36Cl Chronologies and ELA Reconstructions from the Northern Boundary of the South American Arid Diagonal

Total Page:16

File Type:pdf, Size:1020Kb

36Cl Chronologies and ELA Reconstructions from the Northern Boundary of the South American Arid Diagonal 36Cl Chronologies and ELA reconstructions from the northern boundary of the South American Arid Diagonal A thesis submitted to the Graduate School of the University of Cincinnati in partial fulfillment of the requirements of the degree of Master of Science in the Department of Geology of the McMicken College of Arts and Sciences by Rachel Thornton B.S. (Geology), Kent State University, 2011 Advisory Committee: Dylan Ward, Ph.D. (Committee Chair) Thomas Lowell, Ph.D. Aaron Diefendorf, Ph.D. i ABSTRACT This study focused on glaciation in the South American Arid Diagonal (AD) climatic feature which intersects in the Andes mountain range at approximately 24°S. This NE-SW- trending zone of hyper-aridity separates the Atlantic-sourced Easterly moisture belt from the Pacific-sourced Westerly precipitation in the central Andes. We present new geomorphological maps of the landforms, particularly of glacial moraines across two mountain ranges within the Western Cordillera of the central Andes. Additionally, new 36Cl chronologies using surface exposure dating were produced from two sites near the northern boundary of the modern AD. One site is located in the Cordillera del Tatio at ~21°S (Tatio field site), the other is the southernmost valley in a stratovolcano chain called the Cordón de Puntas Negras at ~24°S (SPN field site). Paleo-ELAs were reconstructed utilizing a two-dimensional numerical model to simulate glaciers over a 90m digital elevation model of the upstream catchment. We find that four glacial stages were present at both field sites sampled. Glacial stabilizations from the El Tatio field site, once assumed Lateglacial in age are on the order of 10- 20 thousand years older than previously published. Tatio ages ranged from ~25 ka to as early as MIS 5. We also found that dated glacial stages from El Tatio and the Puntas Negras are not synchronous with lake highstands on the Altiplano, but projected ages of the younger glacial stages indicate both sites were glaciated during the Tauca phase. Regional comparison indicated the possibility of glacial occupation of the Tatio site into the Lateglacial during the Coipasa phase (12 ka) after rapid deglaciation of the SPN field site. Regional ELA comparisons supported the trend of moisture loss from the NE to SW portions of the climatic AD feature. ii iii ACKNOWLEDGEMENTS First and foremost, I thank my advisor Dr. Dylan Ward for this opportunity, his patience, and for pushing me to accomplish things I once considered out of reach. I’d also like to thank my supportive committee Dr. Thomas Lowell and Dr. Aaron Diefendorf for their feedback, guidance, and encouragement. I would not have made it through this project without the help of my lab group, particularly Chris Sheehan and Jason Cesta for their help collecting and processing my samples, for which I also owe thanks to Sarah Hammer. I’d like to acknowledge Dr. Esteban Sagredo for his advice and help during our field season in Chile. For help, support, much-needed laughter, and friendship I thank my friends inside and outside the Department of Geology. Finally, I’d like to thank my family, particularly my husband Robert Naylor, for supporting me and encouraging me the whole way. This project was funded by a National Science Foundation award from Geomorphology & Land-use Dynamics (GLD) (EAR-1226611) to Dr. Dylan Ward. Additional funding was granted by the Geological Society of America and Association for Women Geoscientists. iv TABLE OF CONTENTS Abstract…………………………………………………………………………………………….i Acknowledgements……………………………………………………………….........................iv List of Figures....................................................................................……………………….........ix List of Tables....................................................................................………………………...........x List of Appendices....................................................................................……………..................xi 1. Introduction..............................................................................................................................1 2. Geologic Background..............................................................................................................4 3. Regional Climate......................................................................................................................6 4. Field Sites................................................................................................................................10 4.1. Site selection...............................................................................................................10 4.2. SPN site.......................................................................................................................10 4.3. Tatio site......................................................................................................................12 5. Literature Review..................................................................................................................14 5.1. Overview.....................................................................................................................14 5.2. Lake and salar basins..................................................................................................14 5.3. Hydrologic budget......................................................................................................16 5.4. Glacial history.............................................................................................................17 