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Water Infrastructure in Libya and the Water Situation in Agriculture in the Jefara Region of Libya
African J. Economic and Sustainable Development, Vol. 3, No. 1, 2014 33 Water infrastructure in Libya and the water situation in agriculture in the Jefara region of Libya Abdulmagid Abdudayem and Albert H.S. Scott* School of Commerce, Faculty of Business, Education, Law and Arts, University of Southern Queensland, West Street, Toowoomba QLD 4350, Australia E-mail: [email protected] E-mail: [email protected] *Corresponding author Abstract: Information about the current state of water institutional frameworks, water infrastructure and water management policies in Libya enable the identification and evaluation of a range of options for improving water use efficiency in agriculture and the potential role of water pricing in achieving sustainability of water sources. This paper begins with an overview of the agricultural sector. In order to assess the current water situation in Libya, the water infrastructure will be examined through a review of water legislation, its institutional framework and the infrastructure surrounding the various water resources. The national strategy for the management of water resources and the suggested plans to address the inefficient use of water in the Jefara Plain Region (JPR) will be discussed. The last section will be devoted to the Great Man-made River Project (GMRP) and water investment in JPR’s agriculture, and conclude by identifying the problems and obstacles facing the outcomes for these investments. Keywords: Libya; Jefara Plain Region; JPR; water management policies; water use efficiency; water resources management; water legislation; water institutional frameworks. Reference to this paper should be made as follows: Abdudayem, A. and Scott, A.H.S. -
The Impact of Oil Exports on Economic Growth – the Case of Libya
Czech University of Life Sciences Prague Faculty of Economics and Management Department of Economics The Impact of oil Exports on Economic Growth – The Case of Libya Doctoral Thesis Author: Mousbah Ahmouda Supervisor: Doc. Ing. Luboš Smutka, Ph.D. 2014 Abstract The purpose of this thesis is to evaluate and measure the relationship between oil exports and economic growth in Libya by using advancement model and utilize Koyck disseminated lag regression technique (Koyck, 1954; Zvi, 1967) to check the relationship between the oil export of Libya and Libyan GDP using annual data over the period of 1980 to 2013. The research focuses on the impacts of oil exports on the economic growth of Libya. Being a developing country, Libya’s GDP is mainly financed by oil rents and export of hydrocarbons. In addition, the research are applied to test the hypothesis of economic growth strategy led by exports. The research is based on the following hypotheses for testing the causality and co- integration between GDP and oil export in Libya as to whether there is bi-directional causality between GDP growth and export, or whether there is unidirectional causality between the two variables or whether there is no causality between GDP and oil export in Libya. Importantly, this research aims at studying the impact of oil export on the economy. Therefore, the relationship of oil export and economic growth for Libya is a major point. Also the research tried to find out the extent and importance of oil exports on the trade, investment, financing of the budget and the government expenditure. -
Chronology, Causes and Progression of the Messinian Salinity Crisis
