Estimativa espaço-temporal da superfície potenciométrica do sistema aqüífero guarani na cidade de Ribeirão Preto (SP), Brasil

Pós-graduação em Geociências e Meio Ambiente - IGCE

Caracterização da radioatividade das águas do aquífero Guarani

This research aimed to evaluate the quality of “Aquifer Guarani’s” waters in the context of the current legislation related to the radioactive aspects, besides correlating the values obtained with chemical data already available, seeking to make an integrated analysis of the data in order to establish possible tendencies with directions of underground flow. The determinations of the total radioactivity beta and alpha were accomplished through the employment of the available infrastructure at the LABIDRO – Laboratory of Isotope and Hydrochemistry of the Petrology and Metallogeny of UNESP’s Institute of Geosciences and Exact Sciences, largely implanted through resources supplied by FAPESP and CNPq. The systems were gauged for the determinations of interest with tracer of known activity. Preliminaries tests were accomplished with high radioactivity samples of water to check the applicability of the methods. It was ended that the waters analyzed possess low radioactivity, as much alpha as total beta, and, therefore, they are appropriate for the human consumption; that there is not lineal relationship between the obtained data and the chemical data already available; and that the direction of the underground flow of the Aquifer doesn't check any tendency to the generated data.

Cuidado à saúde de crianças Kaiowá e Guarani: notas de observação de campo

Inicia-se uma discussão sobre as práticas de saúde e cuidado utilizadas pelos Kaiowá e Guarani da Terra Indígena de Caarapó no enfrentamento das doenças diarréicas na infância. Utilizou-se de uma contribuição etnográfica, através do uso da técnica da observação participante e de entrevistas aberta com moradores da comunidade. Em se tratando de uma sociedade que vivencia permanentes transformações de ordem social advindas das relações interétnicas e da sucessiva presença dos serviços de saúde, observa-se que o significado de diarréia infantil, assim como as decisões relativas à prevenção e ao seu tratamento, refletem comportamentos diferenciados e complexos. A diarréia, também conhecida como chiri, é definida através de sinais que, de certa forma, são semelhantes aos biomédicos. No entanto, nem sempre as explicações de causalidade e as formas de tratamento seguem, unicamente, a abordagem biomédica. A variedade de causas da doença diarréica entre as crianças indígenas implica na escolha do processo terapêutico, que pode ser desde a procura por um especialista tradicional, realização de chás e infusões e, ainda, procura pelos serviços de saúde. Tais explicações e formas de tratamento pressupõem a existência de um processo de negociação entre pessoas de uma mesma cultura e de culturas distintas. Neste sentido, os serviços de saúde ao tratar a criança com diarréia, devem considerar não apenas a perspectiva biomédica, mas também dialogar com a percepção e as práticas indígenas na identificação da causalidade, na definição do diagnóstico e do tratamento, sobretudo, pela coexistência destas práticas no contexto local

Groundwater waves in a coastal aquifer: A new governing equation including vertical effects and capillarity

Groundwater waves, that is, water table fluctuations, are a natural phenomenon in coastal aquifers. They represent an important part of the interaction between the ocean and aquifer and affect the mass exchange between them. This paper presents a new groundwater wave equation. Because it includes the effects of vertical flows and capillarity, the new equation is applicable to both intermediate-depth aquifers and high-frequency waves. Compared with the wave equation derived by Nielsen ed al. [1997], the present equation provides a closer representation of groundwater waves. In particular, it predicts high-frequency water table fluctuations as observed in the field. A validation of the new equation has been carried out by comparing the analytical solutions to it with predictions from direct simulations using the numerical model SUTRA. The effects of various physical parameters and their relative importance are also discussed.

Tidal fluctuations in a leaky confined aquifer: Dynamic effects of an overlying phreatic aquifer

Tidal fluctuations in a leaky confined coastal aquifer are damped significantly due to leakage into an overlying phreatic aquifer. Jiao and Tang [1999] presented an analytical solution to a simple model describing this phenomenon. Their solution assumes that the tidal fluctuations in the overlying phreatic aquifer are negligible (i.e,, a static phreatic aquifer), Here we examine dynamic effects of the overlying aquifer based on a new approximate analytical solution. The numerical results indicate that the dynamic effects can be significant for a relatively large leakage and a high transmissivity of the phreatic aquifer.

