The Mississippi River is one of the most intensively managed and altered river systems in the world. The alterations to the Mississippi have been largely made to meet navigation demands and mitigate floods. River training has been undertaken using rock structures, commonly referred to as river training structures (RTS), to modify the shape of the river to maintain the Congressional mandated navigation channel dimensions. In addition to maintaining the navigation channel, newer RTS such as chevrons, have been claimed to be designed as an improvement to the previously existing dikes. They are considered to be tools of improving riverine habitat by increasing physical habitat heterogeneity within the highly engineered and consequently uniform river channel. Thus, to evaluate the differences in physical habitat heterogeneity created by the two RTS; a dike and a chevron, this study models and compares the physical aquatic habitats created along the Middle Mississippi River near Grand Tower, Illinois. The hydraulic modelling software HEC-RAS has been used to develop a two-dimensional model of the study area containing the RTS using detailed 2 m- resolution topobathy digital elevation model (DEM), U.S Geologic Survey’s National Land Cover Database (NLCD), an existing one-dimensional model of the Mississippi and hydrologic data from several hydrologic monitoring stations for the years 2008-2016. Depth and velocity grids were extracted from the HEC-RAS model for three different discharge conditions; 0.5 mean annual flow (MAF) with 40% exceedance probability, MAF with 80% exceedance probability and 1.5 MAF with 15% exceedance probability were used to develop and categorize physical habitat distribution maps of the study area using ArcGIS. The modeled physical aquatic habitat patches were assessed at three buffer distances of 30 m, 90 m, and 150 m from the RTS. The area Simpson diversity and Jaccard similarity indices were calculated for the different discharge conditions and associated habitat mosaics. The distribution of physical habitat modeling revealed a variation in the pattern of habitat patches between the dike and chevron. For the chevron dike evaluated in this study, very-slow deep habitat patches are created in the inner portion of the chevron and slow deep patches around the exterior of the structure which extend both up and downstream of the structure. The dike created slow-deep habitat patches along the structure, very-slow deep patches on the riverbank edge and fast- deep patches on the river side edge. Evaluation of physical habitat patch diversity in relation to the distance from the RTS revealed the highest diversity index values were found within the first 30 m buffer and generally decrease with distance away from the structure. Comparison of the Jaccard index values in vicinity of the two evaluated RTS suggest the habitat patch diversity are similar for both structures at 0.5 MAF and 1.5 MAF flow conditions (index value ranging between 0.60-0.87). However, for the MAF flow conditions the Jaccard index suggests there is more physical habitat patch diversity in the vicinity of the chevron relative to the dike. The modeling results suggest both physical habitat patch richness and diversity declines with an increase in discharge. The decline in physical habitat patch richness and diversity with discharge conditions were greater for the dike relative to the chevron, thus while the chevron retains more types of habitat patches with increase in discharge the diversity indices are still higher for the dike. The modeling also suggests both RTS have created and maintain shallow water habitat (SHW) and overwintering habitat patches (OWH) for the flow conditions evaluated in this study. These habitat patches are utilized by fish species at various life stages. Larger area of OWH habitats; 30% of total area by dikes and 35% of total area by chevrons are created in comparison to SWH; 10% by dike and 7% by chevron. The modeling results show that both the dike and chevron evaluated in this study are associated with and likely maintain ecologically relevant habitats and substantially contribute to physical habitat diversity. If the physical characteristics of the RTS investigated here are similar to other dikes and chevrons along the Mississippi River, the results of this study supports the secondary management objective for these structures, increase in physical aquatic habitat patch diversity, is likely being achieved.

