A presente pesquisa está centrada na interpretação das análises de palinofácies e de geoquímica orgânica realizadas em três perfis sedimentares (T1, T2 e T3) de zonas úmidas continentais influenciadas por diferentes regimes hidrológicos na faixa climática subtropical durante o Quaternário no sul do Brasil (Estado do Rio Grande do Sul) com o principal objetivo de demonstrar a utilidade dessas análises para a obtenção de dados paleoclimáticos e paleoambientais. A análise de palinofácies realizada nos testemunhos T1-Mina do Museu (7.963 anos antes do presente - AP) e T2-Mina Modelo (9.542 anos AP), provenientes de Ametista do Sul, e no testemunho T3-Iraí (10.586 anos BP), proveniente de Iraí, revelou um amplo domínio do Grupo Fitoclasto. Os Palinomorfos são o segundo grupo dominante e o Grupo Produto Amorfo é o menos abundante. Esse tipo de análise foi particularmente eficaz para as interpretações dos eventos de precipitação e de sucessão vegetacional em Ametista do Sul, porque o isolamento hidrológico desses alagados efêmeros de altitude torna-os muito sensíveis aos efeitos climáticos. As flutuações na profundidade da água foram inferidas a partir das concentrações dos elementos autóctones (especialmente Botryoccocus e outras algas), que predominam nos intervalos basais e tendem a diminuir progressivamente em direção ao topo. Pseudoschizaea, por sua vez, parece atuar como um marcador biológico de intervalos de transição. O aumento da frequência e da variedade dos esporomorfos terrestres nas camadas mais superficiais indica um aumento da diversidade vegetal e está relacionado ao processo de evolução sucessional da área. Para Ametista do Sul, os resultados permitiram determinar que as oscilações nos padrões de umidade resultaram em um padrão intermitente do nível de água dos alagados, o qual pode representar um reflexo de mudanças climáticas regionais ou, talvez, de mudanças em escala global relacionadas com os “eventos Bond”. Em Iraí, a fração orgânica melhor representada é constituída por elementos derivados de plantas terrestres, uma característica típica da matéria orgânica preservada em turfeiras Esse tipo de ambiente úmido nunca chegou a secar completamente, uma vez que os teores de umidade eram subsidiados por diferentes fatores, tais como o nível do lençol freático, as inundações do Rio Uruguai e a água da chuva. A ocorrência muito baixa de algas, contudo, indica que a profundidade da água não era suficientemente espessa para o desenvolvimento da biomassa algálica, embora o ambiente anóxico e redutor também possa ter limitado a expansão deste grupo. Os parâmetros organogeoquímicos foram particularmente úteis para interpretações de eventos de anoxia e de mudanças nos regimes hidrológicos dos sedimentos turfosos. Os teores de carbono orgânico total (COT) e enxofre total (ST) são mais altos na porção basal do perfil, diminuindo em direção ao topo, e podem estar relacionados ao regime hidrológico ou à interferência antrópica na dinâmica da paisagem. O teor anômalo de enxofre observado em uma das amostras de Iraí pode ser devido a uma fonte externa e talvez relacionado com a presença de fontes termais na região. A presente pesquisa tem potencial como uma referência moderna capaz de ser aplicada na reconstrução de paleoambientes continentais análogos associados a regiões alagadas em cinturões subtropicais. / The present research focuses on the interpretation of the palynofacies and organic geochemistry analyses performed on three sedimentary cores (T1, T2 and T3) from continental wetlands influenced by different hydrological regimes in the sub-tropical climatic belt during the Quaternary in southern Brazil (Rio Grande do Sul State), with the main goal of demonstrating the usefulness of these analyses for obtaining paleoclimatic and palaeoenvironmental data. Palynofacies analysis was performed for the cores T1-Mina do Museu (7963 years before present - BP) and T2-Mina Modelo (9542 years BP) from Ametista do Sul, and for the T3-Iraí core (10586 years BP) from Iraí and revealed a high dominance of the Phytoclast Group. The Palynomorph is the second most dominant group and the Amorphous Product is the least abundant group. This kind of analysis was particularly effective in the interpretations of rainfall events and vegetation succession in Ametista do Sul, because the hydrological isolation renders the ephemeral ponds at high altitude highly sensitive to climatic effects. The fluctuations in the water depth are inferred from the concentration of the autochthonous elements (especially Botryoccocus and other algae), which predominate in the basal intervals and tend to decrease progressively towards the top. Pseudoschizaea, in its turn, appears to act as a biological marker for transitional intervals. The increasing frequency and variety of the terrestrial sporomorphs in the topmost interval indicate an increased vegetal diversity and is most likely related to the process of successional evolution of the area. For Ametista do Sul, the results allowed to determine that the oscillations in the moisture pattern resulted in the intermittent feature of pond water level and this may reflect the regional climate changes or perhaps the global scale changes related to the Bond events. In Iraí, the better represented organic fraction consists of elements derived from terrestrial plants, a characteristic typical of organic matter preserved in peat bogs. This kind of wetland never dried completely, since the moisture content was subsidized by different factors, such as the groundwater, the flood events of the Uruguay River and the rainfall water. The very low occurrence of algae, however, indicates that the water was not deep enough for the development of algalic biomass, although the anoxic, reducing environment may also have limited the expansion of this group. The organic geochemistry parameters were particularly useful for interpretation of anoxia events and changes of hydrological regimes in the peaty sediment. The total organic carbon (TOC) and the total sulfur (TS) contents are higher in the basal portion of the profile, decreasing towards the top and could be linked to hydrologic regimes or to anthropogenic interference in the landscape dynamics. The anomalous TS content observed in one of the samples from Iraí might be due to an external source and perhaps related to the presence of thermal springs in the region. The present research has potential as a modern reference that can be applied in the reconstruction of past analogous continental paleoenvironments associated to wetland areas in subtropical belts.

