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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. -
Benchmark 3: Evaluation of Alternatives with Respect to Existing Conditions August 2015
Salton Sea Funding and Feasibility Action Plan Benchmark 3: Evaluation of Alternatives With Respect to Existing Conditions August 2015 Prepared by: Prepared for: This document is prepared as a living document for public review and comment. Comments may be provided to: Salton Sea Authority 82995 Hwy 111, Suite 200 Indio, CA 92201 Email: [email protected] Comments will be reviewed and incorporated as appropriate. If substantive comments are received, a revised document may be produced and distributed. Preferred citation: Salton Sea Authority (2015). Salton Sea Funding and Feasibility Action Plan Benchmark 3 Report: Evaluation of Alternatives With Respect to Existing Conditions, August Report. Revision Record Revisions to this document will be reviewed and approved through the same level of authority as the original document. All changes to the Benchmark 3 Report must be authorized by the Principal in Charge. Date Version Changes January Working Posted on Salton Sea Authority website. 2015 Draft Included changes from draft review by Salton Sea TCT. June 2015 First Updated hydrology section and inflow Complete projections including Figures 48-52, along with Document editorial revisions. August Revision 1 Added this Revision Record. Corrected title of 2015 California Department of Fish and Wildlife and other minor editorial revisions. Updated discussion of historical flows from 2003-present. Tetra Tech, Inc. i August 2015 Executive Summary This report presents a review of Salton Sea restoration alternatives and their components and determine how well they would perform under current and future inflows. Alternatives are considered with respect to existing hydrologic conditions at the Sea, as of 2014, and projected future hydrology. -
Consequences of Drying Lake Systems Around the World
Consequences of Drying Lake Systems around the World Prepared for: State of Utah Great Salt Lake Advisory Council Prepared by: AECOM February 15, 2019 Consequences of Drying Lake Systems around the World Table of Contents EXECUTIVE SUMMARY ..................................................................... 5 I. INTRODUCTION ...................................................................... 13 II. CONTEXT ................................................................................. 13 III. APPROACH ............................................................................. 16 IV. CASE STUDIES OF DRYING LAKE SYSTEMS ...................... 17 1. LAKE URMIA ..................................................................................................... 17 a) Overview of Lake Characteristics .................................................................... 18 b) Economic Consequences ............................................................................... 19 c) Social Consequences ..................................................................................... 20 d) Environmental Consequences ........................................................................ 21 e) Relevance to Great Salt Lake ......................................................................... 21 2. ARAL SEA ........................................................................................................ 22 a) Overview of Lake Characteristics .................................................................... 22 b) Economic -
Lled Basins of the Red
Deep-Sea Research I 46 (1999) 1779}1792 Hydrographic changes during 20 years in the brine-"lled basins of the Red Sea Pierre Anschutz! *,GeH rard Blanc!, Fabienne Chatin", Magali Geiller", Marie-Claire Pierret" !De& partement de Ge& ologie et Oce&anographie (D.G.O.), Universite& Bordeaux 1, CNRS UMR 5805, 33405 Talence Cedex, France "Centre de Ge& ochimie de la Surface, Institut de Ge&ologie, Universite& Louis Pasteur, CNRS UMR 7517, 67084, Strasbourg, France Received 16 June 1998; accepted 8 February 1999 Abstract Many of the deep basins "lled by hot brines in the Red Sea have not been investigated since their discovery in the early 1970s. Twenty years later, in September 1992, six of these deeps were revisited. The temperature and salinity of the Suakin, Port Sudan, Chain B, and Nereus deeps ranged from 23.25 to 44.603C and from 144 to 270&. These values were approximately the same in 1972, indicating that the budget of heat and salt was quite balanced. We measured strong gradients of properties in the transition zone between brines and overlying seawater. The contribution of salinity to the density gradient was more than one order of magnitude higher than the opposite contribution of temperature across the seawater}brine interface. Therefore the interface was extemely stable, and the transfer of properties across it was considered to be controlled mostly by molecular di!usion. We calculate that the di!usional transport of salt from the brines to seawater cannot a!ect signi"cantly the salinity of the brines over a 20 year period, which agrees with the observations. -
