Hydrogeology and hydrochemistry of the aquifer systems of Kuttanad area, Kerala: Their role in understanding the evolution of groundwaters

This is an attempt to understand the important factors that control the occurrence, development and hydrochemical evolution of groundwater resources in sedimentary multi aquifer systems. The primary objective of this work is an integrated study of the hydrogeology and hydrochemistry with a view to elucidate the hydrochemical evolution of groundwater resources in the aquifer systems. The study is taken up in a typical coastal sedimentary aquifer system evolved under fluvio-marine environment in the coastal area of Kerala, known as the Kuttanad. The present study has been carried out to understand the aquifer systems, their inter relationships and evolution in the Kuttanad area of Kerala. The multi aquifer systems in the Kuttanad basin were formed from the sediments deposited under fluvio-marine and fluvial depositional environments and the marine transgressions and regressions in the geological past and palaeo climatic conditions influenced the hydrochemical environment in these aquifers. The evolution of groundwater and the hydrochemical processes involved in the formation of the present day water quality are elucidated from hydrochemical studies and the information derived from the aquifer geometry and hydraulic properties. Kuttanad area comprises of three types of aquifer systems namely phreatic aquifer underlain by Recent confined aquifer followed by Tertiary confined aquifers. These systems were formed by the deposition of sediments under fluvio-marine and fluvial environment. The study of the hydrochemical and hydraulic properties of the three aquifer systems proved that these three systems are separate entities. The phreatic aquifers in the area have low hydraulic gradients and high rejected recharge. The Recent confined aquifer has very poor hydraulic characteristics and recharge to this aquifer is very low. The Tertiary aquifer system is the most potential fresh water aquifer system in the area and the groundwater flow in the aquifer is converging towards the central part of the study area (Alleppey town) due to large scale pumping of water for water supply from this aquifer system. Mixing of waters and anthropogenic interferences are the dominant processes modifying the hydrochemistry in phreatic aquifers. Whereas, leaching of salts and cation exchange are the dominant processes modifying the hydrochemistry of groundwater in the confined aquifer system of Recent alluvium. Two significant chemical reactions modifying the hydrochemistry in the Recent aquifers are oxidation of iron in ferruginous clays which contributes hydrogen ions and the decomposition of organic matter in the aquifer system which consumes hydrogen ions. The hydrochemical environment is entirely different in the Tertiary aquifers as the groundwater in this aquifer system are palaeo waters evolved during various marine transgressions and regressions and these waters are being modified by processes of leaching of salts, cation exchange and chemical reactions under strong reducing environment. It is proved that the salinity observed in the groundwaters of Tertiary aquifers are not due to seawater mixing or intrusion, but due to dissolution of salts from the clay formations and ion exchange processes. Fluoride contamination in this aquifer system lacks a regional pattern and is more or less site specific in natureThe lowering of piezometric heads in the Tertiary aquifer system has developed as consequence of large scale pumping over a long period. Hence, puping from this aquifer system is to be regulated as a groundwater management strategy. Pumping from the Tertiary aquifers with high capacity pumps leads to well failures and mixing of saline water from the brackish zones. Such mixing zones are noticed from the hydrochemical studies. This is the major aquifer contamination in the Tertiary aquifer system which requires immediate attention. Usage of pumps above 10 HP capacities in wells taping Tertiary aquifers should be discouraged for sustainable development of these aquifers. The recharge areas need to be identified precisely for recharging the aquifer systems throughartificial means.

Numerical Feasibility Study for Treated Wastewater Recharge as a Tool to Impede Saltwater Intrusion in the Coastal Aquifer of Gaza – Palestine

