DOCSLIB.ORG

Advances in Isotope Hydrology and Its Role in Sustainable Water

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Advances in Isotope Hydrology and Its Role in Sustainable Water 29 mm Resources Management (IHS—2007) Resources and its Role in Sustainable Water Advances in Isotope Hydrology In many parts of the world, surface water and groundwater resources are at risk because of indiscriminate use, rapidly growing populations, increasing Advances in Isotope Hydrology agricultural demands, and the threat of pollution. These risks are often compounded by a lack of understanding about local conditions governing and its Role in Sustainable Water the occurrence, distribution and movement of surface and groundwater resources. Historically, the IAEA has played a key role in advancing isotope Resources Management techniques and in promoting the use of isotopes to address water resource sustainability issues worldwide. The quadrennial IAEA symposia continue to be an important component of the IAEA’s mission in water resources (IHS—2007) management. The 12th symposium in the series was convened from 21 to 25 May 2007 in Vienna with the objectives of: reviewing the state of the art in isotope hydrology; outlining recent developments in the application of isotope techniques to water resources management; and identifying future trends and developments for research and applications. These proceedings — in two volumes — contain the presentations made at the symposium. A Proceedings of a Symposium CD-ROM containing the complete text of these proceedings is attached to the inside back cover of the second volume. Vienna, 21–25 May 2007 Vol. 2 Vol. 2 INTERNATIONAL ATOMIC ENERGY AGENCY VIENNA ISBN 978–92–0–110207–2 ISSN 0074—1884 Offsetdruck_29mm_07-43991_P1310_CovI+IV.indd 1 2007-12-12 14:19:52 ADVANCES IN ISOTOPE HYDROLOGY AND ITS ROLE IN SUSTAINABLE WATER RESOURCES MANAGEMENT (IHS–2007) The following States are Members of the International Atomic Energy Agency: AFGHANISTAN GREECE NORWAY ALBANIA GUATEMALA PAKISTAN ALGERIA HAITI PALAU ANGOLA HOLY SEE PANAMA ARGENTINA HONDURAS PARAGUAY ARMENIA HUNGARY PERU AUSTRALIA ICELAND PHILIPPINES AUSTRIA INDIA POLAND AZERBAIJAN INDONESIA PORTUGAL BANGLADESH IRAN, ISLAMIC REPUBLIC OF QATAR BELARUS IRAQ REPUBLIC OF MOLDOVA BELGIUM IRELAND ROMANIA BELIZE ISRAEL RUSSIAN FEDERATION BENIN ITALY SAUDI ARABIA BOLIVIA JAMAICA SENEGAL BOSNIA AND HERZEGOVINA JAPAN SERBIA BOTSWANA JORDAN SEYCHELLES BRAZIL KAZAKHSTAN SIERRA LEONE BULGARIA KENYA SINGAPORE BURKINA FASO KOREA, REPUBLIC OF SLOVAKIA CAMEROON KUWAIT SLOVENIA CANADA KYRGYZSTAN SOUTH AFRICA CENTRAL AFRICAN LATVIA SPAIN REPUBLIC LEBANON SRI LANKA CHAD LIBERIA SUDAN CHILE LIBYAN ARAB JAMAHIRIYA SWEDEN CHINA LIECHTENSTEIN SWITZERLAND COLOMBIA LITHUANIA SYRIAN ARAB REPUBLIC COSTA RICA LUXEMBOURG TAJIKISTAN CÔTE D’IVOIRE MADAGASCAR THAILAND CROATIA MALAWI THE FORMER YUGOSLAV CUBA MALAYSIA REPUBLIC OF MACEDONIA CYPRUS MALI TUNISIA CZECH REPUBLIC MALTA TURKEY DEMOCRATIC REPUBLIC MARSHALL ISLANDS UGANDA OF THE CONGO MAURITANIA UKRAINE DENMARK MAURITIUS UNITED ARAB EMIRATES DOMINICAN REPUBLIC MEXICO UNITED KINGDOM OF ECUADOR MONACO GREAT BRITAIN AND EGYPT MONGOLIA NORTHERN IRELAND EL SALVADOR MONTENEGRO UNITED REPUBLIC ERITREA MOROCCO OF TANZANIA ESTONIA MOZAMBIQUE UNITED STATES OF AMERICA ETHIOPIA MYANMAR URUGUAY FINLAND NAMIBIA UZBEKISTAN FRANCE NETHERLANDS VENEZUELA GABON NEW ZEALAND VIETNAM GEORGIA NICARAGUA YEMEN GERMANY NIGER ZAMBIA GHANA NIGERIA ZIMBABWE The Agency’s Statute was approved on 23 October 1956 by the Conference on the Statute of the IAEA held at United Nations Headquarters, New York; it entered into force on 29 July 1957. The Headquarters of the Agency are situated in Vienna. Its principal objective is “to accelerate and enlarge the contribution of atomic energy to peace, health and prosperity throughout the world’’. PROCEEDINGS SERIES ADVANCES IN ISOTOPE HYDROLOGY AND ITS