Projected climate change may alter soil carbon dioxide (CO2) efflux from terrestrial ecosystems; yet disentangling effect of plant species from climate drivers remains a key challenge. We explored the effects of the dominant plant species, warming, and precipitation distribution on soil CO2 efflux, its underlying components, and mycorrhizal abundance in southern post oak savannah. Post oak savannah in the south-central US are dominated by three contrasting plant functional types: Schizachyrium scoparium (Michx.) Nash. (little bluestem) a C4 grass, Quercus stellata Wangenh.(post oak)a C3 deciduous tree, and Juniperus virginiana L. (eastern redcedar) a C3 evergreen tree. Monocultures and tree-grass plots were warmed using infrared heaters and precipitation events were manipulated to intensify summer drought and augment cool season precipitation. Soil CO2 efflux, the root, bacterial and hyphal components of CO2 efflux, and mycorrhizal abundance were measured. Soil CO2 efflux varied with seasonal changes in soil VWC and temperature, with higher soil CO2 efflux rates in the spring and lower rates in both the cooler winter season and at the end of the dry summer period. There was no relationship between root length density or root mass density and soil CO2 efflux during the short term precipitation distribution campaigns. Partitioning of root, fungal, and bacterial component contribution to soil CO2 efflux indicated a substantial contribution of bacterial respiration to soil CO2 efflux within this system. There was no relationship between microbial biomass [microbial dissolved organic carbon (DOC)] and soil CO2 efflux, or root length (or mass) density and microbial biomass. This suggests that species and climatic effects on root and microbial activity drive soil CO2 efflux. As plant species within this system differed in their association with mycorrhizal fungi and had a strong effect on the individual components of soil CO2 efflux, we conclude that shifts in vegetation cover and growth and the response of vegetation to long term warming and potential future extreme precipitation events (e.g., large preciptation events, prolonged drought) will be major drivers of changes in soil carbon (C) dynamics and associated soil CO2 efflux.

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Research focusing on the political economy of Mississippian mound centers in the middle Savannah River valley has prompted a reevaluation of current interpretations regarding societal complexity. I conclude the clearest expression of classic Mississippian riverine-adaptation is evident at centers immediately below the Fall Line with their political ties to chiefdom centers in the Piedmont, and especially Etowah. By contrast, those centers on the interior Coastal Plain were politically autonomous with minimal signatures in social ranking. The scale of appropriated labor and resulting level of surplus production, necessitated by upland settlement on the Aiken Plateau, fostered social contradictions making communally-oriented and decentralized societies more sustainable than hierarchical forms.

As the container traffic at the Port of Savannah is expected to increase, its impacts need to be evaluated to address major concerns regarding the roadway network surrounding the port and the overall operations of the port. A federation of two disparate simulators was created in order to model the impacts of increased container traffic. The Port of Savannah was modeled using Rockwell Arena© and the surrounding roadway network was modeled using PTV VISSIM©. These two simulators operated concurrently and continually provided feedback with one another. The challenges that arose from this combination were largely due to the time structure of the models. Arena© is a discrete event simulator and VISSIM© is a continuous traffic simulator. A basic model, where these two pieces of software could pass information between one another, was initially created as a test bed for methods required to federate the two models. These basic concepts were then applied to a comprehensive model of the Port of Savannah and the surrounding area. This federated modeling approach for the Port of Savannah allowed the analysis to reflect the interaction of behaviors unique to the port and local roadway network. For instance, the federated model successfully captured how delays at the Port of Savannah increased as a result of increased congestion in the surrounding roadway network. It is anticipated that this prototypal model will be a base for future research into the area of federating disparate transportation simulators, as well as aid in the further exploration of a transportation run-time interface.

129I is of major concern because of its biophilic nature, excessive inventory, long half-life (~16 million yrs), and high mobility in the natural environment that depends on its chemical speciation. Iodide (I-) has the highest mobility than iodate (IO3-) and is the predominant species in the terrestrial environment due to prevailing pH and Eh conditions. In order to transform I- to less mobile organo-iodine (OI), strong oxidants are necessary to activate the first electron transfer step from I- to reactive intermediates. The aim of this study was to determine the influence of naturally occurring aerobic bacteria isolated from an 129I contaminated aquifer (F-area of the Savannah River Site, SC) on I- oxidation and OI formation. It was demonstrated that 3 of 136 strains accumulated I- (0.2~2%) in the presence of H2O2, when incubated in the presence of an environmentally relevant concentration of I- (0.1 microM). The accumulation was likely through electrophilic substitution resulting in the iodination of cellular constituents. The results indicated that culturable I--accumulating bacteria are not directly responsible for the high fraction of oxidized iodine species (IO3- and OI, >50% of total I) present in the SRS F-area. Several bacterial strains were found to be capable of stimulating I- oxidation through excretion of oxidants and enzymes. Organic acids in spent liquid medium from 27 of 84 aerobic bacterial cultures enhanced H2O2-dependent I- oxidation 2-10 fold. Organic acids enhanced I- oxidation by (1) lowering the pH of the spent medium and (2) reacting with H2O2 to form peroxy carboxylic acids, which are strong oxidizing agents. In the absence of H2O2, spent medium from 44 of 84 bacteria cultures showed I- oxidizing capacities. One I- oxidizing bacterium was studied to characterize its extracellular I- oxidizing component(s). The I- oxidizing capability from the spent medium was inactive by treatments with heat and H2O2 and absent under anaerobic conditions. Conversely, NADH, NADPH and FMN additions stimulated I- oxidation in the spend medium. These results indicate an oxidase(s) catalyzed I- oxidation. Understanding the bacterial activities involved with I- oxidation and OI formation is expected to help reduce 129I mobility in water-soil systems.

