Academic literature on the topic 'SuDS modelling'

In a changing climate with an increasing risk of flooding, developing a sustainable approach to flood management is paramount. Sustainable Drainage Systems (SuDS) present a change in thinking with regards to drainage; storing water in the urban environment as opposed to rapidly removing it to outflows. The Non-Statutory Standards for SuDS (DEFRA 2015a) presented a requirement for all developments to integrate SuDS in their design to reduce runoff. This research models the impact on water quantity of combining different SuDS devices to demonstrate their success as a flood management system, as compared to conventional pipe based drainage. The research uses MicroDrainage®, the UK industry standard flood modelling tool which has an integrated SuDS function, to simulate the role of SuDS in a management train. As space is often cited as the primary reason for rejecting SuDS, determining the most effective technique at reducing runoff is critical. Detention basins were concluded as being highly effective at reducing peak flow (150 l/s when combined with swales), however Porous Pavement Systems (PPS) was nearly twice as effective per m3, reducing peak flow by up to 0.075 l/s/m3 compared to 0.025 l/s/m3. This therefore suggests that both detention basins and PPS should be high priority devices when developing new sites, but that no matter what combination of modelled SuDS are installed a reduction in runoff in comparison to conventional drainage can be achieved. A SuDS decision support tool was developed to assist design in MicroDrainage® by reducing the time spent determining the number of SuDS required for a site. The tool uses outputs from MicroDrainage® to rapidly predict the minimum and maximum peak flow for a site, in comparison to greenfield runoff, based on the site parameters of area, rainfall rate, infiltration, combined with the planned SuDS. The tool was underpinned by a model analysis for each site parameter and each SuDS device, which produced r2 values >0.8, with 70% above 0.9. This ensured a high level of confidence in the outputs, enabling a regression analysis between runoff and each site parameter and SuDS device at the 99% confidence level, with the outputs combined to create the tool. The final aspect of the research validated MicroDrainage® to analyse the accuracy of the software at predicting runoff. Using field data from Hamilton, Leicester, and laboratory data for PPS and filter drains, a comparison could be made with the output from MicroDrainage®. The field data created a Nash-Sutcliffe Efficiency (NSE) of 0.88, with filter drains and PPS providing an NSE of 0.98 and 0.94 respectively. This demonstrates the success with which MicroDrainage® predicts runoff and provides credibility to the outputs of the research. Furthermore, it offers SuDS specialists the confidence to use MicroDrainage® to predict runoff when using SuDS.

The overarching goal of this research is to establish a successful forum for a transition from the existing paradigm of managing wastewater infrastructure to a more sustainable paradigm that achieves a more efficient utilisation of wastewater assets. A transitioning approach to support a more efficient utilisation of surface water and wastewater assets and infrastructure is proposed and developed. The determined transitioning approach possesses key stages namely developing the arena, developing the agenda, case study, and monitoring. The case study stage investigates a drainage utility identifying their improvement drivers, the removal of surface water through detailed drainage modelling and the financial examination of the costs incurred under the various scenarios conducted. Understanding the implications of removing/attenuating surface water from the network is improved through obtaining data by detailed drainage modelling. Infoworks software is used to investigate and assess the current and future operational scenarios of a wastewater system operating over one calendar year. Modelling scenarios were conducted removing surface water from selected areas focusing on the volumes requiring pumping and durations of pumping station(s) operation prior to treatment during storm conditions. The financial implication of removing surface water in combined sewer systems is examined in three main components. Firstly the costs of electricity incurred at the single sewage pumping station (SPS) investigated during the various scenarios modelled require to be addressed. Secondly the costs to retrofit sustainable urban drainage system (SUDS) solutions needs to be identified. Thirdly the implications of removing surface water for the drainage utility at the national level and the potential saving for householder’s committing to a surface water disconnection rebate scheme. When addressed at the macro level i.e., with over 2,100 pumping stations, some operating in sequence and contained within one drainage utility annually treating 315,360 megalitres the significance of the same multiple quantifiable and intangible benefits becomes amplified. The research aims, objectives and findings are presented to the identified and convened stakeholders. The transitioning approach developed encourages positive discourse between stakeholders. The level of success of the transitioning approach determined is then tested using a quantitative methodology through the completion of questionnaires. From the questionnaires completed the respondents unanimously agreed that surface water flows should be removed as well as reduced from the combined sewer system. The respondents agreed that the removal of surface water from a typical combined sewer system is justified by applying a transitioning approach focusing on the energy consumption required to pump increased volumes during storm events. This response is significant based upon the economic evidence and is contrary to the respondents previous position that finance was their most influencing factor. When provided with other potentially available benefits the respondents were even more supportive of the justification to remove surface water from the combined sewer system. The combined findings of the work presented in this thesis provide further justification that the transitioning approach applied to the removal of surface water from a typical combined sewer system, as determined in this research has been successful.