The ongoing depletion of the coastal aquifer in the Gaza strip due to groundwater overexploitation has led to the process of seawater intrusion, which is continually becoming a serious problem in Gaza, as the seawater has further invaded into many sections along the coastal shoreline. As a first step to get a hold on the problem, the artificial neural network (ANN)-model has been applied as a new approach and an attractive tool to study and predict groundwater levels without applying physically based hydrologic parameters, and also for the purpose to improve the understanding of complex groundwater systems and which is able to show the effects of hydrologic, meteorological and anthropogenic impacts on the groundwater conditions. Prediction of the future behaviour of the seawater intrusion process in the Gaza aquifer is thus of crucial importance to safeguard the already scarce groundwater resources in the region. In this study the coupled three-dimensional groundwater flow and density-dependent solute transport model SEAWAT, as implemented in Visual MODFLOW, is applied to the Gaza coastal aquifer system to simulate the location and the dynamics of the saltwater–freshwater interface in the aquifer in the time period 2000-2010. A very good agreement between simulated and observed TDS salinities with a correlation coefficient of 0.902 and 0.883 for both steady-state and transient calibration is obtained. After successful calibration of the solute transport model, simulation of future management scenarios for the Gaza aquifer have been carried out, in order to get a more comprehensive view of the effects of the artificial recharge planned in the Gaza strip for some time on forestall, or even to remedy, the presently existing adverse aquifer conditions, namely, low groundwater heads and high salinity by the end of the target simulation period, year 2040. To that avail, numerous management scenarios schemes are examined to maintain the ground water system and to control the salinity distributions within the target period 2011-2040. In the first, pessimistic scenario, it is assumed that pumping from the aquifer continues to increase in the near future to meet the rising water demand, and that there is not further recharge to the aquifer than what is provided by natural precipitation. The second, optimistic scenario assumes that treated surficial wastewater can be used as a source of additional artificial recharge to the aquifer which, in principle, should not only lead to an increased sustainable yield of the latter, but could, in the best of all cases, revert even some of the adverse present-day conditions in the aquifer, i.e., seawater intrusion. This scenario has been done with three different cases which differ by the locations and the extensions of the injection-fields for the treated wastewater. The results obtained with the first (do-nothing) scenario indicate that there will be ongoing negative impacts on the aquifer, such as a higher propensity for strong seawater intrusion into the Gaza aquifer. This scenario illustrates that, compared with 2010 situation of the baseline model, at the end of simulation period, year 2040, the amount of saltwater intrusion into the coastal aquifer will be increased by about 35 %, whereas the salinity will be increased by 34 %. In contrast, all three cases of the second (artificial recharge) scenario group can partly revert the present seawater intrusion. From the water budget point of view, compared with the first (do nothing) scenario, for year 2040, the water added to the aquifer by artificial recharge will reduces the amount of water entering the aquifer by seawater intrusion by 81, 77and 72 %, for the three recharge cases, respectively. Meanwhile, the salinity in the Gaza aquifer will be decreased by 15, 32 and 26% for the three cases, respectively.

Analysis of water-level response to rainfall and implications for recharge pathways in the Chalk aquifer, SE England

Water table response to rainfall was investigated at six sites in the Upper, Middle and Lower Chalk of southern England. Daily time series of rainfall and borehole water level were cross-corretated to investigate seasonal variations in groundwater-level response times, based on periods of 3-month duration. The time tags (in days) yielding significant correlations were compared with the average unsaturated zone thickness during each 3-month period. In general, for cases when the unsaturated zone was greater than 18 m thick, the time tag for a significant water-level response increased rapidly once the depth to the water table exceeded a critical value, which varied from site to site. For shallower water tables, a linear relationship between the depth to the water table and the water-level response time was evident. The observed variations in response time can only be partially accounted for using a diffusive model for propagation through the unsaturated matrix, suggesting that some fissure flow was occurring. The majority of rapid responses were observed during the winter/spring recharge period, when the unsaturated zone is thinnest and the unsaturated zone moisture content is highest, and were more likely to occur when the rainfall intensity exceeded 5 mm/day. At some sites, a very rapid response within 24 h of rainfall was observed in addition to the longer term responses even when the unsaturated zone was up to 64 m thick. This response was generally associated with the autumn period. The results of the cross-correlation analysis provide statistical support for the presence of fissure flow and for the contribution of multiple pathways through the unsaturated zone to groundwater recharge. (c) 2006 Elsevier B.V. All rights reserved.

