Littérature scientifique sur le sujet « HYDROCHEMICAL CHARACTERIZATION »
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Articles de revues sur le sujet "HYDROCHEMICAL CHARACTERIZATION"
Maghlakelidze, Akaki. « Hydrochemical Characterization of Nabeghlavi Underground Mineral Waters ». Works of Georgian Technical University, no 4(522) (28 décembre 2021) : 71–79. http://dx.doi.org/10.36073/1512-0996-2021-4-71-79.
Texte intégralThyne, Geoffrey, Cuneyt Guler et Eileen Poeter. « Sequential Analysis of Hydrochemical Data for Watershed Characterization ». Ground Water 42, no 5 (septembre 2004) : 711–23. http://dx.doi.org/10.1111/j.1745-6584.2004.tb02725.x.
Texte intégralManu, Evans, Marco De Lucia et Michael Kühn. « Hydrochemical Characterization of Surface Water and Groundwater in the Crystalline Basement Aquifer System in the Pra Basin (Ghana) ». Water 15, no 7 (28 mars 2023) : 1325. http://dx.doi.org/10.3390/w15071325.
Texte intégralBenderev, Aleksey, Stanimir Stanev, Mila Trayanova, Sava Kolev et Aglaida Toteva. « Hydrochemical characterization of thermal waters in Shipkovo thermal field ». Engineering Geology and Hydrogeology 33, no 1 (2019) : 27–39. http://dx.doi.org/10.52321/igh.33.1.27.
Texte intégralRuiz-Pico, Ángel, Álvaro Pérez-Cuenca, Richard Serrano-Agila, Diana Maza-Criollo, Jorge Leiva-Piedra et Johonathan Salazar-Campos. « Hydrochemical characterization of groundwater in the Loja Basin (Ecuador) ». Applied Geochemistry 104 (mai 2019) : 1–9. http://dx.doi.org/10.1016/j.apgeochem.2019.02.008.
Texte intégralNativ, Ronit, et Ilan Nissim. « Characterization of a Desert Aquitard- Hydrologic and Hydrochemical Considerations ». Ground Water 30, no 4 (juillet 1992) : 598–606. http://dx.doi.org/10.1111/j.1745-6584.1992.tb01536.x.
Texte intégralToumi, Faycal, Samir Hani, Nabil Bougherira, Azzedine Hani, Hicham Chaffai et Larbi Djabri. « Hydrochemical and isotopic characterization of a complex aquifer system ». Acque Sotterranee - Italian Journal of Groundwater 12, no 1 (31 mars 2023) : 53–61. http://dx.doi.org/10.7343/as-2023-626.
Texte intégralAntas, Francisco Pio de Souza, Nildo da Silva Dias, André Moreira de Oliveira, Osvaldo Nogueira de Sousa Neto, Cleyton dos Santos Fernandes, Neyton de Oliveira Miranda, Gabriela Cemirames de Sousa Gurgel, Francisco Souto de Sousa Junior, Alexandre de Oliveira Lima et Miguel Ferreira Neto. « Hydrochemical Characterization of Water Resources From Reverse Osmosis Desalination Plants ». Journal of Agricultural Science 10, no 12 (15 novembre 2018) : 445. http://dx.doi.org/10.5539/jas.v10n12p445.
Texte intégralTeixeira, Guilherme Vargas, Antonio Pedro Viero, Claudia Porcelis Vargas et Guilherme D'Ávila Nunes. « Structural, hydrogeological and hydrochemical characterization of aquifers in the Paraná Basin : An integrated literature review ». Research, Society and Development 10, no 9 (26 juillet 2021) : e26610918390. http://dx.doi.org/10.33448/rsd-v10i9.18390.
Texte intégralAbeli, T., S. Orsenigo, N. M. G. Ardenghi, E. C. H. E. T. Lucassen et A. J. P. Smolders. « Hydrochemical Characterization of A Stand of the Threatened EndemicIsoëtes malinverniana ». American Fern Journal 103, no 4 (octobre 2013) : 241–44. http://dx.doi.org/10.1640/0002-8444-103.4.241.
Texte intégralThèses sur le sujet "HYDROCHEMICAL CHARACTERIZATION"
Henry, Sabine. « The hydrochemical and isotopic characterization of groundwater in southern Mozambique ». Master's thesis, Faculty of Science, 2021. http://hdl.handle.net/11427/33835.
