Planning of Geothermal Projects: a Case Study on Central America
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Supply for H Cement
REQUEST OF PROPOSAL FOR EXPRESSION OF INTEREST – SUPPLY OF CLASS H CEMENT. Introduction LaGEO S.A. de C.V. (LAGEO), a power production company of El Salvador, is in the final stages of negotiating a loan with the World Bank (P170089 – financial identifier of the project within the World Bank) to increase the generation of electrical energy based on local geothermal resources. The scope of the project consists of the construction and commissioning of two condensing geothermal plants, one to be installed in the Chinameca geothermal field in eastern El Salvador with a generation capacity of 25 MW and the other to be placed in the San Vicente geothermal field in central El Salvador with a generation capacity of 10 MW. A vital component of these projects is drilling additional geothermal wells, which require the supply of Class H cement supply. This expression of interest request aims to understand the market for the specific requirement for the supply of Class H cement for a total of nine (9) wells in the Chinameca and San Vicente geothermal fields. Likewise, establish communication with interested companies, who will subsequently be informed about the tender process and invited to participate in it. Project Description Chinameca Geothermal Field The Chinameca geothermal field is located 130 km east of San Salvador, the capital city of El Salvador, in the department of San Miguel, within the Pacayal-Limbo volcanic complex. The towns of Chinameca and Nueva Guadalupe, both located to the north of the geothermal field. The supply of Class H cement will be used to drill six (6) geothermal wells. -
OECD Territorial Grids
BETTER POLICIES FOR BETTER LIVES DES POLITIQUES MEILLEURES POUR UNE VIE MEILLEURE OECD Territorial grids August 2021 OECD Centre for Entrepreneurship, SMEs, Regions and Cities Contact: [email protected] 1 TABLE OF CONTENTS Introduction .................................................................................................................................................. 3 Territorial level classification ...................................................................................................................... 3 Map sources ................................................................................................................................................. 3 Map symbols ................................................................................................................................................ 4 Disclaimers .................................................................................................................................................. 4 Australia / Australie ..................................................................................................................................... 6 Austria / Autriche ......................................................................................................................................... 7 Belgium / Belgique ...................................................................................................................................... 9 Canada ...................................................................................................................................................... -
The Unrest of S. Miguel Volcano (El Salvador, CA) 5 New GPS Network Design and Installation A
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Nat. Hazards Earth Syst. Sci. Discuss., 3, 6117–6148, 2015 www.nat-hazards-earth-syst-sci-discuss.net/3/6117/2015/ doi:10.5194/nhessd-3-6117-2015 NHESSD © Author(s) 2015. CC Attribution 3.0 License. 