1 Presented at Short Course on Surface Exploration for Geothermal Resources, organized by UNU-GTP and LaGeo, in Ahuachapan and Santa Tecla, El Salvador, October, GEOTHERMAL TRAINING PROGRAMME LaGeo S.A. de C.V. SEISMICITY AT THE MIRAVALLES GEOTHERMAL FIELD, COSTA RICA ( ): A TOOL TO CONFIRM THE REAL EXTENSION OF THE RESERVOIR* 1 Paul Moya and 2 Waldo Taylor Instituto Costarricense de Electricidad Apartado Postal San José COSTA RICA 1 2 ABSTRACT The seismicity at the Miravalles geothermal field has been analyzed since This study is divided into four phases, depending on the development of the geothermal field. The periods are the following: a) from January 1994 to May 1998, b) from June 1998 to February 2000, c) from March 2000 to December 2003 and d) from January 2004 to March Before the commissioning of Unit 1, the seismicity did not have a defined pattern related to fault systems, geological structures or reservoir extensions. Once production began in 1994, the first stage shows low seismicity while the second stage shows that seismicity decreased almost completely after a seismic swarm in October 1997, and the geothermal system declined to a seismic quiescence for 16 months. Since the year 2000 (third phase) the seismicity has been increasing again and its main characteristic is that it appears in groups of tens of events with short time intervals (less than one hour), at depths of 2 km, with a coda magnitude (Mc) lower than 2.0, and this especially happens when the total mass produced is lower than 4 X 10 6 ton per month. During the last four years, the seismicity distribution increased and has a better relationship with the fault systems (N-S and NE-SW faults). This has allowed us to clearly identify the reservoir extension and its boundaries. The productioninjection relationship is not that clear yet. This methodology is being used at the Las Pailas geothermal field (new geothermal development) in order to give an idea of the possible boundaries of that reservoir. This new field is different from the Miravalles geothermal field and there is a better relationship between fluid injection and its corresponding seismicity. This methodology can help to better understand the extension of the reservoir, once the geothermal field begins production. The analysis of the seismicity and its contribution to better define the reservoir boundaries is described in the following sections. *This document has been submitted and accepted by the Technical Program Committee to be included in the Proceedings of the World Geothermal Congress 2010 in Bali, Indonesia. 1
2 Moya and Taylor 2 Seismicity at Miravalles 1. INTRODUCTION Costa Rica is located in the southern part of the Central American isthmus, between Nicaragua and Panama. The country extends over an area of approximately 51,000 km 2 and has a population of about 4.5 million. 1.2 Miravalles geothermal field The most important Costa Rican geothermal area is located on the south-western slope of the Miravalles volcano. The present field extends over an area of more than 21 km 2 ; and about 16 km 2 are dedicated to production while 5 km 2 to injection. The temperature of the water-dominated geothermal reservoir is about 240 C. Fifty-three geothermal wells have been drilled to date. They include observation, production and injection wells, with depths ranging from 900 to 3,000 meters. Individual wells produce enough steam to generate between 3 and 12 MW; injection wells accept between 70 and 450 kg/s of separated geothermal fluids each, e.g. Moya (2006). Commercial production of electricity using geothermal steam began at Miravalles in early 1994, when Unit 1, a 55 MW single-flash plant, was commissioned. The following year, the Costa Rican Institute of Electricity (ICE) completed the installation of a 5 MW wellhead unit. This unit was located in the middle of the field for almost 12 years ( ), but in early 2007 it was moved to a new location at the south-eastern part of the field. Two temporary 5 MW wellhead plants came on line as part of an agreement between ICE and the Federal Commission of Electricity of Mexico (CFE) during 1996 and These two temporary units were disassembled in April 1998 and 1999 (Table 1) and returned to CFE. Unit 2, the second 55 MW plant, started production in August 1998 and in March 2000, Unit 3, a 29 MW single-flash private plant, started delivering electricity to the national grid. Finally, Unit 5, a 19 MW binary plant, increased the total installed capacity at Miravalles to 163 MW (Table 1), e.g. Moya and Yock (2007). The history of growth of capacity at the field is shown in Figure 1 and the increase in energy production at the geothermal field is shown in Figure 2. Figure 3 shows the location of the geothermal wells at the Miravalles geothermal field. TABLE 1: Power units at the Miravalles geothermal field; Abbreviations stand for: ICE (Instituto Costarricense de Electricidad); CFE (Comisión Federal de Electricidad, Mexico); WHU (wellhead unit); and BOT (build-operate-transfer) Plant name Power Start-up Shut-down Owner (MW) date date Unit 1 55 ICE 3/1994 WHU-1 5 ICE 1/1995 WHU-2 5 CFE 9/1996 4/1999 WHU-3 5 CFE 2/1997 4/1998 Unit 2 55 ICE 8/1998 Unit 3 29 ICE (BOT) 3/2000 Unit 5 19 ICE 1/2004 Unit 5 extracts additional energy from the separated geothermal brine before it is injected back into the geothermal reservoir. Currently, the total steam delivered to the power plants is about 330 kg/s. Around 1,235 kg/s of residual (separated) geothermal water is sent to injection wells, which are distributed in four areas of the field, i.e., the northern, southern, eastern and south-western sectors. A total of about 150 MW is generated from these quantities of steam and brine.