6. Methods...................................................................................................................................21 6.1. Cosmogenic surface exposure dating..........................................................................21 6.1.1. Production & scaling..................................................................................22 6.1.2. Limitations of surface exposure dating......................................................24 v 6.2. This study....................................................................................................................26 6.2.1. Sample locations........................................................................................28 6.2.2. Sampling methodology..............................................................................28 6.3. Bulk rock 36Cl sample preparation..............................................................................29 6.3.1. Physical preparation...................................................................................30 6.3.2. Chemical preparation.................................................................................30 6.3.3. Carrier/Isotope dilution..............................................................................31 6.3.4. Dissolution & procedural blank preparation..............................................31 6.3.5. Precipitation...............................................................................................32 6.3.6. Anion exchange chromatography..............................................................33 6.3.7. Final sample preparation............................................................................34 6.3.8. Target preparation for AMS measurement................................................34 6.4. TCN age calculation...................................................................................................35 6.5. Geomorphological mapping methods.........................................................................37 6.6. Numerical modeling methods.....................................................................................42 7. Results 7.1. El Tatio region mapping.............................................................................................43 7.1.1. Tatio site mapping.....................................................................................45 7.2. Puntas Negras region..................................................................................................48 7.2.1. SPN site mapping.......................................................................................50 7.3. Mapping interpretations..............................................................................................53 7.4. Cosmogenic results.....................................................................................................55 7.4.1. SPN ratios..................................................................................................55 7.4.2. Tatio ratios.................................................................................................57 vi 7.4.3. SPN apparent ages.....................................................................................57 7.4.4. Tatio apparent ages....................................................................................58 7.5. Apparent age interpretations: SPN & Tatio................................................................60 7.5.1. Scenario 1...................................................................................................63 7.5.1.a. SPN...............................................................................................63 7.5.1.b. Tatio..............................................................................................64 7.5.2. Scenario 2...................................................................................................65 7.5.2.a. SPN...............................................................................................65
Recommended publications
  • Vegetation and Fire at the Last Glacial Maximum in Tropical South America
    Past Climate Variability in South America and Surrounding Regions Developments in Paleoenvironmental Research VOLUME 14 Aims and Scope: Paleoenvironmental research continues to enjoy tremendous interest and progress in the scientific community. The overall aims and scope of the Developments in Paleoenvironmental Research book series is to capture this excitement and doc- ument these developments. Volumes related to any aspect of paleoenvironmental research, encompassing any time period, are within the scope of the series. For example, relevant topics include studies focused on terrestrial, peatland, lacustrine, riverine, estuarine, and marine systems, ice cores, cave deposits, palynology, iso- topes, geochemistry, sedimentology, paleontology, etc. Methodological and taxo- nomic volumes relevant to paleoenvironmental research are also encouraged. The series will include edited volumes on a particular subject, geographic region, or time period, conference and workshop proceedings, as well as monographs. Prospective authors and/or editors should consult the series editor for more details. The series editor also welcomes any comments or suggestions for future volumes. EDITOR AND BOARD OF ADVISORS Series Editor: John P. Smol, Queen’s University, Canada Advisory Board: Keith Alverson, Intergovernmental Oceanographic Commission (IOC), UNESCO, France H. John B. Birks, University of Bergen and Bjerknes Centre for Climate Research, Norway Raymond S. Bradley, University of Massachusetts, USA Glen M. MacDonald, University of California, USA For futher
    [Show full text]
  • 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.
