Dissertations / Theses on the topic 'Green and Ampt'
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Oliveira, Alan ébano de. "Modelagem da infiltração de água no solo com modelo Green-Ampt." Universidade Federal de Santa Maria, 2015. http://repositorio.ufsm.br/handle/1/5611.
Full textA modelagem da infiltração de água por meio de modelos de base física, incluindo a variabilidade vertical do solo e da intensidade de chuva ao longo de um evento, permite uma melhor estimativa do escoamento e da infiltração medidos em ambiente não controlado. Neste estudo, foi avaliada a hipótese que, para condições de chuva natural em perfil de solo estratificado e escala de parcela, a presunção de fluxo tipo pistão antes e depois do empoçamento permite simular satisfatoriamente a infiltração e o escoamento superficial. A infiltração e o escoamento superficial foram simulados para dez eventos de precipitação, em parcelas de solo com perfil heterogêneo e usando o modelo Green-Ampt (fluxo tipo pistão). A calibração do modelo foi feita com a modificação de apenas dois parâmetros, o grau de saturação final e o conteúdo de água inicial, os quais implicam modificações nos demais parâmetros do modelo, preservando as relações físicas. Para avaliação do desempenho do modelo, índices estatísticos foram calculados, comparando o escoamento acumulado simulado (Es) com o escoamento acumulado medido (Eo). Para sete dos dez eventos de chuva, o ajuste somente do grau de saturação foi suficiente para que houvesse bom desempenho do modelo. Para os outros três eventos foi necessário ajustar o grau de saturação e o conteúdo inicial de água do solo. Embora algumas simulações não tenham reproduzido o incremento gradual no escoamento medido, o modelo permitiu estimar satisfatoriamente o escoamento em todos os eventos, principalmente nos mais longos.
Sande, Leif Andrew. "Experimental Studies on Infiltration/Soil-Water Movement Processes and Green-AMPT Modeling." Thesis, North Dakota State University, 2011. https://hdl.handle.net/10365/29329.
Full textNational Science Foundation (Grant No. EAR-0907588)
Sabeh, Darwiche. "Adapting the Green and Ampt model to account for air compression and counterflow." [Tampa, Fla.] : University of South Florida, 2004. http://purl.fcla.edu/fcla/etd/SFE0000493.
Full textCecílio, Roberto Avelino. "Modelagem da infiltração da água no solo fundamentada na equação de Green-Ampt-Mein-Larson." Universidade Federal de Viçosa, 2005. http://www.locus.ufv.br/handle/123456789/9761.
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior
O conhecimento do processo de infiltração da água no solo é de extrema importância para diversas áreas da engenharia de conservação de água e solo. O modelo de Green-Ampt-Mein-Larson (GAML) é um dos mais utilizados para a simular a infiltração por ser relativamente simples e por vir apresentando bons resultados na estimativa do processo. Todavia, a difícil determinação dos parâmetros de entrada de GAML e o fato destes parâmetros não representarem efetivamente as condições reais de ocorrência da infiltração ainda dificultam sua aplicação. O presente trabalho teve o objetivo de melhorar a estimativa da infiltração de água no solo, considerando, para tal, duas vertentes distintas e independentes: uma baseada em uma análise físico- matemática mais detalhada do processo de infiltração e do deslocamento da frente de umedecimento pelo perfil do solo; e outra baseada em simples adequações dos parâmetros de entrada de GAML. Desenvolveu-se um novo modelo para a estimativa da infiltração de água no solo (GAML-c), fundamentado no GAML, baseando-se numa descrição mais aproximada da geometria e do deslocamento da frente de umedecimento. O GAML-c realiza uma discretização do teor de água para o qual o solo é umedecido quando da ocorrência do processo de infiltração, simulando o deslocamento simultâneo de diversas sub-frentes de umedecimento pelo perfil do solo. Paralelamente, propôs-se, também, a adequação dos parâmetros de entrada de GAML, a saber: substituir o teor de água do solo na saturação (θ s ) pelo teor de água na zona de transmissão (θ w ); substituir a condutividade hidráulica do solo saturado (K 0 ) pela taxa de infiltração estável (Tie); e calcular o potencial matricial na frente de umedecimento (ψ f ) por meio de uma equação baseada na condutividade hidráulica relativa aos teores de água inicial do solo (θ i ) e da zona de transmissão, e dos parâmetros pressão de borbulhamento (ψ b ) e índice de distribuição do tamanho de poros (λ), oriundos do ajuste da curva de retenção de água no solo feito pelo o modelo de Brooks & Corey. O conjunto de adequações propostas foi denominado GAML-t, não tendo qualquer relação com o procedimento GAML-c. Testes experimentais foram realizados em laboratório a fim de determinar a infiltração em três diferentes classes de solo: Argissolo Vermelho (PV), Latossolo Vermelho (LV) e Latossolo Vermelho-Amarelo (LVA). Avaliou-se o desempenho de GAML-c e de GAML-t, comparando-os com o modelo de GAML aplicado em sua forma original e também adequado segundo cinco diferentes propostas. O GAML-c foi avaliado considerando quatro diferentes cenários, relativos à consideração dos parâmetros de entrada K 0 e θ w : K 0 igual à Tie e θ w experimental (TW); K 0 determinado pelo permeâmetro de carga constante e θ w experimental (KW); K 0 igual à Tie e θ w igual a θ s (TS); e K 0 determinado pelo permeâmetro de carga constante e θ w igual à θ s (KS). Verificou-se que o GAML-c aplicado utilizando-se os parâmetros da simulação TW foi capaz de estimar o perfil de umidade do solo, provendo estimativas de infiltração aceitáveis em todos os tipos de solo estudados; mas ainda necessitando de ajustes. O GAML-t foi capaz de prover boas estimativas da infiltração de água em todos os solos estudados, sendo recomendado para aplicação na estimativa de infiltração.