3 Seismicity at Miravalles 3 Moya and Taylor (Year) FIGURE 1: Geothermal installed capacity ( ) (GWh) 1, , , (Year) 1.2 Las Pailas geothermal field FIGURE 2: Energy production ( ) Due to the excellent results in the production of geothermal energy at the Miravalles geothermal field, ICE is now in the process of developing a new geothermal field on the south-south-western slope of the Rincón de la Vieja volcano. At present there are 9 vertical geothermal wells drilled altogether. The parameters of these wells are shown in Table 7 (See also Figure 4). Two new deviated wells are being drilled at present (PGP-12 and PGP-24). These wells have allowed ICE to define only the southern boundary of the reservoir. The eastern boundary is practically established since ICE is not planning to drill more production wells east of well PGP-02. New deviated wells are being drilled to find the northern and western boundaries of the field as well as the production and injection required for the 35 MW plant. The geothermal area at Las Pailas is next to the Rincón de la Vieja volcano National Park. The boundary of this park sets the northern boundary of the exploitable geothermal area at Las Pailas.
4 Moya and Taylor 4 Seismicity at Miravalles FIGURE 3: Location of the geothermal wells at the Miravalles geothermal field Since in Costa Rica it is not possible to establish any industrial or commercial activity inside a national park, it is not possible to obtain permission to extract energy inside the national park yet. The western boundary is set by a Non-Governmental Organization (NGO) called Guanacaste Dry Forest. This NGO has signed a contractual agreement in which some geothermal development may be allowed, provided the two parties are in agreement. ICE still needs to drill more wells to reach the amount of fluids (steam and brine) that are required by the 35 MW plant. To date (July 2009) there are between 16 and 19 MW on reserve for production (See Table 7); the missing megawatts will be sought towards the northern and western zones of the current production area, e.g. Moya and Pérez (2010).
5 Seismicity at Miravalles 5 Moya and Taylor FIGURE 4: Drilled wells at the Las Pailas geothermal field TABLE 2: Parameters of geothermal wells at Las Pailas geothermal field Well name Depth (m) Temperat. ( C) Enthalpy (kj/kg) Power (MW) PGP-01 1, , PGP-02 1, N. A. N. A. PGP-03 1, , PGP-04 1, PGP-05 1, N. A. N. A. PGP-06 1, N. A. N. A PGP-08 1, PGP-09 1, N. A. N. A. PGP-10 2, N. A N. A
6 Moya and Taylor 6 Seismicity at Miravalles 2. METHODOLOGY The data coming from ICE s departments such as Area de Amenaza y Auscultación Sísmica y Volcánica and the geothermal resources department was utilized to carry out this study. The seismicity was detected using a seismicity network formed by six stations (Lennartz MARS-88) used for the period , which only worked with trigger systems. Later, the stations were changed for stations of continuous record (REFTEK DAS-130) for the period The data utilized at the Miravalles geothermal field is formed of 653 earthquakes that have Root Medium Square (RMS) values of less than 0.2 and a maximum depth of 7 km. For the Las Pailas geothermal field, 318 earthquakes with RMS values of less than 0.2 and a maximum depth of 5 km were used. The analysis of the spatial earthquake distribution is a tool that can be used to define the boundaries of the geothermal reservoir. 3. PRODUCTION PERIODS There have been reports e.g. Barquero (2001a and 2001b) and Taylor (2002, 2003, 2004, and 2006) that indicate that the base micro seismicity at the Miravalles geothermal field is low and it has increased through the years as a response of the exploitation of the field. The exploitation at the Miravalles geothermal field can be divided in four phases: a) Unit 1 from March 1994 to May 1998, b) Unit 2 from June 1998 to February 2000, c) Units 1, 2 and 3 from March 2000 to December 2003 and Units 1, 2, 3 and 5 from January 2004 to March Unit 1 (from March 1994 to May 1998) During this first period, a total of 12 producers (PGM-01, PGM-03, PGM-05, PGM-10, PGM-11, PGM-12, PGM-17, PGM-20, PGM-21, PGM-31, PGM-45, PGM-46) and six injectors (PGM-02, PGM-04, PGM-16, PGM-22, PGM-24, and PGM-26) were utilized to supply the two phase fluid (to the generation units) and to inject the brine, e.g. Moya and Yock (2001). During this period, 24 earthquakes were registered, which indicated a low seismicity, distributed in the centre and northeast of the geothermal field. (Figure 5) The gray dots correspond to injectors, the circles with a cross represent the producers, the back lines (continuous and dash lines) are fractures and the dash lines with triangles represent the caldera border. Also the last lava flow is indicated in this figure. 3.2 Units 1 and 2 (from June 1998 to February 2000) In this second period four producers were added to the exploitation of the field (PGM-08, PGM-42, PGM-43, and PGM-49) as well as three new injectors (PGM-28, PGM-51 and PGM-56). For this period, the injection of the brine was concentrated to the southern sector of the field, around wells PGM-51, PGM-56 and PGM-28, e.g. Moya and Castro (2001 and 2004) and Moya and Yock (2001). In spite of the increase in the quantity of fluids extracted and injected during this second period at the Miravalles geothermal field, the seismicity of the field remained very low, only an additional earthquake took place during this period. This is probably due to the following: a) the injection took place in the southern part of the field and b) a seismic swarm that took place on the south-eastern flank of the Miravalles volcano in 1997 (outside from the boundaries of the Miravalles geothermal field) generated a quiet period (calmness state). This state lasted around 16 months, from November 1998 to April 2000.
