Lithium Extraction in Argentina: a Case Study on the Social and Environmental Impacts
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Salt Lakes and Pans
SCIENCE FOCUS: Salt Lakes and Pans Ancient Seas, Modern Images SeaWiFS image of the western United States. The features of interest that that will be discussed in this Science Focus! article are labeled on the large image on the next page. (Other features and landmarks are also labeled.) It should be no surprise to be informed that the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) was designed to observe the oceans. Other articles in the Science Focus! series have discussed various oceanographic applications of SeaWiFS data. However, this article discusses geological features that indicate the presence of seas that existed in Earth's paleohistory which can be discerned in SeaWiFS imagery. SeaWiFS image of the western United States. Great Salt Lake and Lake Bonneville The Great Salt Lake is the remnant of ancient Lake Bonneville, which gave the Bonneville Salt Flats their name. Geologists estimate that Lake Bonneville existed between 23,000 and 12,000 years ago, during the last glacial period. Lake Bonneville's existence ended abruptly when the waters of the lake began to drain rapidly through Red Rock Pass in southern Idaho into the Snake River system (see "Lake Bonneville's Flood" link below). As the Earth's climate warmed and became drier, the remaining water in Lake Bonneville evaporated, leaving the highly saline waters of the Great Salt Lake. The reason for the high concentration of dissolved minerals in the Great Salt Lake is due to the fact that it is a "terminal basin" lake; water than enters the lake from streams and rivers can only leave by evaporation. -
Palaeoindian Occupation of the Atacama Desert, Northern Chile
Palaeoindian occupation of the Atacama Desert, northern Chile MARTIN GROSJEAN,1* LAUTARO NU´ N˜ EZ2 and ISABEL CARTAJENA3 1 National Center of Excellence in Research on Climate (NCCR Climate) and Institute of Geography, University of Bern, Bern, Switzerland 2 Instituto de Investigaciones Arqueolo´gicas y Museo, Universidad Cato´lica del Norte, San Pedro de Atacama, Chile 3 Departamento de Antropologı´a, Universidad de Chile, N˜ un˜oa, Santiago de Chile ABSTRACT: Palaeoindian occupation of the Atacama Desert in northern Chile has been found between 12 600 and 10 200 cal. yr BP. The new site at Salar Punta Negra (24 280S/60 530W/ 2976 m) includes about 1000 classifiable, mostly unifacial artefacts and, uniquely, three different diagnostic types of early projectile points. Two of the Lateglacial/early Holocene projectile types have wide distribution and are known from different geographical areas in South America: the Palaeoindian ‘Fell’ fish-tail point mainly from the southern cone of South America, and the triangular ‘Tuina’ points typical of the Puna of the south-central Andes in northern Chile and northwestern Argentina. In addition, we found a third type, a stemmed point typical for the Salar Punta Negra. Fill- ing a large geographical gap of ‘Fell’ occupation, the site at Salar Punta Negra provides evidence for generally much higher mobility and diversity of early cultures, and supports an Andean-Pacific route for early human exploration of South America to the south through the desert at intermediate alti- tudes. Contemporaneous high-amplitude climatic changes were fundamental preconditions to pro- vide adequate environments and habitats, and to make Palaeoindian hunting-gathering occupation possible in the Atacama Desert. -
Lpzsttz Et Al Final Ms.Pdf
