Impact of Introducing Reserve Flows on Abstractive Uses in Water Stressed Catchment in Kenya: Application of WEAP21 Model
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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. -
"Afrika-Studien" Edited by Ifo-Institut Für Wirtschafts- Forschung E
© Publication series "Afrika-Studien" edited by Ifo-Institut für Wirtschafts- forschung e. V., München, in connexion with Prof. Dr. PETER VON BLANCKENBURG, Berlin Prof. Dr. HEINRICH KRAUT, Dortmund Prof. Dr. OTTO NEULOH, Saarbriicken Prof. Dr. Dr. h. c. RUDOLP STUCKEN, Erlangen Prof. Dr. HANS WILBRANDT, Gottingen Prof. Dr. EMIL WOERMANN, Gottingen Editors in Cbief: Dr. phil. WILHELM MARQUARDT, München, Afrilca-Studienstelle im Ifo-Institut Prof. Dr. HANS RUTHENDERG, Stuttgart-Hohenheim, Institut für Auslandische Landwirtscliafl AFRIKA-STUDIENSTELLE MWEA An Irrigated Rice Settlement in Kenya Edited by ROBERT CHAMBERS and JON MORIS WELTFORUM VERLAG • MÜNCHEN M. The Perkerra Irrigation Scheme: A Contrasting Case by ROBERT CHAMBERS I. Historical Narrative 345 II. The Problems Experienced 352 1. Construction and Irrigation Problems 352 2. Production and Marketing Problems 353 3. Problems of Tenants and Staff 355 4. Problems of Organisation and Control 358 III. Some Concluding Lessons 361 List of Tables 1. Development Targets and Adiievements 349 2. Finance and Settlement 350 3. Onion Acreages and Yields 354 4. The Perkerra Local Committee 360 It is difficult to appreciate adequately a single development project con- sidered in isolation from its environment and from the record of similar projects elsewhere. To give a sharper focus to our review in this book of the achievements of the Mwea Irrigation Settlement, this chapter describes the very different history of effort and expenditure on a sister scheme whidi was started at the same time and for much the same reasons as Mwea. The Per- kerra Irrigation Scheme is located in the Rift Valley north of Nakuru (see Chapter A, Fig. -
Implications of the Distribution of Seismicity Near Lake Bogoria in the Kenya Rift
Geophys. J. Int. (1991) 105, 665-674 Implications of the distribution of seismicity near Lake Bogoria in the Kenya Rift P. A. V. Young,'" P. K. H. Maguire,' N. d'A. Laffoley' and J. R. Evans2 'Department of Geology, Leicester University, University Road, Leicester LE1 7RH, UK 'British Geological Survey, Murchbon House, West Mains Road, Edinburgh EH9 3LA, UK Accepted 1991 January 2. Received 1990 July 19; in original form 1988 May 5 SUMMARY Previous seismicity studies in the Kenya Rift have not been able to determine accurately depths of earthquakes, nor have most of them determined epicentres precisely enough to allow correlation of the seismicity with particular surface features. We operated a small dense seismic array for 3 months near Lake Bogoria in the Kenya Rift with the aim of locating microearthquakes in 3-D. 572 earthquakes, 81 per cent with ML< 1.0, have been located. The majority of the events are associated with the larger older faults on the Rift shoulder rather than the young 'grid' faults in the centre of the Rift. Seismic activity in the central trough cannot be related directly to the surface faulting; we infer that it indicates the presence of deep buried faults. This possibility has important implications for extension estimates and models of the Rift. Most of the activity occurs at depths less than 12 km, and no normal activity is deeper than 16 km. There is a peak in seismic activity at a depth of 9-10 km and the cut-off depth for brittle failure is taken at 12 km. -
RTJRC24.10 (Baringo GTI Hall, Kabarnet)