7 Seismicity at Miravalles 7 Moya and Taylor FIGURE 5: Location of the earthquakes (black dots) during the first period (Unit 1) at the Miravalles geothermal field 3.3 Units 1, 2 and 3 (from March 2000 to December 2004) During this period, five new producers were utilized to supply the geothermal fluids to the generation units; they were PGM-14, PGM-60, PGM-62, PGM-63, and PGM-65. No extra injection wells were required for this period. The injection in this period was concentrated in wells (PGM-28 and PGM-56, e.g. Moya and Castro (2001 and 2004) and Moya and Yock (2001). The quiet period indicated above, ended in May 2000, only three months after the commissioning of Unit 3, together with full operation of Units 1 and 2. As can be seen in Figure 6 the earthquakes were concentrated in the middle of the field, mainly inside the area limited by the main fractures with the directions N-S and NE-SW, indicating that there is a structural control due to these fractures. In total 99 shallow earthquakes were registered, with an average depth of 1.8 km and with maximum local magnitudes of 3.8 degrees (Richter scale) during 2003 (in general they were all less than 2.1 degrees). 3.4 Units 1, 2, 3 and 5 (from January 2005 to March 2009) This seismicity inside the geothermal field increased during the last years. Figure 7 shows the distribution of the 529 registered earthquakes during this period, where the majority of the earthquakes had local magnitudes of less than 2 degrees. As seen in Figure 7, the seismicity was incremented in the whole area, and this has allowed the establishing of at least two important seismic areas, one in the central and southern part of the field and the other to the northeast of the Miravalles geothermal field.
8 Moya and Taylor 8 Seismicity at Miravalles FIGURE 6: Location of the earthquakes (red dots) during the third period (Units 1, 2 and 3) at the Miravalles geothermal field; the symbols have the same meaning as in Figure 4 FIGURE 7: Location of the earthquakes (red dots) during the last period (Units 1, 2 3 and 5) at the Miravalles geothermal field; the symbols have the same meaning as in Figure 4
9 Seismicity at Miravalles 9 Moya and Taylor 4. RELATIONSHIP BETWEEN THE SEISMICITY AND THE BOUNDARIES OF THE MIRAVALLES GEOTHERMAL FIELD. The exploitation of a geothermal field produces changes in the stress of the geological formations, and therefore, they produce the earthquakes associated with this process. The developed earthquakes will be located inside the affected region, and consequently, they represent an indirect and a good indicator of the extension of the geothermal field. For the Miravalles geothermal field, its associated seismicity seems to indicate that the geothermal field has an L shape, where the major axis has a direction of NNW, 2 km wide, 7 km long, with 2 km thickness, while the minor axis has a direction of NE, 2 km wide, 5 km long and 2 km thickness (see Figures 7, 8 and 9). FIGURE 8: NW Seismicity view in 3D of the Miravalles geothermal field, where the extension of the field can be observed (red dots); the yellow lines represent the injection wells and the blue lines represent the producers FIGURE 9: NE Seismicity view in 3D of the Miravalles geothermal field, where the extension of the field can be observed (red dots); the yellow lines represent the injection wells and the blue lines represent the producers
10 Moya and Taylor 10 Seismicity at Miravalles Figures 8 and 9 show the NW seismicity view and the NE seismicity view in 3D, respectively, for the Miravalles geothermal field. These figures give an idea of the real boundaries of the geothermal system. Also, these figures indicate two seismic nuclei, one in the central-southern sector and the other one in the northeast sector. The identification of these two sectors represents a strong indicator of the existence of a geological or structural barrier between the sectors, affected by the fractures with a NW-SE direction. 5. SEISMICITY AT LAS PAILAS GEOTHERMAL FIELD. As mentioned previously, the Las Pailas geothermal field is being developed these days. The seismic activity in this field has always been related to the injection tests at the geothermal wells. During earthquakes have been registered, the majority of them with local magnitudes of less than 1.7 degrees and with depths less than 3 km. Figure 9 and Figure 10 show the earthquake distribution at the surface and at depth, respectively. The earthquakes have been concentrated in the southwest sector where there is low or no permeability, no production wells are in this sector (PGP-06, PGP-09 and PGP-10 do not produce), the sector is sensitive to the pressure changes in the rock, and this sector is probably related to an area of active faults. Cold water injection perturbs the in-situ stress state, leading to fracture initiation and/or activation of discontinuities such as faults and joints, which often are manifested as multiple micro-seismic events. FIGURE 9: Top view of the Las Pailas geothermal field, where the earthquakes can be observed (red dots); the black lines represent the possible fractures in the zone
