Geothermal Development in Kenya: a Country Update - 2012
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Comparative Overview of Gases Discharged from Menengai and Olkaria High Temperature Geothermal Fields, Kenya
Proceedings 5th African Rift geothermal Conference Arusha, Tanzania, 29-31 October 2014 Comparative Overview of Gases Discharged from Menengai and Olkaria High Temperature Geothermal Fields, Kenya 1Jeremiah K., Ochieng L., Mibei G., Kanda K. and Suwai J. Geothermal Development Company P.O.Box 17700 – 20100, Nakuru Kenya [email protected] Key words: Menengai, reservoir characteristics, Olkaria, discharge vapors, triangular diagrams ABSTRACT An analogy of representative gas compositions from wells drilled into the Menengai and Olkaria volcanic geothermal systems is presented in this paper with a view of drawing parallels as well as identifying variances in the characteristics of the reservoirs tapped by the wells. This contribution seeks to provide an insight into the possible processes that govern the composition of well discharge vapors as well as characterize the Menengai and Olkaria geothermal reservoirs. To achieve this, triangular diagrams comprising two major chemical constituents, H2O and CO2, together with other gas species H2S, H2, CH4 and N2 were employed to compare the chemical characteristics of vapors discharged from these two systems. It is found that the Olkaria reservoir fluids generally exhibit high H2O/CO2 ratios relative to the Menengai fluids. This is attributed to variations in CO2 gas content. High H2S content seems to characterize Menengai wells, particularly those that discharge from the vapor dominated zones. This inference is indicative of either a higher flux of magmatic gas or enhanced boiling in the reservoir as a consequence of a higher heat flux. The latter is found to be common in the wells as this inference is also complemented by the significantly high H2 content reported. -
The Central Kenya Peralkaline Province: Insights Into the Evolution of Peralkaline Salic Magmas
The central Kenya peralkaline province: Insights into the evolution of peralkaline salic magmas. Ray Macdonald, Bruno Scaillet To cite this version: Ray Macdonald, Bruno Scaillet. The central Kenya peralkaline province: Insights into the evolution of peralkaline salic magmas.. Lithos, Elsevier, 2006, 91, pp.1-4, 59-73. 10.1016/j.lithos.2006.03.009. hal-00077416 HAL Id: hal-00077416 https://hal-insu.archives-ouvertes.fr/hal-00077416 Submitted on 10 Jul 2006 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. The central Kenya peralkaline province: Insights into the evolution of peralkaline salic magmas R. Macdonalda, and B. Scailletb aEnvironment Centre, Lancaster University, Lancaster LA1 4YQ, UK bISTO-CNRS, 1a rue de la Férollerie, 45071 Orléans cedex 2, France Abstract The central Kenya peralkaline province comprises five young (< 1 Ma) volcanic complexes dominated by peralkaline trachytes and rhyolites. The geological and geochemical evolution of each complex is described and issues related to the development of peralkalinity in salic magmas are highlighted. The peralkaline trachytes may have formed by fractionation of basaltic magma via metaluminous trachyte and in turn generated pantellerite by the same mechanism. Comenditic rhyolites are thought to have formed by volatile-induced crustal anatexis and may themselves have been parental to pantelleritic melts by crystal fractionation. -
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BRIEFING NOTE November 2013 UP IN SMOKE? MAASAI RIGHTS IN THE OLKARIA GEOTHERMAL AREA, KENYA he Olkaria geothermal power generation project is Ttouted as the largest such project in the world. Lo- cated approximately 120 km west of Nairobi, in Nakuru County, Kenya, the Olkaria geothermal field covers ap- proximately 75 sq. km and was gazetted as a Geothermal Resource Area in 1971. Three power stations are cur- rently adding 158 MW1 to the national grid while a fourth is under construction. The Kenya Electricity Generating Company (KENGEN), a wholly-owned state corporation, operates three of the four power stations while Orpower4 Inc, a wholly-owned subsidiary of US-based Ormat Tech- nologies, will operate the fourth. The Olkaria geothermal power projects generate in- come by selling electricity to the Kenya Power and Light- ing Company, a government-owned power distribution monopoly. Olkaria is also registered as a Clean Develop- ment Mechanism (CDM) project under the Kyoto Protocol to the United Nations Framework Convention on Climate Change. 