Multivariate relationships between groundwater chemistry and toxicity in an urban aquifer

Multivariate statistical methods were used to investigate file Causes of toxicity and controls on groundwater chemistry from 274 boreholes in an Urban area (London) of the United Kingdom. The groundwater was alkaline to neutral, and chemistry was dominated by calcium, sodium, and Sulfate. Contaminants included fuels, solvents, and organic compounds derived from landfill material. The presence of organic material in the aquifer caused decreases in dissolved oxygen, sulfate and nitrate concentrations. and increases in ferrous iron and ammoniacal nitrogen concentrations. Pearson correlations between toxicity results and the concentration of individual analytes indicated that concentrations of ammoinacal nitrogen, dissolved oxygen, ferrous iron, and hydrocarbons were important where present. However, principal component and regression analysis suggested no significant correlation between toxicity and chemistry over the whole area. Multidimensional Scaling was used to investigate differences in sites caused by historical use, landfill gas status, or position within the sample area. Significant differences were observed between sites with different historical land use and those with different gas status. Examination of the principal component matrix revealed that these differences are related to changes in the importance of reduced chemical species.

Geophysical characterization of the complex dynamics of groundwater and seawater exchange in a highly stressed aquifer system linked to a coastal lagoon (SE Spain)

Anthropogenic pressure influences the two-way interactions between shallow aquifers and coastal lagoons. Aquifer overexploitation may lead to seawater intrusion, and aquifer recharge from rainfall plus irrigation may, in turn, increase the groundwater discharge into the lagoon. We analyse the evolution, since the 1950s up to the present, of the interactions between the Campo de Cartagena Quaternary aquifer and the Mar Menor coastal lagoon (SE Spain). This is a very heterogeneous and anisotropic detrital aquifer, where aquifer–lagoon interface has a very irregular geometry. Using electrical resistivity tomography, we clearly identified the freshwater–saltwater transition zone and detected areas affected by seawater intrusion. Severity of the intrusion was spatially variable and significantly related to the density of irrigation wells in 1950s–1960s, suggesting the role of groundwater overexploitation. We distinguish two different mechanisms by which water from the sea invades the land: (a) horizontal advance of the interface due to a wide exploitation area and (b) vertical rise (upconing) caused by local intensive pumping. In general, shallow parts of the geophysical profiles show higher electrical resistivity associated with freshwater mainly coming from irrigation return flows, with water resources mostly from deep confined aquifers and imported from Tagus river, 400 km north. This indicates a likely reversal of the former seawater intrusion process.

Redescription of Anopheles (Nyssorhynchus) lutzii, and Resurrection of Anopheles guarani From Synonymy With An. lutzii (Diptera: Culicidae)

Anopheles lutzii Cruz (Diptera: Culicidae) is redescribed using specimens collected in Pariquera-Acu, Vale do Ribeira, state of Sao Paulo, southeastern Mata Atlantica, Brazil. Specimens of An. lutzii from Vale do Ribeira and two females from Nova Friburgo, Rio de Janeiro, are compared with three syntypes of An. lutzii, deposited in the Instituto Oswaldo Cruz, Rio de Janeiro. Comparisons of external morphology of specimens from the type locality of Anopheles guarani Shannon demonstrate it is a valid species, and that Anopheles niger Theobald is conspecific with Anopheles guarani stat. rev. The adult male, male terminalia, fourth-instar larva, and pupa of An. guarani stat. rev. are described for the first time. Diagnostic characters of the male and female, male terminalia, fourth-instar larva and pupa of An. lutzii and An. guarani stat. rev. are illustrated. An. guarani stat. rev. is herein resurrected from the synonymy with An. lutzii, and Anopheles niger comb. nov. is transferred from the synonymy with An. lutzii to the synonymy of An. guarani stat. rev.