Texte intégralAuler, Augusto. « Hydrogeological and Hydrochemical Characterization of the Matozinhos-Pedro Leopoldo Karst, Brazil ». TopSCHOLAR®, 1994. http://digitalcommons.wku.edu/theses/927.
Texte intégralAsim, Muhammad. « HYDROCHEMICAL CHARACTERIZATION AND NUMERICAL MODELING OF GROUNDWATER FLOW IN A PART OF THE HIMALAYAN FORELAND BASIN ». Kent State University / OhioLINK, 2005. http://rave.ohiolink.edu/etdc/view?acc_num=kent1132262925.
Texte intégralCaetano, Bicalho Cristina. « Hydrochemical characterization of transfers in karst aquifers by natural and anthropogenic tracers. Example of a Mediterranean karst system, the Lez karst aquifer (Southern France) ». AgroParisTech, 2010. http://pastel.archives-ouvertes.fr/docs/00/56/95/44/PDF/these_CCBICALHO_2010.pdf.
Texte intégralThe Lez karst spring, located in the Mediterranean basin (southern France), supplies with water the metropolitan area of Montpellier (France) since the 19th century. Since 1981, an intense pumping is being performed directly in the main conduit with a maximum exploitation flow rate of about 1,700 l/s. To improve the understanding of groundwater origins and circulation dynamics in this karst system, as well as the impact of three decades of intense water exploitation, groundwater samples have been collected during various hydrologic conditions since March 2006. The springs and wells of the Lez karst system as well as surrounding springs and wells have been monitored for: physicochemical parameters, major and trace elements, Total Organic Carbon (TOC), faecal and total coliforms, 18O, 2H, 13CTDIC and 87Sr/86Sr. During the first recharge events of autumn, high-mineralized waters have been observed at the Lez spring. This singular behaviour was monitored in a fine time-lag. A multivariate statistical analysis revealed the existence of different water-types discharging at the Lez spring. A coupled approach integrating geochemistry and isotopes were applied and provided insight into the different end-members, associated lithologies and the main reactions that control groundwater chemistry. Between the five distinguished water-types, the two more contrasting ones are emphasized: the first one correspond to more geochemically evolved, long residence-time waters, issued from deep layers where evaporite fingerprinting was identified. They are characterized by high mineralization and high concentrations in Cl, Na, Mg, Li, B and Br elements, high Sr/Ca, Mg/Ca and Cl/Br ratios and enriched 13CTDIC and 87Sr/86Sr. Between all the studied springs and wells, this chemical fingerprinting has been uniquely observed for the Lez spring groundwaters. The second water-type corresponds to low mineralized waters with high concentrations in NO3, bacteria and TOC, and represents the flux of rapid infiltration waters. They underline the vulnerability of the system to surface infiltration and anthropogenic contamination through the infiltration of waters by sinkholes and well-developed fracture networks. Hydrograph deconvolutions using multiple tracers were used to estimate the participation of two or three end-members in the various flood-events that occurred between 2008 and 2010. If we use chloride as tracer, the mean estimated participation of the different water types are, as follows: 12% for deep waters; 5% for recent waters and 83% for main aquifer waters. The comparison between present and former studies carried out before the installation of the pumping plant (1973-1974 dataset), indicates historical changes in water hydrogeochemistry, evidencing a decrease of the deep compartment participation to the outflow of the Lez spring. This change in water hydrogeochemistry may be attributed to the intense pumping of the karst system and, in the absence of noticeable climatic changes, traduces the direct consequences of anthropogenic forcing on the overall functioning of the aquifer. The multi-tracers approach combined to hydrodynamics appears as a very efficient tool for characterizing groundwater flows and their origins and seems to be potentially applicable to other similar complex Mediterranean karst systems that were subjected to deep karstification during the Messinian crisis. The features of this crisis seem to play a relevant role on the hydrogeological behaviour of the aquifer and chemical characteristics of waters by the participation of a deep compartment to the outflow of the karst system
ROTIROTI, MARCO. « Hydrogeology and hydrogeochemistry of As, Fe, Mn rich groundwater of the multi-layer aquifer in the lower Po Plain, Lombardy region (northern Italy) ». Doctoral thesis, Università degli Studi di Milano-Bicocca, 2013. http://hdl.handle.net/10281/42004.