Knowledge of water infiltration process is extremely important to many areas of Soil and Water Conservation Engineering. Gren-Ampt-Mein-Larson infiltration model (GAML) is one of the models that are most used to predict infiltration process because of its relative simplicity and encouraging results. However, the major obstacle in using GAML model is not just due to the difficulties in estimating it's parameters, but also due to the fact these parameters do not represent field infiltration conditions. This study have had the objective of give better alternatives in predicting infiltration process, considering two different ways: one based on a most detailed physical-mathematical analysis of the infiltration process and of the wetting front movement through the soil profile; and other one based on simple modifications of GAML model parameters. It was developed a new model to simulate infiltration process (GAML-c) that is based on GAML model, and that provides a better description of the wetting front geometry and displacement through the soil profile. GAML-c model simulates the simultaneous displacement of many sub-wetting fronts through the soil profile. It was also proposed the following modifications in GAML model parameters: replace the saturation moisture content parameter (θ s ) with the "filed saturation" moisture content (θ w ); replace the saturated hydraulic conductivity parameter (K 0 ) with the infiltration rate after long time of wetting (Tie); and calculate wetting front suction head (ψ f ) by the use of an equation that makes use of relative hydraulic conductivity in the initial soil moisture (θ i ) and "field saturation" moisture, and also of Brooks & Corey bubbling pressure and pore-size distribution index parameters. These three modifications were called GAML-t and do not have any relation to GAML-c model. Experimental infiltration tests were conduced at laboratory using three different soil types: Red Ultisol (PV), Red Oxisol (LV) and Red-Yellow Oxisol (LVA). The performances of GAML-c model and GAML-t modifications were evaluated and compared to the performances of GAML model applied with its original and modified parameters. Five different ways of modify GAML parameters were used. GAML-c was evaluated using four different scenarios: considering K 0 equals to Tie and the maximum soil moisture equals to θ w (TW); considering K 0 value determined by constant-head permeameter method and the maximum soil moisture equals to θ w (KW); considering K 0 equals to Tie and the maximum soil moisture equals to θ s (TS); and considering K 0 value determined by constant-head permeameter method and the maximum soil moisture equals to θ s (KS). It was verified that GAML-c model applied using TW scenario was able to simulate soil water profile, giving acceptable prediction of infiltration to the three soil types. However, GAML-c still needs better development. GAML-t was able to give very good predictions of infiltration to the three soil types, being strongly suggested to simulate infiltration process.
Tese importada do Alexandria
Cecílio, Roberto Avelino. "Aplicação da equação de Green-Ampt na modelagem da infiltração de água em Latossolo Vermelho-Amarelo estratificado." Universidade Federal de Viçosa, 2002. http://www.locus.ufv.br/handle/123456789/9439.
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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior
A infiltração de água no solo é um dos principais fenômenos componentes do ciclo hidrológico, pois é um dos fatores que determinam a disponibilização de água para as culturas, a recarga dos aqüíferos subterrâneos, a ocorrência e magnitude do escoamento superficial e o manejo do solo e da água. O modelo de Green-Ampt é um dos mais utilizados na previsão da infiltração por se basear em aspectos físicos do processo, entretanto diversos autores alertam para a necessidade de adequação dos parâmetros de entrada deste modelo para as condições de campo. Como este modelo foi desenvolvido para solos homogêneos faz-se necessário a realização de estudos deste em solos estratificados, principalmente para solos típicos de regiões de clima tropical. Neste trabalho, procurou-se avaliar o modelo de Green-Ampt, assim como as diversas proposições de correção dos seus parâmetros de entrada (umidade de saturação, θ s ; condutividade hidráulica do solo saturado, K 0 ; e, potencial matricial na frente de umedecimento, ψ), aplicado a um típico solo brasileiro sob condições de estratificação de sua textura, o Latossolo Vermelho-Amarelo. Foram conduzidos dois experimentos, um utilizando colunas e outro uma caixa de solo, dentro dos quais compactou-se material de solo pertencente a cada um dos três horizontes do Latossolo Vermelho- Amarelo (A, B e C). Determinou-se a infiltração acumulada (I), taxa de infiltração (Ti), bem como as características físicas do perfil necessárias para a aplicação do modelo de Green-Ampt. Verificou-se que o valor de umidade de saturação de campo (θ w ) que melhor simulou os valores medidos de infiltração quando não se considera θ w variável com a textura do solo variou entre 0,81 θ s (caixa de solo) e 0,86 θ s (colunas de solos). Quando se considera, para a caixa de solo, θ w variável com a textura, os melhores valores foram de 0,79 θ s para o material de solo de textura argilosa (horizontes A e B) e 0,86 θ s para o material de solo de textura franca (horizonte C). Utilizando-se estes valores nas simulações de Ti, I e profundidade da frente de umedecimento, percebeu-se que a textura do solo exerce grande influência no valor de θ w , pois todas as simulações foram melhores quando se considerou a variação deste parâmetro de acordo com a granulometria do material de solo. Utilizando-se, nas simulações, combinações entre seis metodologias para o cálculo de ψ e três para a determinação da condutividade hidráulica, percebeu-se que três diferentes combinações simularam bem a infiltração ocorrida nas colunas (condição de baixa umidade inicial) e que quatro diferentes combinações simularam bem o processo de infiltração ocorrido na caixa de solo (condição de alta umidade inicial). Para a condição de baixa umidade inicial (colunas de solo), as proposições que melhor simularam a infiltração foram: K w igual a 0,5 K 0 associada a ψ igual a ψ (θ i ); K w igual a K 0 associada a ψ igual à média entre ψ (θ w ) e ψ (θ i ) e; K w igual à taxa de infiltração estável (T ie ) associada a ψ calculado com base na textura e porosidade do solo. Já para a condição de alta umidade inicial (caixa de solo), estas proposições foram: condutividade hidráulica (K w ) igual a 0,5 K 0 associada ao potencial matricial na frente de umedecimento (ψ) igual a ψ (θ i ); K w igual à T ie associada a ψ igual à média entre ψ (θ w ) e ψ (θ i ); K w igual a K 0 associada a ψ calculado com base na textura e porosidade do solo e; K w igual à T ie associada a ψ calculado com base na textura e porosidade do solo. Duas das combinações foram exatamente as mesmas tanto para a condição de alta, quanto de baixa umidade inicial. O modelo de Green-Ampt simulou melhor o processo de infiltração da água no Latossolo Vermelho- Amarelo estratificado quando este apresentou menor variação na condutividade hidráulica ao longo do perfil.