11 Seismicity at Miravalles 11 Moya and Taylor As mentioned before, due to the fact that the Las Pailas geothermal field is currently under development and there is no production yet, the boundaries of the reservoir are still unknown. Nevertheless, the unstable area has an extension of 2 x 5 x 2 km and it is due to the injection tests already carried out in the region. The detection and interpretation of micro-seismic events can be monitored and analyzed to provide useful information on the stimulated zone, fracture growth, and geometry of the geological structures and in-situ stress state. The seismicity has been triggered when the injection discharge is greater than 50 l/s and the pressure in the well increase up to 7 bar (Taylor 2009). Probably the future seismic registers will help to determine the current extension of the Las Pailas geothermal field. FIGURE 10: Seismicity view in 3D of the Las Pailas geothermal field, where the earthquakes can be observed (red dots); the black lines represent the geothermal wells 6. CONCLUSIONS The seismicity in a geothermal area can help to determine the real extension of the reservoir. Unfortunately, this tool is helpful only once the boundaries of the geothermal reservoir have been confirmed by drilling or if they are known before hand. Nevertheless, this tool (the earthquake distribution at depth and at surface) helps to verify the real extension of the reservoir in a geothermal area. Even though the seismicity at the Miravalles geothermal field has been small, it has increased during the last years, reaching between earthquakes per year. The spatial earthquake distribution at the Miravalles geothermal field has allowed the defining of the real extension of the field, which has an L shape and embraces a volume of about 20 km 3. The L shape coincides very well with the current pressure decline in the reservoir, e.g. Moya and Nietzen (2010). Due to the fact that the Las Pailas geothermal field is now under development, it has not been possible to determine the extension of the geothermal reservoir. The seismic activity in this field has been related to the induced seismicity provoked by the injection tests in the field. Induced seismicity does not set the boundaries of the geothermal reservoir, it is the seismicity produced by the exploitation of the geothermal reservoir, the one that provides the real extension of the reservoir.
12 Moya and Taylor 12 Seismicity at Miravalles REFERENCES Barquero, R., 2001a: Resumen de la Actividad Sísmica en las Zonas de Miravalles y Arenal durante el año Boletín OSIVAM, San José, Costa Rica, 12th (23-24), 1-6. Barquero, R., 2001b: Resumen de la Actividad Sísmica en las Zonas de Miravalles y Arenal durante el año 2000, Boletín OSIVAM, San José, Costa Rica, 12th (23-24): Moya, P., 2006: Costa Rican geothermal energy development, Proceedings of the Workshop for Decision Makers on Geothermal Projects in Central America, San Salvador, El Salvador, UNU-GTP and LaGeo, CD SC-02, 14 pp. Moya, P. and Castro, S., 2001: Comportamiento de la Presión en el Yacimiento del Campo Geotérmico Miravalles. Reunión No. 19 del Panel de Consultores de Miravalles, Guanacaste, Costa Rica, internal report, March. Moya, P. and Castro, S., 2004: Pressure response to production and injection at the Miravalles geothermal field. Proceedings of the 29 th Workshop on Geothermal Reservoir Engineering, Stanford University, Stanford, Ca. Moya, P., and Pérez, L.D., 2010: Las Pailas geothermal project: A 35 MW Plant. Proceedings of the World Geothermal Congress 2010, Bali, Indonesia, preprint. Moya, P. and Yock, A., 2001: First seven years of exploitation at the Miravalles geothermal field. Proceedings of the 26 th Workshop on Geothermal Reservoir Engineering, Stanford University, Stanford, Ca. Moya, P. and Yock, A., 2007: Assessment and development of the geothermal energy resources of Costa Rica. Proceedings of the Short Course on Geothermal Development in Central America Resource Assessment and Environmental Management, San Salvador, El Salvador,UNU-GTP and La Geo, CD SC-04, 18 pp. Taylor, W., 2002: La actividad sismotectónica Durante el 2001 en los