letters to nature the cause, and the effects, of the isolation of the Mediterranean; the two basic explanations are (1) a large glacio-eustatic sea-level drop, Chronology, causes and related to expanding polar ice volume6, and (2) orogenic uplift accompanied by gravity-driven sliding of large nappe complexes in progression of the the Gibraltar arc7. Until now, correlations of stable-isotope (d18O and d13C) records from open-ocean sequences to the Messinian Messinian salinity crisis event stratigraphy of the Mediterranean have been ambiguous because of the absence of a reliable time frame for the MSC. The W. Krijgsman*, F. J. Hilgen², I. Raf®³, F. J. Sierro§ establishment of astronomical polarity timescales for the past & D. S. Wilsonk 10 Myr (refs 3, 11) provided a signi®cant advance in dating the * Paleomagnetic Laboratory ``Fort Hoofddijk'', Utrecht University, geological record and promised a solution for the MSC controver- Budapestlaan 17, 3584 CD Utrecht, The Netherlands sies. Unfortunately, the Mediterranean-based astronomical polarity ² Department of Geology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, timescale showed a gap during much of the Messinian (6.7±5.3 Myr The Netherlands ago)3, related to the presence of less-favourable sediments and the ³ Dipartimento di Scienze della Terra, UniversitaÁ ``G. D'Annunzio'', notoriously complex geological history of the Mediterranean in Campus Universitario, Via dei Vestini 31, 66013 Chieti Scalo, Italy this time interval. However, the classic Messinian sediments § Department de -
Formation Evaluation of Upper Nubian Sandstone Block NC 98 (A Pool), Eastern Sirt Basin, Libya
International Science and العدد Volume 12 Technology Journal ديسمبر December 2017 المجلة الدولية للعلوم والتقنية Formation Evaluation of Upper Nubian Sandstone Block NC 98 (A Pool), Eastern Sirt Basin, Libya. Hussein A. Sherif and Ayoub M. Abughdiri Libyan Academy-Janzour, Tripoli, Libya [email protected] ABSTRACT The Nubian Sandstone Formation (Pre-Upper Cretaceous) in the Sirte Basin, Libya is considered an important reservoir for hydrocarbons. It is subdivided into three stratigraphic members, the Lower Nubian Sandstone, the Middle Shale and the Upper Nubian Sandstone. Generally, the oil wells which have been drilled by Waha Oil Company in A-Pool, NC98 Block, Eastern Sirt Basin, Libya are producing from the Upper Nubian Sandstone reservoir. The main trapping systems in APool-NC98 Block are structural and stratigraphic combination traps, comprising of at least two major NW-SE trending tectonic blocks, with each block being further broken up with several more Pre-Upper-Cretaceous faults. Four wells have been selected to conduct the formation evaluation of the Upper Nubian Sandstone reservoir which lies at a depth of between 14,000 and 15,500 feet. This study is an integration approach using the petrophysical analysis and integrating the sedimentology and petrography from core. The geological and petrophysical evaluation were done using the Techlog software. The clay minerals identification was carried out using the Potassium (K) versus Thorium (Th) concentration cross-plot technique. The main clay minerals identified were; Kaolinite and Chlorite, in agreement with the Petrographical analysis on samples from well A4-NC98. The Petrophysical analysis clearly shows that the Upper Nubian Sandstone is a good reservoir in wells A3, A4 and A5, whereas low reservoir quality in well A6. -
New Isotopic Evidence for the Origin of Groundwater from the Nubian Sandstone Aquifer in the Negev, Israel
Applied Geochemistry Applied Geochemistry 22 (2007) 1052–1073 www.elsevier.com/locate/apgeochem New isotopic evidence for the origin of groundwater from the Nubian Sandstone Aquifer in the Negev, Israel Avner Vengosh a,*, Sharona Hening b, Jiwchar Ganor b, Bernhard Mayer c, Constanze E. Weyhenmeyer d, Thomas D. Bullen e, Adina Paytan f a Division of Earth and Ocean Sciences, Nicholas School of the Environment and Earth Sciences, Duke University, Durham, NC 27708, USA b Department of Geological and Environmental Sciences, Ben Gurion University, Beer Sheva, Israel c Department of Geology and Geophysics, University of Calgary, Calgary, Alberta, Canada d Department of Earth Sciences, Syracuse University, Syracuse, NY, USA e US Geological Survey, Menlo Park, CA, USA f Department of Geological and Environmental Sciences, Stanford University, Stanford, CA, USA Received 10 October 2006; accepted 26 January 2007 Editorial handling by W.B. Lyons Available online 12 March 2007 Abstract The geochemistry and isotopic composition (H, O, S, Osulfate, C, Sr) of