3, 6117–6148, 2015 This discussion paper is/has been under review for the journal Natural Hazards and Earth The unrest of System Sciences (NHESS). Please refer to the corresponding final paper in NHESS if available. S. Miguel volcano (El Salvador, CA) The unrest of S. Miguel volcano A. Bonforte et al. (El Salvador, CA): installation of the monitoring network and observed Title Page volcano-tectonic ground deformation Abstract Introduction Conclusions References 1 2 2 2 2 1 A. Bonforte , D. Hernandez , E. Gutiérrez , L. Handal , C. Polío , S. Rapisarda , Tables Figures and P. Scarlato3 1Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania – Osservatorio Etneo, J I Piazza Roma, 2 95123 Catania, Italy J I 2Ministerio de Medio Ambiente y Recursos Naturales, Kilómetro 5 1/2 Carretera a Santa Tecla, Calle y Colonia Las Mercedes, San Salvador, El Salvador Back Close 3 Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Sismologia e Tettonofisica, Full Screen / Esc Via di Vigna Murata, 605 00143 Roma, Italy Received: 1 August 2015 – Accepted: 13 September 2015 – Published: 9 October 2015 Printer-friendly Version Correspondence to: A. Bonforte ([email protected]) Interactive Discussion Published by Copernicus Publications on behalf of the European Geosciences Union. 6117 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract NHESSD On 29 December 2013, the Chaparrastique volcano in El Salvador, close to the town of S. -
Pacific Offshore Record of Plinian Arc Volcanism in Central America: 2
Article Geochemistry 3 Volume 9, Number 2 Geophysics 8 February 2008 Q02S02, doi:10.1029/2007GC001791 GeosystemsG G ISSN: 1525-2027 AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society Pacific offshore record of plinian arc volcanism in Central America: 2. Tephra volumes and erupted masses S. Kutterolf SFB574 at Kiel University/IFM-GEOMAR, Wischhofstrasse 1-3, D-24148 Kiel, Germany ([email protected]) A. Freundt SFB574 at Kiel University/IFM-GEOMAR, Wischhofstrasse 1-3, D-24148 Kiel, Germany IFM-GEOMAR, Wischhofstrasse 1-3, D-24148 Kiel, Germany W. Pere´z SFB574 at Kiel University/IFM-GEOMAR, Wischhofstrasse 1-3, D-24148 Kiel, Germany [1] Sediment gravity cores collected from the Pacific seafloor offshore Central America contain numerous distal ash layers from plinian-type eruptions at the Central American Volcanic Arc dating back to more than 200 ka. In part 1 of this contribution we have correlated many of those ash layers between cores and with 26 tephras on land. The marine ash layers cover areas of up to 106 km2 in the Pacific Ocean and represent a major fraction (60–90%) of the erupted tephra volumes because the Pacific coast lies within a few tens of kilometers downwind from the volcanic arc. Combining our own mapping efforts on land and published mapping results with our marine data yields erupted volumes of all major tephras along the arc that range from 1 to 420 km3. Recalculated to erupted magma mass, the widespread tephras account for 65% of the total magma output at the arc. -
Miocene to Holocene Marine Tephrostratigraphy Offshore Northern Central America and Southern Mexico: Pulsed Activity of Known Vo
Miocene to Holocene marine tephrostratigraphy offshore northern Central America and southern Mexico: Pulsed activity of known volcanic complexes Schindlbeck, J.C.1, Kutterolf, S.2, Freundt, A.2, Eisele, S. 3, Wang, K.-L.4,5, Frische, M.2 1Heidelberg University, Institute of Earth Sciences, Im Neuenheimer Feld 234-236, 69120 Heidelberg, Germany 2GEOMAR Helmholtz Centre for Ocean Research Kiel, 24148 Kiel, Germany 3 Asian School of the Environment, Nanyang Technological University, Singapore 4Institute of Earth Sciences, Academia Sinica, Taipei 11529, Taiwan 5Department of Geosciences, National Taiwan University, Taipei 106, Taiwan Corresponding author: Julie C. Schindlbeck ([email protected]) Key Points: Stratigraphically classified tephra database of glass compositions with correlations of marine and terrestrial tephra layers New insights into the lifetime of the major volcanic centers in Guatemala and El Salvador and their number of major eruptions Identification of five pulses of enhanced volcanic activity during the Quaternary, the Pliocene, the Late, Middle Miocene and Early This article has been accepted for publication and undergone full peer review but has not been through the copyediting, typesetting, pagination and proofreading process which may lead to differences between this version and the Version of Record. Please cite this article as doi: 10.1029/2018GC007832 © 2018 American Geophysical Union. All rights reserved. Abstract We studied the tephra inventory of fourteen deep sea drill sites of three DSDP and ODP legs drilled offshore Guatemala and El Salvador (Legs 67, 84, 138), and one leg offshore Mexico (Leg 66). Marine tephra layers reach back from the Miocene to the Holocene. We identified 223 primary ash beds and correlated these between the drill sites, with regions along the volcanic arcs, and to specific eruptions known from land. -