alrededores de los proyectos de generación eléctrica Miravalles. ARCOSA y Tejona, Boletín OSIVAM, San José, Costa Rica 12 (25), 1-9. Taylor, W., 2003: La actividad sismotectónica durante el 2002 en los alrededores de los proyectos de generación eléctrica de Guanacaste. Boletín OSIVAM, San José, Costa Rica, 14 (26), 1-9. Taylor, W., 2004: La actividad sismotectónica durante el 2003 en los alrededores de los proyectos de generación eléctrica Miravalles. ARCOSA y Tejona (Guanacaste), Boletín OSIVAM, San José, Costa Rica, 15 (27), Taylor, W., 2005: La actividad sismotectónica durante el 2004 en los alrededores de los proyectos de generación eléctrica Miravalles. ARCOSA y Tejona (Guanacaste), Boletín OSIVAM, San José, Costa Rica, (28-29, Taylor, W., 2007: La actividad sismotectónica durante el periodo en los alrededores de los proyectos de generación eléctrica Miravalles. ARCOSA y Tejona, Boletín OSIVAM, San José, Costa Rica, 16 (28), Taylor, W., 2009: Informe de la sismicidad durante el 2008 en Borinquen y Las Pailas. Informe Interno, 1-7, San José, Costa Rica.
Proceedings World Geothermal Congress 2015 Melbourne, Australia, 19-25 April 2015 The Initial-State Geochemistry as a Baseline for Geochemical Monitoring at Ulubelu Geothermal Field, Indonesia Mulyanto,
Energy efficient use of geothermal energy sustainable use Prof Dr. Uwe Tröger Conference and fare on renewable energy Granada Nicaragua 17.1. 19.1.2012 Geothermal Energy The optimum environment for a geothermal
Proceedings World Geothermal Congress 2015 Melbourne, Australia, 19-25 April 2015 The Use of Non-Parametric Analysis of Subsoil Temperature Data at the Las Pailas Geothermal Field for Low Impact Geothermal
Geothermal power generation in the Upper Rhine Valley The Project Offenbach/Pfalz Horst Kreuter, Norman Harthill, Michael Judt and Bodo Lehmann Email: email@example.com, firstname.lastname@example.org, email@example.com,
PROCEEDINGS, 41st Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 22-24, 2016 SGP-TR-209 Thermal Modeling of the Mountain Home Geothermal Area Sabodh K.
PROCEEDINGS, Thirty-Fourth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 9-11, 2009 SGP-TR-187 SEISMIC MONITORING OF EGS STIMULATION TESTS AT THE COSO
Proceedings Seventh Workshop Geothermal Reservoir Engineering Stanford, December 1981. SGP-TR-55. T W W WOLUTON OF THE COMPOSTON OF THE FLUD FRO4 SERRAZZANO ZONE (LARDERELLO) Franco D'Amore,Claudio Calore
HEAT TRANSFER IN A LOW ENTHALPY GEOTHERMAL WELL Marcel Rosca University of Oradea, Armata Romana 5, RO-37 Oradea, Romania Key Words: low enthalpy, numerical modeling, wellbore heat transfer, Oradea reservoir,
PROCEEDINGS, 42nd Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 13-15, 2017 SGP-TR-212 Early Identification and Management of Calcite Deposition in the
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
A magnitude 7.3 earthquake struck off the Pacific coast of Central America late Monday night, early reports indicate one death. The earthquake occurred at a depth of 40 km (24.9 miles). Its epicenter was
PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, lifornia, January 3 - February 2, 20 SGP-TR-9 GEOCHEMISTRY CHANGE DURING CIRCULATION TEST OF EGS SYSTEM
STATE OF THE GEOTHERMAL RESOURCES IN BOLIVIA LAGUNA COLORADA PROJECT Zenón Delgadillo Terceros * * Unit Chief Laguna Colorda -ENDE Cochabamba-Bolivia Fax (591)(04) 259509, Telf. 259511 SUMMARY This article
Heat (& Mass) Transfer conceptual models of heat transfer temperature-pressure gradients large scale controls on fluid movement distribution of vapor-saturated conditions fluid flow paths surface manifestations
Proceedings World Geothermal Congress 2010 Bali, Indonesia, 25-29 April 2010 Interpretation of Microseismic Events of Large Magnitudes Collected at Cooper Basin, Australia and at Basel, Switzerland Yusuke
Automated Processing of Earthquake Swarm Records at Very Short Epicentral Distances José M. Cepeda Universidad Centroamericana, (UCA) San Salvador, El Salvador 1 Outline 1) Introduction 2) Strong Motion
Current challenges at CO 2 Sites Ola Eiken et al., Statoil R&D Force seminar on injection safety 4 th December 2013 Offshore Sleipner Onshore In Salah Sub-sea Snøhvit 1 - Classification: External 2010-09-23
Dallas-Fort Worth earthquakes coincident with activity associated with natural gas production Cliff Frohlich and Eric Potter, University of Texas at Austin Chris Hayward and Brian Stump, Southern Methodist
Proceedings World Geothermal Congress 2015 Melbourne, Australia, 19-25 April 2015 Geothermometer, Geoindicator and Isotope Monitoring in Lahendong Wells during 2010-2012 Azka G., Suryanto S. and Yani A.