groundwater from the Nubian Sandstone (Kurnub Group) aquifer in the Negev, Israel, were investigated in an attempt to reconstruct the origin of the water and solutes, evaluate modes of water–rock interactions, and determine mean residence times of the water. The results indi- cate multiple recharge events into the Nubian sandstone aquifer characterized by distinctive isotope signatures and deu- terium excess values. In the northeastern Negev, groundwater was identified with deuterium excess values of 16&, 18 2 which suggests local recharge via unconfined areas of the aquifer in the Negev anticline systems. The d OH2O and d H values (À6.5& and À35.4&) of this groundwater are higher than those of groundwater in the Sinai Peninsula and southern Arava valley (À7.5& and À48.3&) that likewise have lower deuterium excess values of 10&. -
TRAVERTINE-MARL DEPOSITS of the VALLEY and RIDGE PROVINCE of VIRGINIA - a PRELIMINARY REPORT David A
- Vol. 31 February 1985 No. 1 TRAVERTINE-MARL DEPOSITS OF THE VALLEY AND RIDGE PROVINCE OF VIRGINIA - A PRELIMINARY REPORT David A. Hubbard, Jr.1, William F. Gianninil and Michelle M. Lorah2 The travertine and marl deposits of Virginia's Valley and Ridge province are the result of precipitation of calcium carbonate from fresh water streams and springs. Travertine is white to light yellowish brown and has a massive or concretionary structure. Buildups of this material tend to form cascades or waterfalls along streams (Figure 1). Marl refers to white to dark yellowish brown, loose, earthy deposits of calcium carbonate (Figure 2). Deposits of these carbonate materials are related and have formed during the Quaternary period. This preliminary report is a compilation of some litei-ature and observations of these materials. A depositional model is proposed. These deposits have long been visited by man. Projectile points, pottery fragments, and firepits record the visitation of American Indians to Frederick and Augusta county sites. Thomas Jefferson (1825) wrote an account of the Falling Spring Falls from a visit prior to 1781. Aesthetic and economic considerations eontinue to attract interest in these deposits. 'Virginia Division of Mineral Resources, Charlot- Figure 1. Travertine waterfall and cascade series tesville, VA on Falling Springs Creek, Alleghany County, 2Department of Environmental Sciences, Univer- Virginia. Note man standing in center of left sity of Virginia, Charlottesville, VA margin. 2 VIRGINIA DIVISION OF MINERAL RESOURCES Vol. 31 Figure 2. An extensive marl deposit located in Figure 3. Rimstone dam form resulting from Frederick County, Virginia. Stream, in fore- precipitation of calcium carbonate in Mill Creek, ground, has incised and drained the deposit. -
Covid-19 Impacts on Agri-Food Value Chains
©FAO/Sia Kambou 1 2 COVID-19 IMPACTS ON AGRI-FOOD VALUE CHAINS LIBYA Food and Agriculture Organization of the United Nations Cairo, 2021 Required citation: FAO and WFP. 2021. COVID-19 impacts on agri-food value chains: Libya. Cairo. https://doi.org/10.4060/cb3089en The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO. ISBN 978-92-5-133889-6 © FAO, 2021 Some rights reserved. This work is made available under the Creative Commons Attribution-NonCommercial-ShareAlike 3.0 IGO licence (CC BY-NC-SA 3.0 IGO; https://creativecommons.org/licenses/by-nc-sa/3.0/igo/legalcode/legalcode). Under the terms of this licence, this work may be copied, redistributed and adapted for non-commercial purposes, provided that the work is appropriately cited. In any use of this work, there should be no suggestion that FAO endorses any specific organization, products or services. -
Transnational Project on the Major Regional Aquifer in North-East Africa