ROLE IN SUSTAINABLE WATER RESOURCES MANAGEMENT (IHS–2007) PROCEEDINGS OF AN INTERNATIONAL SYMPOSIUM ON ADVANCES IN ISOTOPE HYDROLOGY AND ITS ROLE IN SUSTAINABLE WATER RESOURCES MANAGEMENT ORGANIZED BY THE INTERNATIONAL ATOMIC ENERGY AGENCY AND HELD IN VIENNA, 21–25 MAY 2007 In two volumes VOLUME 2 INTERNATIONAL ATOMIC ENERGY AGENCY VIENNA 2007 COPYRIGHT NOTICE All IAEA scientifi c and technical publications are protected by the terms of the Universal Copyright Convention as adopted in 1952 (Berne) and as revised in 1972 (Paris). The copyright has since been extended by the World Intellectual Property Organization (Geneva) to include electronic and virtual intellectual property. Permission to use whole or parts of texts contained in IAEA publications in printed or electronic form must be obtained and is usually subject to royalty agreements. Proposals for non-commercial reproductions and translations are welcomed and considered on a case-by-case basis. Enquiries should be addressed to the IAEA Publishing Section at: Sales and Promotion, Publishing Section International Atomic Energy Agency Wagramer Strasse 5 P.O. Box 100 1400 Vienna, Austria fax: +43 1 2600 29302 tel.: +43 1 2600 22417 email: [email protected] http://www.iaea.org/books © IAEA, 2007 Printed by the IAEA in Austria December 2007 STI/PUB/1310 IAEA Library Cataloguing in Publication Data International Symposium on Advances in Isotope Hydrology and Its Role in Sustainable Water Resources Management (2007 : Vienna, Austria) Advances in isotope hydrology and its role in sustainable water resources management (IHS-2007) : proceedings of an International Symposium on Advances in Isotope Hydrology Hydrology and its Role in Sustainable Water Resources Management (IHS-2007) / organized by the International Atomic Energy Agency and held in Vienna, 21–25 May 2007. — Vienna, IAEA, 2007. p. ; 24 cm. — (Proceedings series, ISSN 0074-1884) STI/PUB/1310 ISBN 978–92–0–110207–2 Includes bibliographical references. 1. Radioisotopes in hydrology — Congresses. 2. Hydrology — Congresses. 3. Water-supply — Congresses. I. International Atomic Energy Agency. II. Series: Proceedings series: (International Atomic Energy Agency). IAEAL 07–00500 FOREWORD Access to safe freshwater is considered a basic human right. However, in many parts of the world, surface water and ground water resources are at risk because of indiscriminate use, rapidly growing populations, increasing agricultural demands, and the threat of pollution. These risks are often compounded by a lack of understanding about local conditions governing the occurrence, distribution and movement of surface and groundwater resources. Historically, the IAEA has played a key role in advancing isotope techniques and in promoting the use of isotopes to address water resource sustainability issues worldwide. The quadrennial IAEA symposia continue to be an important component of the IAEA’s mission in water resources management. The 12th symposium in the series was convened from 21 to 25 May 2007 in Vienna with the objectives of: reviewing the state of the art in isotope hydrology; outlining recent developments in the application of isotope techniques to water resources management; and identifying future trends and developments for research and applications. Over 200 participants from 59 Member States participated in a series of invited lectures, poster sessions, round table discussions, and a scientifi c visit to the Danube River. The breadth of topics addressed was extensive and included analytical developments, the use of isotopes to understand land– atmosphere–biosphere interactions, rivers and surface water, development of deep groundwater resources, ecohydrology, urbanization and water resources management, carbon sequestration, waste management, artifi cial recharge, contamination problems, coastal zone hydrology, geothermal systems, agriculture and water resources management, and