Seattle University School of Law Seattle University School of Law Digital Commons The Truth, Justice and Reconciliation I. Core TJRC Related Documents Commission of Kenya 10-24-2011 Public Hearing Transcripts - Rift Valley - Baringo - RTJRC24.10 (Baringo GTI Hall, Kabarnet) Truth, Justice, and Reconciliation Commission Follow this and additional works at: https://digitalcommons.law.seattleu.edu/tjrc-core Recommended Citation Truth, Justice, and Reconciliation Commission, "Public Hearing Transcripts - Rift Valley - Baringo - RTJRC24.10 (Baringo GTI Hall, Kabarnet)" (2011). I. Core TJRC Related Documents. 107. https://digitalcommons.law.seattleu.edu/tjrc-core/107 This Report is brought to you for free and open access by the The Truth, Justice and Reconciliation Commission of Kenya at Seattle University School of Law Digital Commons. It has been accepted for inclusion in I. Core TJRC Related Documents by an authorized administrator of Seattle University School of Law Digital Commons. For more information, please contact [email protected]. ORAL SUBMISSIONS MADE TO THE TRUTH, JUSTICE AND RECONCILIATION COMMISSION ON MONDAY, 24 TH OCTOBER, 2011 AT BARINGO GTI HALL, KABARNET PRESENT Tom Ojienda - The Presiding Chair, Kenya Ahmed Farah - Commissioner, Kenya Berhanu Dinka - Commissioner, Ethiopia Ronald Slye - Commissioner, USA Margaret Shava - Commissioner, Kenya Gertrude Chawatama - Commissioner, Zambia SECRETARIAT Patrick Njue - Leader of Evidence IN ATTENDANCE Dr. Samuel Tororei - Commissioner, KNCHR Rev. Lawrence Bomet - Commissioner, NCIC (Opening Prayers) (The Commission commenced at 10.05 a.m.) The Presiding Chair (Commissioner Ojienda): Thank you all once again. As part of the process, I want to specifically welcome the dancers from the Ilchamus community who are here to invite the Commission. -
Displacement Situation at Arabal Division and Sibilo Locations In
Displacement situation at Arabal Division and Sibilo Locations in Marigat and Baringo North Districts of Baringo County: - Kenya Initial Rapid Assessment Report Visited the affected areas (Arabal and Sibilo areas) on 22nd and 23rd January 2013 and triangulated it with Secondary Data from Kenya Red Cross Society and Government of Kenya officers CONTEXT: Brief description of the event and the location To undertake a multi-sector rapid assessment in line with the Kenya Initial Rapid Assessment (KIRA) process in areas hosting displaced communities Mission objectives To conduct a multi-sectoral rapid assessment following insecurity in Muchongoi division of Marigat district to identify gaps that need to be addressed in terms of humanitarian needs. Meet with GOK and Partners taking part in resolving issues surrounding the conflict in Marigat and Baringo north Districts Review sectoral issues of the IDP’s and host community and make recommendation on action to be taken Identify the reasons behind the displacement and highlight coping mechanisms of the community and their proposed solutions Mission dates 22nd and 23rd January 2013 Spatial coverage The mission will cover Marigat and Baringo north District the site of the recent cattle rustling incident that resulted in mass displacement of local population Mission team composition Paul Mutinda Kituku 0723 251828 [email protected] (Team leader) Lorraine Ombech 0728 602541 [email protected] Gabriel Wambua 0723 747676 [email protected] Stella Chumo 0722 475693 [email protected] Carlos, Based in Marigat 0721 929112 [email protected] Charlotte Mathysse 0732 436713 [email protected] Dr. S. Wanguru 0720 940577 [email protected] Faith Muriuki 0721 822232 [email protected] Joe Shields 0732 436716 Marigat District Background Information The larger Baringo county is divided into four administrative districts namely: Baringo Central, Baringo North, Marigat and East Pokot. -
Geothermal Potential of the Kenya Rift
