The Case of Olkaria Geothermal Project in Hell's Gate National Park
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Tectonic and Climatic Control on Evolution of Rift Lakes in the Central Kenya Rift, East Africa
Quaternary Science Reviews 28 (2009) 2804–2816 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Tectonic and climatic control on evolution of rift lakes in the Central Kenya Rift, East Africa A.G.N. Bergner a,*, M.R. Strecker a, M.H. Trauth a, A. Deino b, F. Gasse c, P. Blisniuk d,M.Du¨ hnforth e a Institut fu¨r Geowissenschaften, Universita¨t Potsdam, K.-Liebknecht-Sr. 24-25, 14476 Potsdam, Germany b Berkeley Geochronology Center, Berkeley, USA c Centre Europe´en de Recherche et d’Enseignement de Ge´osciences de l’Environement (CEREGE), Aix en Provence, France d School of Earth Sciences, Stanford University, Stanford, USA e Institute of Arctic and Alpine Research, University of Colorado, Boulder, USA article info abstract Article history: The long-term histories of the neighboring Nakuru–Elmenteita and Naivasha lake basins in the Central Received 29 June 2007 Kenya Rift illustrate the relative importance of tectonic versus climatic effects on rift-lake evolution and Received in revised form the formation of disparate sedimentary environments. Although modern climate conditions in the 26 June 2009 Central Kenya Rift are very similar for these basins, hydrology and hydrochemistry of present-day lakes Accepted 9 July 2009 Nakuru, Elmenteita and Naivasha contrast dramatically due to tectonically controlled differences in basin geometries, catchment size, and fluvial processes. In this study, we use eighteen 14Cand40Ar/39Ar dated fluvio-lacustrine sedimentary sections to unravel the spatiotemporal evolution of the lake basins in response to tectonic and climatic influences. We reconstruct paleoclimatic and ecological trends recor- ded in these basins based on fossil diatom assemblages and geologic field mapping. -
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. -
Download Publication
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. -
(Smes) in Gilgil Town of Nakuru County, Kenya
IOSR Journal Of Humanities And Social Science (IOSR-JHSS) Volume 20, Issue 8, Ver. IV (Aug 2015), PP 109-115 e-ISSN: 2279-0837, p-ISSN: 2279-0845. www.iosrjournals.org Socio-Economic Determinants of Performance of Small and Medium Enterprises (SMEs) in Gilgil Town of Nakuru County, Kenya Kamau John Gathii1, and Mathew Mwangi Ngura2, Abstract: This study sought to establish the socio-economic determiners of performance of SMEs in Gilgil town of Nakuru County, Kenya. It adopted a survey research design involving SMEs in Gilgil town. Questionnaires were used as research instruments to gather information on variables of interest. The target population of the study included the 400 SMEs in Gilgil town registered with the County Council of Nakuru in the year 2012 and thereafter a sample size of 196 (49%) SMEs owners were systematically selected as respondents for the study. Data collected was coded and analyzed with the aid of Statistical Package for Social Sciences (SPSS) computer programme. Quantitative data was analyzed using descriptive statistics such as percentages and frequencies while the qualitative data derived from open-ended questions was analyzed according to themes based on the study objectives and research questions and there after inferences and conclusions were drawn. The study revealed that very few SMEs owners had obtained management training; most of them had only obtained secondary education; SMEs lacked access to financial resources and very few had integrated technology in their business operation. These shortcomings have adversely affected the performance of the SMEs in Gilgil town going by the low profits that they are making. -
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 ............................................................................................... -
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. -
World Bank Document