    [Show full text]
  • Freshwater Diatoms in the Sajama, Quelccaya, and Coropuna Glaciers of the South American Andes
    Diatom Research ISSN: 0269-249X (Print) 2159-8347 (Online) Journal homepage: http://www.tandfonline.com/loi/tdia20 Freshwater diatoms in the Sajama, Quelccaya, and Coropuna glaciers of the South American Andes D. Marie Weide , Sherilyn C. Fritz, Bruce E. Brinson, Lonnie G. Thompson & W. Edward Billups To cite this article: D. Marie Weide , Sherilyn C. Fritz, Bruce E. Brinson, Lonnie G. Thompson & W. Edward Billups (2017): Freshwater diatoms in the Sajama, Quelccaya, and Coropuna glaciers of the South American Andes, Diatom Research, DOI: 10.1080/0269249X.2017.1335240 To link to this article: http://dx.doi.org/10.1080/0269249X.2017.1335240 Published online: 17 Jul 2017. Submit your article to this journal Article views: 6 View related articles View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=tdia20 Download by: [Lund University Libraries] Date: 19 July 2017, At: 08:18 Diatom Research,2017 https://doi.org/10.1080/0269249X.2017.1335240 Freshwater diatoms in the Sajama, Quelccaya, and Coropuna glaciers of the South American Andes 1 1 2 3 D. MARIE WEIDE ∗,SHERILYNC.FRITZ,BRUCEE.BRINSON, LONNIE G. THOMPSON & W. EDWARD BILLUPS2 1Department of Earth and Atmospheric Sciences, University of Nebraska-Lincoln, Lincoln, NE, USA 2Department of Chemistry, Rice University, Houston, TX, USA 3School of Earth Sciences and Byrd Polar and Climate Research Center, The Ohio State University, Columbus, OH, USA Diatoms in ice cores have been used to infer regional and global climatic events. These archives offer high-resolution records of past climate events, often providing annual resolution of environmental variability during the Late Holocene.
    [Show full text]
  • And Gas-Based Geochemical Prospecting Of
    Water- and gas-based geochemical prospecting of geothermal reservoirs in the Tarapacà and Antofagasta regions of northern Chile Tassi, F.1, Aguilera, F.2, Vaselli, O.1,3, Medina, E.2, Tedesco, D.4,5, Delgado Huertas, A.6, Poreda, R.7 1) Department of Earth Sciences, University of Florence, Via G. La Pira 4, 50121, Florence, Italy 2) Departamento de Ciencias Geológicas, Universidad Católica del Norte, Av. Angamos 0610, 1280, Antofagasta, Chile 3) CNR-IGG Institute of Geosciences and Earth Resources, Via G. La Pira 4, 50121, Florence, Italy 4)Department of Environmental Sciences, 2nd University of Naples, Via Vivaldi 43, 81100 Caserta, Italy 5) CNR-IGAG National Research Council, Institute of Environmental Geology and Geo-Engineering, Pzz.e A. Moro, 00100 Roma, Italy. 6) CSIS Estacion Experimental de Zaidin, Prof. Albareda 1, 18008, Granada, Spain. 7) Department of Earth and Environmental Sciences, 227 Hutchinson Hall, Rochester, NY 14627, U.S.A.. Studied area The Andean Central Volcanic Zone, which runs parallel the Central Andean Cordillera crossing from North to This study is mainly focused on the geochemical characteristics of water and gas South the Tarapacà and Antofagasta regions of northern Chile, consists of several volcanoes that have shown phases of thermal fluids discharging in several geothermal areas of northern Chile historical and present activity (e.g. Tacora, Guallatiri, Isluga, Ollague, Putana, Lascar, Lastarria). Such an intense (Fig. 1); volcanism is produced by the subduction process thrusting the oceanic Nazca Plate beneath the South America Plate. The anomalous geothermal gradient related to the geodynamic assessment of this extended area gives El Tatio, Apacheta, Surire, Puchuldiza-Tuya also rise to intense geothermal activity not necessarily associated with the volcanic structures.