Lithium and Brine Geochemistry in the Salars of the Southern Puna, Andean Plateau of Argentina Romina Lucrecia Lopez Steinmetz, Stefano Salvi, Carisa Sarchi, Carla Santamans, Lorena Cecilia Lopez Steinmetz To cite this version: Romina Lucrecia Lopez Steinmetz, Stefano Salvi, Carisa Sarchi, Carla Santamans, Lorena Cecilia Lopez Steinmetz. Lithium and Brine Geochemistry in the Salars of the Southern Puna, Andean Plateau of Argentina. Economic Geology, Society of Economic Geologists, 2020, 115, pp.1079 - 1096. 10.5382/econgeo.4754. hal-02989895 HAL Id: hal-02989895 https://hal.archives-ouvertes.fr/hal-02989895 Submitted on 5 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Lithium and Brine Geochemistry in the Salars of the Southern Puna, 2 Andean Plateau of Argentina 3 4 Romina Lucrecia López Steinmetz 1 *, Stefano Salvi 2 , Carisa Sarchi 1 , Carla Santamans 1 , 5 Lorena Cecilia López Steinmetz 3 6 7 1 CONICET (INECOA), Instituto de Geología y Minería, Universidad Nacional de Jujuy, Av. 8 Bolivia 1661, S.S. de Jujuy 4600, Argentina 9 2 Université de Toulouse, CNRS, GET, IRD, OMP, 14 Av. Edouard Belin, Toulouse 31400, 10 France 11 3 Instituto de Investigaciones Psicológicas (IIPsi-UNC-CONICET), Universidad Nacional de 12 Córdoba, Boulevard de la Reforma y Enfermera Gordillo s/n., 2do piso, Córdoba 5000, 13 Argentina 14 * corresponding author: [email protected] 15 16 Abstract 17 The Andean plateau is a small region of South America extending between northwest 18 Argentina, southwest Bolivia and northern Chile. -
Lithium 2 Under the Microscope
The Trouble with Lithium 2 Under the Microscope Meridian International Research Les Legers 27210 Martainville France Tel: +33 2 32 42 95 49 Fax: +33 2 32 41 39 98 29th May 2008 Copyright Meridian International Research, 2008. All rights reserved. Contents 1 Executive Summary 1 2 Current Production Resources 3 The Lithium Triangle 3 Salar de Atacama 4 Geological Structure 5 Conclusion 10 Salar de Hombre Muerto 11 Salar de Uyuni 11 Geological Structure 13 Production Potential 14 Environmental Factors 15 Conclusion 16 Salar del Rincon 17 Other Brine Resources 20 Clayton Valley 20 China 20 Salar del Olaroz 21 Mineral Resources 21 Western Australia - Greenbushes 21 North Carolina 22 Other Producing Resources 23 Zimbabwe 23 Russian Federation 23 Portugal 24 Canada 24 Brazil 24 Conclusion 24 Meridian International Research 2008 i Contents 3 Future Potential Resources 25 Introduction 25 Mineral Resources 25 Osterbotten, Finland 25 China, Jiajika 26 Democratic Republic of the Congo (Zaire) 26 Hectorite Clays 26 Brines 27 Searles Lake 27 Great Salt Lake 28 Salton Sea 28 Smackover Oilfield Brines, Arkansas 32 Bonneville Salt Flats, Utah 33 Dead Sea 34 Other Chilean/ Argentinian/ Bolivian Salars 34 China 35 Seawater 35 4 Production and Market Factors 39 Introduction 39 Lithium Carbonate Production 40 China 41 Other Areas 41 Current Lithium Market Factors 42 Existing Market Demand 42 Market Projection Scenarios 43 Production of Battery Grade (99.95%) Lithium Carbonate 46 Production Factors 46 Battery Recycling 47 Conclusion 48 5 The Wider Environment 49 Geopolitical Environment 49 Nuclear Fusion 51 Environmental and Ecological Factors 52 6 Conclusion 53 ii Meridian International Research 2008 1 Executive Summary This report analyses recently published1 revisions to Lithium Reserves, analyses realistic Lithium Carbonate production potential from existing and future Lithium resources and discusses major factors of increasing importance in the development of future Lithium production for the Automotive Industry. -
D-116-10 REPORTE DE INFORMACIÓN DE LOS GASODUCTOS NORANDINO, ATACAMA, GAS PACÍFICO Y GAS ANDES Sesión No