Indiana University-Purdue University Indianapolis (IUPUI) / Floods are one of the worst disasters in the United States. Each year, the government allocates a tremendous amount of manpower and money on flood prevention initiatives. As the first defense line, levees provide protection from temporary flooding (Makhdoom, 2013). These embankments are broadly classified according to the areas they protect, which could either be urban or agricultural levees within floodplains. In the U.S., most of the levees are handled by government agencies such as the U.S. Army Corps of Engineers and the Federal Emergency Management Services. On the other hand, non-levee embankments created by individual farmers (Olson & Morton, 2013) or naturally formed levee-like structures may not be in the government database. The initial purpose of this research was to assist Polis center on the “Mapping of Non-Levee Embankments in the Indiana” project. The non-levee embankments are not certified or engineered levee-like structures. They, therefore, impose lateral constraints on flood flows, reducing the floodplain storage capacity and increasing the flood velocity. These non-levee embankments can cause stream erosion and downstream flooding. Therefore, it is important to know the locations of these features. The first part of the proposed method adapted the Empirical Bayesian theorem and the low pass filter techniques to extract elevated linear features from LiDAR elevation data – Digital Elevation Model (DEM). The second part of the proposed methods combined the Minimum Bounding Circle (MBC) method and the Youden Index to locate the optimal threshold value that can be used to determine whether the extracted features are levee-like structures. The focus of this study is not only limited to artificial levee-like structures, but also takes the natural levees, or any potential levee-like structures into account because this study assumes all embankments play important roles during flood events.

京都大学 / 0048 / 新制・課程博士 / 博士(工学) / 甲第18560号 / 工博第3921号 / 新制||工||1602(附属図書館) / 31460 / 京都大学大学院工学研究科社会基盤工学専攻 / (主査)教授 中川 一, 教授 藤田 正治, 准教授 川池 健司 / 学位規則第4条第1項該当 / Doctor of Philosophy (Engineering) / Kyoto University / DFAM

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京都大学 / 新制・課程博士 / 博士(工学) / 甲第25253号 / 工博第5212号 / 京都大学大学院工学研究科社会基盤工学専攻 / (主査)教授 川池 健司, 教授 山上 路生, 准教授 米山 望 / 学位規則第4条第1項該当 / Doctor of Philosophy (Engineering) / Kyoto University / DFAM

La plupart des gisements de Ni-Cu sont issus de magmas komatiitique ou tholéiitique associés à des panaches mantelliques. Leur genèse fait intervenir l’exsolution d’un liquide sulfuré immiscible, l’interaction entre les liquides silicaté et sulfuré afin de concentrer ce-dernier en éléments chalcophiles, et l’accumulation du liquide sulfuré en quantités économiques. La saturation en sulfure est généralement atteinte en réduisant la solubilité des sulfures. Celle-ci se fait par assimilation de roches encaissantes siliceuses et/ou sulfurés.Le dyke d’Älgliden de la ceinture de Skellefte, en Suède, contient des sulfures de Cu et Ni dont les quantités ne sont actuellement pas économiques. La minéralisation d’Älgliden est atypique dans la mesure où elle contient d’importantes teneurs en Au, elle a un faible rapport Ni/Cu et enfin est formé dans un contexte de subduction. Le dyke recoupe un gisement porphyrique à Cu-Au contenant des sulfures ce qui laisse suggérer que la minéralisation d’Älgliden est formée par assimilation.Les objectifs de ce projet de recherche étaient d’examiner les processus de formation de la minéralisation d’Älgliden et son potentiel minier ainsi que de mieux comprendre la formation des gisements à Ni-Cu en contexte de subduction. Ce travail inclut l’étude pétrologique du minerai et de ses roches hôtes, la détermination de compositions minérales, l’analyse des éléments majeurs et traces sur roche totale et enfin des analyses des isotopes du soufre. Ce projet a été financé par la compagnie Boliden qui détient le gisement d’Älgliden.Le dyke est composé en majeure partie de norite à olivines, et minoritairement de leucogabbros. Les compositions sur roches totales, les textures magmatiques et les compositions minérales suggèrent que les