Les marges conjuguées de l'Atlantique Sud sont le produit du rifting et de la rupture du continent Pangée. Ce continent présente une hétérogénéité crustale et lithosphérique importante, dont la prise en compte est un objectif de la thèse. Afin de comprendre la rupture continentale à l'échelle lithosphérique de systèmes de rhéologies préexistantes très différentes, nous avons effectué des modélisations, analogique et numérique. Les modèles analogiques s'attachent à montrer l'effet des forces externes sur un tel système hétérogène tandis que les modèles numériques, thermomécaniques, se concentrent sur l'impact des anomalies de fusion du manteau sur le rifting avec une telle configuration.Avec la modélisation analogique, l'effet des forces aux limites sur un système composé de deux segments de rhéologies différentes a été testé à l’échelle de la lithosphère pour comprendre l'influence de l'hétérogénéité rhéologique dans un système en extension. Les résultats montrent que dans un système combiné, toute l'extension se produit dans le segment faible et que le contact entre les deux segments ne joue pratiquement aucun rôle dans l'initiation des failles. Lorsque le segment le plus faible contient une couche résistante dans le manteau supérieur, le rift évolue en deux phases. La première phase montre un système de failles larges où la déformation est distribuée. Une fois que la partie résistante du manteau supérieur est suffisamment affaiblie, l'extension se localise le long d'une zone de faille étroite. Si l'extension continuait, la rupture se produirait à cet emplacement, dans une partie plutôt homogène alors que le système est latéralement hétérogène. Le résultat de ce système extensif serait des marges asymétriques avec une croûte faible/hyper-étirée sur deux marges.Les résultats numériques montrent que, dans le cas de la rupture continentale induite par un panache, le mode de rupture «central», où la rupture se localise au-dessus du point de l'impact du panache, est une forme de rupture continentale parmi d'autres. Ainsi, lorsque l'anomalie de fusion du manteau est localisée de manière décalée par rapport au contact entre les segments rhéologiques, un mode de rupture "décalé" peut se développer. Dans ce cas, le matériel du panache atteint la base de la lithosphère et s’écoule latéralement jusqu’au contact entre les deux segments rhéologiques où le rifting se localise in fine. La partie du matériel qui n’arrive pas au centre de la zone de rupture, se situe au niveau de la croûte inférieure ou bien plus profond, ressemblant aux corps de densité/vitesse élevées imagés le long des marges de l'Atlantique Sud. De plus, le mode «décalé» reproduit l'asymétrie des marges conjuguées<br>The South Atlantic conjugate margins are the product of continental rifting and break-up of Pangea, which was made up of different crustal features prior to rifting. This study investigates continental rift initiation and break-up of alternative lithospheric setups, consisting of large segments with different rheological strength, with the use of analogue and numerical modelling. The analogue models investigate the effect of far-field forces on a system that consist of multiple rheological segments, whereas the numerical models include thermal processes and focus on the impact of initial plume emplacement on such a setup.Lithosphere-scale analogue models consisting of two different rheological compartments have been subjected to extensional forces, to understand effect of far-field forces on large rheological heterogeneities in a system within an extensional tectonic regime. The results show that in such a system, the weaker segment accommodates all the extension. At the contact between the two compartments no rift-initiation is observed. In the presence of a strong sub-Moho mantle, the rift evolution consists of two phases. The first phase is a wide or distributed rift event. Once the strong part of the upper mantle has sufficiently weakened, the rift localizes and a narrow rift continues to accommodate the extension. If extension would continue, break-up would happen at the location of the narrow rift, thereby breaking a rather homogenous part within a laterally heterogeneous system. This would result in asymmetric margins with hyperextended, weak crust on both margins.The numerical results show that, in the case of plume-induced continental break-up, the classical ‘central’ mode of break-up, where the break-up centre develops above the plume-impingement point is not the only form of continental break-up. When the mantle anomaly is located off-set from the contact between rheological segments, a ‘shifted’ mode of break-up may develop. In this case, the mantle plume material