Texte intégralCastro, Lorena Mota de. « Estudo do comportamento de indicadores ambientais nos sistemas fluviais Madeira/Amazonas e Solimões/Amazonas ». Universidade Federal do Amazonas, 2015. http://tede.ufam.edu.br/handle/tede/5092.
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The Amazon basin, the largest watershed in the world, accounts for approximately 16% of the water discharged into the ocean and its broad scope results in greater sensitivity of its rivers to global climate change. The dynamic and availability of chemical elements in a system as complex rely on natural processes such as leaching of chemicals contained in the rocks as well as a source of anthropogenic activity. The objective of this study was to evaluate the spatial variation of physical and chemical parameters (temperature, turbidity, conductivity, total suspended solids, pH) and anion concentration (F-, Cl-, NO3-, NO2- and SO42-) in sections covering the main forming the Amazon: Solimões and Madeira river, in addition to characterize the bottom sediment of these systems in regard to its particle size, mineralogical composition (XRD) and concentration of the metals Fe, Mn, Zn, Cu, Cr, Ni and Pb (ICP-OES). With the exception of turbidity, both the parameters and the ions concentration presented their values below the maximum recommended by the CONAMA resolution 357/2005 for waters class 2. Both evaluated stretches showed medium and fine sand contents as the predominant composition in the bottom sediments, except for RMGua point Guayaramerín-BO, reflecting the higher concentration of metals in this sample. In bottom sediments there was a predominance of quartz, albite, clinochlore, illite, muscovite and microcline in the total fraction of these. The presence of heavy minerals such as andalusite, augite and rutile were viewed in the Solimões / Amazonas stretch where this occurrence may be associated with Içá and Solimões formations. The correlation analysis allowed to evaluate that metals such as Fe, Pb and Ni have high correlation with the mineralogical composition of the Solimões / Amazonas stretch. The high correlation between Zn and Fe with SO42- content indicates their relationship with pyrite deposits, though not rule out the influence of mining activities widespread in the region. In PCA analysis it was observed that the dispersion of data, both in the Solimões / Amazonas stretch and in Madeira / Amazonas, are caused by naturally occurring factors, despite the high incidence of human activities, mainly in the basin of Madeira.
A bacia Amazônica, considerada a maior bacia hidrográfica do mundo, é responsável por aproximadamente 16% da água despejada no oceano e sua ampla extensão resulta na maior sensibilidade dos seus rios às mudanças climáticas globais. A dinâmica e disponibilidade de elementos químicos em um sistema tão complexo dependem de processos naturais como a lixiviação de substâncias químicas contidas nas rochas como também de atividades de fonte antrópica. O objetivo deste estudo foi avaliar a variação espacial de parâmetros físico-químicos (temperatura, turbidez, condutividade, sólidos totais suspensos, pH) e concentração de ânions (F-, Cl-, NO3-, NO2- e SO42-) em trechos que abrangem os principais formadores do rio Amazonas: Rio Solimões e Rio Madeira, além de caracterizar o sedimento de fundo destes sistemas no que se refere à sua granulometria, composição mineralógica (DRX) e concentração dos metais Fe, Mn, Zn, Cu, Cr, Ni e Pb (ICP-OES). Com exceção da turbidez, tanto os parâmetros quanto a concentração de íons apresentaram seus valores abaixo do máximo recomendado pela resolução do CONAMA 357/2005 para águas de classe 2. Ambos os trechos avaliados apresentaram teores de areia fina e média como composição predominante nos sedimentos de fundo, com exceção de um ponto em Guayaramerín-BO (RMGua), refletindo na maior concentração de metais nesta amostra. Nos sedimentos de fundo verificou-se a predominância de quartzo, albita, clinocloro, ilita, muscovita e microclina na fração total. A presença de minerais pesados como a andaluzita, augita e rutilo foram visualizadas no trecho Solimões/Amazonas onde esta ocorrência pode ser associada às formações Içá e Solimões. A análise de correlação permitiu avaliar que metais como Fe, Pb e Ni possuem alta correlação com a composição mineralógica do trecho Solimões/Amazonas. A alta correlação entre o Zn e Fe com o teor de SO42- indica a relação destes com os depósitos de pirita, entretanto não se descarta a influência das atividades mineradoras muito difundidas na região. Na análise de PCA foi possível observar que a dispersão entre os dados, tanto no trecho Solimões/Amazonas quanto no Madeira/Amazonas, são causados por fatores de origem natural, apesar da alta incidência de atividades antrópicas, principalmente na bacia do Rio Madeira.