The World Bank Report No: ISR4369 Implementation Status & Results Kenya Energy Sector Recovery Project (P083131) Operation Name: Energy Sector Recovery Project (P083131) Project Stage: Implementation Seq.No: 15 Status: ARCHIVED Archive Date: Country: Kenya Approval FY: 2005 Public Disclosure Authorized Product Line:IBRD/IDA Region: AFRICA Lending Instrument: Specific Investment Loan Implementing Agency(ies): Ministry of Energy, Kenya Power and Lighting Co. Ltd., KenGen Key Dates Board Approval Date 13-Jul-2004 Original Closing Date 31-Mar-2010 Planned Mid Term Review Date 30-Nov-2011 Last Archived ISR Date 29-Mar-2011 Public Disclosure Copy Effectiveness Date 04-Nov-2004 Revised Closing Date 30-Sep-2013 Actual Mid Term Review Date Project Development Objectives Energy Sector Recovery Project (P083131) Project Development Objective (from Project Appraisal Document) (a) enhance the policy, institutional and regulatory environment for sector development, including private sector participation;and(b) increase access to electricity in urban and peri-urban areas while improving the efficiency, reliability and quality ofservice to customers. Has the Project Development Objective been changed since Board Approval of the Program? Public Disclosure Authorized ● Yes No Component(s) Component Name Component Cost INSTITUTIONAL AND CAPACITY BUILDING 7.50 STUDIES AND ENGINEERING SERVICES 18.70 GENERATION, OLKARIA II PLANT EXTENSION 119.10 DISTRIBUTION UPGRADING 229.60 Overall Ratings Previous Rating Current Rating Public Disclosure Authorized Progress towards achievement of PDO Satisfactory Satisfactory Overall Implementation Progress (IP) Satisfactory Satisfactory Overall Risk Rating Implementation Status Overview Public Disclosure Copy The Generation component is completed. The 3rd geothermal generating unit of 35 megawatts at Olkaria II is operational since May 2010. -
Kenyan Stone Age: the Louis Leakey Collection
World Archaeology at the Pitt Rivers Museum: A Characterization edited by Dan Hicks and Alice Stevenson, Archaeopress 2013, pages 35-21 3 Kenyan Stone Age: the Louis Leakey Collection Ceri Shipton Access 3.1 Introduction Louis Seymour Bazett Leakey is considered to be the founding father of palaeoanthropology, and his donation of some 6,747 artefacts from several Kenyan sites to the Pitt Rivers Museum (PRM) make his one of the largest collections in the Museum. Leakey was passionate aboutopen human evolution and Africa, and was able to prove that the deep roots of human ancestry lay in his native east Africa. At Olduvai Gorge, Tanzania he excavated an extraordinary sequence of Pleistocene human evolution, discovering several hominin species and naming the earliest known human culture: the Oldowan. At Olorgesailie, Kenya, he excavated an Acheulean site that is still influential in our understanding of Lower Pleistocene human behaviour. On Rusinga Island in Lake Victoria, Kenya he found the Miocene ape ancestor Proconsul. He obtained funding to establish three of the most influential primatologists in their field, dubbed Leakey’s ‘ape women’; Jane Goodall, Dian Fossey and Birute Galdikas, who pioneered the study of chimpanzee, gorilla and orangutan behaviour respectively. His second wife Mary Leakey, whom he first hired as an artefact illustrator, went on to be a great researcher in her own right, surpassing Louis’ work with her own excavations at Olduvai Gorge. Mary and Louis’ son Richard followed his parents’ career path initially, discovering many of the most important hominin fossils including KNM WT 15000 (the Nariokotome boy, a near complete Homo ergaster skeleton), KNM WT 17000 (the type specimen for Paranthropus aethiopicus), and KNM ER 1470 (the type specimen for Homo rudolfensis with an extremely well preserved Archaeopressendocranium). -
HIGH FLUORIDE WATER in the GILGIL AREA of NAKURU COUNTY, KENYA Enos W Wambu,A GK Muthakiab Nairobi, Kenya
37 Research report High F water in Nakuru County, Kenya 37 Fluoride 44(1)37–41 Wambu, Muthakia January-March 2011 HIGH FLUORIDE WATER IN THE GILGIL AREA OF NAKURU COUNTY, KENYA Enos W Wambu,a GK Muthakiab Nairobi, Kenya SUMMARY: Fluoride (F) levels were determined in 37 randomly sampled water sources in the Gilgil-Elementaita area and part of the Nakuru municipality in Nakuru County, Kenya using a F ion selective electrode. Lake water had F levels close to 200 ppm. Of the other sources, the highest mean F levels were in piped water (7.69 ppm) and borehole water (6.57 ppm). The level of water F appeared to increase with proximity of the source to the lakes in the region. There was also an apparent increase in the level of F in piped water compared to the original borehole water, which is ascribed to extensive evaporation during treatment and storage of piped water. With one exception, the