rises to the base of the lithosphere and migrates laterally to the contact between two rheological segments where rifting initiates. Mantle material that does not reach the spreading centre and remains at lower crustal depths, resemble high density/high velocity bodies at depth found along the South Atlantic margin and providing geometric asymmetry.Further investigation on the exact influence of the initial plume position with respect to the contact between the rheological compartments shows that there is a critical distance for which the system develops either ‘central’ (or ‘plume-induced’) continental break-up or ‘shifted’ (or ‘structural inherited’) continental break-up. For Moho temperatures of 500 – 600 oC, there is a window of ~50 km where the system creates two break-up branches. These results explain complex rift systems with both vertical penetration of plume material into the overlying lithosphere as well as reactivated inherited structures developing break-up systems both aided by the same mantle plume

Os métodos de controle de qualidade tradicionais aplicados ao radiodiagnóstico, é a melhor maneira de garantir a boa qualidade das imagens produzidas. No entanto, a investigação de particularidades oriundas do processo de formação de imagens radiológicas requer ferramentas computacionais complementares, em função do número de variáveis envolvidas. Entretanto, os fantomas computacionais baseados em voxels não conseguem representar as variações morfométricas necessárias para a simulação de exames cujo diagnóstico é baseado em imagem. Neste trabalho foi desenvolvido um novo tipo de fantoma computacional, baseado em modelagem 3D, que possui as vantagens apresentadas pelos fantomas computacionais tradicionais sem os problemas encontados nestes. A ferramenta de modelagem utilizada, o Blender, é disponibilizada gratuitamente na internet. A técnica utilizada foi a box modeling, que consiste na deformação de uma primitiva básica, nesse caso um cubo, até que apresente a forma da estrutura que se deseja modelar. Para tanto, foram utilizadas como referencia, imagens obtidas de atlas de anatomia e fotografias de um esqueleto fornecido pela Universidade de Mogi das Cruzes. Foram modelados o sistema ósseo, os órgãos internos e a anatomia externa do corpo humano. A metodologia empregada permitiu a alteração de parâmetros do modelo dentro da ferramenta da modelagem. Essa possibilidade foi mostrada através da variação, dos formatos do intestino e do aumento da quantidade de tecido adiposo da malha referente a pele. A simulação das imagens radiológicas foi realizada a partir de coeficientes de atenuação de massa de materiais, ossos e tecidos e de modelos com diversas características físicas. Essa versatilidade permite prever a influência que as diferenças morfométricas entre os indivíduos provocam nas imagens, propriciando dessa forma, uma ferramenta relevante complementar aos métodos de controle de qualidade tradicionais.<br>The conventional methods of quality control applied to radio diagnosis are the best way to have assured good quality of the produced images. Due the amount of variables to consider, the study of particular issues of the process of formation of radiological images requires complementary computational tools. However, the computational voxel based phantoms are not suitable to represent the morphometrical variations, intended for test simulations with image based diagnosis. This work developed a new type of computational phantom, based on 3D modelling. It has the same advantages of the conventional ones, without some of their restrictions. The modeling tool employed, Blender, is available on internet for free download. The project uses the technique called box modeling, which consists in the deformation of a primitive form (a cube, in this case) until it presents a similar form to that it is wanted to model. In order to achieve it, some images, obtained from anatomy atlas and a skeleton pictures obtained from University of Mogi das Cruzes, were used as reference. Were built models from skeletal system, internal organs and external human body anatomy. The applied methodology allowed model´s parameter settings on the modelling tool. This option was presented by means of intestine format variation and increase of adipose tissue on the mesh that represents skin. The simulation of radiological images was done by means of x-ray mass attenuation coefficients, bones and tissues and models with diferent physical characteristics. This flexibility allows the analysis and forecasting of the influences that morphometrical differences of individual implies on images, revealing an important tool that complements the conventional quality control tools.

