Dissertações em Geologia e Geoquímica (Mestrado) - PPGG/IG

URI Permanente para esta coleçãohttps://repositorio.ufpa.br/handle/2011/2604

O Mestrado Acadêmico pertence ao Programa de Pós-Graduação em Geologia e Geoquímica (PPGG) do Instituto de Geociências (IG) da Universidade Federal do Pará (UFPA).

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Agora exibindo 1 - 6 de 6

Acesso aberto (Open Access)
Análise comparativa hidroambiental das bacias do Una e da Estrada Nova, em Belém-PA, e suas implicações socioeconômicas
(Universidade Federal do Pará, 2015-03-26) LEÃO, Eduardo Araujo de Souza; ABREU, Francisco de Assis Matos de; http://lattes.cnpq.br/9626349043103626
To evaluate the effectiveness of public interventions in relation to changing social dynamics and improve the quality of life of a population is necessary to the built and application of social indicators in monitoring public management, especially when dealing with large environmental interventions. As much as these indicators are mapped, the vast majority of environmental studies where these interventions occur, the government has dedicated itself or if it does not perform and monitor efficiently the behavior of these indicators over time. In Belém, the floods in urban areas pose a serious problem for most of the municipality, especially when involving densely occupied areas, at which generate considerable damage and often irreparable, even with losses of human lives. Flooding has been a problem during periods of frequent rainfall, both in the oldest areas of the city and consolidated, as in the areas of urban sprawl, a fact compounded by soil sealing, occupation of wetlands and removal of riparian vegetation, which hinders the infiltration rainwater. Due to these environmental factors and the inattention of government in providing social amenities and physical interventions in the area of the metropolis, populations that occupy the most vulnerable parts of the city of Belém, in general have a poor quality of life, as regards the issue of the environment in which they live. In order to comparatively evaluate two different realities and really consider whether public intervention was effective and efficient and from the same include as practical application of social indicators in monitoring the public administration, was used as case for this research performed by government intervention state in the basin of Una, where he was executed the deployment of Macro Drainage Basin of Una and services contemplated drinking water supply, sewerage, storm water drainage and road system, compared with the intervention of the municipal government to bowl Estrada Nova, running, with the deployment of these services. To develop the research, the study gathered data and information collected in the basin of Una and projected future scenarios for the basin of Estrada Nova, using the same indicators. These indicators in this study were also addressed and strengthened with a hydrogeological assessment of the two basins, the analysis of quality of surface and groundwater, consideration of the incidence of waterborne diseases, the vulnerability of aquifers, configured together in a GIS specifically built for it, with the aim of evaluating the criticality of spatialization basins and identify which areas need more attention or have the best results. The study demonstrated that the physical and socioeconomic study of the two basins are similar and after the intervention in the basin of Una, any kind of indicator was monitored with a view to demonstrate the effectiveness of the intervention. The study also showed that health indicators linked to waterborne (why the intervention was also made) chosen for monitoring before and after the intervention, have partially direct connections to the environmental quality of the basin, but many indicators not could be chosen by the lack of government data. The vulnerability of the aquifer top is also concern in some quarters, in that much of the population obtains its supplies from this aquifer, which has its recharge provided, in part, by draining channels of Belém, known holders of very bad quality indices its waters and can even be characterized as true open sewers. The drainage channels and creeks of Belém, are thus responsible for directing this excess sewage into the Bay of Guajará and river Guamá through interconnection with those that have physiographic elements. Because the city has much of its area located in quotas of up to 4 meters, which is also the average annual tidal amplitude regional, these areas are subject to flooding. By way of consequence throughout the upper aquifer is vulnerable to infiltration of contaminated water channels, which in times of floods are dammed increasing the residence time in them,. The research now being evaluated scenarios and presentation indicators, this reality, leaving open the need to be constructed and monitored indicators other than the act of evaluating the effectiveness of public intervention can be more consistent. Finally the study also notes that several indicators could not be considered in the study due to insufficient and the quality of data provided by the government.
Acesso aberto (Open Access)
Aplicação do modelo hidrodinâmico no estuário do rio Caeté (NE do Pará)
(Universidade Federal do Pará, 2007-10-17) ABREU, Marcelo Wanderley Matos de; EL-ROBRINI, Maâmar; http://lattes.cnpq.br/5707365981163429