Proceedings World Geothermal Congress Antalya, Turkey, - April A Poisson s Ratio Distribution From Wadati Diagram as Indicator of Fracturing of Lahendong Geothermal Field, North Sulawesi, Indonesia Silitonga
Presented at Workshop for Decision Makers on Geothermal Projects in Central America, organized by UNU-GTP and LaGeo in San Salvador, El Salvador, 26 November to 2 December 2006. GEOTHERMAL BOREHOLE INVESTIGATIONS
Chapter 6 Conclusions 6.1 Conclusions and perspectives In this thesis an approach is presented for the in-situ characterization of rocks in terms of the distribution of hydraulic parameters (called SBRC
Drought Monitoring in Mainland Portugal 1. Accumulated precipitation since 1st October 2014 (Hydrological Year) The accumulated precipitation amount since 1 October 2014 until the end of April 2015 (Figure
Advantages of Regional and Global Data Exchange Gavin Hayes U.S. Geological Survey, National Earthquake Information Center USGS NEIC Global Earthquake Response Area of responsibility => Global BUT - domestically,
-60- GEOTHERMAL FIELDS ON THE VOLCANIC AXIS OF MEXICO S. Mercado, Instituto de Investigaciones Electricas, M6xico A. GonzSlez, Comisi6n Federal de Electricidad, M6xico INTRODUCTION At present in Mexico,
Proceedings World Geothermal Congress 2015 Melbourne, Australia, 19-25 April 2015 Changes in Injection Well Capacity During Testing and Plant Start-Up at Ngatamariki Jonathon Clearwater, Lutfhie Azwar,
Prof. Giuseppe Mandrone Prof. Cesare Comina dott. Luca Guglielmetti Dept. Earth Science, Univ. Torino (ITA) Multidisciplinary approach of geothermal prospection at Terme di Vinadio/Valdieri (Cuneo - Italy):
GEOTHERMAL TRAINING PROGRAMME Reports 2004 Orkustofnun, Grensásvegur 9, Number 20 IS-108 Reykjavík, Iceland NUMERICAL MODELLING OF THE KAMOJANG GEOTHERMAL SYSTEM, INDONESIA Agus Aromaharmuzi Zuhro PERTAMINA,
Earthquake and Tsunami Disaster Mitigation Research in Colombia International Symposium on Earthquake and Tsunami Disaster Mitigation in Latin America Tokyo March 7, 2014 CONTENTS 1 2 Earthquakes and seismic
Illinois Drought Update, December 1, 2005 DROUGHT RESPONSE TASK FORCE Illinois State Water Survey, Department of Natural Resources For more drought information please go to http://www.sws.uiuc.edu/. SUMMARY.