2 The Olkaria geothermal power generation project is being funded by the Government of Kenya, and through loans from the World Bank, European Investment Bank, Deutsche Investitions- und Entwicklungsgesellschaft mbH,3 KfW Entwicklungsbank (KfW Development Bank) and the Overseas Private Investment Corporation.4 While the Olkaria geothermal power project lights up the nation, however, the Maasai people living in the area have consistently raised concerns that the project is dimming their lives. Olkaria has been their only home since the 18th century. And not only are they having to 1 Olkaria I (45 MW) and Olkaria II (65 MW), with a third private plant Olkaria III (48 MW) 2 An international agreement linked to the United Nations Framework Con- vention on Climate Change, which commits its Parties by setting interna- tionally binding emission reduction targets: http://cdm.unfccc.int/Projects/ DB/DNV-CUK1276170328.71/view. -
An Electrical Resistivity Study of the Area Between Mt. Suswa and The
AN ELECTRICAL RESISTIVITY STUDY OF THE AREA BETWEEN MT. SUSWA AND * M THE OLKARIA GEOTHERMAL FIELD, KENYA STEPHEN ALUMASA ONACONACHA IIS TUF.sis n\sS rREEN e e n ACCEPTED m ^ e i t e d ^ fFOE HE DECREE of nd A COt'V M&vA7 BE PLACED IN 'TH& njivk.RSITY LIBRARY. A thesis submitted in accordance with the requirement for partial fulfillment of the V Degree of Master of Science DEPT. OF GEOLOGY UNIVERSITY OF NAIROBI 1989 DECLARATION jhis is my original work and has not b e e n submitted for a degree in any other university S . A . ONACHA The thesis has been submitted for examination with our Knowledge as University Supervisors: /] Mr. E. DINDI ACKNOWLEDGEMENTS I wish to thank my supervisors Dr. M.P. Tole and Mr. E. Dindi for their invaluable help and advice during the course of ray studies. I am grateful to the staff of the Ministry of Energy especially Mr. Kinyariro and Mr. Kilele for their tremendous help during the data acquisition. I also wish to express my appreciation of the University of Nairobi for their MSc Scholarship during my study. I am grateful to the British Council for their fellowship that enabled me to carry out data analysis at the University of Edinburgh. A ^ Finally, I wish to thank the members of my family for their love and understanding during my studies. ABSTRACT The D. C. electrical resistivity study of Suswa-Olkaria region was carried out from July 1987 to November, 1988. The main objective was to evaluate the sub-surface geoelectric structure with a view to determining layers that might be associated with geothermal fluid migrations. -
Project: Menengai Geothermal Development Project Country: Kenya
Language: English Original: English PROJECT: MENENGAI GEOTHERMAL DEVELOPMENT PROJECT COUNTRY: KENYA PROJECT APPRAISAL REPORT November, 2011 Team Leader T. BAH, Senior Power Engineer ONEC.2 3184 Team Members Y. ARFAOUI, Chief Renewable Energy Specialist ONEC.3 2308 K. NTOAMPE, Principal Environmentalist ONEC.3 2707 M. HASSANE, Principal Procurement Specialist KEFO 6243 D. MCIVER, Principal Legal Counsel GECL.1 2678 Project F. KANONDA, Senior Financial Analyst ONEC.2 2723 Appraisal R. ARON, Senior Social Development Specialist ONEC.3 2792 Team E. NGODE, Finance Management Specialist KEFO 6230 A. KLEVCHUK, Financial Modelling Specialist OPSM 1975 Sector Manager E. NEGASH, Officer In Charge ONEC.2 3081 Sector Director H. CHEIKHROUHOU ONEC 2140 Regional Director G. NEGATU OREA 2040 N. KULEMEKA, Chief Socio‐Economist ONEC.3 2336 M. CISSE, Chief Investment Officer OPSM.3 1906 Peer R. CLAUDET, Chief Investment Officer OPSM.3 2666 Reviewers G. MAKAJUMA , Infrastructure Specialist KEFO 6073 Martin Njoroge Mwangi, External Peer Reviewer n/a n/a TABLE OF CONTENTS 1 STRATEGIC THRUST AND RATIONALE .................................................................... 1 1.1 Project Linkages with Country Strategy and Objectives ............................................ 1 1.2 Rationale for Bank Involvement ................................................................................. 1 1.3 Aid Coordination ......................................................................................................... 3 2 PROJECT DESCRIPTION ............................................................................................... -