Sudden drawdown and drainage of a horizontal aquifer

Drainage of a saturated horizontal aquifer following a sudden drawdown is reanalyzed using the Boussinesq equation. The effect of the finite length of the aquifer is considered in detail. An analytical approximation based on a superposition principle yields a very good estimate of the outflow when compared to accurate numerical solutions. An illustration of the new analytical approach to analyze basin-scale field data is used to demonstrate possible field applications of the new solution.

Analytical solution for tidal propagation in a coupled semi-confined/phreatic coastal aquifer

An analytical solution is derived for tidal fluctuations in a coupled coastal aquifer system consisting of a semi-confined aquifer, a thin semi-permeable layer and a phreatic aquifer. Based on the solution, we study the interactions (via leakage) between the confined and unconfined aquifers in response to tides. The results show that, under certain conditions, leakage from the confined aquifer can affect considerably the tidal water table fluctuation in the phreatic aquifer and vice versa. Ignoring these effects could lead to errors in estimating aquifer properties based on tidal signals. (C) 2002 Elsevier Science Ltd. All rights reserved.

Tidal fluctuations in a leaky confined aquifer: localised effects of an overlying phreatic aquifer

Damping of tidal head fluctuations in a leaky confined coastal aquifer is enhanced by leakage into an overlying phreatic aquifer. We show that the phreatic aquifer is, however, resistant to the leakage flow and in particular, a deep phreatic aquifer can reduce the leakage effects significantly. An analytical solution, based on a vertical flow model for the phreatic aquifer, is derived for quantifying the role of this upper free water body in tidal propagation in the lower semi-confined aquifer. (C) 2002 Elsevier Science B.V. All rights reserved.

Spring-neap tide-induced beach water table fluctuations in a sloping coastal aquifer

Predictions of water table fluctuations in coastal aquifers are needed for numerous coastal and water resources engineering problems. Most previous investigations have been based on the Boussinesq equation for the case of a vertical beach. In this note an analytical solution based on shallow water expansion for the spring- neap tide- induced water table fluctuations in a coastal aquifer is presented. Unlike most previous investigations, multitidal signals are considered with a sloping coastal aquifer. The new solution is verified by comparing with field observations from Ardeer, Scotland. On the basis of the analytical approximation the influences of higher- order components on water table elevation are examined first. Then, a parametric study has been performed to investigate the effects of the amplitude ratio (lambda), frequency ratio (omega), and phases (delta(1) and delta(2)) on the tide- induced water table fluctuations in a sloping sandy beach.

Tidal influence on behaviour of a coastal aquifer adjacent to a low-relief estuary

The tidal influence on groundwater hydrodynamics, salt-water intrusion and submarine groundwater discharge from coastal/estuarine aquifers is poorly quantified for systems with a mildly sloping beach, in contrast to the case where a vertical beach face is assumed. We investigated the effect of beach slope for a coastal aquifer adjacent to a low-relief estuary, where industrial waste was emplaced over the aquifer. The waste was suspected to discharge leachate towards the estuary. Field observations at various locations showed that tidally induced groundwater head fluctuations were skewed temporally. Frequency analysis suggested that the fluctuation amplitudes decreased exponentially and the phase-tags increased Linearly for the primary tidal signals as they propagated inland. Salinisation zones were observed in the bottom part of the estuary and near the beach surface. Flow and transport processes in a cross-section perpendicular to the estuary were simulated using SEAWAT-2000, which is capable of depicting density-dependent flow and multi-species transport. The simulations showed that the modelled water table fluctuations were in good agreement with the monitored data. Further simulations were conducted to gain insight into the effects of beach slope. In particular the limiting case of a vertical beach face was considered. The simulations showed that density difference and tidal forcing drive a more complex hydrodynamic pattern for the mildly sloping beach than the vertical beach, as well as a profound asymmetry in tidally induced water table fluctuations and enhanced salt-water intrusion. The simulation results also indicated that contaminant transport from the aquifer to the estuary was affected by the tide, where for the mildly sloping beach, the tide tended to intensify the vertical mass exchange in the vicinity of the shorelines, (c) 2005 Elsevier B.V. All rights reserved.

Confined-unconfined flow in a horizontal confined aquifer

Mixed confined and unconfined groundwater flow occurs in a bounded initially dry aquifer when the hydraulic head at the side boundary suddenly rises above the elevation of the aquifer's top boundary. The flow problem as modelled by the Boussinesq equation is non-trivial because of the involvement of two moving boundaries. The transformed equation (based on a similarity transformation) can, however, be dealt with more easily. Here, we present an approximate analytical solution for this flow problem. The approximate solution is compared with an 'exact' numerical solution and found to be a very accurate description for describing the mixed confined and unconfined flow in the confined aquifer. (C) 2002 Elsevier Science B.V. All rights reserved.