-: I /7 LT'UI I I UNITED NATIONS DEVELOPMENT PROGRAMME UNiTED NATIONS ENVIRONMENT PROGRAMME UNITED NATIONS DEPARTMENT OF TECHNICAL COOPERATION FOR DEVELOPMENT TRANSNATIONAL PROJECT ON THE MAJOR REGIONAL AQUIFER IN NORTH-EAST AFRICA PROCEEDINGS OF PROJECT WORKSHOP HELD IN KHARTOUM, SUDAN 12th-14th December, 1987 Under the auspices of the National Corporation for Rural Water Development United Nations New York, February, 1988 J; ;T Al • TRANSNATIONAL PROJECT ON THE MAJOR REGIONAL AQUIFER IN NORTH-EAST AFRICA PROCEEDINGS OF PROJECT WORKSHOP HELD IN KHARTOUM, SUDAN 12th-14th December, 1987 Foreword The United Nations has for many years funded studies of grouidwater in the arid areas and has contributed widely to the understanding of groundwater resources and their evolution in such areas. The eleven papers included in these Workshop proceedings are a welcome addition to arid groundwater knowledge outlining investigations carried out into the "Nubian Sandstone Aquifer" in Egypt and the Sudan with a contribution from Libya. The Department would like to acknowledge the assistance given by J.W. Lloyd in editing these proceedings. a CONTENTS Page INTRODUCTION 1 Background to Project I Project Design 1 Project Area Features 3 OPENING SESSION 5 ADDRESS BY DR. ADAM MADIBO, Minister of Energy and 5 Mining for the Sudan a ADDRESS BY MR. K. SHAWKI, Commissioner, Relief and 8 Rehabilitation Commission of the Sudan ADDRESS BY DR. K. HEFNEY, Project Manager for the 8 Egyptian Component Area PAPER PRESENTATIONS 9 1. Project Regional Coordination Machinery. 9 W. Iskander. Project Coordinator Management Problems of the Major Regional 16 Aquifers of North Africa. A Shata. Desert Institute, Cairo. -
WFP Libya Programme Team
FOREWORD AND ACKNOWLEDGEMENTS This study was prepared by Daniele Barelli, Independent Consultant and Agricultural Livelihoods Needs Assessment Specialist, in collaboration with WFP Libya Programme Team. The study was commissioned by the WFP Libya office. Technical support and advice were provided by this office, the WFP Regional Bureau in Cairo, WFP Headquarters and the FAO Regional Bureau in Cairo. Particular thanks goes to the professional and timely work carried out by the independent non-governmental organization, Fezzan Libya Organization (FLO), which was responsible for the challenging field data collection for this study. Much appreciation also goes to all people who were very supportive during the process of data collection, particularly the representatives of the Libyan Ministry of Agriculture. Design and layout George Kassab TABLE OF SECTION 3 CONTENTS 29 Crop Analysis 3.1 Land ownership 3.2 Access to irrigation and main water sources 3.3 Status of agricultural assets and infrastructure 3.3.1 Agricultural Assets 3.3.2 Agricultural infrastructure 3.4 Seed, fertilizers and pesticides SECTION 1 3.4.1 Seeds and seedling availability and sources Background, objectives 3.4.2 Fertilizer use and access and methodology of the 3.4.3 Pesticide use and access assessment 3.5 Crop and fruit tree profiles 07 3.5.1 Annual crops 3.5.2 Perrenial crops 1.1 Introduction 3.5.3 Conclusion 1.2 Conflict situation 1.3 Objectives of the study 1.3.1 Overall Objective SECTION 4 1.3.2 Specific Objectives 1.4 Assessment Methodology Livestock Production 1.5 The role of Agriculture in Libya and the Fezzan Region 37 Analysis SECTION 2 4.1 Livestock profile The Impact of the Crises 4.2 Livestock ownership on Different Groups and 4.3 Changes in livestock production 4.4. -
1983 This Report Is Prelioinary and Has Not Been Reviewed for Conformity*Vith U.S
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY PROJECT REPORT SUDAN INVESTIGATION (IR)SU-2 GEOLOGIC ASSESSMENT OF THE FOSSIL ENERGY AND GEOTHERMAL POTENTIAL OF THE SUDAN By Lor en W. Setlow U.S. Geological Survey- U.S. Geological Survey Open-File Report £^ Report prepared for the Agency for International Development, U.S. Department of State. 1983 This report is prelioinary and has not been reviewed for conformity*vith U.S. Ge'olozical Survey editorial'standards. CONTENTS Page INTRODUCTION................................................ 1 PRESENT ENERGY SITUTATION................................... 3 REGIONAL GEOLOGY............................................ 5 Precambrian............................................ 5 Paleozoic formations................................... 8 Mesozoic formations.................................... 13 Nubian Sandstone.................................. 