Soil water infiltration is one of the most important components of the hydrological cycle because it is one of the factors that determines the water that will be avaible for the cultures, the recharge of the underground aquifers, the occurrence and magnitude of the surface runoff and the handling of soil and water. The Green-Ampt model is one of the most used in the prediction of infiltration because it’s based in the physical aspects of the process, however several authors alerts for the need of some adaptation in the model’s input parameters for field conditions. As the Green and Ampt model was developed for homogeneous soils it’s necessary the accomplishment of studies in stratified soils, mainly for typical soils of tropical climate areas. In this work, it was tried to evaluate the Green-Ampt model, as well as several propositions of correction of its entrance parameters (saturation moisture, θ s ; saturated hydraulic conductivity, K 0 ; and, matric potential in the wetting front, ψ), applied to a typical Brazilian soil under stratified conditions, the Red-Yellow Latosol. Two experiments were led, one using soil columns and other using a soil box, were soil material belonging to each one of the three horizons (A, B and C) of the studied soil was compacted. The accumulated infiltration (I) was determined, as well as the infiltration rate (Ti) and the physical characteristics of the profile that were needed for the application of the Green-Ampt model. It was verified that the value of field saturation moisture (θ w ) that best fitted experimental data when it’s not considered θ w variable with the texture of the soil varied among 0,81 θ s (soil box) and 0,86 θ s (soil columns). For the soil box, when was considered that θ w was variable with the texture, the best values were 0,79 θ s for the material of soil of clay texture (horizons A and B) and 0,86 θ s for the material of soil of sandy loam texture (horizon C). Using these values in the Ti, I and wetting front depth simulations, it was noticed that the soil texture exercises great influence in the value of θ w , because all the simulations were better when it was considered the variation of this parameter in agreement with the soil material texture. Using, in the simulations, combinations among six methodologies for the ψ calculation and three for the hydraulic conductivity determination, it was noticed that three different combinations simulated well the infiltration that happened in the columns (condition of low initial moisture) and that four different combinations simulated well the infiltration process that happened in the soil box (condition of high initial moisture). For the condition of low initial moisture (soil columns), the propositions that best simulated the infiltration process were: hydraulic conductivity (K w ) equals to 0,5 K 0 associated with ψ equals to ψ (θ i ); K w equals to K 0 associated to ψ equals to the average among ψ (θ w ) and ψ (θ i ) and; K w equals to the stable infiltration rate (T ie ) associated to ψ calculated with base in soil texture and soil porosity. For the high initial moisture condition (soil box), these propositions were: hydraulic conductivity (K w ) equals to 0,5 K 0 associated with ψ equals to ψ (θ i ); K w equals to T ie associated to ψ equal to the average among ψ (θ w ) and ψ (θ i ); K w equals to K 0 associated to ψ calculated with base in soil texture and soil porosity and; K w equals to T ie associated to ψ equal to calculated with base in soil texture and soil porosity. Two of the combinations were exactly the same for both of the experiments. The Green-Ampt model simulated better the water infiltration process when the soil profile presented lower variation in the hydraulic conductivity.
Dissertação importada do Alexandria
Mello, Luis Tomás Azevedo de. "Avaliação de metodologias para obtenção dos parâmetros do modelo de Green-Ampt modificado por Mein e Larson." Universidade Federal de Viçosa, 2003. http://www.locus.ufv.br/handle/123456789/9551.
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Conselho Nacional de Desenvolvimento Científico e Tecnológico
Os modelos de infiltração embasados em princípios físicos são uma importante ferramenta a ser utilizada na modelagem hidrológica. O modelo de Green-Ampt é uma dessas ferramentas que vem sendo usada em diversas áreas relacionadas ao assunto. Entretanto, a adequação de seus parâmetros a solos brasileiros ainda precisa ser melhor estudada. Este trabalho teve por objetivo avaliar diferentes proposições de determinação dos parâmetros (umidade de saturação, θ s ; condutividade hidráulica, K e potencial matricial na frente de umedecimento, ψ f ) do modelo de Green-Ampt modificado por Mein e Larson (GAML) e sua aplicabilidade a diferentes condições de perfis homogêneo e heterogêneo de solo. O experimento foi conduzido em oito colunas de solo montadas com combinações distintas de horizontes (A, B e C) e massa específica (1,03 g/cm 3 e 1,23 g/cm 3 ), sendo seis colunas com perfil homogêneo e duas com perfil estratificado, sob condições de precipitação constante. Determinaram as características físico-hídricas dos solos das colunas necessárias à aplicação do modelo de GAML e, por meio da técnica chamada de “Time Domain Reflectometry” (TDR), foi possível determinar o avanço da frente de umedecimento a partir da qual foram determinadas a infiltração acumulada (Ia) e a taxa de infiltração (Ti). Os valores da umidade na zona de transmissão (θ w ), determinada ao final dos testes de infiltração, variaram de 0,76 a 0,94 da porosidade, dependendo da textura e da massa específica em questão. Esses valores foram usados como um dos parâmetros de entrada no modelo GAML. Curvas de avanço da frente de umedecimento, de infiltração acumulada e de taxa de infiltração foram simuladas usando o modelo GAML com 36 combinações de proposições para correção de Kw e ψ f . Os resultados simulados e experimentais foram comparados, usando-se coeficientes estatísticos e análise gráfica. Também foram comparados os tempos correspondentes ao início do escoamento superficial determinados experimentalmente e simulados. Não foi encontrada uma única combinação de proposições que melhor representasse todos os casos. No entanto, o uso da condutividade hidráulica (K w ) sendo igual a taxa de infiltração básica (Tib) e o do potencial matricial (ψ f ) calculado em função da textura e da porosidade do solo, fez com que o modelo GAML simulasse bem o processo de infiltração em solos com perfil de massa específica homogênea. Outra combinação que merece destaque é o uso de K w igual à condutividade hidráulica do solo saturado (K 0 ), determinada pelo método do permeâmetro de carga constante, associado ao potencial matricial (ψ f ) correspondente à umidade na zona de transmissão, que representou muito bem as curvas de infiltração obtidas nas colunas com perfil homogêneo dos horizontes A e B, para as duas condições de compactação. De modo geral, quando os parâmetros de entrada do modelo de GAML são bem determinados, o mesmo pode ser usado para a estimativa do processo de infiltração, em solos homogêneos. Em solos heterogêneos, o modelo foi sensível às variações físico-hídricas do perfil do solo, mas não foi preciso em estimar o tempo de ocorrência das mudanças na taxa de infiltração devido à estratificação do solo.