Ocean Storage
277 6 Ocean storage Coordinating Lead Authors Ken Caldeira (United States), Makoto Akai (Japan) Lead Authors Peter Brewer (United States), Baixin Chen (China), Peter Haugan (Norway), Toru Iwama (Japan), Paul Johnston (United Kingdom), Haroon Kheshgi (United States), Qingquan Li (China), Takashi Ohsumi (Japan), Hans Pörtner (Germany), Chris Sabine (United States), Yoshihisa Shirayama (Japan), Jolyon Thomson (United Kingdom) Contributing Authors Jim Barry (United States), Lara Hansen (United States) Review Editors Brad De Young (Canada), Fortunat Joos (Switzerland) 278 IPCC Special Report on Carbon dioxide Capture and Storage Contents EXECUTIVE SUMMARY 279 6.7 Environmental impacts, risks, and risk management 298 6.1 Introduction and background 279 6.7.1 Introduction to biological impacts and risk 298 6.1.1 Intentional storage of CO2 in the ocean 279 6.7.2 Physiological effects of CO2 301 6.1.2 Relevant background in physical and chemical 6.7.3 From physiological mechanisms to ecosystems 305 oceanography 281 6.7.4 Biological consequences for water column release scenarios 306 6.2 Approaches to release CO2 into the ocean 282 6.7.5 Biological consequences associated with CO2 6.2.1 Approaches to releasing CO2 that has been captured, lakes 307 compressed, and transported into the ocean 282 6.7.6 Contaminants in CO2 streams 307 6.2.2 CO2 storage by dissolution of carbonate minerals 290 6.7.7 Risk management 307 6.2.3 Other ocean storage approaches 291 6.7.8 Social aspects; public and stakeholder perception 307 6.3 Capacity and fractions retained -
Lawrence Berkeley National Laboratory Recent Work
Lawrence Berkeley National Laboratory Recent Work Title Assessment of high enthalpy geothermal resources and promising areas of Chile Permalink https://escholarship.org/uc/item/9s55q609 Authors Aravena, D Muñoz, M Morata, D et al. Publication Date 2016 DOI 10.1016/j.geothermics.2015.09.001 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Assessment of high enthalpy geothermal resources and promising areas of Chile Author links open overlay panel DiegoAravena ab MauricioMuñoz ab DiegoMorata ab AlfredoLahsen ab Miguel ÁngelParada ab PatrickDobson c Show more https://doi.org/10.1016/j.geothermics.2015.09.001 Get rights and content Highlights • We ranked geothermal prospects into measured, Indicated and Inferred resources. • We assess a comparative power potential in high-enthalpy geothermal areas. • Total Indicated and Inferred resource reaches 659 ± 439 MWe divided among 9 areas. • Data from eight additional prospects suggest they are highly favorable targets. • 57 geothermal areas are proposed as likely future development targets. Abstract This work aims to assess geothermal power potential in identified high enthalpy geothermal areas in the Chilean Andes, based on reservoir temperature and volume. In addition, we present a set of highly favorable geothermal areas, but without enough data in order to quantify the resource. Information regarding geothermal systems was gathered and ranked to assess Indicated or Inferred resources, depending on the degree of confidence that a resource may exist as indicated by the geoscientific information available to review. Resources were estimated through the USGS Heat in Place method. A Monte Carlo approach is used to quantify variability in boundary conditions. -
Okeanos Explorer Rov Dive Summary
OKEANOS EXPLORER ROV DIVE SUMMARY Site Name GB907 Expedition Kelley Elliott/ Coordinator/ Brian Bingham ROV Lead Stephanie Farrington (Biology) Science Team Leads Jamie Austin (Geology) General Area Gulf of Mexico Descriptor Cruise Season Leg Dive Number ROV Dive Name EX1402 3 DIVE02 ROV: Deep Discoverer Equipment Deployed Camera Platform: Seirios CTD Depth Altitude Scanning Sonar USBL Position Heading ROV Measurements Pitch Roll HD Camera 1 HD Camera 2 Low Res Cam 1 Low Res Cam 2 Low Res Cam 3 Low Res Cam 4 Low Res Cam 2 Equipment N/A Malfunctions Dive Summary: EX1402L3_DIVE02 ^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^ In Water at: 2014-04-13T13:45:38.439000 27°, 05.899' N ; 092°, 37.310' W Out Water at: 2014-04-13T19:12:34.841000 27°, 05.096' N ; 092°, 36.588' W ROV Dive Summary Off Bottom at: 2014-04-13T18:24:04.035000 (From processed ROV 27°, 05.455' N ; 092°, 36.956' W data) On Bottom at: 2014-04-13T14:31:16.507000 27°, 05.519' N ; 092°, 37.099' W Dive duration: 5:26:56 Bottom Time: 3:52:47 Max. depth: 1266.7 m Special Notes Primary Jamie Austin, EX, UT Austin, [email protected] Stephanie Farrington, EX, HBOI/FAU, [email protected] Andrea Quattrini, Temple, Temple, [email protected] Scientists Involved Bernie Ball, Duke, Duke, [email protected] (please provide name / Brian Kinlan, NOAA NMFS, [email protected] location / affiliation / email) Carolyn Ruppel, Woods Hole, USGS, [email protected] Erik Cordes, Temple, Temple, [email protected] Larry Mayer, UNH, UNH CCOM, [email protected] Michael Vecchione, -