PROCEEDINGS, Thirty-Ninth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 24-26, 214 SGP-TR-22 A Study on the Production and Reservoir Performance of the
El Nino 2015 in South Sudan: Impacts and Perspectives Raul Cumba El Nino 2015-2016 The El Nino Event of 2015-2016 The 2015/16 El Nino Event Officially declared in March 2015 Now approaching peak intensity
2017-18 SEASONAL RAINFALL FORECAST FOR ZIMBABWE METEOROLOGICAL SERVICES DEPARTMENT 28 August 2017 THE ZIMBABWE NATIONAL CLIMATE OUTLOOK FORUM Introduction The Meteorological Services Department of Zimbabwe
Proceedings World Geothermal Congress 2015 Melbourne, Australia, 19-25 April 2015 Microearthquake (MEQ) Investigation Reveals the Sumatran Fault System in Hululais Geothermal Field, Bengkulu, Indonesia
Overview of Microseismic in Sustainable Monitoring of Geothermal Reservoirs in Indonesia* Bagus Guspudin 1, Febriwan Mohamad 1, and Hetty Triastuty 2 Search and Discovery Article #80347 (2013) Posted December
Issued: 10 th November 2017 Valid Period: December 2017 May 2018 South & South East Asian Region: Indonesia Tobacco Regions 1 A] Current conditions: 1] El Niño-Southern Oscillation (ENSO) ENSO Alert System
RELOCATION OF THE MACHAZE AND LACERDA EARTHQUAKES IN MOZAMBIQUE AND THE RUPTURE PROCESS OF THE 2006 Mw7.0 MACHAZE EARTHQUAKE Paulino C. FEITIO* Supervisors: Nobuo HURUKAWA** MEE07165 Toshiaki YOKOI** ABSTRACT
LV-2016-008 Seismic Monitoring in Krafla November 2014 to November 2015 LV-2016-008 ÍSOR-2016/002 Project no.: 14-0089 January 2016 Key Page LV report no: LV-2016-008 Date: January 2016 Number of pages:
REGIONALIZATION OF PRECIPITATION ANOMALIES ASSOCIATED WITH EL NIÑO EVENTS IN SOUTHERN SOUTH AMERICA ABSTRACT Alice M. Grimm (1); Moira E. Doyle (2) (1) Department of Physics Federal University of Paraná
Geological data for geothermal evaluation: Italy Adele Manzella Italy is a geothermal country Italian National Research Council Earth and Environment Department, Geothermal power production: 8,5 % world
Geothermal Energy in the UK Jon Busby British Geological Survey Outline Geothermal energy in the UK Background to geothermal in the UK context UK geothermal resources Engineered geothermal systems Direct
PROCEEDINGS, Thirty-Eighth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 11-13, 2013 SGP-TR-198 LOCAL SEISMICITY IN THE EXPLOITATION OF LOS HUMEROS GEOTHERMAL
Geothermal Potential of the Kenya Rift: energy estimates based on new data Peter Omenda and Silas Simiyu KenGen 1 Introduction Kenya relies on three major sources of energy in the electricity sub sector:
Proceedings World Geothermal Congress 2010 Bali, Indonesia, 25-9 April 2010 Geology and Hydrothermal Alteration in the Reservoir of the Hellisheiði High Temperature System, SW-Iceland Helga Margrét Helgadóttir,
An Overview of the Tapia Canyon Field Static Geocellular Model and Simulation Study Prepared for Sefton Resources Inc. Jennifer Dunn, Chief Geologist Petrel Robertson Consulting Ltd. Outline Background
FOCAL MECHANISM DETERMINATION OF LOCAL EARTHQUAKES IN MALAY PENINSULA Siti Norbaizura MAT SAID Supervisor: Tatsuhiko HARA MEE10505 ABSTRACT Since November 30, 2007, small local earthquakes have been observed
PROCEEDINGS, Thirty-Eighth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 11-13, 2013 SGP-TR-198 FULL MOMENT TENSOR ANALYSIS USING FIRST MOTION DATA AT
Assessment of Snowpack-Influencing climate Change in the Colorado Rockies and Oregon Cascades using a Simple Winter Precipitation Index Has recent climate change benefited mountain snowpack? Mark Losleben,
UK data for geothermal resource assessments Jon Busby UK data for geothermal resource assessments Outline 1. Data availability 2. Sub-surface temperatures 3. The EGS resource 4. Deep saline aquifers Publicly
Proceedings World Geothermal Congress 2015 Melbourne, Australia, 19-25 April 2015 Geophysics Field Camp (GFC): A Student Project Aimed to Investigate the Low to Moderate Temperature Geothermal System in
1 of 11 4/18/2017 3:42 PM Precipitation NIDIS Intermountain West Drought Early Warning System April 18, 2017 The images above use daily precipitation statistics from NWS COOP, CoCoRaHS, and CoAgMet stations.