The infiltration models based on physical principles are important tools to be used on the hydrological modeling. The Green-Ampt model is one of these tools that has been being used in different areas related to the subject. However, the adequacy of its parameters to Brazilian soils still needs to be better studied. This work’s objective is to evaluate the different propositions of parameters determination (saturation humidity, q s ; hydraulic conductivity, K and matrix potential before humidification, y f ) of the Green-Ampt model modified by Mein and Larson (GAML) and its applicability to different conditions of homogeneous and heterogeneous soil profiles. The experiment was carried out in eight columns of soil mounted with different horizons combinations (A, B and C) and specific mass (1.03 g/cm 3 and 1.23 g/cm 3 ), being six of the columns with homogeneous profile and two of them with stratified profile, under constant precipitation conditions. The physical-hydric characteristics of the columns soils needed to the GAML model application were determined, and through the technique called “Time Domain Reflectometry” (TDR), it was possible to determine the advancement of the humidification front from which the accumulated infiltration (Ia) and the infiltration rate (Ti) were determined. The humidity value on the transmission zone (θ w ), determined at the end of the infiltration tests, varied from 0.76 to 0.94 of porosity, depending on the texture and on the specific mass in question. These values were used as one of the entrance parameters into the GAML model. Advancement curves of the humidification front, of the accumulated infiltration, and of the infiltration rate were simulated using the GAML model with 36 propositions combinations for the correction of Kw and ψ f . The simulated and experimental results were compared using statistic coefficients and graphic analyses. The times correspondent to the beginning of the superficial drainage experimentally determined and simulated were also compared. A sole combination of proposition that better represented all the cases was not found. However, the use of hydraulic conductivity (K w ) as being equals to the basic infiltration rate (Tib) and to the matrix potential (ψ f ) calculated in relation to the texture and porosity of the soil, made the GAML model simulate well the infiltration process on soils with profile of homogeneous specific mass. Another combination that deserves to be highlighted is the use of Kw equals to the hydraulic conductivity of the saturated soil (K 0 ), determined by the constant charge permeameter method, associated to the matrix potential (ψ f ) correspondent to the transmission zone humidity, that represented very well the infiltration curves obtained on the columns with homogeneous profile of the A and B horizons, for both compactness conditions. In general, when the entrance parameters of the GAML model are well determined, it can be used for the estimate of the infiltration process in homogenous soils. In heterogeneous soils the model was sensitive to the physical-hydric variations of the soil profile, but it was not necessary to estimate the occurrence time of changes on the infiltration rate due to the soil stratification.
Dissertação imortada do Alexandria
Zhang, Jie, and s3069216@student rmit edu au. "A laboratory scale study of infiltration from Pervious Pavements." RMIT University. Civil, Environmental and Chemical Engineering, 2006. http://adt.lib.rmit.edu.au/adt/public/adt-VIT20070125.164003.
Full textLukyanets, Yuliya. "The Green and Ampt Infiltration Model Accounting for Air Compression and Air Counterflow in the Shallow Water Table Environment: Laboratory Experiments." Scholar Commons, 2010. http://scholarcommons.usf.edu/etd/3471.
Full textBrevnova, Elena V. "Green-Ampt infiltration model parameter determination using SCS curve number (CN) and soil texture class, and application to the SCS runoff model." Morgantown, W. Va. : [West Virginia University Libraries], 2001. http://etd.wvu.edu/templates/showETD.cfm?recnum=2039.
Full textTitle from document title page. Document formatted into pages; contains ix, 149 p. : ill. (some col.). Vita. Includes abstract. Includes bibliographical references (p. 60-63).
CASTRO, Thiago Quintiliano de. "Avaliação do desempenho de pavimentos permeáveis." Universidade Federal de Goiás, 2011. http://repositorio.bc.ufg.br/tede/handle/tde/620.
Full textThis study aimed to evaluate the experimental performance of three types of permeable pavements constructed in three different structural conditions in order to control runoff in urbanized areas of the city of Goiania, Goias, adapting to the legal requirements and using local manufactured materials. It was evaluated nine experimental plots of 3.2 m² as the following types: PAV - concrete block "paver", PCP - porous concrete plate and GCC - concrete block "concregrama" and the following structural conditions: I - base of sand and natural subgrade, II - base of sand and compacted subgrade and III - base of sand, gravel subbase and compacted subgrade. Using an artificial rain simulator, 18 tests were performed with two pre-defined rain, a medium intensity (69 mm / h) and a high intensity (180 mm / h). The subgrade soil and building materials were characterized, measured the surface and subsurface runoff, and moisture of the layers of the pavement. The parameters of the models of Horton and Green-Ampt were obtained by adjusting the calculated data infiltration. Combinations PCP-II, PCP-III, II-CCG, CCG-III and PAV-III showed little or no runoff. The delay and persistence in critical times of the runoff hydrograph also secured good results to the PCP, which generally showed higher soaking times (7,2 to 30,4 minutes) compared to the other types of pavement. The structure that showed the best hydrological performance was the III, whose results ranged from 0 to 0,19 for the runoff coefficient. The results showed that porous pavements evaluated in this study contribute to the reduction of runoff, because of low runoff coefficients (0 to 0,36) obtained. Constructive guidelines on the type of permeable pavement that performed better were drawn and described.
O presente trabalho teve como objetivo avaliar o desempenho experimental de três tipos de pavimentos permeáveis construídos em três condições estruturais diferentes com vistas ao controle do escoamento superficial em áreas urbanizadas do município de Goiânia, Goiás, adequando-se às exigências legais e utilizando-se de materiais provenientes de fabricantes locais. Foram avaliadas nove parcelas experimentais de 3,2 m² conforme os seguintes tipos de revestimento: PAV - Bloco de concreto maciço tipo paver , PCP Placa de concreto poroso e CCG Bloco de concreto vazado tipo concregrama , e as seguintes condições estruturais: I - base de areia e subleito natural, II - base de areia e subleito compactado e III - base de areia, sub-base de brita tipo 1 e subleito compactado. Utilizando-se de um simulador de chuva artificial, foram realizados 18 ensaios com duas chuvas pré-definidas, uma de média intensidade (69 mm/h) e outra de alta intensidade (180 mm/h). Foram caracterizados o solo do subleito e os materiais de construção, medidos os escoamentos superficial e subsuperficial, bem como a umidade das camadas dos pavimentos. Os parâmetros dos modelos de Horton e de Green-Ampt foram obtidos por meio do ajuste dos dados calculados de taxa de infiltração. Os pavimentos PCP-II, PCP-III, CCG-II, CCG-III e PAV-III apresentaram pouco ou nenhum escoamento superficial. O retardo e o prolongamento nos tempos críticos do hidrograma de escoamento superficial também garantiram bons resultados ao revestimento PCP, que no geral apresentou os maiores tempos de embebição (7,2 a 30,4 minutos) em comparação aos demais tipos de revestimento. A estrutura que apresentou o melhor desempenho hidrológico foi o Trecho III, cujos resultados variaram de 0 a 0,19 para o coeficiente de escoamento. A análise dos resultados mostrou que os pavimentos permeáveis avaliados neste trabalho contribuem à redução do escoamento superficial, em razão dos baixos coeficientes de escoamento (0 a 0,36) obtidos, assim como ao armazenamento temporário de águas de chuva e ao incremento da infiltração de água no solo urbano. As diretrizes construtivas do tipo de pavimento permeável que obteve melhor desempenho foram traçadas e descritas.