Comisión de Regulación de Energía y Gas REPORTE DE INFORMACIÓN DE LOS GASODUCTOS NORANDINO, ATACAMA, GAS PACÍFICO Y GAS ANDES DOCUMENTO CREG-116 1 de octubre de 2010 CIRCULACIÓN: MIEMBROS DE LA COMISIÓN DE REGULACIÓN DE ENERGÍA Y GAS 33 Sesión No. 467 REPORTE DE INFORMACIÓN DE LOS GASODUCTOS NORANDINO, ATACAMA, GAS PACÍFICO Y GAS ANDES El siguiente documento muestra la información de los gasoductos Norandino, Atacama, Gas Pacífico y Gas Andes que se recogió durante las evaluaciones de los datos de esos gasoductos: 1. Información de la Pontificia Universidad Católica de Chile En la dirección http://web.¡na.puc.cl/~power/alumno02/aasmarket/3.2.htm (Fecha: 24.08.2010 y hora: 4: 15 pm) se encontró la siguiente información: Gasoducto zona Norte: Tabla N° 3 Gasoducto Inicio de actividades Tramos Diámetro Capacidad Longitud (Origen/Destino) (puig) (MMm3/día) (km) Gasatacama Jul-99 Cornejo (Salta, Argentina)/ Paso de Jama (frontera) 20 8,5 530 (internacional) Paso de Jama (frontera) / Mejillones 20 8,5 411 Norandino Nov-99 Pichanal (Salta, Argentina) / Paso de Jama (frontera) 20 7,1 450 (Internacional) Paso de Jama (frontera) / Crucero 20 7,1 260 Crucero/Tocopilla 12 1,6 79 Crucero / Quebrada Ordóñez 16 5,5 252 Quebrada Ordóñez / Mejillones 16 3,9 35 Quebrada Ordóñez / Coloso 16 1,6 104 Taltal Diciembre de 1999 Mejillones / La Negra 16 2,4 89 (nacional) (en construcción) La Negra / Paposo (Taltal) 12 3/4 1,8 135 Gasoducto zona Centro Sur: Tabla N° 4 Gasoducto Inicio de actividades Tramos Diámetro Capacidad Longitud (Origen/Destino) (puig) (MMm3/día) (km) GasAndes Ago-97 La Mora (Mendoza, Argentina) / Paso Maipo (frontera) 24 9 313 (internacional) Paso Maipo (frontera) / San Bernardo (City Gate II) 24 9 150 Válvula 17/City Gate I 12 9 4 Electrogas Feb-98 San Bernardo / Maipú 30 4,1 12 (nacional) Maipú / Quillota 24 4,1 111 Km 121 línea principal / Est. -
Versión Taquigráfica Cámara De Senadores De La Nación
REPÚBLICA ARGENTINA VERSIÓN TAQUIGRÁFICA CÁMARA DE SENADORES DE LA NACIÓN REUNIÓN DE LA COMISIÓN DE PRESUPUESTO Y HACIENDA Salón Auditorio — H. Senado de la Nación 21 de octubre de 2008 Presidencia del señor senador Ríos 2 Reunión de la Comisión de Presupuesto y Hacienda – 21/10/08 — En el Salón Auditorio del H. Senado de la Nación, a las 13 y 27 del martes 21 de octubre de 2008: Sr. Presidente (Ríos). — Buenas tardes. Damos inicio al tratamiento de la Ley de Presupuesto para 2009. En esta primera reunión de comisión, habíamos establecido el informe por parte del Ministerio de Infraestructura y Desarrollo Federal. Nos acompañan el ingeniero José Francisco López, secretario de Obras Públicas de la Nación; el arquitecto Luis Bontempo, subsecretario de Desarrollo Urbano y Vivienda; el ingeniero Fabián López, de Recursos Hídricos; el ingeniero Abel Fatala, subsecretario de Obras Públicas de la Nación; el ingeniero Nelson Periotti, administrador de la Dirección Nacional de Vialidad; el ingeniero Edgardo Bortolozzi, administrador del Ente Nacional de Obras Hídricas y Saneamiento; el doctor Pablo Abal Medina, director adjunto de la Unidad Coordinadora de Proyectos y Programas con Financiamiento Externo; el licenciado Fernando Miguel Suárez, director ejecutivo del Organismo Nacional de Administración de Bienes; el señor Carlos Ben, presidente de Aysa; el doctor Carlos Vilas, presidente del Ente Regulador de Aguas y Saneamiento; la ingeniera Emma Albrieu, directora ejecutiva del Órgano de Concesiones Viales; el señor Ariel Santamaría, coordinador de Presupuesto de la Secretaría de Obras Públicas; y el arquitecto Germán Nivello, coordinador de la Unidad Secretario. Para comenzar la reunión, proponemos la siguiente metodología: en primer lugar, expondrá el secretario de Obras Públicas, con un tiempo de aproximadamente quince minutos. -