USGS Open-File Report 2009-1133, V. 1.2, Table 3
Table 3. (following pages). Spreadsheet of volcanoes of the world with eruption type assignments for each volcano. [Columns are as follows: A, Catalog of Active Volcanoes of the World (CAVW) volcano identification number; E, volcano name; F, country in which the volcano resides; H, volcano latitude; I, position north or south of the equator (N, north, S, south); K, volcano longitude; L, position east or west of the Greenwich Meridian (E, east, W, west); M, volcano elevation in meters above mean sea level; N, volcano type as defined in the Smithsonian database (Siebert and Simkin, 2002-9); P, eruption type for eruption source parameter assignment, as described in this document. An Excel spreadsheet of this table accompanies this document.] Volcanoes of the World with ESP, v 1.2.xls AE FHIKLMNP 1 NUMBER NAME LOCATION LATITUDE NS LONGITUDE EW ELEV TYPE ERUPTION TYPE 2 0100-01- West Eifel Volc Field Germany 50.17 N 6.85 E 600 Maars S0 3 0100-02- Chaîne des Puys France 45.775 N 2.97 E 1464 Cinder cones M0 4 0100-03- Olot Volc Field Spain 42.17 N 2.53 E 893 Pyroclastic cones M0 5 0100-04- Calatrava Volc Field Spain 38.87 N 4.02 W 1117 Pyroclastic cones M0 6 0101-001 Larderello Italy 43.25 N 10.87 E 500 Explosion craters S0 7 0101-003 Vulsini Italy 42.60 N 11.93 E 800 Caldera S0 8 0101-004 Alban Hills Italy 41.73 N 12.70 E 949 Caldera S0 9 0101-01= Campi Flegrei Italy 40.827 N 14.139 E 458 Caldera S0 10 0101-02= Vesuvius Italy 40.821 N 14.426 E 1281 Somma volcano S2 11 0101-03= Ischia Italy 40.73 N 13.897 E 789 Complex volcano S0 12 0101-041 -
Volcanism and Geochemistry in Central America: Progress and Problems M
Volcanism and Geochemistry in Central America: Progress and Problems M. J. Carr1, M.D. Feigenson1, L. C. Patino2 and J.A. Walker3 1Department of Geological Sciences, Rutgers University 2Department of Geological Sciences, Michigan State University 3Department of Geology and Environmental Geosciences, Northern Illinois University Most Central American volcanoes occur in an impressive volcanic front that trends parallel to the strike of the subducting Cocos Plate. The volcanic front is a chain, made of right-stepping, linear segments, 100 to 300 Km in length. Volcanoes cluster into centers, whose spacing is random but averages about 27 Km. These closely spaced, easily accessible volcanic centers allow mapping of geochemical variations along the volcanic front. Abundant back-arc volcanism in southeast Guatemala and central Honduras allow two cross-arc transects. Several element and isotope ratios (e.g. Ba/La, U/Th, B/La, 10Be/9Be, 87Sr/86Sr) that are thought to signal subducted marine sediments or altered MORB consistently define a chevron pattern along the arc, with its maximum in Nicaragua. Ba/La, a particularly sensitive signal, is 130 at the maximum in Nicaragua but decreases out on the limbs to 40 in Guatemala and 20 in Costa Rica, which is just above the nominal mantle value of 15. This high amplitude regional variation, roughly symmetrical about Nicaragua, contrasts with the near constancy, or small gradient, in several plate tectonic parameters such as convergence rate, age of the subducting Cocos Plate, and thickness and type of subducted sediment. The large geochemical changes over relatively short distances make Central America an important margin for seeking the tectonic causes of geochemical variations; the regional variation has both a high amplitude and structure, including flat areas and gradients. -
The History of El Salvador Advisory Board