Ataide, Wendy Fonseca. "Modelagem do potencial matricial na frente de umedecimento." Universidade Federal de Viçosa, 2005. http://www.locus.ufv.br/handle/123456789/9744.
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Infiltração é o processo pelo qual a água passa da superfície para o interior do solo, sendo dependente da carga hidráulica na superfície, do teor de água inicial, da textura, da estrutura, da condutividade hidráulica e da porosidade do solo. Diversos modelos se propõem a estimar este processo, dentre os quais se destaca o de Green-Ampt modificado por Mein e Larson (GAML), baseado numa análise física do processo. Embora seja bastante utilizado, este modelo apresenta como desvantagem a dificuldade de obtenção de seus parâmetros de entrada, principalmente do potencial matricial na frente de umedecimento ( ψ m ). Assim sendo, este trabalho teve como objetivos: obter as variáveis necessárias à estimativa do potencial matricial na frente de umedecimento, utilizando-se para tal o modelo de Green-Ampt modificado por Mein e Larson, e estabelecer modelo matemático que relacione o potencial matricial na frente de umedecimento com as características físicas e a condutividade hidráulica do solo saturado, para sua aplicação no modelo de Green-Ampt modificado por Mein e Larson. Foram utilizadas três classes de solos (Latossolo Vermelho - Amarelo – LVA; Latossolo Vermelho – LV; e Argissolo Vermelho – PV). Estes solos foram secos ao ar, destorroados e peneirados em peneira de malha 10 mm, sendo posteriormente acondicionados em colunas de PVC de 200 mm de diâmetro e 800 mm de altura, de modo que a densidade do solo ficasse próxima daquela observada em campo. Na lateral das colunas, foram instaladas horizontalmente sondas de TDR para a determinação do teor de água e para o acompanhamento da frente de umedecimento. Aplicou-se água sobre a superfície das colunas sob taxa constante, por meio de um simulador de chuvas, sendo que o excesso escoado superficialmente foi conduzido para uma caixa de coleta na qual foi instalado um medidor de nível denominado Thalimedes. O volume infiltrado foi determinado por diferença entre o volume precipitado e o escoado. Após a realização dos testes, foram coletadas amostras de solo para determinação da granulometria, densidade do solo, porosidade, macroporosidade e microporosidade. Foram determinados, ainda, os teores volumétricos de água na zona de transmissão e no início do processo e a condutividade hidráulica do solo saturado. O potencial matricial foi calculado por intermédio de um rearranjo no modelo de GAML, considerando a taxa de infiltração estável (Tie) como representativa da condutividade hidráulica do solo saturado e o teor volumétrico de água na zona de transmissão em lugar do teor volumétrico de água correspondente à saturação. De posse dos valores de ψ m e das características do solo, foram ajustados modelos de regressão, sendo a escolha do melhor modelo feita por meio dos coeficientes de determinação (R 2 ), pela significância dos parâmetros no modelo, pelo menor número de variáveis envolvidas e pela facilidade de obtenção dessas variáveis (características do solo). Os valores de condutividade hidráulica do solo saturado, de porcentagem de silte e de macroporosidade foram significativos em todos os modelos nos quais foram utilizados. A Tie não foi significativa em nenhum dos modelos. Todas as equações obtidas utilizando-se a porcentagem de silte em combinação com outras variáveis apresentaram bons resultados na modelagem do ψ m , sendo que, os melhores resultados foram obtidos para o modelo que relaciona o ψ m com a porosidade, a condutividade hidráulica do solo saturado e a porcentagem de silte.
Infiltration is the process by which water passes through the soil surface down to the soil, being dependent on hydraulic load in the surface, on the antecedent moisture, on texture, structure, soil hydraulic conductivity and soil porosity. Several models aim to estimate this process, among which the Green-Ampt modified by Mein and Larson (GAML) model is based on a physical analysis of the process. Although it is frequently used, this model has a limitation for obtaining input parameters, such as the potential head at the wetting front ( ψ m ). This work aimed to obtain the ψ m for GAML model for soils typical of tropical areas, using three classes of soils (Red-Yellow Oxisol, Red Ultisol and Red Oxisol). These soils were air-dried, ground and sieved through 10 mm mesh sieve, placed in PVC columns of 200 mm diameter and 800 mm height, so that the soil density was similar to the field. In the lateral of the columns, horizontal TDR probes were installed for the moisture determination and for the monitoring of the wetting front. The water was applied to the surface of the columns at a constant rate by means of a rain simulator device and the excess drained superficially, was collected and measured in a box using a “Thalimedes” device. The infiltrated volume was calculated by the difference among the precipitate volume and the runoff. After the tests, soil samples were collected for determination of the texture, soil density, porosity, macroporosity, microporosity, volumetric moisture (before and after the tests) and soil hydraulic conductivity. The pressure head at the wetting front was calculated through an adjustment in the GAML model, considering the rate of stable infiltration (Tie) as representative of the hydraulic conductivity, and the transmission zone moisture instead of the moisture saturation. Once having the ψ m values and soil characteristics, regression models were adjusted, choosing the best fit by R 2 , significance of parameters, less number of variables and easy of obtaining soil variables. The soil hydraulic conductivity values, percentage of silt and macroporosity were all significant for all equations. Tie was not significant in none of the equations. All the obtained equations using the amount of silt in combination with another variable showed good results in the ψ m modeling. The best fitted equation was the one which related the ψ m with the porosity, the soil hydraulic conductivity and the percentage of silt.