Urbanization involves the conversion of natural areas to impervious surfaces, which can lead to an increase in the frequency and severity of flood events in cities. To mitigate flood risk, stormwater ponds are constructed to manage urban runoff. Stormwater ponds can also be colonized by wildlife, but their suitability as habitat is disputed due to potential toxicological risks. This study assessed the suitability of stormwater ponds as habitat for the bioindicators Odonata (dragonflies and damselflies) and determined environmental factors that impact their community structure. Odonata (adults, nymphs and exuviae) were sampled at 41 stormwater ponds and 10 natural reference ponds across the National Capital Region of Canada, with a subset of ponds sampled over four years (2015-2018). Plant communities, water quality and surrounding land cover were analyzed at each pond to determine their impacts on Odonata community structure. Overall, stormwater ponds had lower Odonata abundance and a greater variation in species richness and community structure compared to natural ponds but had comparable dragonfly reproduction rates. Plants were the most significant driver of Odonata communities, as stormwater ponds with a high richness of native wetland plants had higher Odonata abundance and community structures similar to natural ponds. Water quality was the second most important driver of Odonata communities with dragonflies showing greater sensitivity to urban contaminants than damselflies. While stormwater ponds had higher concentrations of trace elements than natural ponds (e.g. Ni, V, As), concentrations were generally below toxic levels for all elements except copper and chloride, the latter likely an input from winter road salting. Surrounding land cover was the least important factor affecting Odonata communities. In conclusion, this research demonstrated the importance of local-scale factors related to plants and water quality in sustaining Odonata communities and specifies recommendations for stormwater pond design and maintenance that enhance urban biodiversity.

Coal seams are commonly associated with poor quality water that requires treatment. Water treatment can be very expensive and can severely affect the profitability of mining projects. This study investigated the potential cultivation of Arthrospira maxima (Spirulina) in coal seam water to beneficiate coal seam water in order to effectively offset the water treatment cost. The study was conducted in Northern South Africa and formed part of a larger Coal Seam Water Beneficiation Project (CSWBP). The study consisted of laboratory based Flask Studies and outdoor High Rate Algal Pond Studies. The Flask Studies that were carried out in the on-site field laboratory, found that the coal seam water could provide a suitable medium for Spirulina cultivation. In addition, it was found that the optimal pH for the selected strain ranged between 9 - 10.5 and that the addition of excess iron, up to 100 times the concentration found in defined growth media such as Schlösser’s, to the culture media could enhance productivity. The High Rate Algal Pond Studies (HRAP) were carried out over a period of 18 months. The studies showed that the coal seam water at the CSWBP is a valuable resource that can reduce media costs by 50% without affecting productivity. In a study encompassing 334 days it was shown that heating the culture through plate heat exchangers would result in a significant increase in productivity and a heated productivity of 19.86 g/m2/day was recorded. An unheated productivity of 14.11 g/m2/day was recorded. Therefore, it was found that it would be economically feasible to beneficiate coal seam water found at the CSWBP through the cultivation of Arthrospira maxima (Spirulina). / Environmental Sciences / M. Sc. (Environmental Science)

This interdisciplinary project offers new insights into the reclamation history of two of the most controversial and contaminated sites in Canadian history: the Sydney tar ponds and coke ovens and the Athabasca oil sands. It argues that Canada’s natural resource-dependent economy, combined with jurisdictional uncertainty, created a hesitant, fragmentary site cleanup regime, one that left room for different ideas about landscapes to shape and even distort reclamation’s goals and processes. In the absence of substantive reclamation standards and legislation, researchers struggled to accommodate the unique challenges of the oil sands during the 1960s and 1970s. Ambitious goals for reclamation faltered, and even the most successful examples of oil sands reclamation differed significantly from the pre-extraction environment; reclamation was not restoration. Planners envisioned transforming northeastern Alberta into a managed wilderness and recreation nirvana, but few of these plans were realised. The Sydney tar ponds experience suggests that truly successful reclamation cannot exist unless past injustices are fully acknowledged, reparations made, and a more complete narrative of contamination and reclamation constructed through open deliberation. Reclamation, after all, does not repair history; nor can it erase the past. Effective oil sands reclamation, then, requires a reconsideration of the site’s past and an acknowledgement of the perpetuated vulnerabilities and injustices wrought by development and reclamation.