Presented at Short Course III on Exploration for Geothermal Resources, organized by UNU-GTP and KenGen, at Lake Naivasha, Kenya, October 24 - November 17, 2008. GEOTHERMAL TRAINING PROGRAMME Kenya Electricity Generating Co., Ltd. STATUS OF GEOTHERMAL EXPLORATION IN KENYA AND FUTURE PLANS FOR ITS DEVELOPMENT Peter A. Omenda Kenya Electricity Generating Company Ltd. (KenGen) P.O. Box 785, Naivasha KENYA [email protected] ABSTRACT The high temperature geothermal prospects in Kenya are located within and are associated with the development of the Kenya Rift. Kenya Rift is a continental scale volcano-tectonic feature that stretches from northern to southern Africa. Development of the Rift started during the Oligocene (30million years ago) and activity has continued to recent times. The last 2 million years saw the development of large shield volcanoes within the axis of the rift. These centres are the most important geothermal prospects within the rift. Association between rifting and most of the occurrences of geothermal energy is mainly due to shallow magma chambers underneath the young volcanoes within the rift axis. KenGen in collaboration with the Ministry of Energy of the Government of Kenya has undertaken detailed surface studies of most of the prospects in the central sector of the rift which comprises Suswa, Longonot, Olkaria, Eburru, Menengai, Lakes Bogoria and Baringo, Korosi and Paka volcanic fields. Electric power is currently being generated at Olkaria with 130MWe installed while exploration drilling has been undertaken at Eburru and a 2.5MWe pilot plant is planned for development by KenGen and commissioning by 2009. Common methods that have been used by KenGen during exploration expeditions include geology (lithology, geochronology, structures); geophysics (seismic, gravity, magnetic, and resistivity); geochemistry (fluid and thermometry), heat flow and environmental baseline assessments. -
Irrigation Agriculture in Kenya
i IRRIGATION AGRICULTURE IN KENYA Impact of the Economic Stimulus Programme and Long-term Prospects for Food Security in an Era of Climate Change Nairobi March 2011 ii Research and draft by: Francis Z. Karina and Alex Wambua Mwaniki, Sower Solutions Ltd P.O. Box 14852-00100 Nairobi, Kenya Edited by: Zachariah Mairura Kiyondi For : Heinrich Böll Stiftung East & Horn of Africa Heinrich-Böll-Stiftung East Africa / Horn of Africa Regional Office Forest Road, P.O. Box 10799-00100 GPO, Nairobi, Kenya T +254 (0)20 2680745 -2613992 -2613997 Email: [email protected]: www.boell.or.ke Heinrich Böll Stiftung Schumannstr. 8D-10117 Berlin, Germany Tel: +49-30-28534-0 Email: [email protected] Web: www.boell.de About the Heinrich Böll Foundation The Heinrich Böll Stiftung / Foundation (HBF) is the Green Political Foundation, affiliated to the “Greens / Alliance ‘90” political party represented in Germany’s federal parliament. Headquartered in Berlin and with offices in more than 28 different countries, HBF con- ducts and supports civic educational activities and projects world-wide. HBF understands itself as a green think-tank and international policy network, working with governmental and non-governmental actors and focusing on gender equity, sustainable development, and democracy and human rights. HBF’s Regional Office for East & Horn of Africa oper- ates in Nairobi, Kenya, since 2001. © 2011 Heinrich Böll Stiftung, East and Horn of Africa All rights reserved. No part of this book may be reproduced without written permission from the publisher, except for brief quotation in books and critical reviews. For information and permissions, write to Heinrich Böll Stiftung. -
Geothermal Mapping Using Temperature Measurements
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 Kenya Electricity Generating Co., Ltd. GEOTHERMAL MAPPING USING TEMPERATURE MEASUREMENTS Godwin M. Mwawongo Geothermal Development Company P. O. Box 100746, Nairobi 00101 KENYA [email protected] ABSTRACT Shallow temperature gradient holes are reliable in mapping geothermal prospects with heat loss features as surface manifestation. The sun least affects ground temperatures at 1 m depth and temperatures in the North rift are least affected by seasonal changes. Over 10,736 MWt is lost naturally from Menengai to Paka along the Kenyan rift. Most of the geothermal surface manifestations associated with the heat loss are oriented in the NW-SE with a few located in the NE-SW direction. Estimated down-hole temperature at I km depth is over 200oC. Fluid flow in the prospects from Lake Baringo to Paka is from East to West with an outflow to the north. 