river water had the lowest mean F concentrations (<0.1 ppm). These results indicate that most of the rivers in this region are relatively low in F and therefore are the safest sources of water for domestic and industrial use. Keywords: Borehole water; Fluoride in water; Gilgil area; Kenya water sources; Lake Elementaita; Nakuru County, Kenya. INTRODUCTION Endemic fluorosis in Kenya has been a public health problem for many years,1 and now there is a heightened public health concern about the fate of fluoride (F) in soil and groundwater sources, particularly in areas associated with the Great Rift Valley and the Central Highlands.2 In addition, rapid population growth3 and changes in rainfall patterns in many parts of Kenya have exacerbated the problem of water scarcity, forcing communities to turn to poor quality water sources for their needs.4 Primary sources of water for rural populations in Kenya are rivers, streams, springs, and wells in well-watered areas and boreholes in arid and semi-arid regions. -
The Estimation of Lake Naivasha Area Changes Using of Hydro-Geospatial Technologies
http://dx.doi.org/10.4314/rj.v1i1S.3D The Estimation of Lake Naivasha Area Changes Using of Hydro-Geospatial Technologies A. Ruhakana Soil and Water Management Research Program Rwanda Agriculture Board, Huye, Rwanda [email protected] Abstract: Remote Sensing (RS) and Geographical Information System (GIS) were proved as new technology to intervene in monitoring, managing and protecting environmental resources among others lake and water reservoir are mostly anxious resources. The objective of the study was to estimate the surface area change of the lake Naivasha using RS, GIS techniques and hydrological modeling for the lake water balance. Landat images Thematic Mapper/Enhanced Thematic Mapper Plus (TM/ETM+) taken respectively in the same month of January 1986; 1995; 2003 and 2010 were the input data used to assess the different changes of the lake area on one hand. on other hand the spread sheet data set helped to build the hydrological model to estimate the long term lake Level fluctuation, the rainfall versus evaporation as in flow and out flow from the lake. The lake volume showed the dynamic of ground water to simulate the long-term fluctuation of the lake level. The lake area changes from the model were calculated from the spread sheet input data from 1986 to 2003 while the lake area changes from the Landsat images were calculated from 1986 to 2010. The comparative results from the area lake changes both from Landsat images and hydrological model confirmed the correlation results, 45.72 Km2 or 32.03 % in 2010 for the Landsat while the hydrological model estimated to 12km2 or 8% area reduction in 2003. -
Nature [October 12, 1929
574 NATURE [OCTOBER 12, 1929 The alkali reserve of Lake N aivasha, expressed in Letters to the Editor. normality, was 0·004 (cf. Cambridge tap water 0·0042 N.), but instead of calcium, as in English hard waters, [The Editor does not hold himself responsible for the base was sodium derived from the surrounding opinions expressed by his correspondents. Neither alkaline lavas. This may have had a specific effect, can he undertake to return, nor to correspond with as in increasing concentrations the alkalinity appeared the writers of, rejected manuscripts intended for this to effect a marked reduction in quantity of both fauna or any other part of NATURE. No notice is taken and flora. The other lakes illustrated this, since their of anonymous communications.] alkalinity increased in the order: L. Baringo (0·01 N.), Crater Lake (0·11 N.), L. Elmenteita (0·22 N.), and L. Biology of Lakes in Kenya. Nakuru (0·27 N.). This increase raised the hydrogen WESENBURG-LUND, Thienemann, and others have ion concentration from pH 9·0 to about pH ll·2. for years been emphasising the need for more detailed Lake Baringo contained Crustacea, Rotifera, insect studies of tropical fresh waters. Having recently larvre, and fish, and also Microcystis sp., but no higher plants were seen. The three others, ' soda ' lakes, contained chiefly Roti fera and insect larvre, Lake Nakuru having apparently only one species of Brachionus. They were further characterised by the presence of a very abundant blue - green alga, Spirulina sp., in the plankton and an entire absence of shore vegetation, which was replaced by foul, barren mud, largely admixed with flamingo excreta.