    [Show full text]
  • Jürgen Reinmüller
    JÜRGEN REINMÜLLER KLIMAVERHÄLTNISSE IN EXTREMEN HOCHGEBIRGEN DER ERDE Ergebnisse eines Sonderklimamessnetzes Diplomarbeit zur Erlangung des akademischen Grades „Magister der Naturwissenschaften“ an der Naturwissenschaftlichen Fakultät der Karl-Franzens-Universität Graz Betreuung durch: Ao. UNIV. PROF. DR. REINHOLD LAZAR Institut für Geographie und Raumforschung 2010 Eidesstattliche Erklärung 2 Eidesstattliche Erklärung Ich, Jürgen Reinmüller, erkläre hiermit, dass die vorliegende Diplomarbeit von mir selbst und ohne unerlaubte Beihilfe verfasst wurde. Die von mir benutzten Hilfsmittel sind im Literaturverzeichnis am Ende dieser Arbeit aufgelistet und wörtlich oder inhaltlich entnommene Stellen wurden als solche kenntlich gemacht. Admont, im März 2010 Jürgen Reinmüller Vorwort 3 Vorwort Die höchstgelegenen Bereiche der Hochgebirge der Erde weisen bis dato eine außerordentlich geringe Dichte an Klimastationen und damit ein Defizit an verfügbaren Klimadaten auf. Aussagen zu den thermischen Aspekten in den Gipfellagen extremer Hochgebirge jenseits der 6000 m Grenze konnten bis dato nur unbefriedigend erörtert werden. Als staatlich geprüfter Berg- und Schiführer und begeisterter Höhenbergsteiger liegen die beeindruckenden, hochgelegenen Gipfel seit Jahren in meinem Interessensbereich. Zudem sehe ich mich in meinem bergführerischen Arbeitsbereich zunehmend mit den Zeichen des aktuellen Klimawandels konfrontiert. Schmelzende Gletscher oder auftauender Permafrost stellen für Bergsteiger ein nicht unwesentliches Gefahrenpotential dar. Die durch das von Univ. Prof. Dr. Reinhold Lazar ins Leben gerufene Projekt HAMS.net (High Altitude Meteorological Station Network) gewonnenen Daten können künftig bei der Tourenplanung diverser Expeditionen miteinbezogen werden und stellen eine wichtige Grundlage für klimatologische Hochgebirgsforschung in großen Höhen dar. Ich selbst durfte dieses interessante Projekt durch den Data-Logger-Tausch am Aconcagua im Februar 2007 ein wenig unterstützen und werde dem Projekt auch in Zukunft mit Rat und Tat zur Seite stehen.
    [Show full text]
  • 1 the Stratigraphic Record of Changing Hyperaridity in the Atacama Desert Over the 1 Last 10 Ma 2 3 4 5 6 7 8 9 10 11 12 13 14 1
    *Manuscript Click here to view linked References 1 1 The stratigraphic record of changing hyperaridity in the Atacama Desert over the 2 last 10 Ma 3 Alberto Sáez1*; Lluís Cabrera1; Miguel Garcés1, Paul van den Bogaard2, Arturo Jensen3, Domingo 4 Gimeno4 5 1 Departament d’Estratigrafia, Paleontologia i Geociencies Marines, Grup de Geodinàmica i Anàlisi de Conques, 6 Universitat de Barcelona, Spain. *Corresponding author: [email protected] 7 2 GEOMAR | Helmholtz Centre for Ocean Research Kiel, Germany 8 3 Departamento de Ciencias Geológicas. Universidad Católica del Norte. Antofagasta, Chile. 9 4 Departament de Geoquímica, Petrologia i Prospecció Geológica. Universitat de Barcelona, Spain. 10 11 ABSTRACT 12 New radiometric and magnetostratigraphic data from Quillagua and Calama basins (Atacama Desert) 13 indicate that the stratigraphic record over the last 10 Ma includes two hiatuses, lasting approximately 2 and 4 14 million years respectively. These sedimentary gaps are thought to represent prolonged periods of 15 hyperaridity in the region, with absence of sediment production and accumulation in the central depressions. 16 Their remarkable synchrony with Antarctic and Patagonian glacial stages, Humboldt cold current 17 enhancement and cold upwelling waters lead us to suggest long-term climate forcing. Higher frequency 18 climate (orbital precession and eccentricity) forcing is thought to control the sequential arrangement of the 19 lacustrine units deposited at times of lower aridity. Hyperaridity trends appear to be modulated by the activity 20 of the South American Summer Monsoon, which drives precipitation along the high altitude areas to the east 21 of Atacama. This precipitation increase combined with the eastward enlargement of the regional drainage 22 during the late Pleistocene enabled water transfer from these high altitude areas to the low lying closed 23 Quillagua basin and resulted in the deposition of the last widespread saline lacustrine deposits in this 24 depression, before its drainage was open to the Pacific Ocean.