Alcolapia Grahami ERSS
Lake Magadi Tilapia (Alcolapia grahami) Ecological Risk Screening Summary U.S. Fish & Wildlife Service, March 2015 Revised, August 2017, October 2017 Web Version, 8/21/2018 1 Native Range and Status in the United States Native Range From Bayona and Akinyi (2006): “The natural range of this species is restricted to a single location: Lake Magadi [Kenya].” Status in the United States No records of Alcolapia grahami in the wild or in trade in the United States were found. The Florida Fish and Wildlife Conservation Commission has listed the tilapia Alcolapia grahami as a prohibited species. Prohibited nonnative species (FFWCC 2018), “are considered to be dangerous to the ecology and/or the health and welfare of the people of Florida. These species are not allowed to be personally possessed or used for commercial activities.” Means of Introductions in the United States No records of Alcolapia grahami in the United States were found. 1 Remarks From Bayona and Akinyi (2006): “Vulnerable D2 ver 3.1” Various sources use Alcolapia grahami (Eschmeyer et al. 2017) or Oreochromis grahami (ITIS 2017) as the accepted name for this species. Information searches were conducted under both names to ensure completeness of the data gathered. 2 Biology and Ecology Taxonomic Hierarchy and Taxonomic Standing According to Eschmeyer et al. (2017), Alcolapia grahami (Boulenger 1912) is the current valid name for this species. It was originally described as Tilapia grahami; it has also been known as Oreoghromis grahami, and as a synonym, but valid subspecies, of -
Geology, Hydrothermal Alteration and Fluid Inclusion Studies of Olkaria Domes Geothermal Field, Kenya
Proceedings World Geothermal Congress 2005 Antalya, Turkey, 24-29 April 2005 Geology, Hydrothermal Alteration and Fluid Inclusion Studies of Olkaria Domes Geothermal Field, Kenya John Lagat1, Stefan Arnorsson2 and Hjalti Franzson3 Kenya Electricity Generating Company Ltd, Olkaria Geothermal Project, P. O. Box 785, Naivasha 20117, Kenya1 University of Iceland, Science Institute, Dunhagi IS 101 Reykjavik, Iceland2 Icelandic Geosurvey, Grensasvegur 9, IS 108 Reykjavik, Iceland3 [email protected], [email protected], [email protected] Keywords: Kenya Rift, Olkaria Domes, Geothermal, The Greater Olkaria geothermal area is within the Greater Geology, Hydrothermal Alteration, Fluid Inclusion Olkaria volcanic complex. It is subdivided into seven fields for geothermal development purposes namely Olkaria East, ABSTRACT Olkaria Northeast, Olkaria Central, Olkaria Northwest, Olkaria Southwest, Olkaria Southeast and Olkaria Domes Three geothermal exploration wells OW-901, OW-902 and (Figure 2). OW-903 were drilled in Olkaria Domes field to evaluate its geothermal potential. The three wells were drilled to a o depth of 2200 m and all encountered a high temperature 38 E North Island system and discharged on test. Rocks encountered in the 4oN wells include pyroclastics, rhyolite, tuff, trachyte, basalt L. Turkana ETHIOPIA and minor dolerite and microsyenite intrusives. Little or no Central Island hydrothermal alteration is observed in the upper parts of the wells but in the deeper parts, hydrothermal alteration ranged from high to extensive. The most important hydrothermal alteration controls in the field are South Island temperature, rock types and permeability. Four Cenozoic Barrier Volcano volcanics hydrothermal alteration zonations can be recognized in the UGANDA Namarunu field based on the distribution of the hydrothermal alteration minerals. -
Direct Utilization of Geothermal Resources in Kenya