Dissertação importada do Alexandria
Malam, Abdou Moussa. "Etats de surface et fonctionnement hydrodynamique multi-échelles des bassins sahéliens ; études expérimentales en zones cristalline et sédimentaire." Thesis, Grenoble, 2014. http://www.theses.fr/2014GRENU004/document.
Full textThis work aims at characterizing and comparing the hydrodynamical functioning at several spatial scales within the granitic-basement and sedimentary zones of Western Niger. Then, a simple hydrological model that could be suitable for use at larger scales is proposed and tested.Qualitatively, the two geological domains have common and specific surface features.The experimental work carried out onto common surface features (biological crust, BIOL; erosion crust, ERO; fallow structural surface, ST and cultivated, C) shows that, at the point scale, ERO has the same hydraulic conductivity K value in both contexts. On the other hand, surfaces features C and especially ST have lower K values in granitic context.Monitoring of the ST and C sites along the rainy season proved the stationarity of the ST conductivity value. On the contrary, K varies widely with the amount of rain received from an initial value of 170 mm/h after weeding down to 20 mm/h (i.e. the ST measured value) after 70 mm of rain and even 10 mm/h after 180 mm of rain. This variation shows the short-term benefit of weeding onto infiltration but a degradation of the soil surface on the long term.At the plot scale (10 m2), runoff measurements are consistent with point measurements. ERO has the same runoff coefficient (Kr) in granitic and sedimentary zones while ST and C surfaces have a higher Kr in granitic context.Runoff monitoring of the granitic site cultivated plots showed that from a total of 63 rain events between 2011 and 2013, 22 had a Kr value higher than the average value (0.25) from which 2/3 are observed after the surface had received more than 70 mm rain after weeding.Results obtained at the two scales (point and 10-m2 plot) are thus consistent and show that the cultivated surface gets crusted and may produce runoff more than fallow ST sites and as much as ERO features.At the basin scale (5 ha), Kr values are higher in the granitic site, not only because of the higher Kr value for a given surface feature but also because of the specific low-infiltrating surfaces which are granite outcrops and gravel crusts (Kr = 0.58).At the three previous scales (point, plot and small basin), runoff volume was found independent of soil initial moisture.Using the previous point-scale results in a Green-Ampt infiltration model led to calibrate the wetting front pressure head for each surface feature and to satisfactorily describe runoff volumes obtained at the plot scale.By estimating runoff with the Green-Ampt infiltration model at any given point, basin-scale hydrograms were obtained by adding the contribution of all elementary surfaces. Assuming no re-infiltration of runoff water within the basins, a simple transfer function was chosen accounting for the distance of each surface to the hydrological network, a constant water velocity of 0.05 m.s-1 and a volume of 3-4 mm of water necessary to fill the kori sand cover, which is much less than that in the sedimentary context. Finally, simulated hydrograms reproduce nicely the measured ones, which offers the perspective of applying some principles of the model to larger basins
Rosnoblet, Jérôme. "Dynamique du bilan hydrique parcellaire au sein de l'espace rural-conséquences sur les transferts hydrologiques." Phd thesis, INAPG (AgroParisTech), 2002. http://pastel.archives-ouvertes.fr/pastel-00000266.
Full textMilvet, Karly R. "Green, Green, & Tender." Kent State University / OhioLINK, 2016. http://rave.ohiolink.edu/etdc/view?acc_num=kent1461168477.
Full textGonzalez-Ramirez, Noemi. "Simulating Flood Propagation in Urban Areas using a Two-Dimensional Numerical Model." Scholarly Repository, 2010. http://scholarlyrepository.miami.edu/oa_dissertations/648.
Full textPan, Qingyu. "Green & Clean Al-Cu Alloys." Digital WPI, 2018. https://digitalcommons.wpi.edu/etd-theses/1273.
Full textIp, Man-ting Angel, and 葉敏婷. "The investigation & exporation of green belt in Hong Kong : evaluation method & design solution for green belt." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2014. http://hdl.handle.net/10722/207147.
Full textAdanir, Suleyman. "Efficient Computation Of The Green'." Master's thesis, METU, 2011. http://etd.lib.metu.edu.tr/upload/12612968/index.pdf.
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s function. First, the spectral domain Green&rsquo
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Jeong, Hyoung-Wook. "Green democratization in a developing country : a case study of South Korean green politics." Thesis, University of Newcastle Upon Tyne, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.250190.
Full textGardner, Ambar. "Green School Guidelines & Application in Arid Regions." The University of Arizona, 2015. http://hdl.handle.net/10150/607231.
Full textThere is a worldwide movement towards sustainability. A stepping-stone towards a sustainability conscience population starts in the education of the younger generation. Focusing on improving education specifically in middle schools in arid regions regarding sustainability will shift and shape youths’ interests and lifestyles into an educated community. This sustainability conscience community will continue to make moral sustainable decisions in their future endeavors. The curriculum implemented will reduce the dropout rate because it is a hand-on curriculum that is interesting and enjoyable for kids. The focus of the curriculum is to rely on outdoor activities to create an outdoor learning environment. The curriculum is based on three different sections: 1) campus-wide adaptable strategies implemented by the students, 2) long term investments implemented by professionals, 3) and hands-on activities that will encourage students to go outdoors and experience real-life problems. To create this education system, the author will propose design guidelines and applications that will be used to improve middle schools particularly in arid regions to become “Green Schools”. This program will validate the sustainable strategies, projects, and efforts done at schools and will also market their school as a model to follow. This will explain what it takes to become a Green School in arid regions and how to achieve these standards.
Rahman, Md Minur. "Green Products : A Study on Young & Native Swedish Consumers’ Purchase Intentions of Green Products." Thesis, Umeå universitet, Företagsekonomi, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-83525.
Full textSILVA, DENNIS C. JR. "GREEN VALLEY: RECREATION RETIREMENT COMMUNITY & AGE SPECIFIC DEMOGRAPHIC PROJECTION PLAN FOR GREEN VALLEY, ARIZONA." The University of Arizona, 1998. http://hdl.handle.net/10150/555296.
Full textSabbi, Enrico, and Triantafyllia Karampini. "Venture Capital & Green Ventures : Developing an Understanding of the Investment Decision." Thesis, Umeå universitet, Företagsekonomi, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-161360.