Title: Educational projects focused on the area of Milíčov forest and ponds. This graduation thesis deals with project education in the field of natural monument Milíčov forest and ponds. It directly borders with southern city housing estate. Result of this work is a collection of materials focusing on environmental education and upbringing pupils on 2nd stage of basic schools, which are located near this monument. These are mainly a methodology for teachers, manual to the project education, worksheets for pupils and creative solution of worksheets for teachers. The starting point for creating projects has been a partial study, questionnaire and open discussion with students. Teoretical part at its beginning describes general conservation and special nature protection, to place issues in a boarder context. The historical aspect is also mentioned. In the thesis are also defined Milíčov forests and ponds characteristics, taking into account their rarities. It is mainly dealt with occurring of important species and specially protected species in this area. In my work is also given the emphasis on the General educational program, environmental education, analysis of schoolbooks and organizational forms of teaching. I bear on didactic theory of which I issued in projects creating. Keywords: General...

No description available.

From the Proceedings of the 1973 Meetings of the Arizona Section - American Water Resources Assn. and the Hydrology Section - Arizona Academy of Science - May 4-5, 1973, Tucson, Arizona / Five livestock watering ponds on the walnut gulch experimental watershed were instrumented to evaluate the use of these ponds as a method for comparing rainfall amounts with runoff sediment volumes. Pond drainage area, vegetative cover, soil type, percent slope, and years of record were tested. Instrumentation consisted of water level recorders, and a topographic survey of each stock pond to ascertain its storage capacity. The results to date have been insufficient to reach definite conclusions due to instrumentation and surveying problems, and because of the natural variability of thunderstorm rainfall. Since most of these problems have now been corrected, future data should yield valuable hydrologic data for semiarid rangelands by means of these instrumented stock ponds.

From the Proceedings of the 1977 Meetings of the Arizona Section - American Water Resources Assn. and the Hydrology Section - Arizona Academy of Science - April 15-16, 1977, Las Vegas, Nevada / With the advent of ever -increasing energy needs, large-scale surface mining has gained new impetus, and there is much concern about reclaiming the mine spoils to bring about beneficial land uses. This paper presents a decision making algorithm labeled PROTRADE, and a case study of the Black Mesa region in Northern Arizona. PROTRADE considers a set of objective functions, a set of physical constraints, articulates the preferences of the decision maker in a progressive manner, and generates a set of alternative solutions. The decision maker is then able to trade level of achievement, for each objective function, against the probability of achieving that level.

From the Proceedings of the 1978 Meetings of the Arizona Section - American Water Resources Assn. and the Hydrology Section - Arizona Academy of Science - April 14-15, 1978, Flagstaff, Arizona / Surface mining of coal in the western U.S. can cause problems of increased salinity and heavy metal contamination in runoff along with a lack of enough rainfall to sustain plant growth for reclamation. To facilitate the planning of reclamation efforts in such areas results are described of a water quality sampling experiment on the ponds and runoff at the University of Arizona Experimental Watershed on Black Mesa in northern Arizona. A systems theoretic framework is employed to model the watershed and the results of a computer simulation based on this model is used to indicate that salinity buildup could be expected over time, given a minimal change in watershed configuration, with possible development of fluoride contamination being of particular concern. Water quality tests of the pond water and runoff on Black Mesa indicated that the water is within Federal standards for drinking and irrigation, except for sodium and fluoride. It is suggested that if it is economically desirable, the collection of more data on the ponds could be used to develop a simulation model of pond subsystems along the lines of the methodology outlined in this analysis.

Reclamation on the Cardinal River and Gregg River coal mines includes the construction of mine pit lakes connected to stream environments. Key physical, chemical and biological parameters of these “truck and shovel” lakes and their streams were investigated, and hypotheses regarding ecosystems and populations were tested. Findings include: Sphinx Lake and Pit Lake CD exhibit meromictic (partial-mixing) tendencies, but still function in a similar fashion to shallower, natural sub-alpine lakes. Elevated selenium concentrations as high as 16 ug/g (dry weight) were recorded in Rainbow trout (Oncorhynchus mykiss) eggs taken from gravid Sphinx Lake and Pit Lake CD fish. Potential detrimental effects associated with the bioaccumulation of selenium on fish reproduction were not observed. Stream water temperatures downstream of Sphinx Lake and Pit Lake CD were significantly warmer than in inlet streams and streams without pit lakes. Streambed concretions caused by calcite precipitation were documented and found to affect portions of the upper Gregg River basin. Remediation of this concretion is important for sustainability of trout populations. Aquatic communities including fish, invertebrates, zooplankton and aquatic plants are present in these pit lake systems. Athabasca Rainbow trout populations are self-propagating (spawning at the outlets) with higher densities downstream than there were prior to lake reclamation. The development of sub-alpine mine-pit lakes connected to the stream environment appears to be an appropriate and beneficial reclamation technique in this area. / xvi, 224 leaves : col. ill., map ; 28 cm