13 Yirol Formation................................... 14 Gedaref Formation................................. 17 Other Mesozoic formations.............................. 17 Tertiary formations.................................... 17 Red Sea coastal deposits............................... 22 Hamamit Formation................................. 22 Maghersum Formation............................... 23 Abu Imama Formation............................... 23 Dungunab Formation................................ 24 Quaternary formations.................................. 24 Abu Shagara Formation........................^.... 24 Umm Rawaba Formation............................. -
Nubian Sandstone Aquifer System Isotopes and Modelling to Support the Nubian Sandstone Aquifer System Project
Transboundary aquifers and river basins Mediterranean Sea Benghazi ! Port Said Alexandria ! ! 30°N Cairo! ! Suez Nile ! Asyût R e d S e a Egypt Libyan Arab Jamahiriya Lake Nasser Administrative Chad Boundaries 20°N NSAS boundary ! Major city National boundary Khartoum/ ! Omdurman Blue Nile Kilometres 0 100 200 300 400 500 White Nile Sudan 20°E 30°E Nubian Sandstone Aquifer System Isotopes and modelling to support the Nubian Sandstone Aquifer System Project he Nubian Sandstone Aquifer System (NSAS) underlies Tthe countries of Chad, Egypt, Libyan Arab Jamahiriya and Sudan, the total population of which is over 136 million. It is the world’s largest ‘fossil’ water aquifer system. This gigantic reservoir faces heavy demands from agriculture and for drinking water, and the amount drawn out could double in the next 50–100 years. Climate change is expected to add significant stress due to rising temperatures as well as changes in precipitation patterns, inland evaporation and salinization. Groundwater has been identified as the biggest and in some cases the only future source of water to meet growing demands and the development goals of each NSAS country, and evidence shows that massive volumes of groundwater are still potentially available. Since the 1960s, groundwater has been actively pumped out of the aquifer to support irrigation and water supply needs. Over-abstraction has already begun in some areas, which leads to significant drawdowns and can induce salinization. In the approximately 20 000 years since the last glacial period, the aquifer has been slowly draining; the system faces low recharge rates in some areas, while others have no recharge at all. -
Chad Poverty Assessment: Constraints to Rural Development
Report No. 16567-CD Chad Poverty Assessment: Constraints to Rural Public Disclosure Authorized Development October 21, 1997 Human Development, Group IV Atrica Region Public Disclosure Authorized Public Disclosure Authorized Documentof the World Bank Public Disclosure Authorized ABBREVIATIONS AND ACRONYMS AMTT Agricultural Marketing and Technology Transfer Project AV Association Villageoise BCA Bceufs de culture attelde BEAC Banque des Etats de l'Afrique Centrale BET Borkou-Ennedi-Tibesti BIEP Bureau Interminist6rieI d'Etudes et des Projets BNF Bureau National de Frdt CAER Compte Autonome d'Entretien Routier CAR Central African Republic CFA Communautd Financiere Africaine CILSS Comite Inter-etats de Lutte Contre la Sdcheresse au Sahel DCPA Direction de la Commercialisation des Produits Agricoles DD Droit de Douane DPPASA Direction de la Promotion des Produits Agricoles et de la Sdcur DSA Direction de la Statistique Agricole EU European Union FAO Food and Agriculture Organization FEWS Famine Early Warning System FIR Fonds d'Investissement Rural GDP Gross Domestic Product GNP Gross National Product INSAH Institut du Sahel IRCT Institut de Recherche sur le Coton et le Textile LVO Lettre de Voiture Obligatoire MTPT Ministare des Travaux Publics et des Transports NGO Nongovernmental Organization ONDR Office National de Developpement Rural PASET Projet d'Ajustement Sectoriel des Transports PRISAS Programme Regional de Renforcement Institationnel en matie sur la Sdcuritd Alimentaire au Sahel PST Projet Sectoriel Transport RCA Republique Centrafrcaine