Les marges conjuguées de l'Atlantique Sud sont le produit du rifting et de la rupture du continent Pangée. Ce continent présente une hétérogénéité crustale et lithosphérique importante, dont la prise en compte est un objectif de la thèse. Afin de comprendre la rupture continentale à l'échelle lithosphérique de systèmes de rhéologies préexistantes très différentes, nous avons effectué des modélisations, analogique et numérique. Les modèles analogiques s'attachent à montrer l'effet des forces externes sur un tel système hétérogène tandis que les modèles numériques, thermomécaniques, se concentrent sur l'impact des anomalies de fusion du manteau sur le rifting avec une telle configuration.Avec la modélisation analogique, l'effet des forces aux limites sur un système composé de deux segments de rhéologies différentes a été testé à l’échelle de la lithosphère pour comprendre l'influence de l'hétérogénéité rhéologique dans un système en extension. Les résultats montrent que dans un système combiné, toute l'extension se produit dans le segment faible et que le contact entre les deux segments ne joue pratiquement aucun rôle dans l'initiation des failles. Lorsque le segment le plus faible contient une couche résistante dans le manteau supérieur, le rift évolue en deux phases. La première phase montre un système de failles larges où la déformation est distribuée. Une fois que la partie résistante du manteau supérieur est suffisamment affaiblie, l'extension se localise le long d'une zone de faille étroite. Si l'extension continuait, la rupture se produirait à cet emplacement, dans une partie plutôt homogène alors que le système est latéralement hétérogène. Le résultat de ce système extensif serait des marges asymétriques avec une croûte faible/hyper-étirée sur deux marges.Les résultats numériques montrent que, dans le cas de la rupture continentale induite par un panache, le mode de rupture «central», où la rupture se localise au-dessus du point de l'impact du panache, est une forme de rupture continentale parmi d'autres. Ainsi, lorsque l'anomalie de fusion du manteau est localisée de manière décalée par rapport au contact entre les segments rhéologiques, un mode de rupture "décalé" peut se développer. Dans ce cas, le matériel du panache atteint la base de la lithosphère et s’écoule latéralement jusqu’au contact entre les deux segments rhéologiques où le rifting se localise in fine. La partie du matériel qui n’arrive pas au centre de la zone de rupture, se situe au niveau de la croûte inférieure ou bien plus profond, ressemblant aux corps de densité/vitesse élevées imagés le long des marges de l'Atlantique Sud. De plus, le mode «décalé» reproduit l'asymétrie des marges conjuguées<br>The South Atlantic conjugate margins are the product of continental rifting and break-up of Pangea, which was made up of different crustal features prior to rifting. This study investigates continental rift initiation and break-up of alternative lithospheric setups, consisting of large segments with different rheological strength, with the use of analogue and numerical modelling. The analogue models investigate the effect of far-field forces on a system that consist of multiple rheological segments, whereas the numerical models include thermal processes and focus on the impact of initial plume emplacement on such a setup.Lithosphere-scale analogue models consisting of two different rheological compartments have been subjected to extensional forces, to understand effect of far-field forces on large rheological heterogeneities in a system within an extensional tectonic regime. The results show that in such a system, the weaker segment accommodates all the extension. At the contact between the two compartments no rift-initiation is observed. In the presence of a strong sub-Moho mantle, the rift evolution consists of two phases. The first phase is a wide or distributed rift event. Once the strong part of the upper mantle has sufficiently weakened, the rift localizes and a narrow rift continues to accommodate the extension. If extension would continue, break-up would happen at the location of the narrow rift, thereby breaking a rather homogenous part within a laterally heterogeneous system. This would result in asymmetric margins with