norites à olivine se sont formées par accumulation d’olivine tandis que les leucogabbros représentent des liquides résiduels avec ou sans cristaux cumulus de plagioclase ± orthopyroxene. Les norites sont interprétées comme étant formées par une ou deux injections de bouillie cristalline suivie de cristallisation fractionnée. Le magma parent des roches d’Älgliden était un basalte hydraté et évolué dont la teneur en MgO est estimé à 6%.Le minerai sulfuré est principalement disséminé à travers l’ensemble de l’intrusion d’Älgliden. Quelques concentrations modérées de minerai se présentent sous la forme de sulfures en réseaux, de veines de sulfures et de sulfures massifs, lesquelles sont spatialement associées aux leucogabbros et aux xénolites de l’encaissant. L’association entre les leucogabbros et les concentrations en sulfures, leur faible teneur en métaux et leur faible rapport Ni/Cu suggèrent que la phase sulfuré s’est exsolvée tardivement au cours de la différentiation magmatique. Ce timing semble défavorable pour la minéralisation d’Älgliden puisqu’il inhibe à la fois l’interaction entre les liquides silicaté et sulfuré et l’accumulation du liquide sulfuré.La contamination du magma d’Älgliden par son encaissant n’est pas corroboré par les concentrations en élément trace et les compositions isotopiques du soufre. En revanche, ces données indiquent que le magma d’Älgliden s’est mis en place dans une zone de subduction où l’on pense que la saturation en sulfure a été atteinte par réduction d’un magma oxydé et riche en élément volatiles, via la cristallisation de magnétite et/ou dégazage. Les valeurs positives de δ34S suggèrent que l’apport de matériel dérivé du slab est responsable du caractère oxydé du magma d’Älgliden.L’état d’oxydation des magmas d’arc leur permet de dissoudre de grandes quantités de S et d’Au. Leur caractère évolué est responsable de leur fortes concentrations relatives en Au et leur faible rapport Ni/Cu. Ainsi, en contexte subduction les sulfures magmatiques sont susceptibles d’avoir ces caractéristiques, et si l’exsolution du liquide sulfuré a lieu plus tôt que dans le cas d’Älgliden cela pourrait conduire à la formation de gisements économiques. / Most major sulfide Ni-Cu deposits originated from komatiitic or tholeiitic magmas that formed in association with mantle plumes. Their genesis involves the segregation of a immiscible sulfide liquid, reaction of the sulfide liquid with silicate melt to upgrade the sulfide in chalcophile elements, and the concentration of the sulfide liquid in economic amounts. Saturation in sulfide is commonly achieved by lowering the sulfide solubility via assimilation of siliceous wall rock or by increasing the S content by adding S-bearing materials.The Älgliden dike in the Skellefte Belt in Sweden contains currently uneconomic Ni-Cu sulfide mineralization. The Älgliden mineralization is atypical insofar as it contains a significant amount of Au, has a low Ni/Cu ratio and formed in a subduction-related geodynamic setting. The host intrusion intrudes sulfide-bearing Cu-Au porphyry mineralization which led to the suggestion that the Älgliden Ni-Cu-Au mineralization was linked to the assimilation of sulfide-bearing wall rocks.The goals of this research project were to investigate the ore forming processes of the Älgliden mineralization and its ore potential, as well as to improve our understanding of the genesis of Ni-Cu deposits in subduction zones. The work is based on a petrological study of the ore and its host rocks, determination of mineral compositions, analyses of major and trace elements in bulk rocks, and sulfur isotope analyses. This was supported by the Boliden company which owns the deposit.The dike is composed mainly of olivine norites with minor leucogabbros. Bulk rock compositions, magmatic textures and mineral compositions suggest that the olivine norites formed by accumulation of olivine and that the leucogabbros represent residual melts with or without cumulus plagioclase ± orthopyroxene. The norites are interpreted to form by one or two injections of an olivine-rich crystal mush and subsequent fractional crystallization. The parental melt of the Älgliden rocks was a hydrous and evolved basalt estimated to contain ≈6 wt.