Hydrochemical Features Of Groundwater From Aquifer Systems Occurring Near Central São Paulo State, Brazil

dc.creatorBonotto D.M.
dc.creatorMancini L.H.
dc.creatorTonetto E.M.
dc.date2012
dc.date2015-06-25T20:26:59Z
dc.date2015-11-26T15:23:37Z
dc.date2015-06-25T20:26:59Z
dc.date2015-11-26T15:23:37Z
dc.date.accessioned2018-03-28T22:32:31Z
dc.date.available2018-03-28T22:32:31Z
dc.identifier9781619420915
dc.identifierAquifers: Types, Impacts And Conservation. Nova Science Publishers, Inc., v. , n. , p. 33 - 58, 2012.
dc.identifier
dc.identifier
dc.identifierhttp://www.scopus.com/inward/record.url?eid=2-s2.0-84891979458&partnerID=40&md5=5495b7d3941d41851b3894507aade973
dc.identifierhttp://www.repositorio.unicamp.br/handle/REPOSIP/90628
dc.identifierhttp://repositorio.unicamp.br/jspui/handle/REPOSIP/90628
dc.identifier2-s2.0-84891979458
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1260507
dc.descriptionBrazil owns the highest availability of renewable hydrological resources in world. However, in the beginning of the 21st century, it was the 26th country in terms of social water availability as a consequence of the great unequal distribution of the hydrological resources in the country. This is because it is mainly concentrated in northern and portions of northeastern and central western regions, where the population density is low. This advanced degree of unequal water distribution has caused special attention to the groundwater resources due to problems related to the interaction between the society and the environment. São Paulo is the most populous Brazilian state, comprising ~ 40 million inhabitants distributed over 645 municipalities. It has the highest number of industries and economic production, reaching 31% of the Brazilian GDPgross domestic product. Despite the vigorous industrial production that includes high technology goods, the state also is well developed in agriculture and cattle breeding. This advanced stage of agricultural and industrial growth causes to São Paulo State an accentuated use of groundwater resources in water-supply systems. Several lithologies of the Paraná sedimentary basin outcrop in São Paulo State. They consist on sandstones, conglomerates, diamictites, tillites, siltstones, mudstones, limestones, shales, silex, rythmites, basalts, diabases and different types of Cenozoic covers like the recent deposits, terrace sediments and the Rio Claro Formation (sandstones, conglomerate sandstones and muddy sandstones). Many of these rock types are important reservoirs for groundwater in São Paulo State. Rio Claro city is located at the northeastern edge of the Paraná basin, cropping-out several units of the basin in the region. Rio Claro city is the most important municipality in Corumbataí River basin that extends over an area of about 1581 km2. The area considered in this chapter includes Rio Claro city and portions of Araras, Leme, Cordeirópolis, Santa Gertrudes, Itirapina, Corumbataí and Ipeúna municipalities. Different groundwater systems have been focused in this chapter, among them: a phreatic aquifer comprising a cover of unconsolidated materials from Rio Claro Formation; sediments from Tubarão Group, comprising a confined aquifer about 40 m thick; deep bodies of diabase that store water within their fractures. In general, sedimentary aquifers exhibit different flow and hydrochemical characteristics in relation to that of the fractured rock aquifers and these aspects will be considered in this chapter. © 2012 Nova Science Publishers, Inc. All rights reserved.
dc.description
dc.description
dc.description33
dc.description58
dc.descriptionAgudo, E.G., Guia de coleta e preservação de amostras de água (1987), CETESB (Companhia de Tecnologia de Saneamento Ambiental): São PauloAlmeida, F.F.M., (1964) Bol Inst Geogr Geol, 41, pp. 169-263
dc.descriptionAlmeida, F.F.M., Melo, M.S., Mapa geológico do Estado de São Paulo (1981), 1, pp. 46-81. , Pró-Minério
dc.descriptionEd.
