aggregates which are measurable with DLS and to quantify the method’s sensitivity to changes in these properties. The investigations presented here are split up into four parts, simulations that establish a relation between structural and hydrodynamic properties, experiments validating the simulation results, the characterization of concentrated suspensions and the application-oriented analysis of DLS data for specific industrially relevant measurement tasks. / Die Dynamische Lichtstreuung (DLS) ist eine Messmethode zur Größenbestimmung submikroner Partikel. Dabei wird primär die stochastische Bewegung der Teilchen (Diffusion) in Suspensionen und Emulsionen bewertet. Die Stokes-Einstein Gleichung, die das Verhältnis zwischen gemessenem Diffusionskoeffizienten und Partikelgröße wiedergibt, ist jedoch nur für kugelförmige Teilchen, die in sehr niedriger Konzentration vorliegen, gültig. In der vorliegenden Arbeit wird die dynamische Lichtstreuung zur Charakterisierung von Suspensionen pyrogener Kieselsäure eingesetzt. Diese besteht aus fraktalen Aggregaten, die wiederum aus versinterten aber meist kugelförmigen Primärpartikeln zusammengesetzt sind. Diese strukturellen Eigenschaften erschweren die Anwendbarkeit der DLS bzw. die Interpretation der Messergebnisse und verhinderten bisher den Einsatz der DLS als Routinemethode zur Charakterisierung pyrogener Kieselsäuren. Das Hauptziel dieser Arbeit ist daher eine Bewertung der Möglichkeiten der DLS für die Produktentwicklung und Qualitätssicherung in der Herstellung pyrogener Kieselsäuren. Das bedeutet im Besonderen, dass sowohl die messbaren granulometrischen Eigenschaften als auch die Sensitivität der Methode bei Eigenschaftsänderungen ermittelt werden müssen. Die hier durchgeführten Arbeiten sind in vier Teile gegliedert: Simulationen, die eine Beziehung zwischen strukturellen und hydrodynamischen Eigenschaften herstellen, Experimente zur Validierung der Simulationsergebnisse, die Charakterisierung konzentrierter Suspensionen und die anwendungsorientierte Auswertung von DLS-Daten für spezifische industrierelevante Messaufgaben.

A Terra Preta Antropogênica (TPA) tem essa denominação porque é encontrada em sítios arqueológicos, onde viveram grupos pré-históricos e é considerada um dos solos mais férteis do mundo. Nela é encontrada grande quantidade de material deixado por grupos indígenas como fragmentos cerâmicos, artefatos líticos, e especialmente carvão pirogênico. Estudos realizados com o carvão pirogênico verificaram que ele aumenta a capacidade de trocas catiônicas nesses solos. Por meio de microscopia de fluorencência, foi observada a presença de microrganismos habitando esse carvão, no entanto, não se sabe quais seriam. Devido à falta de informações sobre a diversidade bacteriana nessas estruturas, este trabalho estudou a diversidade bacteriana em amostras de carvão pirogênico de solos TPA coletadas nos sítios Lagoa Balbina (Amazônia Central- Amazonas) e Mina I (Amazônia Oriental - Pará), através de técnicas moleculares independentes de cultivo. O estudo visou também comparar essa diversidade com a encontrada no solo de onde carvão foi isolado. As estruturas de carvão foram separadas fisicamente dos solos e seu DNA genômico total extraído e usado como molde em reação de PCR utilizando oligonucleotídeos do gene 16S rRNA para o Domínio Bacteria. O produto da PCR foi clonado em vetor e os clones foram sequenciados e comparados com o banco de dados de 16S rRNA do RDPX. Com a construção das bibliotecas de clones do gene 16S rRNA a partir das amostras de carvão pirogênico observou-se que existe maior número de bactérias desconhecidas no carvão pirogênico do que no solo onde ele foi isolado. Acidobacteria foi o filo predominante nas bibliotecas de carvão pirogênico das duas localidades de estudo, assim como na biblioteca do solo do sítio Mina I. Já na biblioteca do solo do sítio Lagoa Balbina houve predominância do filo Firmicutes. Por meio do método de rarefação foi possível constatar uma menor riqueza de UTOs nas comunidades bacterianas presentes nas estruturas de carvão pirogênico quando comparado à riqueza de UTOs das comunidades bacterianas cujo habitat é o solo. Mas quando se compara a riqueza de UTOs entre as estruturas de carvão isoladas das duas localidades, observa-se que a riqueza é maior no sítio Mina I. Os valores obtidos com os índices de diversidade revelaram menor diversidade de UTOs nas bibliotecas obtidas para o carvão pirogênico das duas regiões estudadas se comparado dos valores para as bibliotecas