Hydrochemistry of groundwater suprapermafrost in the Machu Picchu aquifer

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Machu Picchu Peruvian station is located on King George Island, South Shetland Islands, Antarctic Peninsula. Hydrogeology research were conducted during the austral summer 2015, we took groundwater samples in 7 piezometers for analysis of major and minor components, and dissolved metals. Machu Picch...

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Detalles Bibliográficos
Autores: Ng Cutipa, Wai Long, Masías Alvarez, Pablo Jorge, Cerpa Cornejo, Luis Moroni, Peña Laureano, Fluquer, Torres Gonzalez, Daniel Enrique, Morales Reyna, María del Carmen, Ramos Palomino, Domingo A.
Formato: objeto de conferencia
Fecha de Publicación:2016
Institución:Instituto Geológico, Minero y Metalúrgico
Repositorio:INGEMMET-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.ingemmet.gob.pe:20.500.12544/2668
Enlace del recurso:https://hdl.handle.net/20.500.12544/2668
Nivel de acceso:acceso abierto
Materia:Aguas subterráneas
Hidrogeología
Piezometría
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dc.title.es_PE.fl_str_mv Hydrochemistry of groundwater suprapermafrost in the Machu Picchu aquifer
title Hydrochemistry of groundwater suprapermafrost in the Machu Picchu aquifer
spellingShingle Hydrochemistry of groundwater suprapermafrost in the Machu Picchu aquifer
Ng Cutipa, Wai Long
Aguas subterráneas
Hidrogeología
Piezometría
title_short Hydrochemistry of groundwater suprapermafrost in the Machu Picchu aquifer
title_full Hydrochemistry of groundwater suprapermafrost in the Machu Picchu aquifer
title_fullStr Hydrochemistry of groundwater suprapermafrost in the Machu Picchu aquifer
title_full_unstemmed Hydrochemistry of groundwater suprapermafrost in the Machu Picchu aquifer
title_sort Hydrochemistry of groundwater suprapermafrost in the Machu Picchu aquifer
author Ng Cutipa, Wai Long
author_facet Ng Cutipa, Wai Long
Masías Alvarez, Pablo Jorge
Cerpa Cornejo, Luis Moroni
Peña Laureano, Fluquer
Torres Gonzalez, Daniel Enrique
Morales Reyna, María del Carmen
Ramos Palomino, Domingo A.
author_role author
author2 Masías Alvarez, Pablo Jorge
Cerpa Cornejo, Luis Moroni
Peña Laureano, Fluquer
Torres Gonzalez, Daniel Enrique
Morales Reyna, María del Carmen
Ramos Palomino, Domingo A.
author2_role author
author
author
author
author
author
dc.contributor.author.fl_str_mv Ng Cutipa, Wai Long
Masías Alvarez, Pablo Jorge
Cerpa Cornejo, Luis Moroni
Peña Laureano, Fluquer
Torres Gonzalez, Daniel Enrique
Morales Reyna, María del Carmen
Ramos Palomino, Domingo A.
dc.subject.es_PE.fl_str_mv Aguas subterráneas
Hidrogeología
Piezometría
topic Aguas subterráneas
Hidrogeología
Piezometría
description Machu Picchu Peruvian station is located on King George Island, South Shetland Islands, Antarctic Peninsula. Hydrogeology research were conducted during the austral summer 2015, we took groundwater samples in 7 piezometers for analysis of major and minor components, and dissolved metals. Machu Picchu aquifer is a detrital aquifer and it is composed of glacial, alluvial, marine, fluvial, alluvial fluvial and alluvial glacial deposits. Lithological data in piezometers show that about 3 meters deep, there are 3 horizons (Ng et al., 2015): Horizon H1 (more superficial, permeable and porous soil), Horizon 2 (intermediate, semi-permeable to impermeable) and Horizon 3 (depper horizon, permeable and porous ground where groundwater is stored). Groundwater flow is from South to North. Electrical conductivity in the piezometers are low: 92.45 (PZ-08), 126.1 (PZ-07), 218.0 (PZ-04), 219.2 (PZ-03), 219.6 (PZ-06), 324.4 (PZ-09) and 512.5 uS/cm (PZ-05). Watertypes are mixing: Na-Ca-Cl-SO4 (PZ-08), Ca-Na-SO4-HCO3-Cl (PZ-07), Ca-Na-SO4 (PZ-04), Na-Ca-Mg-SO4-Cl (PZ-03), Ca-Na-SO4-Cl-HCO3 (PZ-06), Na-Ca-Mg-SO4-Cl (PZ-09) and Ca-SO4 (PZ-05). Na and Cl values are related to local recharge by thawing snow. Groundwater has low values of Al, Cu, Sr, He, Li, Mn, Ni and Zn; while values of Sb, As, Be, Bi, Cd, Cr, Sn, Hg, Mo, Ag, Pb, Se, Ti, U y V were below the detection limit.