1. INTRODUCTION Kenya is located in East Africa where the Great African Rift virtually splits the landmass into two. 14 geothermal prospects have been identified within the Kenyan Rift Valley starting from Barrier in the north to Lake Magadi in the south with a potential of over 3,000 MWe (Figure 1). The rift is a graben and during the formation of the prospects, hot rocks were brought closer to the surface and with intensive faulting and presence of water, the geothermal systems were formed as shown in the model in Figure 2. -
World Bank Document
Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized Page | ELRP-Integrated Pest Management Plan – IPMP-Component 1 1 TABLE OF CONTENTS EXECUTIVE SUMMARY .............................................................................................. 6 1 INTRODUCTION................................................................................................... 20 1.1 Emergency Locust Response Program ............................................................... 20 1.2 Project Development Objective ......................................................................... 20 1.3 ELRP Project Components ................................................................................ 20 1.4 Selected Pesticides ............................................................................................. 21 1.5 Project Activities ................................................................................................ 22 1.6 Project Beneficiaries .......................................................................................... 23 1.7 Aims and Objectives of IPMP ............................................................................ 23 1.8 Component 1 Implementation Arrangements .................................................... 24 2 STAKEHOLDER ENGAGEMENT ..................................................................... 25 2.1 Stakeholder Identification .................................................................................. 25 2.2 Stakeholder -
Status of Geothermal Exploration in Kenya and Future Plans for Its Development
Presented at Short Course IV on Exploration for Geothermal Resources, organized by UNU-GTP, KenGen and GDC, at Lake Naivasha, Kenya, November 1-22, 2009. Kenya Electricity Generating Co., Ltd. GEOTHERMAL TRAINING PROGRAMME Geothermal Development Company STATUS OF GEOTHERMAL EXPLORATION IN KENYA AND FUTURE PLANS FOR ITS DEVELOPMENT Peter A. Omenda Geothermal Development Company P. O. Box 100746, Nairobi 00101 KENYA [email protected] ABSTRACT The high temperature geothermal prospects in Kenya are located within and are associated with the development of the Kenya Rift. Kenya Rift is a continental scale volcano-tectonic feature that stretches from northern to southern Africa. Development of the Rift started during the Oligocene (30million years ago) and activity has continued to recent times. The last 2 million years saw the development of large shield volcanoes within the axis of the rift. These centres are the most important geothermal prospects within the rift. Association between rifting and most of the occurrences of geothermal energy is mainly due to shallow magma chambers underneath the young volcanoes within the rift axis. KenGen in collaboration with the Ministry of Energy of the Government of Kenya has undertaken detailed surface studies of most of the prospects in the central sector of the rift which comprises Suswa, Longonot, Olkaria, Eburru, Menengai, Lakes Bogoria and Baringo, Korosi and Paka volcanic fields. Electric power is currently being generated at Olkaria with 130MWe installed while exploration drilling has been undertaken at Eburru and a 2.5MWe pilot plant is planned for development by KenGen and commissioning by 2009. Common methods that have been used by KenGen during exploration expeditions include geology (lithology, geochronology, structures); geophysics (seismic, gravity, magnetic, and resistivity); geochemistry (fluid and thermometry), heat flow and environmental baseline assessments. -