WIDER Working Paper 2021/18-Are We Measuring Natural Resource
A Service of Leibniz-Informationszentrum econstor Wirtschaft Leibniz Information Centre Make Your Publications Visible. zbw for Economics Lebdioui, Amir Working Paper Are we measuring natural resource wealth correctly? A reconceptualization of natural resource value in the era of climate change WIDER Working Paper, No. 2021/18 Provided in Cooperation with: United Nations University (UNU), World Institute for Development Economics Research (WIDER) Suggested Citation: Lebdioui, Amir (2021) : Are we measuring natural resource wealth correctly? A reconceptualization of natural resource value in the era of climate change, WIDER Working Paper, No. 2021/18, ISBN 978-92-9256-952-5, The United Nations University World Institute for Development Economics Research (UNU-WIDER), Helsinki, http://dx.doi.org/10.35188/UNU-WIDER/2021/952-5 This Version is available at: http://hdl.handle.net/10419/229419 Standard-Nutzungsbedingungen: Terms of use: Die Dokumente auf EconStor dürfen zu eigenen wissenschaftlichen Documents in EconStor may be saved and copied for your Zwecken und zum Privatgebrauch gespeichert und kopiert werden. personal and scholarly purposes. Sie dürfen die Dokumente nicht für öffentliche oder kommerzielle You are not to copy documents for public or commercial Zwecke vervielfältigen, öffentlich ausstellen, öffentlich zugänglich purposes, to exhibit the documents publicly, to make them machen, vertreiben oder anderweitig nutzen. publicly available on the internet, or to distribute or otherwise use the documents in public. Sofern die Verfasser die Dokumente unter Open-Content-Lizenzen (insbesondere CC-Lizenzen) zur Verfügung gestellt haben sollten, If the documents have been made available under an Open gelten abweichend von diesen Nutzungsbedingungen die in der dort Content Licence (especially Creative Commons Licences), you genannten Lizenz gewährten Nutzungsrechte. -
Asx Announcement Galan Acquires Option to Purchase Key Tenement at Hombre Muerto West
ASX ANNOUNCEMENT 15 July 2021 GALAN ACQUIRES OPTION TO PURCHASE KEY TENEMENT AT HOMBRE MUERTO WEST • Option to purchase strategic new tenement executed • Right to acquisition increases flexibility and more area for pond location and infrastructure such as camp and processing plant for HMW • Potential to increase lithium resource to be assessed with geophysics work to follow Galan Lithium Limited (ASX:GLN) (Galan or the Company) is pleased to announce that it has executed a binding Option Agreement (Agreement) with a private Argentinian individual for the purchase of the right to earn a 100% interest in the Casa Del Inca III lithium brine tenement. The acquisition increases and consolidates our Hombre Muerto West (HMW) project footprint located in the South American Lithium Triangle in Catamarca, Argentina (Figure 1). Galan has agreed to initially acquire 300ha for a total of US$150,000 with the initial deposit of US$80,000 being paid. Figure 1 shows that the project abuts the east side of the Pata Pila tenement and highlights the initial 300ha to be purchased under the Agreement plus the total 900ha, if required. Casa del Inca III is located within the world-class, Salar del Hombre Muerto, where Livent Corporation (NYSE:LTHM) is currently producing lithium carbonate and Galaxy Resources Limited (ASX:GXY) is developing its Sal de Vida project. More importantly, it abuts Galan’s Pata Pila interest, which shares the same geology setting forming part of the suite of tenements that comprise the HMW project. The HMW project currently houses a high-grade, low impurity lithium brine resource of ~2.3Mt LCE @ 946mg/l Li. -