CHEA, ANTHONY NIMELY. « HYDROCHEMICAL CHARACTERIZATION OF GROUNDWATER FOR DRINKING AND IRRIGATION IN HISAR, HARYANA, INDIA ». Thesis, 2021. http://dspace.dtu.ac.in:8080/jspui/handle/repository/20041.
Texte intégralLivres sur le sujet "HYDROCHEMICAL CHARACTERIZATION"
Weissberg, I. Characterization of hydrological and hydrochemical cycles as a tool for evaluation of environmental impact of mining in Serra dos Carajas, Amazonia, Brazil. S.l : s.n, 1991.
Trouver le texte intégralChapitres de livres sur le sujet "HYDROCHEMICAL CHARACTERIZATION"
Todorović, Maja, Jana Štrbački, Marina Ćuk, Jakov Andrijašević, Jovana Šišović et Petar Papić. « Mineral and Thermal Waters of Serbia : Multivariate Statistical Approach to Hydrochemical Characterization ». Dans Mineral and Thermal Waters of Southeastern Europe, 81–95. Cham : Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-25379-4_5.
Texte intégralGouasmia, Mouez, Abdelkader Mhamdi, Ferid Dhahri et Mohamed Soussi. « Hydrogeological and Hydrochemical Characterization of Mejel Bel Abbes Aquifer (West-Central Tunisia) ». Dans New Prospects in Environmental Geosciences and Hydrogeosciences, 547–49. Cham : Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-72543-3_123.
Texte intégralLegrioui, Radhia, Fethi Baali, Ilhem Abdeslam, Amor Hamad, Philippe Audra, Didier Cailhol et Stéphane Jaillet. « Hydrochemical and Isotopic Characterization of Karst Aquifer in the Region of Tebessa, Northeast Algeria ». Dans Advances in Karst Science, 223–31. Cham : Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-14015-1_25.
Texte intégralBarberá, J. A., et B. Andreo. « Duality of Functioning in a Karst System Under Mediterranean Climate Conditions, Deduced from Hydrochemical Characterization ». Dans Advances in Research in Karst Media, 189–94. Berlin, Heidelberg : Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-642-12486-0_29.
Texte intégralSánchez, D., B. Andreo, M. López, M. J. González et M. Mudarra. « Characterization of Carbonate Aquifers (Sierra de Grazalema, S Spain) by Means of Hydrodynamic and Hydrochemical Tools ». Dans Hydrogeological and Environmental Investigations in Karst Systems, 171–80. Berlin, Heidelberg : Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-17435-3_20.
Texte intégralDenimal, Sophie, Catherine Bertrand, Marc Steinmann et Nicolas Carry. « Comparison of Flow Processes in Drains and Low Permeability Volumes of a Karst System in the French Jura Mountains : High-Resolution Hydrochemical Characterization During a Flood Event ». Dans EuroKarst 2016, Neuchâtel, 303–17. Cham : Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-45465-8_29.
Texte intégralDelgado, F., M. Manzano, E. Lozano, E. Custodio et C. Coleto. « Hydrochemical characterization of ground and surface waters in 'the Cotos' area, Donana National Park, southwestern Spain ». Dans Groundwater and Human Development. Taylor & Francis, 2005. http://dx.doi.org/10.1201/9781439833599.ch18.
Texte intégralBelghitia, Moulay Lafdil, Abdelkader Chahlaoui, Abdelhak Saidi, Elhammioui Youssef et Driss Bengoumi. « Hydrochemical and microbiological characterization of the waters of some springs in the province of Elhajeb-Morocco ». Dans 1ST INTERNATIONAL CONFERENCE ON GEOGRAPHY AND ENVIRONMENTAL SCIENCES (ICGES’22), 28–36. Sciendo, 2023. http://dx.doi.org/10.2478/9788367405263-005.