Full textHammarsten, Anna, and Emma Ohlsson. "Attitudes & Incentives of Green Marketing in the Clothes and Accessory Industry - Companies Perspectives." Thesis, Högskolan i Borås, Akademin för textil, teknik och ekonomi, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:hb:diva-21691.
Full textImad, Fadel. "Green Relationship." VCU Scholars Compass, 2014. http://scholarscompass.vcu.edu/etd/3465.
Full textCrute, Stephen John. "Computer simulations of green spruce aphid populations." Thesis, University of Ulster, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.281228.
Full textColdwell, Deborah F. "Cultural ecosystem service delivery from green-space : impacts of urbanisation, green-space visits & landscape-scale restoration." Thesis, University of Sheffield, 2017. http://etheses.whiterose.ac.uk/17309/.
Full textPopa, Tiberiu. "Metal oxide catalysts for green applications." Laramie, Wyo. : University of Wyoming, 2009. http://proquest.umi.com/pqdweb?did=1955861591&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.
Full textErythropel, Hanno. "Designing green plasticizers." Thesis, McGill University, 2011. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=103728.
Full textLes plastifiants sont des additifs ajoutés au poly (chlorure de vinyle) (PVC) pour obtenir des plastiques souples; une propriété importante pour plusieurs applications. Ces plastifiants ne forment pas de liens covalents avec la matrice de polymères, ils peuvent donc graduellement migrer hors de celle-ci. Dû à la grande utilisation du PVC souple, il n'est pas étonnant que certains plastifiants, tel le di(2-éthyle hexyl) de phtalate (DEHP), soient considérés comme des polluants omniprésents dans l'environnement. Des études ont démontrées que la biodégradation du DEHP mène à l'accumulation de produits métaboliques toxiques. Ces considérations, entre autres, ont déjà conduit à l'abolition ou à la restriction, au Canada, aux États-Unis et dans l'Union Européenne, de l'utilisation de certains phthalates. Ainsi, il y a un intérêt prononcé pour le développement de nouveaux plastifiants « verts » complètements biodégradables. Une série de composés diesters ayant l'acide maléique comme molécule de base et ressemblant partiellement à la structure chimique des phthalates, a été testée. De même, des séries basées sur l'isomère structurel de l'acide maléique, l'acide fumarique, et son équivalent saturé, l'acide succinique ont aussi été testées. L'estérification des ces acides a été réalisée avec des alcools de longueur variable allant de l'éthanol à l'octanol, incluant aussi le 2-éthyle hexanol. Tous ces diesters ont été incorporés à du PVC à une composition d'environ 30% de la masse du matériau. La température de transition vitreuse (Tg) et la résistance à la traction ont été mesurées pour déterminer l'efficacité de ces plastifiants potentiels. Ces données ont été comparées entre elles ainsi qu'avec des résultats obtenus avec le DEHP. Des échantillons de plastifiants potentiels ont été testés pour déterminer leur biodégradabilité par la bactérie Rhodococcus rhodocrous (ATCC 13808); l'hexadécane étant utilisé comme source principale de carbone. Les résultats obtenus pour les diesters de l'acide succinique et de l'acide maléique ont démontrés qu'ils étaient d'aussi bons ou de meilleurs plastifiants que le DEHP. Dans le groupe des diesters de l'acide succinique, ceux contenant des alcools plus longs étaient de meilleurs plastifiants. Il a été déterminé que la présence d'une chaîne 2-éthyle dans certains diesters avait un effet significatif sur les propriétés des composés. Les expériences de biodégradabilité avec Rhodococcus rhodocrous ont démontré l'importance de la structure chimique de l'acide central des diesters. Les maléates en particulier, dans lesquels la position des deux groupes esters ressemble à celle du DEHP, n'ont démontré aucune susceptibilité à être biodégradés après 30 jours. Les fumarates ont été dégradés partiellement tandis que les succinates l'ont été très rapidement. Ces résultats indiquent que l'orientation des deux groupes esters, comme dans le cas du DEHP, est responsable de la stabilité de ces composés dans l'environnement. L'autre facteur influençant le taux de biodégradation est la longueur des alcools utilisés pour l'estérification: les molécules les plus longues avaient des taux plus bas. Toutefois, tous les alcools sans chaîne secondaire furent dégradés sans accumulation de métabolites stables. Inversement, tous les plastifiants potentiels contenant du 2-éthyle hexanol, ont démontrés une telle accumulation. Plusieurs diesters testés pourraient être considéré comme « verts ». En ce qui a trait au choix de l'acide central, les diesters de l'acide succinique représente probablement le meilleur choix. Pour les alcools utilisés pour l'estérification, les alcools longs démontrent de meilleures propriétés plastifiantes, alors que pour la biodégradation, les alcools courts étaient meilleurs. Un candidat représentant un bon compromis entre ces propriétés est le dihexyl de succinate.
Youngquist, Timothy Dennis. "What is green infrastructure? an evaluation of green infrastructure plans from across the United States /." [Ames, Iowa : Iowa State University], 2009. http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:1464412.
Full textYazgan, Uzunefe Yasemin. "Vestiges Of Greek Tragedy In Three Modern Plays &." Master's thesis, METU, 2003. http://etd.lib.metu.edu.tr/upload/1252238/index.pdf.
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s Journey Into the Night, to find out whether they share certain themes with classical Greek tragedies. These themes are namely values and conflict, hamartia and learning through suffering. Three Greek plays, Agamemnon, Oedipus Rex and Medea will be used as foils to conduct this comparative study. The study will aim to support the view that these major themes appear both in ancient Greek and modern tragedies.
Talebi, Mujtaba. "Computer power consumption benchmarking for green computing." Click here for download, 2008. http://proquest.umi.com/pqdweb?did=1490085671&sid=1&Fmt=2&clientId=3260&RQT=309&VName=PQD.
Full textThorud, Joshua D. "Limelight & Indigestion." VCU Scholars Compass, 2015. http://scholarscompass.vcu.edu/etd/3863.
Full textCarkner, Andrew. "Green metal nanoparticle synthesis." Thesis, McGill University, 2008. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=22037.