publishDate 2016
dc.date.accessioned.none.fl_str_mv 2020-07-05T05:42:18Z
dc.date.available.none.fl_str_mv 2020-07-05T05:42:18Z
dc.date.issued.fl_str_mv 2016
dc.type.es_PE.fl_str_mv info:eu-repo/semantics/conferenceObject
format conferenceObject
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12544/2668
dc.identifier.bibliographicCitation.es_PE.fl_str_mv Conference XXXIV SCAR, Kuala Lumpur, 20-30 August 2016. Abstract book
url https://hdl.handle.net/20.500.12544/2668
identifier_str_mv Conference XXXIV SCAR, Kuala Lumpur, 20-30 August 2016. Abstract book
dc.language.iso.es_PE.fl_str_mv eng
language eng
dc.rights.es_PE.fl_str_mv info:eu-repo/semantics/openAccess
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eu_rights_str_mv openAccess
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dc.format.es_PE.fl_str_mv application/pdf
dc.coverage.spatial.es_PE.fl_str_mv Isla Rey Jorge
Antártida
dc.publisher.es_PE.fl_str_mv Scientific Committee on Antarctic Research
dc.publisher.country.es_PE.fl_str_mv MY
dc.source.es_PE.fl_str_mv Instituto Geológico, Minero y Metalúrgico – INGEMMET
Repositorio Institucional INGEMMET
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instname:Instituto Geológico, Minero y Metalúrgico
instacron:INGEMMET
instname_str Instituto Geológico, Minero y Metalúrgico
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spelling Ng Cutipa, Wai LongMasías Alvarez, Pablo JorgeCerpa Cornejo, Luis MoroniPeña Laureano, FluquerTorres Gonzalez, Daniel EnriqueMorales Reyna, María del CarmenRamos Palomino, Domingo A.Isla Rey JorgeAntártida2020-07-05T05:42:18Z2020-07-05T05:42:18Z2016https://hdl.handle.net/20.500.12544/2668Conference XXXIV SCAR, Kuala Lumpur, 20-30 August 2016. Abstract bookMachu Picchu Peruvian station is located on King George Island, South Shetland Islands, Antarctic Peninsula. Hydrogeology research were conducted during the austral summer 2015, we took groundwater samples in 7 piezometers for analysis of major and minor components, and dissolved metals. Machu Picchu aquifer is a detrital aquifer and it is composed of glacial, alluvial, marine, fluvial, alluvial fluvial and alluvial glacial deposits. Lithological data in piezometers show that about 3 meters deep, there are 3 horizons (Ng et al., 2015): Horizon H1 (more superficial, permeable and porous soil), Horizon 2 (intermediate, semi-permeable to impermeable) and Horizon 3 (depper horizon, permeable and porous ground where groundwater is stored). Groundwater flow is from South to North. Electrical conductivity in the piezometers are low: 92.45 (PZ-08), 126.1 (PZ-07), 218.0 (PZ-04), 219.2 (PZ-03), 219.6 (PZ-06), 324.4 (PZ-09) and 512.5 uS/cm (PZ-05). Watertypes are mixing: Na-Ca-Cl-SO4 (PZ-08), Ca-Na-SO4-HCO3-Cl (PZ-07), Ca-Na-SO4 (PZ-04), Na-Ca-Mg-SO4-Cl (PZ-03), Ca-Na-SO4-Cl-HCO3 (PZ-06), Na-Ca-Mg-SO4-Cl (PZ-09) and Ca-SO4 (PZ-05). Na and Cl values are related to local recharge by thawing snow. Groundwater has low values of Al, Cu, Sr, He, Li, Mn, Ni and Zn; while values of Sb, As, Be, Bi, Cd, Cr, Sn, Hg, Mo, Ag, Pb, Se, Ti, U y V were below the detection limit.application/pdfengScientific Committee on Antarctic ResearchMYinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/4.0/deed.esInstituto Geológico, Minero y Metalúrgico – INGEMMETRepositorio Institucional INGEMMETreponame:INGEMMET-Institucionalinstname:Instituto Geológico, Minero y Metalúrgicoinstacron:INGEMMETAguas subterráneasHidrogeologíaPiezometríaHydrochemistry of groundwater suprapermafrost in the Machu Picchu aquiferinfo:eu-repo/semantics/conferenceObjectGeologíaORIGINALNg-Hydrochemistry_groundwater_Machu_Picchu_aquifer.pdfNg-Hydrochemistry_groundwater_Machu_Picchu_aquifer.pdfResumen de pósterapplication/pdf898235https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2668/1/Ng-Hydrochemistry_groundwater_Machu_Picchu_aquifer.pdf70d6a4caa31b3e27ea15b67eb76e7b16MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81567https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2668/2/license.txtecccc10c448afdeacc04912e07a3ed65MD52TEXTNg-Hydrochemistry_groundwater_Machu_Picchu_aquifer.pdf.txtNg-Hydrochemistry_groundwater_Machu_Picchu_aquifer.pdf.txtExtracted texttext/plain1908https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2668/3/Ng-Hydrochemistry_groundwater_Machu_Picchu_aquifer.pdf.txta5354c04a0f4e439a29dfb8300b88b7dMD53THUMBNAILNg-Hydrochemistry_groundwater_Machu_Picchu_aquifer.pdf.jpgNg-Hydrochemistry_groundwater_Machu_Picchu_aquifer.pdf.jpgGenerated Thumbnailimage/jpeg26334https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2668/6/Ng-Hydrochemistry_groundwater_Machu_Picchu_aquifer.pdf.jpg1ad39d73ba378be719128a88be229b62MD5620.500.12544/2668oai:repositorio.ingemmet.gob.pe:20.500.12544/26682022-05-27 12:29:42.343Repositorio Institucional INGEMMETrepositorio@ingemmet.gob.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Hydrochemistry of groundwater suprapermafrost in the Machu Picchu aquifer
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