Proceedings World Geothermal Congress 2010 Bali, Indonesia, 25-29 April 2010 Direct Utilization of Geothermal Resources in Kenya John Lagat Kenya Electricity Generating Company Ltd, P. O. Box 785 Naivasha 20117 E-mail: [email protected] Keywords: Geothermal, direct use, balneology, space 38oE heating, greenhouses, agriculture, aquaculture, industrial North Island processes 4oN L. Turkana ETHIOPIA ABSTRACT Central Island Geothermal resources in Kenya are mainly located along the Kenyan Rift, which is part of the eastern arm of the South Island African Rift. The primary forms of utilization of Cenozoic Barrier Volcano geothermal energy in Kenya currently are mainly electric volcanics power generation (168 MWe) and direct uses (~18 MWt) to UGANDA Namarunu a small extent. Though about 99% of geothermal utilization in the country is generation of electricity, direct uses are Emuruangogolak gaining momentum in various parts of the country. Farmers Mt. Elgon Silali have for decades, used geothermal heat to dry pyrethrum Paka KENYA Korosi flowers and condense steam for drinking at Eburru while L. Baringo Nyambeni the Oserian Development Company in Naivasha is using Arus-Bogoria geothermal energy to heat 50 hectares of greenhouses of cut Kisumu Oo roses for export. A tourist hotel at Lake Bogoria is utilizing Menengai Mt. Kenya spring water at 38°C to heat a spa pool. Despite the Eburru availability and enormous potential in direct use L. Naivasha applications, little use has been made of low enthalpy fluids Olkaria Longonot in Kenya. This paper therefore discusses direct use Suswa applications and available opportunities in swimming, Ol'Esakut Nairobi bathing, balneology, agricultural, aquiculture and in Olorgesaille o residential and industrial sectors L. -
Working Paper Or Information Paper
APIRG/19 WP/14 Appendix 3.2J INTERNATIONAL CIVIL AVIATION ORGANIZATION VOLCANIC ASH CONTINGENCY PLAN AFI REGION First Edition - October 2012 THIS DOCUMENT IS ISSUED BY THE DAKAR AND NAIROBI ICAO REGIONAL OFFICES UNDER THE AUTHORITY OF THE APIRG 1 Page 2 of 32 Volcanic Ash Contingency Plan – AFI Region FOREWARD Within and adjacent to the Africa and Indian Ocean (AFI) Region there are areas of volcanic activities which are likely to affect flight in the AFI Region. The major volcanoes in the region are located in the following States: Algeria, Cameroon, Cape Verde Islands, Chad, Comoros Island, Democratic Republic of Congo, Djibouti, Eritrea, Ethiopia, France (Reunion Island), Kenya, Madagascar, Mali, Niger, Nigeria, Rwanda, Sao Tome and Principe, Spain (Canary Islands, Madeira), Sudan, Tanzania and Uganda. The names of the concerned volcano are listed in APPENDIX K (source: Smithsonian Institution). This document is the AFI Air Traffic Management (ATM) Volcanic Ash Contingency Plan which sets out standardised guidelines and procedures for the provision of information to airlines and en-route aircraft before and during a volcanic eruption. Volcanic contamination, of which volcanic ash is the most serious, is a hazard for safe flight operations. Mitigating the hazards posed by volcanic ash in the atmosphere and/or at the aerodrome cannot be resolved in isolation but through collaborative decision-making (CDM) involving all stakeholders concerned. During an eruption volcanic contamination can reach and exceed the cruising altitudes of turbine-powered -
Geology Area South of Magadi
_£I Report No. 61 GOVERNMENT OF KENYA MINISTRY OF COMMERCE AND INDUSTRY GEOLOGICAL SURVEY OF KENYA GEOLOGY OF THE AREA SOUTH OF MAGADI DEGREE SHEET 58, N.W. QUARTER (with coloured geological map) by B. H. BAKER, B.Sc, F.G.S. Geologist Eight Shillings - 1963 "ISfiICrLIBSARY ïIE-- :i963l4 j». ^itfageningen _ .The'Netherlands Li / J Scanned from original by ISRIC - World Soil Information, as ICSU World Data Centre for Soils. The purpose is to make a safe depository for endangered documents and to make the accrued information available for consultation, following Fair Use Guidelines. Every effort is taken to respect Copyright of the materials within the archives where the identification of the Copyright holder is clear and, where feasible, to contact the originators. For questions please contact soil.isricPwur.nl indicating the item reference number concerned. GEOLOGY OF THE AREA SOUTH OF MAGADI DEGREE SHEET 58, N.W. QUARTER (with coloured geological map) by B. H. BAKER, B.Sc, F.G.S. Geologist 165^G FOREWORD