obtidas do solo da mesma região. Os valores obtidos com os métodos não paramétricos revelaram maior riqueza de UTOs para as bibliotecas do carvão do sítio Mina I e solo TPA do sítio Balbina. A análise da PCA revelou que as bibliotecas do sítio Balbina mostraram-se altamente similares. Em adição, a análise com S-Libshuff, verificou que todas as bibliotecas comparadas são significativamente diferentes quanto à composição das comunidades bacterianas. O carvão pirogênico não é uma estrutura inerte, pois é capaz de ser habitado por diferentes bactérias e a sua estrutura da comunidade bacteriana é diferente daquela de onde ele foi segregado / Anthropogenic Dark Earth (ADE) has this denomination because it is found at archeological sites, where prehistoric groups lived, and it is considered one of the most fertile soils of the world. In this soil a great amount of material left by indigenous groups was found as ceramic fragments, lithic workmanships, and especially pyrogenic black carbon. Studies accomplished with the pyrogenic black carbon verified that it increases the capacity of cationic changes in soils. Through fluorescence microscopy, the presence of microorganisms was observed inhabiting that black carbon, however, this community is still unknown,due to the lack of information about the bacterial diversity in those structures.This work studied the bacterial diversity in samples of pyrogenic black carbon of ADE soils, collected at the sites Lagoa Balbina (Central Amazon) and Mina I (Oriental Amazon), through molecular techniques independent of cultivation. The study also sought to compare that diversity with the one of the soil where black carbon was isolated. The structures of black carbon were separate physically from the soils and total genomic DNA was extracted and used as template in a PCR reaction, using primers of the 16S rRNA gene for the Bacteria Domain. The PCR product was used for construction of clone libraries and the clones were sequenced and compared with the 16S rRNA of RDPX database. The 16S rRNA gene clone libraries from the samples of pyrogenic black carbon, it shown that is a larger number of unknown bacteria in the black carbon than in the soil where it was isolated. Acidobacteria was the predominant phylum in the pyrogenic black carbon libraries from the both studied places, as well as in the soil library from Mina I site. However in the library Lagoa Balbina site there was predominance of the phylum Firmicutes. Through the rarefaction method it was possible to verify a smaller richness of OTUs in the bacterial communities presents in the pyrogenic black carbon structures when compared to the OTUs richness of the bacterial soil communities.But, when the OTUs richness is compared among the isolated structures of pyrogenic black carbon of the two places, it is observed that the richness is higher in the Mina I site. The values from diversity indexes revealed smaller diversity of OTUs in the pyrogenic black carbon libraries when compared with the soil libraries for the two studied areas. The obtained values with the nonparametric methods revealed larger OTUs richness in the black carbon library of Mina I site and in the ADE soil library of the Balbina site. The PCA analysis showed that the libraries of the site Balbina site were highly similar. In addition, the analysis with S-Libshuff verified that all of the compared libraries were significantly different in bacterial communities composition. The pyrogenic black carbon is not an inert structure, once it is capable of being inhabited by different bacteria, and its bacterial community structure is different from that one where is was segregated

Les sols stockent trois fois plus de carbone que l'atmosphère sous la forme d'un mélange de molécules, la matière organique des sols (MOS). Certaines de ces molécules sont présentes dans le sol depuis des centaines voire des milliers d'années. Trois mécanismes de protection sont utilisés pour expliquer cette persistance à long terme des matières organiques dans les sols : (i) la récalcitrance chimique, (ii) la protection physique dans les agrégats et (iii) la protection physicochimique par adsorption sur les surfaces minérales. Le but de ce projet de thèse est d’améliorer la compréhension de ces processus de protection et de leur importance relative. Mon projet de thèse utilise des échantillons permettant l'accès au carbone persistant : les jachères nues de longue durée (5 sites en Europe). Il s'agit de parcelles maintenues vierges de toute végétation