A Phytoremediation Pilot Project at the LCP Chemicals
Case Study LCP Chemicals Site Phytoremediation Pilot Project Shea Jones Remedial Project Manager EPA Region 4 Outline of Presentation z Background Information z Groundwater Quality z Groundwater Seeps z Project Goal z Implementation of Project z Community and Agency Concerns z Current Status z Next Steps z Lessons Learned Background Information z 550-acre site z Former oil refinery, paint manufacturing co., power plant, and chlor-alkali facility operated from 1919- 1994 z Significant PRP-led removal actions in 1999 ($60 million) z Soil and sediment contaminated with lead, mercury, and PCBs z Fish advisories z Currently in RI/FS phase Groundwater Quality z Multiple rounds of horizontal and vertical well data z Hg levels as high as 330 ppb and Pb as high as 120 ppb z Hg found below a sandstone layer z Caustic Brine Pool below old cell buildings z Removal Action Groundwater Seeps z During conditions of high water table, seepage of groundwater occurs along portions of the shoreline that separates the upland soils from the tidal marsh z Dark brown color z Some COCs present at elevated levels (74 ppb Hg and 60 ppb Pb) Project Goal z To locally suppress the groundwater table (0.9 ft) and therefore, prevent the seeps from recontaminating the marsh z Secondary Goals – Create a root zone that will degrade organic contaminants through microbial degradation – Stabilize metals and take them up (lower mobility and availability) z Insert first scanned picture showing seep location z Insert scanned pics showing conceptual site model Plant Selection z List of potentially applicable plants was examined z List narrowed based on tolerance to site conditions (i.e. -
Algae Flora of Graduation Towers in the Town of Ciechocinek
Ecological Questions 14/2011: 25 – 29 DOI: 10.2478/v10090-011-0007-6 Algae flora of graduation towers in the town of Ciechocinek Marta Luścińska, Malwina Gadziemska Department of Plant Ecology and Nature Protection Nicolaus Copernicus University, Gagarina 9, 87–100 Toruń e-mail: [email protected] Summary. The research was focused on algae occurring on wooden constructions of three graduation towers, which are the main ele- ments of historical salt production technology, located in the health-resort of Ciechocinek in the region of Kujawy. The research also included algae occurring in reservoirs with brine condensed on graduation towers, as well as algae from puddles and the soil under the graduation towers. 52 algae taxa were recorded in the collected material. Representatives of the following phyla were distinguished: 5 taxa of Cyanoprokaryota, 46 taxa of Heterokontophyta (including 44 taxa of diatoms) and 7 taxa of Chlorophyta. Samples from the sites with brine of the lowest salt concentration (4%) turned out to be the most abundant in species. Key words: halophylic algae, diatoms Chlorophyta, Dunalulla, brine, saline soils. 1. Introduction ers no. 1 and 3 (Fig. 1). She reported the occurrence of 44 algae species, mainly diatoms. All the aforementioned studies focused on algae in- The occurrence of algae in the environment with extreme habiting puddles and small water bodies with different de- salinity, such as gradually thickened brine flowing down grees of salinity, located within salt marshes. Whereas the the graduation towers in Ciechocinek, evoked interest present paper aims at investigating the algae flora occur- among researchers already since the end of the 19th cen- ring on construction elements of the graduation towers, as tury. -
Restoration of the Salton Sea Summary Report
RECLAMATION Managing Water in theWest Restoration of the Salton Sea Summary Report U.S. Department of the Interior Bureau of Reclamation Lower Colorado Region September 2007 Mission Statements The mission of the Department of the Interior is to protect and provide access to our Nation’s natural and cultural heritage and honor our trust responsibilities to Indian Tribes and our commitments to island communities. The mission of the Bureau of Reclamation is to manage, develop, and protect water and related resources in an environmentally and economically sound manner in the interest of the American public. Restoration of the Salton Sea Summary Report U.S. Department of the Interior Bureau of Reclamation Lower Colorado Region Boulder City, Nevada September 2007 Salton Sea location map. iii Abbreviations and Acronyms ALL Annualized Loss of Life APF Annualized Probability of Failure AQM air quality