Uranium series disequilibria in ground waters from a fractured bedrock aquifer (Morungaba Granitoids-Southern Brazil): Implications to the hydrochemical behavior of dissolved U and Ra

Activity concentrations of dissolved U-234, U-238, Ra-226 and Ra-228 were determined in ground waters fromtwo deep wells drilled in Morungaba Granitoids (Southern Brazil). Sampling was done monthly for little longer than 1 year. Significant disequilibrium between U-238, U-234 and Ra-226 were observed in all samples. The variation of U-238 and U-234 activity concentrations and U-234/U-238 activity ratios is related to seasonal changes. Although the distance between the two wells is short (about 900m), systematic differences of activity concentrations of U isotopes, as well as of U-234/U-238, Ra-226/U-234 and Ra-228/Ra-226 activity ratios were noticed, indicating distinct host rock-water interactions. Slightly acidic ground water percolation through heterogeneous host rock, associated with different recharge processes, may explain uranium and radium isotope behavior. (c) 2008 Elsevier Ltd. All rights reserved.

Geochemistry of natural chromium occurrence in a sandstone aquifer in Bauru Basin, Sao Paulo State, Brazil

Anomalous concentrations of Cr(VI) occur in groundwaters of the Adamantina Aquifer, in a large region in the western state of Sao Paulo, sometimes exceeding the potability limit (0.05 mg L(-1)). To identify the possible geochemical reactions responsible for the occurrence of Cr in groundwater in Urania, borehole rock samples were collected in order to carry out mineralogical and chemical analyses. In addition, multilevel monitoring wells were installed and groundwater samples were analyzed. Analyses of the borehole rock samples show the occurrence of a geochemical anomaly of Cr in the quartzose sandstones (average concentrations of 221 ppm). Chrome-diopside is one of the main minerals contributing to this anomaly, having an average Cr content of 1505 ppm. Sequential extraction experiments indicated weakly adsorbed Cr in the order of 0.54 ppm, and this quantity is enough to provide the Cr concentrations observed in groundwater. Groundwaters from the monitoring wells proved to be stratified, with the highest concentrations of Cr(VI) (0.13 mg L(-1)) being associated with high redox and pH values (over 10) and high concentrations of Na. Geochemical reactions that may explain the release of Cr from the solid phase to groundwater involve the release of Cr(III) from minerals (like chrome-diopside and Cr-Fe hydroxide), followed by oxidation of Cr(III) to Cr(VI), probably related to the reduction of Mn oxides present in the aquifer. Then cation exchange occurs and dissolution of carbonates which increases the pH of groundwater, resulting in the desorption and mobilization of Cr(VI) into groundwater. (C) 2011 Elsevier Ltd. All rights reserved.

Anomalous content of chromium in a Cretaceous sandstone aquifer of the Bauru Basin, state of Sao Paulo, Brazil

Anomalous and natural concentrations of Cr(6+), occasionally exceeding the permitted limit for human consumption (0.05 mg/L), have been detected in groundwater in the northwestern region of the state of Sao Paulo. As part of a water-rock interaction investigation, this article describes the chemical and mineralogical characterization of rock samples taken from boreholes in the municipality of Urania, with the objective of identifying Cr-bearing minerals and determining how chromium is associated with these minerals. Rock sample analysis were performed using X-ray Fluorescence, X-ray Diffraction, Scanning Electron Microscopy, electron microprobe and sequential extraction techniques. Chemical analyses indicated that the quartzose sandstones show a geochemical anomaly of chromium, with an average content of 221 ppm, which is higher than the reported chromium content of generic sandstones (35 ppm). Diopside was identified as the primary Cr-bearing mineral potentially subject to weathering processes, with a chromium content of up to 1.2% as Cr(2)O(3). Many of the diopside grains showed dissolution features, confirming the occurrence of weathering. Sequential extraction experiments indicated that 99.3% of the chromium in samples is tightly bonded to minerals, whereas 0.24% is weakly bonded via adsorption. Assuming hypothetically that all adsorbed chromium is released via desorption, the theoretical Cr concentration in water would be one order of magnitude higher than the concentrations of Cr(6+) detected in groundwater. (C) 2010 Elsevier Ltd. All rights reserved.