AV Detailed Structural Interpretation Using 3D Seismic Curvature Analysis, Neuquen and San Jorge Basins, Argentina* Scott A. Haberman 1, Mariana Aguiar Rolon 2, José Cavero 2, Victor Sancho 2, Miguel Mendez
Proceedings World Geothermal Congress 2010 Bali, Indonesia, 25-29 April 2010 Correlation Between Resistivity Index, Capillary Pressure and Kewen Li Stanford Geothermal Program, Stanford University, Stanford,
Presented at Short Course VII on Exploration for Geothermal Resources, organized by UNU-GTP, GDC and KenGen, at Lake Bogoria and Lake Naivasha, Kenya, Oct. 27 Nov. 18, 2012. GEOTHERMAL TRAINING PROGRAMME
Quantifying Bypassed Pay Through 4-D Post-Stack Inversion* Robert Woock 1, Sean Boerner 2 and James Gamble 1 Search and Discovery Article #40799 (2011) Posted August 12, 2011 *Adapted from oral presentation
Current status of the high enthalpy conventional geothermal fields in Europe and the potential perspectives for their exploitation in terms of EGS A. Manzella CNR IGG, Pisa, Italy Hervé Traineau CFG-Services,
Annað veldi ehf Geothermal Provinces of Kenya David Köndgen and Skuli Johannsson September 29, 2009 OUTLINE Overview Geology of Kenya Excursus: The Wilson Cycle How do rifts form? The world of Platetectonics
The Climate of Seminole County Seminole County is part of the Crosstimbers. This region is a transition region from the Central Great Plains to the more irregular terrain of southeastern Oklahoma. Average
The Climate of Payne County Payne County is part of the Central Great Plains in the west, encompassing some of the best agricultural land in Oklahoma. Payne County is also part of the Crosstimbers in the
Click to view oral presentation (3.00 MB) JAPEX s 60 Years Experience Exploring Volcanic Reservoirs in Japan* Kentaro Takeda 1 and Yasuo Yamada 2 Search and Discovery Article #70297 (2017)** Posted October
NAME DATE PARTNER(S) SHAKE, RATTLE, AND ROLL INVESTIGATING EARTHQUAKES The city of San Francisco was destroyed by a 7.8 magnitude earthquake that ruptured gas lines and set the city ablaze. March 28, 1964
Integration of Uncertain Subsurface Information For Reservoir Modeling Ali Ashat Institut Teknologi Bandung Wednesday, March 5, 2013 Successful appraisal and development of geothermal fields requires the
Chiang Rai Province CC Threat overview AAS1109 Mekong ARCC This threat overview relies on projections of future climate change in the Mekong Basin for the period 2045-2069 compared to a baseline of 1980-2005.
International Journal of ChemTech Research CODEN (USA): IJCRGG ISSN: 0974-4290 Vol.9, No.02 pp 60-64, 2016 Development of wind rose diagrams for Kadapa region of Rayalaseema Anil Kumar Reddy ChammiReddy
SEISMOTECTONIC ANALYSIS OF A COMPLEX FAULT SYSTEM IN ITALY: THE GARFAGNANA-NORTH (NORTHERN TUSCANY) LINE. Eva Claudio 1, Eva Elena 2, Scafidi Davide 1, Solarino Stefano 2, Turino Chiara 1 1 Dipartimento
THE GUANACASTE (COSTA RICA) EARTHQUAKE OF SEPTEMBER 5th, 2012 (Mw 7,6) Rafael Barquero & Wilfredo Rojas National Seismic Network (RSN: UCR-ICE) /University of Costa Rica (UCR) and Costarrican Institute
3D Finite Element Modeling of fault-slip triggering caused by porepressure changes Arsalan Sattari and David W. Eaton Department of Geoscience, University of Calgary Suary We present a 3D model using a
Geofísica Internacional (), ol., 39, Num. 1, pp. 97-11 Solar activity and climate in Central America Esteban Araya, Javier Bonatti and Walter Fernández Laboratory for Atmospheric and Planetary Research,
Proceedings, 6 th African Rift Geothermal Conference Addis Ababa, Ethiopia, 2 nd 4 th November 2016 GEOTHERMAL DEVELOPMENT IN THE COMOROS AND RESULTS OF GEOTHERMAL SURFACE EXPLORATION Mohamed Chaheire,
The Climate of Kiowa County Kiowa County is part of the Central Great Plains, encompassing some of the best agricultural land in Oklahoma. Average annual precipitation ranges from about 24 inches in northwestern
1 Research Update on Solar Polar Fields/Coronal Hole IMF and Large Earthquakes, and a Proposed Method for Quantifying Coronal Hole Geo effectiveness Ben Davidson Space Weather News, LLC & The Mobile Observatory
THERMAL THERMAL AND AND RHEOLOGIC SIGNATURES OF OF HIGH HIGH ENTHALPY ENTHALPY RESOURCES ENGINE ENGINE Workshop Workshop Exploring Exploring high high temperature temperature reservoirs: reservoirs: new
Geo-scientific Data Integration to Evaluate Geothermal Potential Using GIS (A Case for Korosi-Chepchuk Geothermal Prospects, Kenya) Levi Shako and Joseph Mutua Geothermal Development Company, P. O. Box
Proceedings World Geothermal Congress 2010 Bali, Indonesia, 25-29 April 2010 Geology and Hydrothermal Alteration of the Hverahlid HT-System, SW-Iceland Steinþór Níelsson and Hjalti Franzson ISOR Iceland
94. Kuchinoerabujima Continuously Monitored by JMA Latitude: 30 26'36" N, Longitude: 130 13'02" E, Elevation: 657 m (Furudake) (Elevation Point) Overview of Kuchinoerabujima taken from the East on July
AAPG European Region Annual Conference Paris-Malmaison, France 23-24 November 2009 RESOURCES PERSPECTIVES of the SOUTHERN PERMIAN BASIN AREA J.C. DOORNENBAL, TNO Built, Environment and Geosciences, Geological