% MgO.The sulfide ore is mainly disseminated throughout the whole Älgliden intrusion. Some weak ore concentrations occur as network to vein and massive sulfides that are spatially associated with the leucogabbros and wallrock xenoliths. The association between the leucogabbros and the concentrations of sulfide, their low ore grade and Ni/Cu ratio suggest that the sulfide segregated late in the differentiation process. This timing appears unfavorable for the Älgliden mineralization because it inhibited both sulfide-silicate liquid interaction and the accumulation of sulfide.Contamination of the Älgliden magma by its wall rocks is not supported by trace element data and S isotope compositions. Instead these data indicate that the Älgliden magma was emplaced above a subduction zone where the sulfide saturation is thought to occur by reduction of the oxidized and volatile-rich magma by magnetite fractionation and/or by degassing. Positive δ34S values suggest addition of slab-derived material which is thought to be responsible for the oxidized character of the Älgliden magma.The oxidation state of arc magmas allows them to carry large amounts of S and Au. Their evolved character is also responsible for their relatively high Au contents and low Ni/Cu. Such characteristics are likely to occur in magmatic sulfide mineralization in subduction zone settings, and if sulfide liquid segregation had occurred earlier than at Älgliden the process may have produced economic sulfide deposits.

Master of Science / Department of Biology / Craig Paukert / I evaluated sampling strategies and the effects of dike structure modifications in the lower Missouri River to better develop sampling and mitigation strategies to protect and enhance native river fishes. Sampling occurred in the lower 1,212 km of the Missouri River during October-June (coldwater season) and June-October (warmwater season) with stationary gill nets (GN), drifted trammel nets (TN), towed otter trawls (OT), and mini fyke nets (MF) from 2003-2006. We compared probabilities of detection (p), variability (coefficient of variation; CV) in catch per unit effort, and lengths for 25 species. Over 80% of adult large-bodied fishes were collected in GN during coldwater, >90% of chub spp. (Macrhybopsis) were collected in OT, and >90% of nine small-bodied and juvenile fishes were collected in MF. Trammel nets never had the highest p during coldwater, but had the highest or equally high p for 85% of adult large-bodied fishes during warmwater. Mean CV was lowest with GN for adult large-bodied fishes; chub spp. had the lowest CV in OT. Mean lengths were typically greater in GN and TN. Large river monitoring programs might best achieve the highest p, lowest variability, and widest size range of fishes by employing GN and OT during coldwater and TN, OT, and MF during warmwater sampling periods. We also compared fish community composition and the probability an un-notched and notched dike structure and channel sand bar (referred to as channel structures) was occupied by various fish species. Few differences in species richness and diversity were evident among channel structures. Notching a dike structure had no effect on proportional abundance for any habitat guild. Catch per unit effort (CPUE) was greater at notched dikes for only three (lake sturgeon Acipenser fulvescens, paddlefish Polyodon spathula, and shovelnose sturgeon Scaphirhynchus platorynchus) of 12 great river species. Occupancy at notched dikes increased for blue catfish Ictalurus furcatus and decreased for blue sucker Cycleptus elongatus, but did not differ for 17 (81%) other species. No distinct increase in occupancy at natural channel sand bars compared to engineered dike structures was evident. Mean CPUE was higher in dike structures than channel sand bars for four great river species (goldeye Hiodon alosoides, lake sturgeon, paddlefish, and shortnose gar Lepisosteus platostomus), but did not differ for ten. Our results suggest dike structures may provide necessary habitats for many fluvial species when compared to channel sand bars, but notching did not increase abundance or occupancy of most native Missouri River fishes.