mitigation BMPs best management practices CEQA California Environmental Quality Act CVWD Coachella Valley Water District DEIS Draft Environmental Impact Statement DO dissolved oxygen DWR California Department of Water Resources EIR Environmental Impact Report EPA Environmental Protection Agency ERS Ecosystem Restoration Studies H2S hydrogen sulfide IID Imperial Irrigation District IMPLAN IMpact Analysis for PLANning IPCC Intergovernmental Panel on Climate Change LOL loss of life m meters μg/L micrograms per liter maf/yr million acre-feet per year mg/L milligrams per liter msl mean sea level NaCl halite NED national economic development NEPA National Environmental Policy Act NH3 ammonia NWR National Wildlife Refuge OMER&R operation, maintenance, energy, replacement, and risk v Restoration of the Salton Sea Summary Report Abbreviations and Acronyms (continued) P Phosphorus P.L. -
Geothermal Development in Chile
Proceedings World Geothermal Congress 2010 Bali, Indonesia, 25-29 April 2010 Geothermal Development in Chile Alfredo Lahsen1, Nelson Muñoz2 and Miguel Angel Parada1 1Departamento de Geología, Universidad de Chile; 2Empresa Nacional del Petróleo (ENAP) [email protected] Keywords: Country update, geothermal exploration, geothermal exploration in the country between 1995 and government policies. 1999. In 1995, a 274 m deep slim exploratory well drilled in the Nevados de Chillán geothermal area, encountered ABSTRACT wet steam with a temperature of 198°C (Salgado and Raasch, 2002). Geothermal exploration in Chile is currently very active and is driven by the need for energy security. Considering the In January 2000, the Chilean government enacted a fact that Chile has to depend on imports to meet more than Geothermal Law providing the framework for the 75% of its energy requirements, the interest of the exploration and development of geothermal energy in government to encourage the development of the Chile. The law provides the regulations for exploration and geothermal resources has been renewed. In this country, exploitation concessions, which are granted by the Ministry there are more than 300 geothermal areas located along the of Mines. Exploration concessions are valid for two years Chilean Andes, associated with Quaternary volcanism, and can be extended for two more years after completing occurs in the extreme north (17°-28°S) and central-southern 25% of committed budget. Exploitation concessions give part (33°-46°S). Preliminary assessment of the geothermal the exclusive right to own the geothermal power and by potential of these two volcanic-geothermal zones gives a products, to use the land and to transfer or sell it without value in the order of 16,000 MW for at least 50 years from any restriction. -
Gulf Facts: Also Occur Here
Note to Teachers Chemistry in the Gulf of Mexico is a teacher’s instructional guide to accompany the poster of the same title. In this guide, you will find information that relates principles from a basic chemistry class to actual processes occurring in the ocean. This guide will focus on four of these processes. The information and activities are intended for use at the 11-12 grade levels. Additional topics and resources are included at the end of the guide. The Minerals Management Service (MMS) has funded numerous scientific studies to understand better the oceanographic processes in the Gulf of Mexico. This Teacher’s Companion contains information that was gathered during these studies. The MMS is the Federal agency that regulates oil and gas activities on the U.S. Outer Continental Shelf. To learn more about the MMS, please visit our website at www.mms.gov. Author: Mary C. Boatman Graphics: Allan Linker Editors: Michael Dorner Deborah Miller Acknowledgments: We wish to thank Ranell Troxler, a sixth grade teacher in St. Charles Parish, for her review of this document. Where to get the Poster and Teacher’s Companion Copies of the poster and Teacher’s Companion may be obtained from the Public Information Office (MS 5034) at the following address: U.S. Department of the Interior Minerals Management Service Gulf of Mexico OCS Region Public Information Office (MS 5034) 1201 Elmwood Park Boulevard New Orleans, Louisiana 70123-2394 Telephone Number: (504) 736-2519 or 1-800-200-GULF 1 Table of Contents Page Number About This Lesson 3 Where It Fits into the Curriculum 3 Objectives for Students 4 Materials for Students 4 What is Chemical Oceanography? 5 Chemical Oceanography in the Gulf of Mexico 5 Temperature and Salinity Plots 6 Thermocline 6 Suspended Sediments 6 Nutrients 6 Phytoplankton 7 Detrital Rain 7 Hypoxia 7 Currents, Eddies, and Upwelling - The Eddy Graveyard 8 Naturally Occurring Oil Seeps 8 Barite Chimneys 8 Gas Hydrates and Chemosynthetic Communities 9 Naturally Occurring Brine Pools 9 Vocabulary 10 Suggested Topics for Term Papers 11 Activities 1.