Water table waves in an unconfined aquifer: Experiments and modeling

[1] Comprehensive measurements are presented of the piezometric head in an unconfined aquifer during steady, simple harmonic oscillations driven by a hydrostatic clear water reservoir through a vertical interface. The results are analyzed and used to test existing hydrostatic and nonhydrostatic, small-amplitude theories along with capillary fringe effects. As expected, the amplitude of the water table wave decays exponentially. However, the decay rates and phase lags indicate the influence of both vertical flow and capillary effects. The capillary effects are reconciled with observations of water table oscillations in a sand column with the same sand. The effects of vertical flows and the corresponding nonhydrostatic pressure are reasonably well described by small-amplitude theory for water table waves in finite depth aquifers. That includes the oscillation amplitudes being greater at the bottom than at the top and the phase lead of the bottom compared with the top. The main problems with respect to interpreting the measurements through existing theory relate to the complicated boundary condition at the interface between the driving head reservoir and the aquifer. That is, the small-amplitude, finite depth expansion solution, which matches a hydrostatic boundary condition between the bottom and the mean driving head level, is unrealistic with respect to the pressure variation above this level. Hence it cannot describe the finer details of the multiple mode behavior close to the driving head boundary. The mean water table height initially increases with distance from the forcing boundary but then decreases again, and its asymptotic value is considerably smaller than that previously predicted for finite depth aquifers without capillary effects. Just as the mean water table over-height is smaller than predicted by capillarity-free shallow aquifer models, so is the amplitude of the second harmonic. In fact, there is no indication of extra second harmonics ( in addition to that contained in the driving head) being generated at the interface or in the interior.

Educação escolar Tupinikim e Guarani : experiências de interculturalidade em aldeias de Aracruz, no Estado do Espírito Santo

A pesquisa analisa as relações entre interculturalidade, práxis e educação escolar indígena Tupinikim e Guarani do município de Aracruz, Espírito Santo, Brasil. Investiga a práxis da educação intercultural no espaço da educação escolar indígena como meio de revitalização das culturas Tupinikim e Guarani. Objetiva problematizar a formação inicial e continuada dos professores indígenas; discutir a práxis da interculturalidade no contexto da educação escolar indígena; e, identificar outros espaços educativos da cultura e educação indígena. Analisa aspectos teóricos e práticos sobre cultura (WILLIAMS, 2008; BRANDÃO, 1989; FORQUIN, 1993; CANDAU, 2011; GEERTZ, 1989), interculturalidade (D‘AMBROSIO,1996; FLEURI, 2002; 2003; SCANDIUZZI, 2009;), identidade e alteridade (MELIÁ, 2000; FREIRE, 1981; 1987; LITAIFF, 2004) e práxis (FREIRE, 1989; VÁSQUEZ, 2011; SEMERARO, 2006) e educação (escolar) indígena de acordo com a legislação vigente. Realiza pesquisa interpretativa (GEERTZ, 1989) na educação escolar indígena junto aos professores indígenas Guarani das Aldeias de Boa Esperança e Três Palmeiras (2009-2010) e professores indígenas Tupinikim da Aldeia de Comboios (2011-2013) na perspectiva de um diálogo intercultural. Contribuem nos processos investigativos para produção, sistematização e análise de dados a realização de observações, entrevistas semiestruturadas, registros no caderno de campo, fotografias, gravações em áudio e em vídeo e análise documental sobre a educação escolar indígena de Aracruz. (ANDRÉ, 2007; GIL, 1999; 2004). Os resultados deste trabalho levantam questões relativas a duas realidades de educação escolar nas comunidades indígenas pesquisadas que se constituem em aspectos de sobrevivência e desencadeia formas para interagir e reagir em defesa de sua identidade e dignidade. Nesse sentido, a escola é um local de vivências e de encontro, vista e sentida pelas lideranças e pela comunidade como uma possibilidade real para desenvolver um elo entre as formas tradicionais de vida e as formas contemporâneas. O desafio de garantir uma escola nestes termos significa concretizar a proposta de um projeto de educação escolar para os povos indígenas, constituído por especificidades de como trabalhar a terra, pelo reconhecimento de suas tradições, das línguas e da memória coletiva. Distante de apresentar respostas conclusivas propõe uma educação escolar, coletiva e participativa, que critica e dialoga com todos os envolvidos no processo educativo.