The northern coast of Brazil is trimmed by a big and complex hydrographic net, where the main river is the Amazon. This river, as well as others smaller, flow into in the Atlantic Ocean finalist the estuaries, that are frequently defined like a stretch of the river, where occurs the interaction of the ocean and fluvial waters (transition zone). The Caeté estuary is inserted at the northeast of Pará (00º43’18" – 00º04’17" S and 46º32’16" – 46º55’11" W) that suffers influence of macro-tides and semi-diurnal with medium amplitude of 5,6 m, coastal currents (mean velocity approximately 0,75 m/s), waves of 0,7 m and Trade winds that possess NE preferential direction with medium speed of 6 m/s. That estuary is situated in a tropical region of humid climate, with annual medium temperature of 27ºC and elevated precipitation with annual medium of 2500 mm/year. In this area, are also showed, the existence of seasons with distinct characteristics: rainy (December to May), dry (June to November) and intermediate. The estuary of the Caeté river is a tide-dominated estuary (as regards the physical process), that forms an extensive coastal plain (as regards the coastal geomorphology) and well mixed (as regards waters circulation).The hydrodynamic circulation in estuary is considered as an important trial and it has a lack of studies in this area until today, principally in the North’s region of Brazil, where still have a few the studies of estuarine modeling. So, for this work were adopted the use of the hydrodynamic model with the Modeling program called SisBAHIA (Environmental Hydrodynamics Base System), aiming the observation of the general aspects of the hydrodynamic circulation in different phases of tide (high tide, low tide, flood and ebb tide) in the Caeté estuary (PA) and like this validate, through the modeling, the facts (current, tides and amplitude of tide) collected in the estuary. The methodology was performed in two phases,( fieldwork and laboratory). The phase of fieldwork consisted of: (1) hoist bathymetric, linked to the Research’s Project of the SET PROGRAM/ CT-Hidro that utilized a cartographic base previously digitalized, having like base a satellite image LANDSAT-ETM+7, beyond a digital ecobatymetric and a DGPS (Differential Global Positioning System); (2) records of elevation of the sea level, through the fixation of two digital tide predictors Orphimedes OTT-Hydrometric, located in the Maguary city, where was observed daily values to each 20 minutes during 7 consecutive days with results varying of a minimum of 0,01 m to a maximum one of 5,08 m and of 0,42 to 5,18 in the point situated in the bridge about the hole of the Maguary and in the Bacuriteua city, respectively; and (3) measure the speed of the shackles utilizing a current predictor Falmouth 2D YMCA in a point inside the model, that stayed coupled to the boat during seven consecutive days and that presented values for the currents varying of a minimum of 2,95 cm/s to a maximum one of 154,59 cm/s. In the laboratory’s phase, was carried out the trial of calibration between the facts of the model with the measurements taken in the fieldwork. They were generated simulations of the hydrodynamics conditions during the flood, ebb tide, half tide flood, half tide ebb tide, and the high value of high tide and low tide, and in the neap and spring tides. Through those simulations were generated superficial maps of currents to see the different standards of circulation.
Acesso aberto (Open Access)
Caracterização hidrogeológica em área de agricultura intensiva, na microbacia do iguarapé Cumaru, nordeste do Pará
(Universidade Federal do Pará, 2003-06-30) CHAVES, Luciene Mota de Leão; TANCREDI, Antonio Carlos Felice Nicola Saverio; http://lattes.cnpq.br/3080055631075788
Acesso aberto (Open Access)
Caracterização hidroquímica dos aquíferos freáticos costeiros na cidade de Salinópolis-PA.
(Universidade Federal do Pará, 2016-06-08) RODRIGUES, Érika do Socorro Ferreira; CORRÊA, José Augusto Martins; http://lattes.cnpq.br/6527800269860568
The city of Salinópolis is located in northeast Pará, Bragantina region, on Pará State. The geology of the area is characterized by a sedimentary cover Tertiary represented by Pirabas Formation , Barreiras Group and overlying these rocks may occur sandy-clay sediments to clay-sand the quaternary called Pós -Barreiras sediments. The main hydrogeological systems Salinópolis, in general, are: a) upper aquifer system developed in the Pós-Barreiras, unconfined aquifers; b) aquifer system Barreiras, unconfined aquifers and semi-confined; c) aquifer system Pirabas, deeper confined aquifers, which is an outcropping aquifer in the region. For the study were registered 22 wells of which 17 shallow wells with depths up to 30 m (PT), two dug wells (AM) and 3 sources (FT). The collection of samples was performed at intervals of two months for a full hydrological cycle, May 2014 to March 2015. The main quality parameters investigated were water temperature, pH, electrical conductivity, alkalinity, total dissolved solids and main ions : cations (Na+, K+, NH4+, Ca2+, Mg2+) and anions (F-, Cl-, NO3- and SO42-). Hydrochemical four groups were identified in the Piper diagram: group 1 (SO4-, Cl- and Na+) that resembles the aquifer Barreiras. In the waters of group 3 rich in calcium and bicarbonate is identified with the Pirabas water aquifer (HCO3- and Ca2+) since the water in groups 2 and 4 showed characteristics of group 1 and 3. From Piper diagrams, it was observed that with increasing water recharge the group 2 and 4 water had a water connection behavior, migrating to another group hydrochemical. In Scholler diagram, even identifying the main ions was possible to see that there are mixtures in water of the same hydrochemical group, visualized by the provision in fan. In Diagram Van Wirdum was identified climate and rocks actions on the aquifers hydrochemistry. Range distribution has been observed that with the beginning of the drought wells located in car washes and near gas stations as well as near the beach and estuarine rivers showed an increase of ions dissolved in the water. As well as in natural sources or springs there was a large increase in number of ions, especially the sulfate Climate Influence, rock, ocean waters, estuarine rivers, as well as the contribution of the aquifer Barreiras and Pirabas showed a peculiar hydrochemical composition in the waters of aquifers shallow coastal city in Salinópolis.