Thesis (M. S.)--Civil and Environmental Engineering, Georgia Institute of Technology, 2009. / Committee Chair: Hunter, Michael; Committee Member: Laval, Jorge; Committee Member: Rodgers, Michael. Part of the SMARTech Electronic Thesis and Dissertation Collection.

Submitted by Náthali Maria Machado de Lima (nathalimachadolima@gmail.com) on 2018-09-06T17:50:08Z No. of bitstreams: 1 Nathali Maria Machado de Lima - Copia (2)-pages-1-3,5-101-merged.pdf: 3526956 bytes, checksum: 5f5c8cc704c14910caa7d290299d4c24 (MD5) / Approved for entry into archive by Elza Mitiko Sato null (elzasato@ibilce.unesp.br) on 2018-09-06T18:17:51Z (GMT) No. of bitstreams: 1 lima_nmm_me_sjrp.pdf: 3526956 bytes, checksum: 5f5c8cc704c14910caa7d290299d4c24 (MD5) / Made available in DSpace on 2018-09-06T18:17:51Z (GMT). No. of bitstreams: 1 lima_nmm_me_sjrp.pdf: 3526956 bytes, checksum: 5f5c8cc704c14910caa7d290299d4c24 (MD5) Previous issue date: 2016-10-31 / Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) / Crostas biológicas consistem de uma comunidade composta por cianobactérias, algas verdes, microfungos, bactérias, líquens e musgos. Estas ocorrem em uma variedade de solos e regiões climáticas ao redor do globo, exercendo funções importantes como a de conferir estabilidade e proteger o solo contra forças erosivas, acumular e aumentar o tempo de residência da água no solo, além de, favorecer a germinação e permitir a fixação de nitrogênio e carbono. Em crostas biológicas de regiões quentes e temperadas há o predomínio de líquens e cianobactérias, sendo que as cianobactérias são consideradas os primeiros organismos a estruturarem a crosta, sendo seguidas por outros grupos de organismos. A partir da investigação de cianobactérias em crostas biológicas, muitos novos gêneros e espécies têm sido descritos, o que também enfatiza a grande necessidade da investigação sobre tais comunidades. Devido às condições propícias do ambiente, em termos de exposição do solo e fitofisionomia, o bioma Cerrado (Savana) foi escolhido para ser o local de estudo de assembleias de cianobactérias de crostas. Além disso, devido a estudos prévios que relatam o potencial de produção de enzimas celulolíticas e hemicelulolíticas por cianobactérias heterocitadas e a presença comum deste tipo de organismos em crostas biológicas, também foram feitas análises para avaliar a produção de tais substâncias. Desse modo, os estudos objetivaram contribuir com conhecimento da biodiversidade de cianobactérias de crostas biológicas de solo e avaliar a capacidade de produção enzimática das cianobactérias encontradas em crostas biológicas de solo. Para isto, amostras de crostas foram coletadas nos Parques Nacionais da Serra da Canastra (MG) e da Serra do Cipó (MG), no Parque Estadual Furnas do Bom Jesus (SP) e na região de Caldas Novas (GO). As cianobactérias encontradas nas amostras foram estudadas morfologicamente a partir do material da natureza e também isoladas em cultivos artificiais, visando além do estudo morfológico, as análises moleculares e enzimáticas. No total, foram estudados 28 morfotipos, provenientes de 31 populações, dos quais 12 foram identificados em nível específico (destes, três ainda exigem confirmação de identidade = cf) e 16 foram identificados apenas em nível genérico. Dezenove populações foram analisadas também em nível molecular por meio do sequenciamento parcial do gene 16S rRNA, e completo da Região Espaçadora Interna Transcrita 16S-23S (ITS). Seis populações foram também investigadas quanto a produção de enzimas. Entre os gêneros encontrados, muitos são comuns em assembleias de cianobactérias de crostas biológicas em outras regiões do mundo, entretanto, algumas identificações em nível de espécie não foram possíveis por diferenças importantes com os táxons já descritos em literatura. As análises moleculares enfatizaram e contribuíram com a problemática polifilia de gêneros como Leptolyngbya, Nostoc e Calothrix, reafirmaram a existência de um novo gênero próximo a Wilmottia e Microcoleus e apresentaram um novo grupo composto até o momento por uma espécie representada por duas populações. Este grupo revelou sequências moleculares que se aproximam de Brasilonema, entretanto os indivíduos apresentam ramificações verdadeiras e, portanto, investigações mais aprofundadas são necessárias para definição da identidade das populações. Dessa forma, as análises morfológicas e moleculares demonstraram a grande diversidade não acessada em localidades e habitats pobremente investigados e enfatizaram a contribuição deste trabalho ao enfocar pela primeira vez a flora de cianobactérias de solo de Cerrado. As análises de atividade enzimática revelaram que não houve produção de tais proteínas, tendo como possíveis explicações a ausência de habilidade para produção deste tipo de enzimas por parte das cepas, ou a ineficiência do método utilizado. De qualquer forma os resultados enfatizaram a necessidade de estudo nesta área, principalmente pela dificuldade no encontro de cepas produtoras e o desconhecimento sobre quais poderiam ser os fatores a estarem influenciando certas cepas a ativarem ou