ABSTRACTS ACTAS IAGOD 2019 31Ene.Pmd
SALTA, ARGENTINA 28-31 AUGUST 2018 15th Quadrennial International Association on the Genesis of Ore Deposits Symposium SPONSORS PLATINUM SPONSORS GOLD SPONSORS SILVER SPONSORS BRONZE SPONSORS COPPER SPONSORS Co-sponsored by SALTA, ARGENTINA 28-31 AUGUST 2018 15th Quadrennial International Association on the Genesis of Ore Deposits Symposium SYMPOSIUM PROCEEDINGS SCIENTIFIC COMMITTEE CHAIR Lira Raúl – (University of Córdoba – CONICET, Argentina) MEMBERS Bineli-Betsi Thierry – (Botswana International University of Science and Technology) Chang Zhaoshan – (Colorado School of Mines, USA) Cherkasov Sergey – (Vernadsky State Geological Museum of Russian Academy of Sciences) Cook Nigel – (University of Adelaide, Australia) Gozalvez Martín – (Geological and Mining Survey of Argentina) Guido Diego – (CONICET/Austral Gold S.A, Argentina) Lentz David – (University of New Brunswick, Economic Geology Chair) López Luis – (National Atomic Energy Commission, Argentina) Mao Jingwen – (Chinese Academy of Geological Sciences/Hebei GEO University, China) Meinert Larry – (Consultant) Pons Josefina – (IIPG – University of Río Negro – University of Comahue – CONICET, Argentina) Rubinstein Nora – (IGEBa–University of Buenos Aires – CONICET) Sanematsu Kenzo – (Geological Survey of Japan, AIST) Schutesky Della Giustina Maria Emilia – (University of Brasília, Brasil) Tornos Fernando – (Spanish National Research Council – CSIC) Watanabe Yasushi – (Faculty of International Resource Sciences, Akita University, Japan) EDITED BY Daniel Rastelli, Dolores Álvarez, Noelia -
Orthoptera, Acrididae) at Non-Outbreaking and Outbreaking Situations
SHORT COMMUNICATION Longevity and fecundity of Dichroplus maculipennis (Orthoptera, Acrididae) at non-outbreaking and outbreaking situations Yanina Mariottini1, María Laura De Wysiecki1 & Carlos Ernesto Lange1,2 1Centro de Estudios Parasitológicos y de Vectores (UNLP- CCT La Plata- CONICET). Calle 2 Nº 584, Código postal 1900, La Plata, Argentina. [email protected], [email protected] 2Comisión de Investigaciones Científicas provincia de Buenos Aires. [email protected] ABSTRACT. Longevity and fecundity of Dichroplus maculipennis (Orthoptera, Acrididae) at non-outbreaking and outbreaking situations. Dichroplus maculipennis is one of the most characteristic and damaging grasshopper species of Argentina, mainly in areas of the Pampas and Patagonia regions. We estimated and compared the longevity and fecundity of adult female D. maculipennis under controlled conditions (30°C, 14L:10D, 40% RH) from individuals collected as last instar nymphs (VI) in the field and with a known recent history of low and high density conditions. Densities of D. maculipennis at the collecting sites were 0.95 individuals per m2 in 2006 and 46 ind/m2 in 2009, representing non-outbreaking and outbreaking situations, respectively. Adult female longev- ity in 2006 (67.96 ± 3.2 days) was significantly higher (p < 0.05) than in 2009 (37.44 ± 1.98 days). The number of egg-pods per female was 3.32 ± 0.44 for 2006 and 1.62 ± 0.26 for 2009. The average fecundity in 2006 (89.29 ± 11.9 eggs/female) was signifi- cantly greater (p < 0.05) than that in 2009 (36.27 ± 5.82 eggs/female). While it was observed that the oviposition rate was higher in 2006, this difference was not significant (p > 0.05). -
Unraveling the Peruvian Phase of the Central Andes: Stratigraphy, Sedimentology and Geochronology of the Salar De Atacama Basin (22°30-23°S), Northern Chile