hyperextended, weak crust on both margins.The numerical results show that, in the case of plume-induced continental break-up, the classical ‘central’ mode of break-up, where the break-up centre develops above the plume-impingement point is not the only form of continental break-up. When the mantle anomaly is located off-set from the contact between rheological segments, a ‘shifted’ mode of break-up may develop. In this case, the mantle plume material rises to the base of the lithosphere and migrates laterally to the contact between two rheological segments where rifting initiates. Mantle material that does not reach the spreading centre and remains at lower crustal depths, resemble high density/high velocity bodies at depth found along the South Atlantic margin and providing geometric asymmetry.Further investigation on the exact influence of the initial plume position with respect to the contact between the rheological compartments shows that there is a critical distance for which the system develops either ‘central’ (or ‘plume-induced’) continental break-up or ‘shifted’ (or ‘structural inherited’) continental break-up. For Moho temperatures of 500 – 600 oC, there is a window of ~50 km where the system creates two break-up branches. These results explain complex rift systems with both vertical penetration of plume material into the overlying lithosphere as well as reactivated inherited structures developing break-up systems both aided by the same mantle plume

Orientador: Ingrid Koch<br>Resumo: Neste estudo, nós desenvolvemos marcadores moleculares e aplicamos abordagens integrativas em filogeografia e ecologia para investigar e descrever a história biogeográfica das chapadas da região oeste do Cerrado brasileiro. Utilizando como modelo duas espécies do gênero Rauvolfia L. (Apocynaceae, Rauvolfioideae), Rauvolfia weddelliana Müll.Arg. e Rauvolfia gracilis I.Koch & Kin.-Gouv., típicas destes ambientes, nós desenvolvemos um conjunto de marcadores nucleares microssatélites e sequenciamos espaçadores de cloroplasto, com os quais estimamos métricas de diversidade genética e estruturação populacional. A partir destes dados, nós reconstruímos relações filogenéticas entre as linhagens, estimamos tempos de divergência e realizamos simulações demográficas e modelos de distribuição, com o intuito de testar possíveis cenários biogeográficos. Em sequência, nós desenvolvemos modelos de distribuição potencial em escala de comunidade e análises espaciais, para estimar o impacto relativo das flutuações climáticas do Pleistoceno sobre o endemismo no Cerrado, quando comparadas a outros processos. Os resultados estão apresentados em três capítulos. No primeiro, intitulado “Development and cross-validation of microsatellite markers for Rauvolfia weddelliana Müll.Arg. (Apocynaceae) species complex”, nós descrevemos o desenvolvimento de uma biblioteca de microssatélites específica para R. weddelliana e testamos sua transferabilidade para a espécie R. gracilis. Nós isolamos dez marcadores ... (Resumo completo, clicar acesso eletrônico abaixo)<br>Abstract: In this study, we developed molecular markers and applied integrative approaches in phylogeography and ecology to investigate and describe the biogeographic history of the plateaus of the west region of the Cerrado in Brazil. Using as models two species of the genus Rauvolfia L. (Apocynaceae, Rauvolfioideae), Rauvolfia weddelliana Müll.Arg. and Rauvolfia gracilis I.Koch & Kin.-Gouv., typical from these habits, we developed a set of nuclear microsatellite markers and sequenced chloroplast spacers, which we used to estimate metrics of genetic diversity and population structure. From this data, we reconstructed phylogenetic relationships between lineages, estimated divergence times and conducted demographic simulations and distribution models, intending to test possible biogeographic scenarios. In sequence, we also developed community wise models of potential distribution and conducted spatial analysis to estimate the relative impact of climatic shifts of the Pleistocene on the endemism of the Cerrado, when compared to other processes. Our results are presented in three chapters. In the first, entitled “Development and cross-validation of microsatellite markers for Rauvolfia weddelliana Müll.Arg. (Apocynaceae) species complex”, we describe the development of a specific microsatellite library to R. weddelliana and tested its transferability to the species R. gracilis . We isolated ten transferable markers with high polymorphism content that may now be applied to genetics studies ... (Complete abstract click electronic access below)<br>Doutor