La façade littorale du Grand Port Maritime de Dunkerque est une cellule sédimentaire quasi-fermée où les formes dunaires résultent de l’imbrication de facteurs humains et naturels. Ce littoral peut être divisé en deux parties : la partie Ouest est constituée d’un cordon bordier sur une longueur de 7 km (plage du Clipon) et le long de la partie Est, la plage est adossée à une digue en enrobé bitumineux de 6 km de long (digue du Braek) où des transferts sableux se produisent. L’objectif de cette étude est de (1) caractériser les formes dunaires et leur évolution sur un site artificiel, (2) quantifier le transport éolien sur le haut de plage, le versant externe de la dune bordière et la digue du Braek, et (3) proposer des mesures de gestion afin de remédier aux contraintes d’exploitation engendrées par les dépôts éoliens sur les infrastructures. A moyen terme (28 ans), l’analyse diachronique de photographies aériennes montre que les superficies dunaires ont fortement augmenté depuis 1983. A court terme (2 ans), des mesures topographiques révèlent que les dunes continuent de se développer aujourd’hui mais gardent la marque des interventions anthropiques passées. Sur la digue du Braek, des formes dunaires se sont naturellement constituées sur l’asphalte. Le sable a été colonisé par Ammophila arenaria qui s’est enraciné sous l’enrobé par l’intermédiaire de fissures. Une typologie de ces dunes de digue a été proposée. A l’Est, des dunes se développent en pied de digue en raison de l’interruption des transferts sédimentaires longitudinaux par une jetée. Des piégeages éoliens in situ ont montré que le transport éolien était essentiellement contrôlé par la vitesse du vent et la source de sable disponible. Par vents frontaux et obliques, les dunes de pied de digue constituent la principale source des envols, et le transport éolien est favorisé par une accélération du vent sur le versant exposé. Différents types de brise-vent ont été testés sur l’ensemble du site afin de trouver le meilleur mode de gestion souple de ces envols de sable. Ces analyses montrent que si la localisation des structures brise-vent a une grande influence sur leur efficacité, les systèmes habituellement utilisés sur les plages (ganivelles, filets synthétiques) peuvent aussi favoriser le développement de dunes sur une digue en asphalte. Les mesures de gestion envisagées sont la stabilisation des principales sources de sable en pied de digue ainsi que le renforcement de la dune bordière aux endroits les plus fragiles. / The coastline of Dunkirk seaport is a sedimentary cell where dune morphology is the result of both natural processes and human intervention. This shoreline can be divided in two parts: a western part of 7 km long, where a macrotidal beach is backed by naturally developing coastal dunes, and an eastern part consisting of a 6 km long asphalt dike overtopped in places by low elevated aeolian dunes. This study aims at (1) describing aeolian dunes and their evolution on a human-altered coast, (2) quantifying aeolian sand transport on the upper beach, the seaward slope of the foredune and the asphalt dike, and (3) suggesting management measures in order to solve windblown sand accumulation problems on harbour infrastructures. On the middle term (28 years), diachronic analysis of aerial photographs shows rapid development of dunes area since 1983. On the short term (2 years), topographic surveys reveal that dune development is still ongoing, although dune morphology keeps the marks of passed human interventions. Dunes have naturally developed on asphalt and their formation is initiated by Ammophila arenaria colonisation of numerous perpendicular cracks in the dike. A typology of these dunes is proposed. Dike toe dunes have developed at the beach/dike contact in the most eastern part of the site, where a jetty is interrupting net sediment transport. In situ field measurements revealed that aeolian sand transport is mainly controlled by wind speed and the source of sand available. Under oblique to direct onshore winds, dike toe dunes are the main source of windblown sand on the dike, and aeolian transport is enhanced by a wind speedup on the windward slope. Different kinds of windbreaks have been tested in order to solve uncontrolled aeolian sand transport problems on the dike, as well as to consolidate foredunes. It appeared from the topographic surveys carried out on the windbreaks that although their location seemed to play a major role on the amount of sand captured, fences and synthetic fabrics deployed on sandy surfaces were also able to trap windblown sand on a seaport dike. Management measures considered are a stabilisation of main sand sources at the dike toe and consolidation of foredunes with windbreaks.