Nhembo'e : enquanto o encanto permanece! : processos e práticas de escolarização nas aldeias Guarani

A escola nas aldeias Guarani do Rio Grande do Sul é um acontecimento recente. Algumas TEKOÁ decidiram não abrigá-la em seu meio, considerando que a educação tradicional, assentada na cosmologia Guarani, é suficiente para o seu viver e, portanto, prescindem dos saberes escolares. Outras, evidenciando a necessidade de saberes que se relacionam à escola – como a escrita, a leitura, a Língua Portuguesa e o sistema monetário, entre outros –, a solicitam e a acolhem, iniciando processos e práticas de escolarização que afirmam o desejo de se apropriar de instrumentos que permitam um diálogo mais eqüitativo com a sociedade não indígena. Num movimento de interlocução com os gestores das políticas públicas, tensionam a Secretaria de Estado da Educação para criar condições de implementar a Escola Específica e Diferenciada nas aldeias. No entanto, experimentam a ambigüidade de uma aproximação e de um afastamento, de um querer e um não querer a escola em suas aldeias, pois intuem as mudanças que poderá desencadear no modo de vida tradicional. Para compreender os processos de implementação da escola do povo Guarani, e os significados que atribuem à educação escolar, dirigi o olhar e aprofundei o estudo em três aldeias do Rio Grande do Sul: TEKOÁ JATAÍTY (Cantagalo, município de Viamão), TEKOÁ ANHETENGUÁ (Lomba do Pinheiro, Porto Alegre) e TEKOÁ IGUA´PORÃ (Pacheca, município de Camaquã). Os movimentos de aproximação com a cosmologia Guarani e com o universo das aldeias, constituído através de um estar-junto sensível, e o com-viver com a totalidade cosmológica de cada lugar pesquisado possibilitou a elaboração de um contorno antropológico etnográfico que busca dizer dos Guarani desde si. A perspectiva teórica, assentada principalmente na aproximação da Educação com uma Antropologia Filosófica latino-americana, possibilitou a compreensão do pensamento indígena e da ambigüidade do “ser” europeu e do “estar” americano, presente nas aldeias e fora delas também. A pesquisa mostra que há nos preceitos educacionais da cosmologia Guarani um admirável mundo a ser desvendado, em que os significados de cada gesto, de cada ação mostram a integridade de um povo que sobrevive e se recria e a escola na aldeia poderá se inserir nesse universo e dialogar com todos os princípios que compõem a educação tradicional e a cosmologia Guarani.

"O que o guarani vende?" um estudo sobre sitema econômico e pessoa mbyá-guarani num contexto de relações interétnicas em São Miguel das Missões-RS

Este trabalho, realizado entre agosto de dois mil e quatro e março de dois mil e cinco, trata de compreender a partir das análises da historiografia, da noção de pessoa e do sistema econômico - nas formas de produção, distribuição e consumo - o processo de integração dos Mbyá-Guarani, de São Miguel das Missões, Estado do Rio Grande do Sul, à sociedade nacional envolvente, dentro de um contexto de contato interétnico. Com isso, demonstra algumas transformações e tensões, advindas da situação colonial de contato, dentro do sistema cultural tradicional mbyá-guarani.

Orerémbiú : a relação das práticas alimentares e seus significados com a identidade étnica e a cosmologia Mbyá-Guarani

A alimentação não é uma simples ingestão de calorias, necessárias à sobrevivência. Ela também envolve uma vasta gama de aspectos simbólicos, que expressam relações e pertencimentos grupais. Os Mbyá-Guarani atribuem sentidos aos seus alimentos (desde a sua produção, armazenamento, processamento, preparação e consumo) que mantêm estreita relação com seus atributos étnicos e cosmológicos. Desta maneira, a presente dissertação tem como objetivo uma análise antropológica das práticas alimentares que ocorrem neste grupo indígena. Mais precisamente, busca-se verificar de que maneira as práticas alimentares estão relacionadas com suas concepções cosmológicas e de que forma são utilizadas como sinais diacríticos delimitadores de suas especificidades étnicas.