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/271538622 Unraveling the Peruvian Phase of the Central Andes: Stratigraphy, sedimentology and geochronology of the Salar de Atacama Basin (22°30-23°S), northern Chile Article in Basin Research · March 2015 DOI: 10.1111/bre.12114 CITATIONS READS 5 127 4 authors: Sebastián Bascuñán Cesar Arriagada University of Chile University of Chile 4 PUBLICATIONS 5 CITATIONS 90 PUBLICATIONS 664 CITATIONS SEE PROFILE SEE PROFILE Jacobus Philippus Le Roux Katja Deckart University of Chile University of Chile 141 PUBLICATIONS 1,668 CITATIONS 28 PUBLICATIONS 610 CITATIONS SEE PROFILE SEE PROFILE All in-text references underlined in blue are linked to publications on ResearchGate, Available from: Jacobus Philippus Le Roux letting you access and read them immediately. Retrieved on: 09 August 2016 EAGE Basin Research (2015) 1–28, doi: 10.1111/bre.12114 Unraveling the Peruvian Phase of the Central Andes: stratigraphy, sedimentology and geochronology of the Salar de Atacama Basin (22°30–23°S), northern Chile Sebastia´ n Bascun˜ a´ n,* Ce´ sar Arriagada,* Jacobus Le Roux*,† and Katja Deckart* *Departamento de Geologıa, Universidad de Chile, Santiago, Chile †Centro de Excelencia en Geotermia de los Andes (CEGA), Universidad de Chile, Santiago, Chile ABSTRACT The Salar de Atacama Basin holds important information regarding the tectonic activity, sedimen- tary environments and their variations in northern Chile during Cretaceous times. About 4000 m of high-resolution stratigraphic columns of the Tonel, Purilactis and Barros Arana Formations reveal braided fluvial and alluvial facies, typical of arid to semi-arid environments, interrupted by scarce intervals with evaporitic, aeolian and lacustrine sedimentation, displaying an overall coarsening- upward trend. -
Late Mesozoic to Paleogene Stratigraphy of the Salar De Atacama Basin, Antofagasta, Northern Chile: Implications for the Tectonic Evolution of the Central Andes
Late Mesozoic to Paleogene stratigraphy of the Salar de Atacama Basin, Antofagasta, Northern Chile: Implications for the tectonic evolution of the Central Andes Constantino Mpodozisa,T,Ce´sar Arriagadab, Matilde Bassoc, Pierrick Roperchd, Peter Cobbolde, Martin Reichf aServicio Nacional de Geologı´a y Minerı´a, now at Sipetrol. SA, Santiago, Chile bDepartamento de Geologı´a, Universidad de Chile, Santiago, Chile cServicio Nacional de Geologı´a y Minerı´a, Santiago, Chile dIRD/Dep. de Geologı´a, Universidad de Chile, Santiago, Chile eGe´osciences-Rennes (UMR6118 du CNRS), France fDepartment of Geological Sciences University of Michigan, United States Abstract The Salar de Atacama basin, the largest bpre-AndeanQ basin in Northern Chile, was formed in the early Late Cretaceous as a consequence of the tectonic closure and inversion of the Jurassic–Early Cretaceous Tarapaca´ back arc basin. Inversion led to uplift of the Cordillera de Domeyko (CD), a thick-skinned basement range bounded by a system of reverse faults and blind thrusts with alternating vergence along strike. The almost 6000-m-thick, upper Cretaceous to lower Paleocene sequences (Purilactis Group) infilling the Salar de Atacama basin reflects rapid local subsidence to the east of the CD. Its oldest outcropping unit (Tonel Formation) comprises more than 1000 m of continental red sandstones and evaporites, which began to accumulate as syntectonic growth strata during the initial stages of CD uplift. Tonel strata are capped by almost 3000 m of sandstones and conglomerates of western provenance, representing the sedimentary response to renewed pulses of tectonic shortening, which were deposited in alluvial fan, fluvial and eolian settings together with minor lacustrine mudstone (Purilactis Formation).