Kenya IDP Transit Sites, Rift Valley Province Molo, Uasin Gishu, Kwanza, Trans Nzoia West & Koibatek Districts
UN Office for the Coordination of Humanitarian Affairs, Kenya Kenya IDP Transit Sites, Rift Valley Province Molo, Uasin Gishu, Kwanza, Trans Nzoia West & Koibatek Districts Go-down: West Pokot Distrib.P.* SalamNa N Kenya Provinces GSUNKimondo N N Matumbee NNChepkoilel TobooN Gathata Geta Farm Kalaha N N Patwaka Trans Marakwet EASTERN N Nasianda Nzoia N Gatina Village RIFT VALLEY NORTH EASTERN N Gitwamba WESTERN N Kokwet N CENTRAL Mt. NYANZA Elgon NAIROBI Sirikwa N Moiben- Mafuta COAST N Moiben BenmNoi Farm !(Kimilili Ziwa Rayfarm machine Moiben Bungoma N N Baringo WESTERN Soy Soy TransitN!( Turbo Uasin !( Gishu Gilgil- Maili Tarigo Chepkanga Nne/Kambi N transit Thomas N N Kimumu Huruma N Transit N !(Eldoret Yamumbi Kipkaren Kabarnet N Keiyo !( Mkt RIFT !( Ndeffo N!(Marigat KasarinaN VALLEY Losuru Jasho & Kiamba MalelN NNOutspan Kaptagat Geticha Kihingo Lugaria !( N N Kabiyet Transit Kamwaura N !(Mkt Nyakinyua N Matunda Langwenda N N Beestone Grassland N Njokerio N N Kipkabus/waunifor N Kuresoi Sasumua Baringo BN Kio Farm Centre N Bindura N N Sosiot Usalama !(Kakamega Kimkaza Farm N N N (&Nyakinyua) Kakamega Rurigi N N Geti Cheptiret BF Town !( N NFarm Kamuyu Center Lessos BurnNt Ngarua Kapsabet !( Farm !( !( N FoNrNest Farm N N Nandi KondoN-N Kondo- 7 Farm Center NSDA N N & Bisaria Kio Farm BaptisNtNNPAG N Charismata Chavakali Kuresoi CeNnatnredi Molo !( Hills Baraka Police Rongai Koibatek !( N N Kapdening N Kahuho N Mbale Vihiga Matharu NVillage N !( Center !(Timboroa Eldama Majengo Usalama (&Nyakinyua) ravine !( Rurigi N NKangema BodeniN!( -
Land Use/Land Cover Dynamics and Anthropogenic Driving Factors in Lake Baringo Catchment, Rift Valley, Kenya
Natural Resources, 2019, 10, 367-389 https://www.scirp.org/journal/nr ISSN Online: 2158-7086 ISSN Print: 2158-706X Land Use/Land Cover Dynamics and Anthropogenic Driving Factors in Lake Baringo Catchment, Rift Valley, Kenya Molly Ochuka1,2*, Chris Ikporukpo2, Yahaya Mijinyawa3, George Ogendi4 1Department of Agricultural and Environmental Engineering, Pan African University, Life and Earth Sciences Institute, University of Ibadan, Ibadan, Nigeria 2Department of Geography, University of Ibadan, Ibadan, Nigeria 3Department of Agricultural and Environmental Engineering, University of Ibadan, Ibadan, Nigeria 4Department of Environmental Science, Egerton University, Njoro, Kenya How to cite this paper: Ochuka, M., Ik- Abstract porukpo, C., Mijinyawa, Y. and Ogendi, G. (2019) Land Use/Land Cover Dynamics and Anthropogenic activities have altered land cover in Lake Baringo Catchment Anthropogenic Driving Factors in Lake Ba- contributing to increased erosion and sediment transport into water bodies. ringo Catchment, Rift Valley, Kenya. Nat- The study aims at analyzing the spatial and temporal Land Use and Land ural Resources, 10, 367-389. https://doi.org/10.4236/nr.2019.1010025 Cover Changes (LULCC) changes from 1988 to 2018 and to identify the main driving forces. GIS and Remote Sensing techniques, interviews and field ob- Received: August 19, 2019 servations were used to analyze the changes and drivers of LULCC from Accepted: October 8, 2019 1988-2018. The satellite imagery was selected from SPOT Image for the years Published: October 11, 2019 1988, 1998, 2008 and 2018. Environment for Visualizing Images (ENVI 5.3) Copyright © 2019 by author(s) and was used to perform image analysis and classification. The catchment was Scientific Research Publishing Inc.