Acesso aberto (Open Access)
Contribuição ao conhecimento das formações Barreiras Pirabas utilizando-se ferramentas da análise estrutural com vistas à aplicação em hidrogeologia
(Universidade Federal do Pará, 2016-10-17) SILVA, Larissa Silva e; ABREU, Francisco de Assis Matos de; http://lattes.cnpq.br/9626349043103626
The existence of hydraulic connection between Barreiras and Pirabas aquifers systems in the northeast area of the State of Pará, more specifically in the metropolitan region of Belém - RMB has been raised, a few years ago, by different authors from the application of various analytical techniques. This work presents further contribution to this theme, that has been aggregated to the data and to the information obtained from the use of structural analysis tools, to understand the groundwater flow mechanism and recharge conditions, which takes place in area under consideration. The work was performed from the databases on existing wells in private and public agencies. The performed structural analysis considered the geometric-kinematic elements present in the mentioned water systems and it advanced in the knowledge of the tectonic processes that have led to the conformation of the geometric arrangement present in the area, considered essentially as neotectonic. It was found that the development of brittle tectonic structures, especially holes, printed on regional rocks that enclose the water systems, leading to spatial composition of morpho-structural blocks arrangements horsts and grabens limited preferably by the NE and SW discontinuities resulting from the interaction of normal faults with strike-slip faults. The boundaries of these blocks, always marked by failures allow the interconnection of the movement of water from aquifers of different spatial positions systems, sustained by the principle of communicating vessels, the elapsing the mixture of water contained in each one of them individually. So it is impossible to keep the model advocated by several authors in the literature of regional aquifer confinement. On the other hand, the development of potentiometric maps and flow in regions of sedimentary rocks, where it is called homogeneous media, as this case is of the RMB cannot be done without considering the structural analysis, geometry and kinematics, otherwise it would be misunderstood in the preparation of such results and mistaken hydrogeological interpretation. Thus, it is necessary to review the methodologies for the preparation of these important instruments in order to obtain more precise results on the flow mechanisms, recharge and discharge of water systems which has been developed and answered in this work.
Acesso aberto (Open Access)
Influência da sazonalidade sobre as águas estuarinas dos furos da ilha de Colares (baía do Marajó)
(Universidade Federal do Pará, 2014-12-17) GUIMARÃES, Robledo Hideki Ebata; EL-ROBRINI, Maâmar; http://lattes.cnpq.br/5707365981163429
The characterization of surface and interstitial waters in estuaries is critical to unravel the environmental conditions, environmental quality and seasonal changes, which may occur in smaller space such as the hole in the island of Colares. This work aims to show the influence of seasonality in estuarine waters in the north and south of the mouth of the hole island of Colares and the contribution of pore waters to surface waters. The physical and chemical parameters and nutrients are included: rainfall (IP), temperature, salinity, pH, electrical conductivity, total dissolved solids, suspended particulate matter, dissolved oxygen, Secchi depth, nitrate, nitrite, N-ammonia, phosphate, silicate and sulfate. The determination of these parameters occurred simultaneously in each mouth of the hole necklaces over a tidal cycle (13 hours) in rainy (04/10/2013) and drier (10/05/2013) periods. The results show that seasonality affects abiotic conditions of estuarine waters bore the island of Colares and deduces that P1 is the most important factor to effect the changes of physical and chemical parameters, and especially the higher charge mobility, availability and distribution of dissolved nutrients, which were found in higher concentrations in the rainy season. Although the nutrients nitrate and N-ammonia were considered very high at the mouth North, possibly related to the influence of anthropogenic activities. However were considered within the limits established by CONAMA Resolution 357/05. Mouth occurred in South pH levels outside the standard stipulated by Resolution CONAMA, but the phenomenon was considered natural since in this specific is distant from anthropogenic activities. In less rainy period the N-ammonia was found to be absent in mouth North and South. The mangrove was considered as a source of salinity, silicate and sulfate to surface waters.

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