THE HISTORY OF EL SALVADOR ADVISORY BOARD John T. Alexander Professor of History and Russian and European Studies, University of Kansas Robert A. Divine George W. Littlefield Professor in American History Emeritus, University of Texas at Austin John V. Lombardi Professor of History, University of Florida THE HISTORY OF EL SALVADOR Christopher M. White The Greenwood Histories of the Modern Nations Frank W. Thackeray and John E. Findling, Series Editors Greenwood Press Westport, Connecticut • London Library of Congress Cataloging-in-Publication Data White, Christopher M., 1974– The history of El Salvador / Christopher M. White. p. cm. — (The Greenwood histories of the modern nations, ISSN 1096–2905) Includes bibliographical references and index. ISBN 978–0–313–34928–7 (alk. paper) 1. El Salvador—History. I. Title. II. Series. F1486.W46 2009 972.84—dc22 2008030539 British Library Cataloguing in Publication Data is available. Copyright © 2009 by Christopher M. White All rights reserved. No portion of this book may be reproduced, by any process or technique, without the express written consent of the publisher. Library of Congress Catalog Card Number: 2008030539 ISBN: 978 – 0 –313 –34928 –7 ISSN: 1096 –2905 First published in 2009 Greenwood Press, 88 Post Road West, Westport, CT 06881 An imprint of Greenwood Publishing Group, Inc. www.greenwood.com Printed in the United States of America The paper used in this book complies with the Permanent Paper Standard issued by the National Information Standards Organization (Z39.48–1984). 10987654321 -
El Volcan De Izalco
VOLCAN DC IZALGO v POR JORGB LARDÉ, DIRECTOR DEL OBSERVATORIO SISM0LÔG1C0 DE EL SALVADOR SAN SALVADOR, EL VOLCAN DE IZALCO Viaje geológico a ©se Volcán. — Descripción del mismo y de sus contornos. — Sus últimas erup- ciones, — Origen e historia docu- mentada y crítica de ese Volcán desde el año 1524 hasta nues- tros días (año 1923) POR 10RSE LñRQE, DIRECTOR DEL OBSERVATORIO SISMOLÓGICO DE EL SALVADOR OBRA PUBLICADA POR EL SUPREMO GOBIERNO SAN SALVADOR, G. A., 1923 IMPRENTA NACIONAL AL LECTOR A principios de noviembre de 1920 tuvimos noti- cias de que al pie del Volcán de Izalco, entre él y el Cerro Verde, se había abierto la tierra, y que por las grietas salía lava y se producían grandes explosiones. El fenómeno eruptivo por sí mismo, y el hecho de iniciarse la formación de un nuevo cono volcánico (co- mo decían los partes), eran motivos suficientes- para ir a estudiar de cerca los fenómenos que allí tenían lugar y reunir todos los testimonios que fuera posible acerca del proceso que hasta entonces había seguido. En consecuencia, fui enviado al nuevo centro volcá- nico por el Dr. Hermógenes Alvarado (h.), Subsecreta- rio de Estado, encargado de la Cartera de Instrucción Pública, con el fin de estudiar los nuevos fenómenos eruptivos. La ocasión que me proporcionaba el Dr. Alvarado para completar los estudios que desde 1915 había em- pezado a hacer del Volcán de Izalco, debía ser apro- vechada, y con tal motivo, además de hacer un estudio de los fenómenos eruptivos que tenían lugar, recorrí los contornos, ascendí a la cima del volcán, llevando el instrumental necesario, parte del cual bondadosamente me fue proporcionado por el Dr. -
Ground-Water Resources of the Republic of El Salvador Central America
Ground-Water Resources of the Republic of El Salvador Central America By A. N. SAYRE and G. C. TAYLOR, JR. GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1079-D Geologic and hydrologic studies of water supply as a part of the program of the Health and Sanitation Division of El Salvador UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1951 i i UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary I . GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1.00 (paper cover) CONTENTS Page Abstract_______________________________________________________ 155 Introduction- __ ____________________-_____________-___-,____-.-__-_ 157 Scope and purpose of the investigation________________________ 157 Acknowledgments___ _ _________'_________--________-_--__-____ 157 Historical sketch____________________________________________ 158 Geographic sketch.____________________________________________ 158 Climate_______________._____________________ 159 Physiography___________________________________________________ 162 General features.______-________-_-______---________-_----_-__- 162 Physiographic districts______________________________________ 162 Central highlands__________________________________ 163 Western plateau__-_________-_________-_________-_-_-_____- 168 Eastern uplands..__________-_-___-_-_----__________--____- 169 Northern highlands________________________________________ 169 Coastal plain___________________________________________ 169 -