selecionarem diferentemente seus metabolismos. Em linhas gerais, os resultados do presente estudo apresentam, pela primeira vez, a composição das cianobactérias de crostas biológicas do território brasileiro e indicam uma flora diversificada e, em grande parte, desconhecida. Esses resultados fornecem subsídios e abrem caminho para outras pesquisas dentro do campo do conhecimento da biodiversidade presente em crostas biológicas. Complementarmente, estes trabalhos compõem a base para estudos sobre a ecologia de ambientes mais restritivos (como a caatinga ou o próprio Cerrado), permitindo abordagens como sucessão ecológica, produtividade primária, fluxos de nutrientes e dinâmicas de solo. / Biological soil crusts (BSCs) are communities potentially composed of cyanobacteria, green algae, micro fungi, bacteria, lichens and mosses. They occur in a variety of soils and climatic regions around the world, playing important roles as giving soil stability protecting against erosive forces, accumulating and increasing residence time for water in soil, besides promoting germination and performing nitrogen and carbon fixation. Biological soil crusts from hot deserts are frequently composed of cyanobacteria and lichens, and the cyanobacteria are considered the first colonizers in structuring the crust, being followed by other groups of organisms. A lot of new genera and species have been described based on crusts investigations and this fact also emphasizes the necessity of works on those communities. Due to environmental conditions, as soil exposition and phytophysiognomy, the biome Cerrado (Savannah) was chosen to be the place for studies on cyanobacterial assemblages of biological soil crusts. Besides, due to previous studies that indicate the production capability of celulolitic and hemicelulolitic enzymes by heterocytous cyanobacteria and the common presence of this kind of cyanobacteria in biological soil crusts, analyses of such production were also conducted. In this way, the studies aimed to contribute with knowledge about cyanobacterial biodiversity in biocrusts and evaluate the bioprospection capability of cyanobacterial from these biocrusts. Therefore, BSCs were sampled at the National Parks of Serra da Canastra (Minas Gerais State) and Serra do Cipó (Minas Gerais State), at the State Park of Furnas do Bom Jesus (São Paulo State) and in the region of the municipality of Caldas Novas (Goiás State). The cyanobacteria found in the samples had their morphology analyzed from the natural and cultivated conditions. Besides, molecular and enzymatic analysis were carried out. The results summarized 28 morphotypes from 31 populations, which 12 were identified at specie level (three of them need identity confirmation = cf) and 16 were identified only at genus level. Nineteen populations also were studied with molecular methods, through partial sequencing of 16S rRNA gene and complete sequencing of the Internal Transcribed Space Region (16S-23S ITS). In addition, six populations also were explored as possible enzymatic producers. Among the found genera, many are cyanobacteria frequently found in BSCs distributed around the world, however, some identifications at specific level were not possible due to considerable divergences in comparison with described taxa. The molecular analysis reaffirmed and emphasized the polyphyletic nature of Leptolyngbya, Nostoc and Calothrix, reinforced the existence of a new genus close related with Wilmottia and Microcoleus and presented a new group composed, until now, of one species represented by two populations. This group showed molecular sequences related with Brasilonema, however, the specimens are true branched, what requires more detailed studies to confirm the identification of the populations. In this way, the morphological and molecular analyses showed the wide diversity whose has not been accessed in poorly investigated places and habitats and reinforced the contribution of this work in focusing the cyanobacterial flora of crusts of Brazilian savannah area for the first time. The enzymatic activity analysis revealed that the strains studied did not produce celulolitic or hemicelulolitic compounds, having as possible explanations the absence of the production ability or the inefficiency of the utilized method. Either way, the results emphasized the necessity of studies in this area, mainly because of the difficulty in find producer strains and the lack of knowledge about which could be the factors influencing the strains in activate or select differently their metabolism. In general, our results presented for the first time the cyanobacterial composition for BSCs from Brazil and indicated a diverse, and sometimes, unknown flora. These results provided foundation and opened doors to investigations inside the biodiversity knowledge with biological soil crusts. Complementary, these works compound the basis for investigations in the ecology of extreme environments (as Caatinga and Cerrado), permiting studies about successional ecology, primary productivity, flow of nutrients and soil dynamics. / 2014/06245-8