dans lesquelles, au fur et à mesure de la biodégradation, la quantité totale de carbone diminue, entraînant un enrichissement relatif en carbone persistant. La première étude expérimentale de ce travail de thèse vise à tester l'efficacité des méthodes d'oxydation chimique. Les deux réactifs les plus couramment utilisés -l'hypochlorite de sodium NaOCl et le peroxyde d'hydrogène H2O2- ont été testés sur des échantillons de la plus longue jachère nue (Versailles). Il est conclu que les méthodes d'oxydation chimique n'arrivent pas à isoler efficacement un réservoir de carbone persistant à l'échelle du siècle.En termes de mécanismes de persistance, les résultats obtenus montrent que la récalcitrance chimique n'est pas le principal mécanisme de protection. En effet, sur la durée de la jachère nue, la composition chimique de la MOS, caractérisée par spectroscopie NEXAFS, ne présente que peu de changements. Un enrichissement en composés présentant des groupements acides carboxyliques est détecté pour tous les sites testés. Une étude poussée de la persistance spécifique du carbone pyrogénique des sols a aussi été réalisée, ces composés sont actuellement considérés cinq fois plus persistants que le carbone total. Les résultats montrent que le carbone pyrogénique est moins persistant que prévu. En effet, le temps de résidence moyen du carbone pyrogénique obtenu par la méthode BPCA (116 ans) est seulement 1,6 fois supérieur à celui de la MOS (73 ans). L'étude du contrôle minéralogique de la persistance des MOS montre que les argiles contenant du potassium (illite) protègent moins de carbone que les argiles smectitiques. Le rapport C/N décroit avec le temps dans toutes les fractions argiles, ce qui prouve que les composés riches en azote sont préférentiellement préservés. Enfin, la présence de microagrégats dans la fraction grossière des argiles implique la coexistence de deux mécanismes de protection : la protection physique et la protection par adsorption sur les minéraux. / Soils store three times more carbon than the atmosphere, under the form of a complex mixture of molecules called soil organic matter (SOM). Some of these molecules have been standing in the soil for hundreds to thousands of years. Three main mechanisms are invoked to explain this long term carbon persistence in soils, (i) chemical recalcitrance, (ii) physical protection in aggregates and (iii) protection by adsorption on mineral surfaces. One of the major challenges in SOM science is to better understand the relative importance of each mechanism, that is the aim of this PhD project. Here, we use samples from by long term bare fallows (5 sites across Europe). These experimental plots have been kept free of vegetation by manual or chemical weeding for several decades and have been regularly sampled and stored. As the duration of the bare fallow increases, biodegradation occurs and samples get enriched in persistent carbon.First experiments consisted in testing the efficiency of chemical oxidations (two reagent were tested, sodium hypochlorite –NaOCl- and hydrogen peroxide –H2O2) on the longest bare fallow. We concluded that oxidation methods were not able to efficiently isolate a pool of persistent carbon at the centennial timescale. In terms of mechanisms of persistence, the obtained results show that chemical recalcitrance does not seem to be the major mechanism. Indeed, over the duration of the bare fallow, the chemical composition of SOM, as seen by synchrotron based NEXAFS spectroscopy, shows little changes. There is a consistent increase in carboxylics for all sites (12% increase on average) though it is significant for 2 out of the 4 selected sites. We also studied the particular persistence of soil pyrogenic carbon, which is thought to be at least five times more persistent than bulk SOM. Results show that pyrogenic carbon lacks long term persistence. Indeed the BPCA-estimated mean residence time of pyrogenic carbon (116 years) is on average 1.6 times longer than MRT for bulk SOM (73 years). Finally, the study of mineralogical control of the persistence of SOC showed that clay minerals containing potassium (illite) seemed to protect less carbon. As seen by NEXAFS-STXM, more mineral surfaces with very little SOM appear with the duration of bare fallow. C:N ratio decreased in all clay fractions, suggesting a preferential persistence of N-rich compounds. Presence of microaggregates in the coarser clay fraction led to the coexistence of two protection mechanisms: adsorption and physical protection.