research frontiers. Out of 152 oral and poster presentations, 136 contributions submitted by the authors are included in two volumes of the proceedings with editorial corrections. These proceedings are intended for those using isotopes for applied problems in hydrology as well as the research community. It is also hoped that these proceedings will promote increased use of isotopes for water resource sustainability problems and greater utilization of these techniques by hydrologists in general. EDITORIAL NOTE The papers in these Proceedings (including the fi gures, tables and references) have undergone only the minimum copy editing considered necessary for the reader’s assistance. The views expressed remain, however, the responsibility of the named authors or participants. In addition, the views are not necessarily those of the governments of the nominating Member States or of the nominating organizations. The fi gures in volumes 1 and 2 of these Proceedings have been reproduced as received from the authors. The reader is referred to the electronic fi le of the proceedings in the attached CD-ROM in those cases where details of the fi gures in the print volumes are unclear. The report does not address questions of responsibility, legal or otherwise, for acts or omissions on the part of any person. Although great care has been taken to maintain the accuracy of information contained in this publication, neither the IAEA nor its Member States assume any responsibility for consequences which may arise from its use. The use of particular designations of countries or territories does not imply any judgement by the publisher, the IAEA, as to the legal status of such countries or territories, of their authorities and institutions or of the delimitation of their boundaries. The mention of names of specifi c companies or products (whether or not indicated as registered) does not imply any intention
Load more

Recommended publications
  • O Estudo Do Desenvolvimento Rural Integrado Das Bacias Hidrográficas Da Ilha De Santiago
    DAS BACIAS HIDROGRÁFICAS DA ILHA DE SANTIAGO DE HIDROGRÁFICAS DA ILHA BACIAS DAS INTEGRADO RURAL DO DESENVOLVIMENTO O ESTUDO VERDE CABO DE A REPÚBLICA DIRECÇÃO GERAL DA AGRICULTURA, SILVICULTURA E PECUÁRIA (MADRRM) A REPÚBLICA DE CABO VERDE O ESTUDO DO DESENVOLVIMENTO RURAL INTEGRADO DAS BACIAS HIDROGRÁFICAS DA ILHA DE SANTIAGO DA REPÚBLICA DE CABO VERDE (RELATÓRIO PRINCIPAL) RELATÓRIO FIN RELATÓRIO FINAL AL (RELATÓRIO PRINCIPAL) NOVEMBRO 2010 DEZEMBRO 2010 AGÊNCIA DE COOPERAÇÃO INTERNACIONAL JAPÃO NTC INTERNATIONAL CO., LTD. SNO JR 10-007 DIRECÇÃO GERAL DA AGRICULTURA, SILVICULTURA E PECUÁRIA (MADRRM) A REPÚBLICA DE CABO VERDE O ESTUDO DO DESENVOLVIMENTO RURAL INTEGRADO DAS BACIAS HIDROGRÁFICAS DA ILHA DE SANTIAGO DA REPÚBLICA DE CABO VERDE RELATÓRIO FINAL (RELATÓRIO PRINCIPAL) DEZEMBRO 2010 AGÊNCIA DE COOPERAÇÃO INTERNACIONAL JAPÃO NTC INTERNATIONAL CO., LTD. Composição do Relatório Final RELATÓRIO PRINCIPAL ANEXOS Prefácio O Governo do Japão, em resposta à solicitação do Governo da República de Cabo Verde, decidiu realizar um estudo relativo ao Plano Integrado de Desenvolvimento Rural das Bacias Hidrográficas da Ilha de Santiago, daquela República, e este foi implementado pela Agência de Cooperação Internacional do Japão. Esta Agência, então, enviou a Cabo Verde uma delegação chefiada pelo Sr. Shigeru Nakada da empresa NTC International, no período de Janeiro de 2008 a Dezembro de 2010. A Delegação de Estudo, além de manter discussões com as autoridades competentes da República de Cabo Verde, realizou uma série de estudos de campo e, após trabalhos relativos no Japão, hoje tem o prazer de apresentar o Relatório concluído. O nosso desejo é de que este Relatório venha não só a dar contributos ao desenvolvimento rural sustentado da República de Cabo Verde, como também corrobore no fortalecimento ainda maior dos laços de amizade entre as duas Nações.