Texte intégralActes de conférences sur le sujet "HYDROCHEMICAL CHARACTERIZATION"
Shim, Byoung Ohan, Hanna Choi et Jaeyeon Kim. « Hydrochemical Characterization in Shallow Geothermal System Operation ». Dans Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2366.
Texte intégralMeyers, Zachary, Laura K. Rademacher, Marty D. Frisbee, Sara Warix, Brian Hedlund et Ariel Friel. « DESERT SPRING CHARACTERIZATION FROM HYDROCHEMICAL DATA ANALYSIS ». Dans GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285320.
Texte intégralOyen, Toritseju, et Duke U. Ophori. « HYDROCHEMICAL CHARACTERIZATION OF GROUNDWATER OF THE RARITAN BASIN ». Dans GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-370961.
Texte intégralGoyburo, Cindy, Karla Villamar Marazita, Michelle Villalta, Juan Andrés Cedeño, Tomas Vitvar, Priscila Valverde Armas et Samantha Jiménez Oyola. « Hydrochemical characterization of water in Santa Rosa community, southern Ecuador. » Dans 21st LACCEI International Multi-Conference for Engineering, Education and Technology (LACCEI 2023) : “Leadership in Education and Innovation in Engineering in the Framework of Global Transformations : Integration and Alliances for Integral Development”. Latin American and Caribbean Consortium of Engineering Institutions, 2023. http://dx.doi.org/10.18687/laccei2023.1.1.594.
Texte intégralBeamish, D., B. A. Klinck et J. Trick. « Ground-Truthing Airborne EM – Hydrochemical Characterization of a Coal Mine Plume ». Dans Near Surface 2004 - 10th EAGE European Meeting of Environmental and Engineering Geophysics. European Association of Geoscientists & Engineers, 2004. http://dx.doi.org/10.3997/2214-4609-pdb.10.a010.
Texte intégralTrayanova, Mila. « HYDROCHEMICAL CHARACTERIZATION OF GROUNDWATER IN MESOZOIC AQUIFERS IN CENTRAL NORTHERN BULGARIA ». Dans 19th SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings. STEF92 Technology, 2019. http://dx.doi.org/10.5593/sgem2019/1.2/s02.039.
Texte intégralCardona, Antonio, Socrates Alonso Torres, Socrates Alonso Torres, Guillermo Javier Castro Larragoitia, Guillermo Javier Castro Larragoitia, Jorge Aceves de Alba, Jorge Aceves de Alba, José Joel Carrillo-Rivera et José Joel Carrillo-Rivera. « HYDROCHEMICAL CHARACTERIZATION OF BRACKISH GROUNDWATER IN LOWER RIO BRAVO AQUIFER, TAMAULIPAS, MEXICO ». Dans 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289223.
Texte intégralRascon, Kirstie E., et Barry J. Hibbs. « HYDROCHEMICAL CHARACTERIZATION OF GEOLOGICAL AND ANTHROPOGENIC INPUTS OF SALINITY IN THE EL PASO/JUAREZ VALLEY ». Dans GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359249.
Texte intégralRascon, Kirstie, Barry J. Hibbs et Christopher Eastoe. « HYDROCHEMICAL CHARACTERIZATION OF GEOLOGICAL AND ANTHROPOGENIC INPUTS OF SALINITY IN THE EL PASO/JUAREZ VALLEY ». Dans 116th Annual GSA Cordilleran Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020cd-347548.
Texte intégralCardona, Antonio, Cristian Abraham Rivera-Armendariz, Socrates Alonso Torres et Isidro Montes-Avila. « HYDROCHEMICAL AND ISOTOPIC CHARACTERIZATION OF GROUNDWATER FLOW SYSTEMS IN NORTH-CENTRAL MEXICO : IMPLICATIONS FOR WATER MANAGEMENT ». Dans 54th Annual GSA South-Central Section Meeting 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020sc-343820.
Texte intégralRapports d'organisations sur le sujet "HYDROCHEMICAL CHARACTERIZATION"
Richardson, M. High-resolution landscape characterization for modelling terrestrial-aquatic hydrochemical interactions in Precambrian Shield lake districts : Recommendations for the Lac Dasserat science program. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/297769.
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