No description available.

Ce travail de thèse a porté sur le développement de revêtements organiques/inorganiques photopolymérisables superhydrophobes à partir de procédés d’élaboration simples associés à des produits commerciaux largement diffusés. Pour cela, des revêtements à matrice polyuréthane acrylate (PUA), intrinsèquement hydrophiles, incluant différents composés à base de silicium ont été élaborés par enduction ou pulvérisation. L’objectif a été d’apporter en surface des revêtements une structuration multi-échelle et une chimie à caractère hydrophobe nécessaires pour atteindre la superhydrophobie, c’est-à-dire un angle de contact avec l’eau supérieur à 150° et une hystérésis de mouillage inférieure à 10°. L’introduction de molécules de polysilsesquioxane polyédrique (POSS), présentant un ligand acrylate et sept ligands isobutyle, a apporté une nanostructuration et un comportement hydrophobe aux revêtements PUA à des concentrations très faibles (≤ 1% en masse.). Cependant, la rugosité apportée se révèle trop faible et cette stratégie ne peut aboutir à la superhydrophobie des revêtements. L’introduction de particules de silice pyrogénée, modifiées en surface par des chaînes polydiméthylsiloxane, a permis d’établir une structuration multi-échelle et une chimie à caractère hydrophobe à la surface des revêtements PUA, leur conférant ainsi la superhydrophobie. De plus, le procédé d’élaboration a joué un rôle majeur sur les modifications physico-chimiques de surface des revêtements : la superhydrophobie est obtenue à une concentration relativement élevée de 30 et 60% en masse de silice pyrogénée respectivement par pulvérisation et enduction. Afin de diminuer ces concentrations, la combinaison des deux stratégies précédentes, c’est-à-dire l’introduction simultanée de POSS et de silice pyrogénée, a été considérée. Ceci a permis d’exacerber le caractère hydrophobe des revêtements tout en préservant la rugosité établie par la silice pyrogénée. Cette approche a conduit à la diminution de la concentration de silice nécessaire pour obtenir la superhydrophobie dans le cas des revêtements élaborés par pulvérisation. / This work deals with the development of organic/inorganic superhydrophobic UV-curable coatings manufactured through simple processes and from commercially available products. To achieve this goal, a hydrophilic polyurethane acrylate matrix (PUA) was used, in which several silicon-based compounds were introduced. The coatings were deposited using either bar- or spray-coating. The main objective was to structure the surface thanks to a multiscale roughness, while bringing a hydrophobic character, two properties needed to obtain a superhydrophobic coating (defined by a water contact angle superior to 150° and a water contact angle hysteresis inferior to 10°). The introduction of polyhedral oligomeric silsesquioxane molecules (POSS), presenting one acrylate and seven isobutyl ligands, brought a nanostructuration and a hydrophobic behavior to PUA coatings, even at low concentrations (≤ 1%wt.). However, the roughness obtained was not sufficient to bring the superhydrophobicity to the coatings.The introduction of fumed silica particles, functionalized by PDMS chains, established multiscale roughness and hydrophobic behavior at the surface, leading to superhydrophobic coatings. Moreover, the process had a high influence on physico-chemical modifications at the coatings’surface: superhydrophobicity is obtained for a relatively high concentration of fumed silica, 30%wt. and 60%wt. respectively for spray and bar-coating. In order to decrease these concentrations, we tried the combination of the two previous strategies: introduction of POSS molecules and fumed silica particles. This path raised the hydrophobic behavior of the coatings while keeping intact the roughness brought by fumed silica particles. This approach allowed to decrease the silica concentration needed to obtain superhydrophobicity for spray-coated coatings.