dc.descriptionPROMOCET: São PauloAmaral, G., Cordani, U.G., Kawashita, K., Reynolds, J.H., (1966) Geochim Cosmochim Acta, 30, pp. 159-189
dc.descriptionAraújo, L.M., França, A.B., Potter, P.E., Giant Mercosul aquifer of Brazil, Argentina, Uruguay and Paraguay: hydrogeologic maps of Botucatu Pirambóia, Rosário do Sul, Buena Vista, Misiones and TacuarembóFormations (1995), Universidade Federal do Paraná: CuritibaBagolini, B., (1971) Mem Mus Tudentino di Sci Nat Ireuts, 19, pp. 71-122
dc.descriptionBonotto, D.M., Mancini, L.H., (1992) Geochim Brasil, 6 (2), pp. 153-167
dc.descriptionBrookins, D.G., Eh-pH diagrams for geochemistry (1988), Springer-Verlag: BerlinCastany, G., Traité pratique des eaux souterraines (1967), Dunod: ParisAtlas ambiental da Bacia do Rio Corumbataí (2001), http://www.rc.unesp.br/igce/ceapla/atlas/index.html, CEAPLA (Centro de Análise e Planejamento Ambiental)CETESB (Companhia de Tecnologia de Saneamento Ambiental) Relatório de qualidade das águas subterrâneas do estado de São Paulo 1997 (1998), CETESB: São PauloCottas, L.R., Estudos geológicos-geotécnicos aplicados ao planejamento urbano de Rio Claro (SP) (1983), PhD Thesis
dc.descriptionUSP: São PauloDAEE (Departamento de Águas e Energia Elétrica) Estudo de águas subterrâneas-Região Administrativa 5-Campinas (1981), p. 639. , Secretaria de Obras e Meio Ambiente: São PauloFraga, C.G., Origem de fluoreto em águas subterrâneas dos sistemas aqüíferos Botucatu e Serra Geral da Bacia do Paraná (1992), PhD Thesis
dc.descriptionUSP: São PauloGilboa, Y., Mero, F., Mariano, I.B., (1976) J Hydrol, 29, pp. 165-179
dc.descriptionHirata, R.C.A., Bastos, C.R.A., Rocha, G.A., Mapa de vulnerabilidade das águas subterrâneas no Estado de São Paulo (1997), CETESB (Companhia de Tecnologia de Saneamento Ambiental): São PauloInácio, A., Santos, M.J.Z., (1988) Bol Geografia Teorética, 18, pp. 87-104
dc.descriptionMapa geológico do Estado de São Paulo (1981), IPT (Instituto de Pesquisas Tecnológicas), Monografias
dc.descriptionIPT (Instituto de Pesquisas Tecnológicas): São Paulo, SPKimmelmanne Silva, A.A., Rebouças, A.C., Santiago, M.M.F., (1989) Radiocarbon, 31, pp. 926-933
dc.descriptionKöffler, N.F., Diagnóstico do uso de solos agrícolas da bacia do Rio Corumbataí (1993), São Paulo
dc.descriptionIGCE-UNESP: Rio ClaroMelfi, A., (1967) J. Geochim Cosmochim Acta, 31, pp. 1079-1089
dc.descriptionOliva, A., Caracterização hidroquímica de águas subterrâneas no município de Rio Claro (SP) (1999) Graduation monography, , IGCE-UNESP: Rio Claro
dc.descriptionPenteado, M.M., Geomorfologia do setor central-ocidental da Depressão Periférica no Estado de São Paulo (1976), Série Teses e Monografias, 22
dc.descriptionUniversidade de São Paulo: São Paulo, SPPiper, A.M., (1944) Trans Amer Geophysical Union, 25, pp. 914-928
dc.descriptionRebouças, A.C., Recursos hídricos subterrâneos da Bacia do Paraná-Análise de pré-viabilidade (1976), Post PhD Thesis
dc.descriptionUSP: São PauloRebouças, A.C., Anais I Congresso Brasileiro de Águas Subterrâneas (1980), pp. 35-47. , ABAS (Associação Brasileira de Águas Subterrâneas)
dc.descriptionEd.
dc.descriptionABAS: RecifeRebouças, A.C., (1988) Episodes, 11, pp. 209-214
dc.descriptionRebouças, A.C., Anais VIII Congresso Brasileiro de Águas Subterrâneas (1994), pp. 500-509. , ABAS (Associação Brasileira de Águas Subterrâneas)
dc.descriptionEd.
dc.descriptionABAS: RecifeRenne, P.R., Ernesto, M., Pacca, I.G., Coe, R.S., Glen, J.M., Prévot, M., Perrin, M., (1992) Science, 258, pp. 975-979
dc.descriptionSawyer, C.N., McCarty, P.L., Chemistry for sanitary engineers (1967), McGraw-Hill: New YorkSilva, R.B.G., Estudo hidroquímico e isotópico das águas subterrâneas do aqüífero Botucatu no Estado de São Paulo (1983), PhD Thesis
dc.descriptionUSP: São PauloSoares, P.C., (1975) Rev Bras Geoc, 5, pp. 229-251
dc.descriptionTodd, D.K., Ground Water Hydrology (1959), p. 320. , John Wiley & Sons, Inc: New YorkTonetto, E.M., Bonotto, D.M., (2005) Environ Geol, 47 (7), pp. 942-955
dc.descriptionTurner, S., Regelous, M., Kelley, S., Hawkesworth, C.J., Mantovani, M.S.M., (1994) Earth Planet Sci Lett, 121, pp. 333-348
dc.descriptionde Vries, J.J., Environmental isotopes in the hydrological cycle (2000), 39 (1). , Mook, W. G.
dc.descriptionEd.
dc.descriptionUNESCO-IAEA: Paris-Vienna, International Hydrological Programme, IHP-V, Technical Documents in HydrologyWhite, I.D., Relatório final da Comissão de Estudos das Minas de Carvão de Pedra do Brasil (1908), Imprensa Nacional: Rio de JaneiroZaine, J.E., Penteado-Orellana, M.M., Anais XXXVIII Congresso Brasileiro de Geologia (1994), 1, pp. 441-447. , SBG (Sociedade Brasileira de Geologia)
dc.descriptionEd.
dc.descriptionSBG: Camboriú
dc.languageen
dc.publisherNova Science Publishers, Inc.
dc.relationAquifers: Types, Impacts and Conservation
dc.rightsfechado
dc.sourceScopus
dc.titleHydrochemical Features Of Groundwater From Aquifer Systems Occurring Near Central São Paulo State, Brazil
dc.typeCapítulos de libros


Este ítem pertenece a la siguiente institución