The publication of the report on the geology of the area south of Magadi completes the account of the southern end of the Rift Valley as it occurs in Kenya. The Magadi area itself was described by Mr. Baker in Report No. 42 (1958). During the mapping of the continua tion of the Magadi area the discovery of some critical exposures enabled the correction of an error of succession in the lower Pleistocene rocks that had been made during the survey of the Magadi area. The area is wild and desolate, but of considerable interest scenically, with the western Rift wall a little beyond its west boundary, rugged hills of ancient rocks in the south-east and two prominent volcanoes, Lenderut and Shombole, rising from the Rift floor. -
Country Update Report for Kenya 2010–2015
Proceedings World Geothermal Congress 2015 Melbourne, Australia, 19-25 April 2015 Country Update Report for Kenya 2010-2014 Peter Omenda and Silas Simiyu Geothermal Development Company, P. O. Box 100746, Nairobi 00101, Kenya [email protected] Keywords: Geothermal, Kenya rift, Country update. ABSTRACT Geothermal resources in Kenya have been under development since 1950’s and the current installed capacity stands at 573 MWe against total potential of about 10,000 MWe. All the high temperature prospects are located within the Kenya Rift Valley where they are closely associated with Quaternary volcanoes. Olkaria geothermal field is so far the largest producing site with current installed capacity of 573 MWe from five power plants owned by Kenya Electricity Generating Company (KenGen) (463 MWe) and Orpower4 (110 MWe). 10 MWt is being utilized to heat greenhouses and fumigate soils at the Oserian flower farm. The Oserian flower farm also has 4 MWe installed for own use. Power generation at the Eburru geothermal field stands at 2.5 MWe from a pilot plant. Development of geothermal resources in Kenya is currently being fast tracked with 280 MWe commissioned in September and October 2014. Production drilling for the additional 560 MWe power plants to be developed under PPP arrangement between KenGen and private sector is ongoing. The Geothermal Development Company (GDC) is currently undertaking production drilling at the Menengai geothermal field for 105 MWe power developments to be commissioned in 2015. Detailed exploration has been undertaken in Suswa, Longonot, Baringo, Korosi, Paka and Silali geothermal prospects and exploration drilling is expected to commence in year 2015 in Baringo – Silali geothermal area. -
Ol'orien Farm
Ol’orien Farm South Kinangop, Maraigushu, Naivasha Main Farmhouse Outbuildings Outstanding farm Sitting room, dining room, kitchen, veranda, Staff accommodation, garages and stores 4 bedrooms, 2 bathrooms, ancillary with Unbelievable accommodation Farm Buildings & Ancillary 2 supervisor’s houses, 2 calf houses, 2 barns, hay views on the edge of Secondary Farmhouse barn, spray race, machinery shed, engine room, 2 Sitting room, dining room, kitchen, veranda, milking sheds, stables, 2 irrigation dams and borehole the Great Rift ValleY 5 bedrooms, 2 bathrooms, ancillary accommodation In all about 754 acres (305 hectares) Naivasha 9.5 kms, Nakuru 80 kms, Nairobi 90 kms Situation Maraigushu Ol’Orien is situated in close proximity to Maraigushu on the main Nairobi to Naivasha highway. The farm is approximately 9.5 kilometres south of Naivasha and 90 kilometres to the north west of Nairobi. Naivasha is in Nakuru County within the Great Rift Valley. The main industry in the area is agriculture and is internationally renowned for its horticulture and floriculture. In addition to agriculture the area around Naivasha is becoming increasingly popular for people looking for second/weekend homes in order to escape the congestion of Nairobi. The area is also a well known tourist destination with attractions such as Lake Naivasha itself and its beautiful surrounds which contrast to the nearby Mount Longonot and Hells Gate National Park. The latter is popular for its wildlife and interesting geographical formations. Activities at the park include bird watching, viewings and visits to the geo-thermal springs of Olkaria. The area is also becoming increasingly populer for golf resort development.