    [Show full text]
  • Field Excursion Report 2010
    Presented at “Short Course on Geothermal Drilling, Resource Development and Power Plants”, organized by UNU-GTP and LaGeo, in Santa Tecla, El Salvador, January 16-22, 2011. GEOTHERMAL TRAINING PROGRAMME LaGeo S.A. de C.V. GEOTHERMAL ACTIVITY AND DEVELOPMENT IN SOUTH AMERICA: SHORT OVERVIEW OF THE STATUS IN BOLIVIA, CHILE, ECUADOR AND PERU Ingimar G. Haraldsson United Nations University Geothermal Training Programme Orkustofnun, Grensasvegi 9, 108 Reykjavik ICELAND [email protected] ABSTRACT South America holds vast stores of geothermal energy that are largely unexploited. These resources are largely the product of the convergence of the South American tectonic plate and the Nazca plate that has given rise to the Andes mountain chain, with its countless volcanoes. High-temperature geothermal resources in Bolivia, Chile, Ecuador and Peru are mainly associated with the volcanically active regions, although low temperature resources are also found outside them. All of these countries have a history of geothermal exploration, which has been reinvigorated with recent changes in global energy prices and the increased emphasis on renewables to combat global warming. The paper gives an overview of their main regions of geothermal activity and the latest developments in the geothermal sector are reviewed. 1. INTRODUCTION South America has abundant geothermal energy resources. In 1999, the Geothermal Energy Association estimated the continent’s potential for electricity generation from geothermal resources to be in the range of 3,970-8,610 MW, based on available information and assuming the use of technology available at that time (Gawell et al., 1999). Subsequent studies have put the potential much higher, as a preliminary analysis of Chile alone assumes a generation potential of 16,000 MW for at least 50 years from geothermal fluids with temperatures exceeding 150°C, extracted from within a depth of 3,000 m (Lahsen et al., 2010).
    [Show full text]
  • Stratigraphy and Correlation of Glacial Deposits of the Rocky Mountains, the Colorado Plateau and the Ranges of the Great Basin
    STRATIGRAPHY AND CORRELATION OF GLACIAL DEPOSITS OF THE ROCKY MOUNTAINS, THE COLORADO PLATEAU AND THE RANGES OF THE GREAT BASIN Gerald M. Richmond u.s. Geological Survey, Box 25046, Federal Center, MS 913, Denver, Colorado 80225, U.S.A. INTRODUCTION glaciations (Charts lA, 1B) see Fullerton and Rich- mond, Comparison of the marine oxygen isotope The Rocky Mountains, Colorado Plateau, and Basin record, the eustatic sea level record, and the chronology and Range Provinces (Fig. 1) together occupy much of of glaciation in the United States of America (this the western interior United States. These regions volume). include approximately 140 mountain ranges that were glaciated during the Pleistocene. Most of the glaciers Historical Perspective were valley glaciers, but ice caps formed on uplands Following early recognition of deposits of two alpine locally. Discussion of the deposits of all of these ranges glaciations (Gilbert, 1890; Ball, 1908; Capps, 1909; would require monographic analysis. To avoid this, Atwood, 1909), deposits of three glaciations gradually representative ranges in each province are reviewed. became widely recognized (Alden, 1912, 1932, 1953; Atwood and Mather, 1912, 1932; Alden and Stebinger, Purpose and Scope 1913; Blackwelder, 1915; Atwood, 1915; Fryxell, 1930; This report summarizes the evidence for correlation Bradley, 1936). Subsequently drift of the intermediate of the Quaternary glacial deposits in 26 broadly glaciation was shown to represent two glacial advances distributed mountain ranges selected on the basis of (Fryxell, 1930; Horberg, 1938; Richmond, 1948, 1962a; availability of detailed information and length of glacial Moss, 1951a; Nelson, 1954; Holmes and Moss, 1955), record. and the older drift was shown to include deposits of Because the glacial deposits rarely are traceable from three glaciations (Richmond, 1957, 1962a, 1964a).