Reconhecimento dos direitos territoriais indígenas: uma mediação entre os Guarani e o Estado

A presente dissertação foi desenvolvida através de um estudo das dinâmicas de relação entre o grupo indígena Guarani-Mbya e o Estado, no âmbito da FUNAI, durante o período de 2006 a 2011. O estudo foi realizado por meio da análise da construção dos sentidos do processo de reivindicação e reconhecimento dos direitos territoriais. No entanto, neste trabalho é identificado que o grupo analisado possui entendimentos sobre o direito e o território que divergem daqueles definidos pelo Estado, o que gera dificuldades e entraves à política de reconhecimento de seus territórios. Para realizar uma análise das especificidades dos sentidos atribuídos ao território e à reivindicação pelo reconhecimento do mesmo seleciona-se como unidade de análise a Comissão Guarani Yvyrupa (CGY), organização que representa os Guarani neste processo. Por meio desta organização é reivindicado às instituições governamentais o reconhecimento e inclusão de suas especificidades na política de terra. Utiliza-se o método da análise dos discursos e do conteúdo com o objetivo de compreender as especificidades dos sentidos atribuídos ao território e à luta pelo reconhecimento deste direito. Para obter uma compreensão mais profunda sobre o caso estudado foi realizada uma imersão no campo através da observação participante da organização e ação política da CGY durante oito meses. Foram utilizadas como fonte de análise atas de encontros, cartas de reivindicação, depoimentos, entrevistas e diversas conversas informais. A análise é construída à luz das teorias do reconhecimento de Axel Honneth, da pluralidade dos princípios do direito por Ammy Gutmann e Michael Ignatieff, e da construção das esferas civis por Jeffrey Alexander.

Sementes e saberes... : trocas e aprendizados com a cultura Guarani e a agroecologia

Esta dissertação é o relato de uma aproximação, dos encontros e dos saberes compartilhados a partir das sementes de milho preservadas e recriadas pelo povo Guarani e suas relações com redes agroecológicas. Realizo uma reflexão sobre os potenciais educativos das sementes, do plantio e do reconhecimento da diversidade cultural e ambiental que (ainda) encontramos em nossos povos e ambientes a partir de registros etnográficos, no encontro com a cultura Guarani da Aldeia de Itapuã/RS e Piraquara/PR e com agricultores agroecológicos. Tendo como principais referências Enrique Leff, Paulo Freire, Dan Baron e Boaventura de Souza Santos apresento meus caminhos de pesquisa, reflexões e buscas enquanto educadora e pesquisadora. Junto com estes autores inicio um diálogo em torno das sementes como elemento constituinte dos saberes ambientais que simbolizam a busca por modos de vida mais sustentáveis que resgatam e recriam culturas.

Na negação dos muros, a mirada ambiental na perspectiva do ser guarani : a questão da educação escolar

A presente Dissertação tem como objeto a perspectiva ambiental na educação escolar Guarani. Para se constituir enquanto tal, buscou, no próprio seio da comunidade e da Escola Indígena, as respostas para o questionamento de como se dará, na Escola pensada pelos Guarani, a perspectiva ambiental: na sua própria teko’a, na relação com a Cidade e na relação com a tecnologia cidadã. Na busca de uma sistematização de possíveis respostas, primeiro, traça-se uma perspectiva antropológica da própria Cidade, lugar fundante da Escola, desde a ótica de Rodolfo Kusch sobre a relação entre o ambiente natural - no qual o granizo e a chuva, la ira de Dios, representam o temor – e o ambiente artificial – constituído no ambiente cidadão, onde reina la ira del hombre, representado no objeto e no afã de ser alguém; em segundo, apresenta-se os próprios Guarani e seu mero estar e, finalmente, em terceiro, a Escola e a perspectiva ambiental que perpassa o pensá-la e o próprio ensinar. A pesquisa foi realizada a partir das observações e conversas com as lideranças, os professores e os Karaí. Para tanto, serviu-se de instrumento do Diário de Campo, das gravações de entrevistas e dos registros fotográficos. A análise dos dados teve como substrato teórico a perspectiva do Cuidado, fundamentada em Martin Heidegger e da antropologia filosófica americana, fundamentada em Rodolfo Kusch. O trabalho mostra duas culturas – a cultura cidadã e a cultura Mbyá-Guarani – que se colocam na intersecção da própria Escola, onde um embrião de uma nova Escola, que já não aponta para o conhecimento científico como fundamento das suas práticas, parece estar se constituindo no ambiente da Tekoá.