Full textTitre: Production vert de nanoparticules métalliques Les nanoparticules d'argent et de nickel ont de diverses applications en catalyse, matériaux composites et électronique. Cependant la production actuelle utilise soit beaucoup d'énergie soit de composés dangereux ; il sera mieux pour la santé et l'environnement de trouver d'alternatives. Ce projet a examiné le glucose et le formate comme alternatifs au hydrazine pour la synthèse aqueuse des nanoparticules. Quoique les conditions thermodynamiques sont favorables, je n'ai pas pu produire de nanoparticules de nickel sauf avec le hydrazine dans la région pH 4-12 et T ≤ 100oC. Avec le glucose ou le formate, la conversion demeure insignifiant après 8h. Avec le hydrazine, une haute température et pH sont nécessaires pour une réaction rapide. Avec pH 12, 100oC et 20 mM d'acetate de nickel, la conversion est 70% après 30 minutes. Sous pH 10 et 80oC, la conversion est négligeable même après 3 heures.
LIMA, Cícero Aurélio Grangeiro. "Estudo da variabilidade espacial da infiltração: aspectos teóricos e experimentais." Universidade Federal de Campina Grande, 1992. http://dspace.sti.ufcg.edu.br:8080/jspui/handle/riufcg/2165.
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Testes de infiltração com infiltrômetro duplo anel de nível constante foram efetuados em 32 pontos de uma malha retangular de uma parcela agrícola da Fazenda Experimental da EMEPA - Pb. Ajustamentos as Leis de Philip e de Green e Ampt foram efetuados. Medições da granulometria, densidade aparente seca do solo e umidade volumétrica antes e depois dos testes foram também efetuadas. Utilizou-se a seguir técnicas de análises estatística clássica e geoestatística para caracterizar a variabilidade espacial dos parâmetros de infiltração obtidos pelos ajustamentos. Nenhum dos parâmetros estudados apresentou estrutura espacial definida. Correlações simples e múltiplas evidenciaram dependência da percentagem de Argila + Silte com o espaço físico, e independência entro os parâmetros de infiltração. Ilustrações sobre o efeito da variabilidade espacial sobro o ponto de vista agronômico o hidrológico são mostradas.
Infiltration tests with double-ring infiltrometers were performed in a 33 paint reiangular regular]y spaced grid of an agri cultural site. Fitting of the infiltration curve obtained by Philip and Green and Ampt laws allowed to obtain the sorptivity, the infiltration rate at steady state and the suction parameters of Green and Ampt,for each point. Measurements of pre- and post-humidi ty, granulometry and dry density were also performed. Classical statistical and geo-statistical techniques were used to characterize spatial variability. None of the parameters studied showed a defined spatial structure. Single and muitiple correlations showed a dependence between Cclay + siltD percentage with space but no correlation between parameters was obtained. I11ustrative considerations about spatial variability were ma de with agronomic and hydrologic applications.
Scott, Caroline Daphne. "The role of blue-green algae as marine fouling organisms." Thesis, University of Portsmouth, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.282555.
Full textValassakis, Antonios. "Greek & the Internet, the affects of electronic mail exchange on the Greek language." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2001. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/mq62994.pdf.
Full textPowtongsook, Sorawit. "Physiology and biotechnology of glycerol production using the green microalga Dunaliella." Thesis, University of Sheffield, 1998. http://etheses.whiterose.ac.uk/15086/.
Full textHenderson, Julius Nathan. "Crystallographic and spectroscopic studies of photoswitching in fluorescent proteins /." view abstract or download file of text, 2007. http://proquest.umi.com/pqdweb?did=1417810431&sid=5&Fmt=2&clientId=11238&RQT=309&VName=PQD.
Full textTypescript. Includes vita and abstract. Includes bibliographical references (leaves 143-151). Also available for download via the World Wide Web; free to University of Oregon users.
Barnett, Faires Anthony. "Upper Green River Basin streamflow reconstructions and drought variability." Laramie, Wyo. : University of Wyoming, 2007. http://proquest.umi.com/pqdweb?did=1445046271&sid=9&Fmt=2&clientId=18949&RQT=309&VName=PQD.
Full textRuggero, E. Colin. "Radical Green Populism environmental values in DIY/Punk communities /." Access to citation, abstract and download form provided by ProQuest Information and Learning Company; downloadable PDF file, 125 p, 2009. http://proquest.umi.com/pqdweb?did=1885562141&sid=1&Fmt=2&clientId=8331&RQT=309&VName=PQD.
Full textFollum, Michael Lee. "Upper Green River Basin precipitation reconstructions and drought analysis." Laramie, Wyo. : University of Wyoming, 2009. http://proquest.umi.com/pqdweb?did=1798481411&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.
Full textAdkin, Kevin R. "India's 'Garden City'? Bangalore's disappearing greenbelt green to gone /." Access to citation, abstract and download form provided by ProQuest Information and Learning Company; downloadable PDF file, 183 p, 2009. http://proquest.umi.com/pqdweb?did=1694328971&sid=5&Fmt=2&clientId=8331&RQT=309&VName=PQD.
Full textAlabdullatif, Talal. "SABIC Green Logistics Systems & Profitability : To explore chemical industries green logistics and contribution to profitability with a particular case of SABIC." Thesis, Internationella Handelshögskolan, Högskolan i Jönköping, IHH, Centre of Logistics and Supply Chain Management (CeLS), 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:hj:diva-36513.
Full textWells, Tyrone. "Lignin for bioenergy & biomaterials." Diss., Georgia Institute of Technology, 2015. http://hdl.handle.net/1853/53575.
Full textMavrommatis, Ioannis. "Classroom assessment in Greek primary schools." Thesis, University of Bristol, 1995. http://hdl.handle.net/1983/5a055807-d52e-4432-8c14-3c4aa27050ec.
Full textVarelas, Dimitris. "Orff-Schulwerk applications in Greek settings." Thesis, University of Reading, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.272706.
Full textHanos, Stergios. "Developing information skills in Greek schools." Thesis, Loughborough University, 1997. https://dspace.lboro.ac.uk/2134/28124.
Full textSweeney, Julia. "Societal Value Change and Change inProduct Portfolio : A Case Study of Henkel AG & Co. KGaA with Special Considerationof ‘Green’ Product Innovations in Germany 1970-2010." Thesis, Linköpings universitet, Företagsekonomi, 2011. http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-71157.
Full textMoreo, Andrew. "Green Consumption in the hotel industry a an examination of consumer attitudes /." Access to citation, abstract and download form provided by ProQuest Information and Learning Company; downloadable PDF file, 67 p, 2008. http://proquest.umi.com/pqdweb?did=1597631261&sid=16&Fmt=2&clientId=8331&RQT=309&VName=PQD.
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