    [Show full text]
  • 1 ENSO-Triggered Floods in South America
    Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2018-107 Manuscript under review for journal Hydrol. Earth Syst. Sci. Discussion started: 3 April 2018 c Author(s) 2018. CC BY 4.0 License. 1 ENSO-triggered floods in South America: 2 correlation between maximum monthly discharges during strong events 3 Federico Ignacio Isla 4 Instituto de Geología de Costas y del Cuaternario (UNMDP-CIC) 5 Instituto de Investigaciones Marinas y Costeras (UNMDP-CONICET) 6 Funes 3350, Mar del Plata 7600, Argentina, +54.223.4754060, [email protected] 7 8 Abstract 9 ENSO-triggered floods altered completely the annual discharge of many watersheds of South America. Anomalous 10 years as 1941, 1982-83, 1997-98 and 2015-16 signified enormous fluvial discharges draining towards the Pacific 11 Ocean, but also to the Atlantic. These floods affected large cities built on medium-latitudinal Andes (Lima, Quito, 12 Salta), but also those located at floodplains, as Porto Alegre, Blumenau, Curitiba, Asunción, Santa Fe and Buenos 13 Aires. Maximum discharge months are particular and easily distinguished along time series from watersheds located 14 at the South American Arid Diagonal. At watersheds conditioned by precipitations delivered from the Atlantic or 15 Pacific anti-cyclonic centers, the ENSO-triggered floods are more difficult to discern. The floods of 1941 affected 16 70,000 inhabitants in Porto Alegre. In 1983, Blumenau city was flooded during several days; and the Paraná River 17 multiplied 15 times the width of its middle floodplain. That year, the Colorado River in Northern Patagonia 18 connected for the last time to the Desagûadero – Chadileuvú - Curacó system and its delta received saline water for 19 the last time.
    [Show full text]
  • 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.
    [Show full text]
  • Energy, Water and Alternatives – Chilean Case Studies
    A Global Context and Shared Implications • Change • Uncertainty • Ambiguity Social • Technical Challenge Technical • Expansion • Constraint • Knowledge • Rapid Pace Suzanne A. Pierce Research Assistant Professor Assistant Director Center for International Energy & Environmental Policy Digital Media Collaboratory Jackson School of Geosciences Center for Agile Technology The University of Texas at Austin The University of Texas at Austin ‘All the instances of scientific development and practice . are as much embedded in politics and cultures as they are creations of the researchers, practitioners, and industries.’ (Paraphrased from Heymann, 2010; Dulay, unpublished image) Common Pool Resources Come into Conflict Integrated Water Resources Management Collaborative processes meld the use of scientific information with citizen participation and technical decision support systems Finding rigorous and effective approaches to science- based resource management and dialogue. IWRM Case Study – Northern Chile Coyahuasi Copper Mine February 2012 Mining Water Energy Multi-Scale Complexity Global demand for Copper drives localized use of energy and water resources Energy and Water Primary Resource Candidates Geothermal: Estimated 3,300 and 16,000 MW potential estimated by the Energy Ministry. Key sites throughout country with highest potential sites currently at Puchuldiza, Tatio, and Tolhuaca. Playa lake: an arid zone feature that is transitional between a playa, which is completely dry most of the year, and a lake (Briere, 2000). In this study, a salar is an internally drained evaporative basin with surface water occurring mostly from spring discharge. Energy Context Installed Capacity: 15.420 MW NextGen: 33.024 MW Per Ministerio de Energía, Perez-Arce, May 2011 Renewables Recurso Eólico Recurso Solar Recurso Hidrológico Recurso Geotérmico (Concesiones) (En desarrollo) Per Ministerio de Energía, Perez-Arce, May 2011 Geothermal Energy Resource Development • Chile has about 3000 volcanoes along the Andes, and ~150 are active.
    [Show full text]
  • Lithium Extraction in Argentina: a Case Study on the Social and Environmental Impacts
    Lithium extraction in Argentina: a case study on the social and environmental impacts Pía Marchegiani, Jasmin Höglund Hellgren and Leandro Gómez. Executive summary The global demand for lithium has grown significantly over recent years and is expected to grow further due to its use in batteries for different products. Lithium is used in smaller electronic devices such as mobile phones and laptops but also for larger batteries found in electric vehicles and mobility vehicles. This growing demand has generated a series of policy responses in different countries in the southern cone triangle (Argentina, Bolivia and Chile), which together hold around 80 per cent of the world’s lithium salt brine reserves in their salt flats in the Puna area. Although Argentina has been extracting lithium since 1997, for a long time there was only one lithium-producing project in the country. In recent years, Argentina has experienced increased interest in lithium mining activities. In 2016, it was the most dynamic lithium producing country in the world, increasing production from 11 per cent to 16 per cent of the global market (Telam, 2017). There are now around 46 different projects of lithium extraction at different stages. However, little consideration has been given to the local impacts of lithium extraction considering human rights and the social and environmental sustainability of the projects. With this in mind, the current study seeks to contribute to an increased understanding of the potential and actual impacts of lithium extraction on local communities, providing insights from local perspectives to be considered in the wider discussion of sustainability, green technology and climate change.
    [Show full text]