Links between the pond and surrounding land for horticulture is a distinctive feature of farming households in Bangladesh. It was hypothesised that the role of fishponds in integrated aquaculture systems has potential towards improving livelihoods and poverty alleviation. Rural and peri-urban settlements in Mymensingh District, Bangladesh were selected for assessing the importance and role of pond-dike systems on the livelihoods of households of different socio-economic level. The study was carried out in view of the sustainable livelihood approaches of the Department for International Development, U.K. Participation of all levels of stakeholders was ensured in the first and last phase of the study. The combination of quantitative and qualitative analysis at community and household level was a major strength and challenge of the study, and was used to explore the potential of integrated farming and factors that undermine such potential to contribute to a sustainable livelihood. The research commenced with a comprehensive situation appraisal and baseline survey to explore the context and characterize farming systems, followed by a longitudinal household survey to understand the effect of seasons on livelihoods. Households with access to ponds were identified as active or passive integrators based on a simple set of criteria and their resources and livelihoods assessed in comparison with non-pond households. During the last phase of the study a farmer participatory research (FPR) trial, based on a priority issue identified during the 1st phase of the study, was launched to investigate the potential of the integrated systems. The situation appraisal conducted within four communities revealed the effects of gender, well-being and location on farmers' regular activities and food consumption patterns. Fish culture was equally important as an enterprise among richer and poorer men, whereas vegetable cultivation was more important to men than women but wealth and location also affected its importance. Lack of knowledge was a particular problem for farmers growing fish and vegetables in the rural areas. Fish disease, high price of input, lack of money were also identified as constraints by fish producers. The expected use and current use of ponds, problems and benefits associated with fish culture were also found to be affected by groups emphasising vegetable, orchard and fish culture within their systems. The role of the pond for family use, which was a major objective for pond construction, was found to be significantly different between rural and peri-urban areas. Fish culture is now the dominant use of ponds for households irrespective of their focus on vegetable, orchard or fish production and they are utilised less for general domestic use. Ponds are relatively more important as a source of irrigation water in rural than in peri-urban communities. Significant differences were observed between locations and well-being categories for the percentage of fish retained for consumption and that sell. Rice bran was the most commonly used pond input (80% of all pond households) but active integrated farmers applied rice bran more frequently than passive groups (91 compared to 63 times/season). ‘Ease of production’ was a major incentive for farmers to integrate fish and vegetable production and this opinion was related to household type i.e. active integrators were more aware and confident about the practice. The literacy levels of household heads, access to information and capital and contact with formal and informal institutions of active producers and the better-off households was significantly higher than other groups and poorer households respectively. It is revealed from the longitudinal households’ analysis that the consumption pattern in terms of food types and amount are linked with income, expenses and food availability in different well-being categories between seasons across locations. The empirical analysis showed that as active households’ income increased, expenditure on food purchases, agricultural labour, pond inputs and poultry per household also increased. However, on-farm contributions as a source of fish and vegetables were important during the lower income and least productive months. Performance of integrated farming systems varied by location. Resource base, accessibility to market and information played key roles in the development of integrated farming system in the study area. Active integrated households in peri-urban areas, in response to higher demand in the nearby market, produced significantly more fish and vegetables than those in the rural areas. The result showed clearly the need for due consideration of these factors while promoting IAA systems in Bangladesh. Farmer participatory research showed that production of fish could be increased by a substantial level through increasing pond nutrient inputs rather than stocking an additional species (tilapia), although this may be related to the ‘improved’ nutrition used by farmers still being well below the level required for optimal tilapia performance. Rural households benefited more than peri-urban through direct consumption of both fish and vegetables; in contrast peri-urban households benefited more through cash sales of both fish and vegetables than rural households. Higher production did not lead to increased consumption, rather households benefited financially through selling fish. Similar production levels of vegetables between groups followed different levels of fish culture practices suggesting that increased investment in fish production is complementary rather than competitive with associated vegetable production. It could be concluded that considerable potential exists for further integration and development of pond-dike systems, which could contribute towards improved livelihoods of both better off and worse off people.