Geothermal Development in Central America: Opportunities and Difficulties
Presented at “Short Course on Surface Exploration for Geothermal Resources”, organized by UNU-GTP and LaGeo, in Ahuachapan and Santa Tecla, El Salvador, 17-30 October, 2009. GEOTHERMAL TRAINING PROGRAMME LaGeo S.A. de C.V. GEOTHERMAL DEVELOPMENT IN CENTRAL AMERICA: OPPORTUNITIES AND DIFFICULTIES Carlos Pullinger LaGeo S.A. de C.V. 15 Av. Sur, Col. Utila, Santa Tecla, EL SALVADOR [email protected] ABSTRACT Geothermal exploration in Central America began in the 1960’s and electricity generation from this resource, a decade later. Despite a potential capacity of 8 GW available with the present technology and 13 GW using enhanced technology, only a fraction has been developed. Three and a half decades after the initial production began in Ahuachapán, El Salvador; the total installed capacity from geothermal resources in Central America adds up to 530 MW, only about 5% of the total geothermal potential of the region. Clearly, several factors have contributed to the delay in the development of the geothermal resources in the region. Amongst these are political instability, regulatory, institutional, political, economic and financial barriers, which are common problems in the whole region. In order to revert this trend and accelerate the geothermal development in the future, the National Energy Authorities have to take clear actions to promote the development of known high enthalpy resources and invest in basic exploration of low-medium enthalpy resources, in order to fully take advantage of this indigenous source of energy that has several economic, social and environmental advantages over other renewable and non-renewable sources of energy. 1. INTRODUCTION Central America’s location along the tectonically active margin between the Cocos and Caribbean tectonic plates is the main reason for the existence of many high temperature geothermal areas. -
El Salvador Country Update
Proceedings World Geothermal Congress 2005 Antalya, Turkey, 24-29 April 2005 El Salvador Country Update José Antonio Rodríguez and Ada Herrera LaGeo S.A. de C.V., 15 Av. Sur, Colonia Utila, Santa Tecla, El Salvador [email protected], [email protected] Keywords: El Salvador, geothermal development, heat sources are the magma chambers, the structures are electricity market reform, new developments, Ahuachapán, calderas or grabens associated to volcanic activity (mostly Berlín, San Vicente, Chinameca, Obrajuelo. quaternary, but some tertiary), and the reservoirs are formed by infiltration of rainwater into the high part of the volcanic ABSTRACT craters. El Salvador, a country of 6.5 million inhabitants in the heart Temperatures of geothermal resources are 230°C in of Central America, is one of the most densely populated in Ahuachapán, 300°C in Berlín, 250°C in San Vicente, and the Western Hemisphere. Geothermal has been one of the ° main sources of electricity since the mid-1970’s, when there are several resources below 200 C all along the Ahuachapán power plant came on line. Today the country volcanic chain. Depths range from as little as 800m in the has a competitive electricity market, and geothermal shallow areas of Ahuachapán, to about 2800m in the deep sources provide 22% of the electricity needs. parts of Berlín. 1. INTRODUCTION 2. A “STRATEGIC PARTNER” SELECTED FOR GEOTHERMAL The main use for geothermal energy in El Salvador is power generation. There is some potential for direct use to LaGeo, S.A. de C.V. (formerly called Geotérmica dry grains and fruit, but none are as yet a significant Salvadoreña) was separated from the government electric economic activity.