Submitted by (lucia.rodrigues@ufrpe.br) on 2016-10-11T14:11:57Z No. of bitstreams: 1 Renato Paiva de Lima.pdf: 524535 bytes, checksum: 47be2d27255026d21fdeb8e8a90a484f (MD5)<br>Made available in DSpace on 2016-10-11T14:11:57Z (GMT). No. of bitstreams: 1 Renato Paiva de Lima.pdf: 524535 bytes, checksum: 47be2d27255026d21fdeb8e8a90a484f (MD5) Previous issue date: 2013-07-18<br>Models that predict pre-consolidation stress in Ultisol are scarce, given the importance of these soils for the production of sugarcane in the Northeast. The current study aimed to fit linear and nonlinear regression models and study the relationship of soil physical attributes on pre-consolidation stress (σp) variation. On a plot, 42 points were delimited to get samples in the layers 0-0.20 and 0.20-0.40 m, totaling 84 samples. Deformed and undeformed samples were collected to obtain the variables: water content (θ), bulk density (BD), soil resistance to penetration (RP), organic carbon (OC), clay content (C), plastic limit (PL) and liquid limit (LL), as well as the pre-consolidation stress (σp). Four models were fitted to predict the σp: linear multiple regression, two nonlinear multiple model and charge supporter capacity model. Was also held for each layer a principal component analysis was performed and, after obtaining the scores for those components retained, a linear multiple regression model was fitted for the σp data to establishment of the relationships. The average of σp was 73.0 kPa. The multiple linear regression model was the best fit soil conditions and management of the area in the two analyzed layers. Only soil bulk density and penetration resistance contributed significantly to variation σp models with the best settings. The θ and the OC showed negative relations with σp; while BD, RP, C, LL and PL showed positive relation. Higher values of σp are associated with higher values of BD, RP, C, LL and PL, as well as smaller values are linked with the increase of OC concentration and θ.<br>Modelos que predizem a tensão de pré-consolidação em Argissolo Amarelo distrocoeso são escassos na literatura, dada a importância desses solos para produção de cana-de-açúcar no Nordeste. O presente estudo teve como objetivos ajustar modelos de regressão lineares e não lineares e estudar as relações dos atributos físicos do solo na variação da tensão de pré-consolidação (σp). O trabalho foi realizado em área de Argisssolo Amarelo distrocoeso cultivado com cana-de-açúcar. Em um talhão, foram demarcados 42 pontos e coletadas amostras nas camadas 0-0,20 e 0,20-0,40 m, totalizando 84 pontos amostrais. Foram coletadas amostras deformadas e não deformadas para obtenção das variáveis: umidade do solo (θ), densidade do solo (DS), resistência à penetração (RP), carbono orgânico (CO), teor de argila (TA), limite de plasticidade (LP) e limite de liquidez (LL), além da tensão de pré-consolidação (σp). Foram ajustados quatro modelos para predição da σp: regressão linear múltipla, dois modelo não lineares e um modelo não linear de capacidade de suporte de carga, bem como, foi realizada análise de componentes principais, em cada uma das camadas estudadas, que após obtenção dos escores dos componentes principais retidos em cada camada de solo, um modelo de regressão linear múltiplo foi ajustado aos dados de σp para estabelecimento das relações. A σp média foi de 73,0 kPa; sendo o modelo de regressão linear múltipla o que melhor se ajustou as condições de solo e manejo da área nas duas camadas analisadas. Apenas a densidade do solo e a resistência à penetração contribuíram significativamente para variação da σp nos modelos com os melhores ajustes. A θ e o CO apresentaram relações negativas com a σp, enquanto DS, RP, TA, LL e LP positivas. Maiores valores de σp estão associados a maiores valores de DS, RP, TA, LL e LP, assim como os menores a um aumento da concentração de CO e da θ.