    [Show full text]
  • Porosity and Permeability Lab
    Mrs. Keadle JH Science Porosity and Permeability Lab The terms porosity and permeability are related. porosity – the amount of empty space in a rock or other earth substance; this empty space is known as pore space. Porosity is how much water a substance can hold. Porosity is usually stated as a percentage of the material’s total volume. permeability – is how well water flows through rock or other earth substance. Factors that affect permeability are how large the pores in the substance are and how well the particles fit together. Water flows between the spaces in the material. If the spaces are close together such as in clay based soils, the water will tend to cling to the material and not pass through it easily or quickly. If the spaces are large, such as in the gravel, the water passes through quickly. There are two other terms that are used with water: percolation and infiltration. percolation – the downward movement of water from the land surface into soil or porous rock. infiltration – when the water enters the soil surface after falling from the atmosphere. In this lab, we will test the permeability and porosity of sand, gravel, and soil. Hypothesis Which material do you think will have the highest permeability (fastest time)? ______________ Which material do you think will have the lowest permeability (slowest time)? _____________ Which material do you think will have the highest porosity (largest spaces)? _______________ Which material do you think will have the lowest porosity (smallest spaces)? _______________ 1 Porosity and Permeability Lab Mrs. Keadle JH Science Materials 2 large cups (one with hole in bottom) water marker pea gravel timer yard soil (not potting soil) calculator sand spoon or scraper Procedure for measuring porosity 1.
    [Show full text]
  • 6.8.3 Costs of Each Irrigation Technology (Per Ha) Water Requirements Water Price (ECV) Equipment Water Price & Equip
    Cost Comparison among Irrigation Technologies: Cost c omparison a mong t he i rrigation technologies w as made ba sed on t he w ater r equirements derived from the experiment. The costs of each irrigation technology were calculated on the water prices and the equipment costs which varied with the irrigation technologies. The water prices set by São Domingos County were used, namely 25 ECV/m3 and 15 ECV/m3 for the t raditional irrigation and the w ater s aving i rrigation respectively. F or the w ater s aving irrigation, the price was set low for its promotion with the government subsidy. The drip irrigation equipment which was durable for 3 years cost 500,000 ECV/ha. One pot for pitcher irrigation cost 500 ECV and its total cost came to 1,500,000 ECV, as 3,000 pots/ha were needed. The pots were durable for 3 years as well. The result of the calculation are shown in the following table. Table 6.8.3 Costs of Each Irrigation Technology (per ha) Water Requirements Water Price (ECV) Equipment Water Price & Equip. Cost Irrigation System day 270 days/year m3 year Cost (ECV) 3 years (ECV) year (ECV) Traditional without mulch 55 m3/day 14,850 m3/year 25 371,250 - 1,113,750 371,250 Drip without mulch 32 m3/day 8,640 m3/year 15 129,600 500,000 888,800 296,267 Drip with mulch 26 m3/day 7,020 m3/year 15 105,300 500,000 815,900 271,967 Pitcher without mulch 35 m3/day 9,450 m3/year 15 141,750 1,500,000 1,925,250 641,750 3 3 Pitcher with mulch 30 m /day 8,100 m /year 15 121,500 1,500,000 1,864,500 621,500 As a r esult, t he an nual t otal co sts o f t he w ater price and equipment co st of each i rrigation technology are as follows; Traditional Irrigation without mulch: 371,250 ECV Drip Irrigation without mulch: 296,267 ECV Drip Irrigation with mulch: 271,967 ECV Pitcher Irrigation without mulch: 641,750 ECV Pitcher Irrigation with mulch: 621,500 ECV The c osts of d rip i rrigation w ith m ulch w ere t he c heapest, and the d ifference f rom t hose of traditional irrigation came to 99,283 ECV.
    [Show full text]
  • Sandra Maria Moniz Tavares
    Departamento de Geociência HIGROGEOLOGIA E RECURSOS HÍDRICOS NO CONCELHO DE SANTA CATARINA Licenciatura em Geologia – Ramo Cientifico Sandra Maria Moniz Tavares INSTITUTO SUPERIOR DE EDUCAÇÃO Praia, Setembro 2006 Sandra Maria Moniz Tavares TEMA: HIGROGEOLOGIA E RECURSOS HÍDRICOS NO CONCELHO DE SANTA CATARINA Trabalho Científico apresentado ao ISE para obtenção do Grau de Licenciatura em Geologia-Ramo Científico sob a Orientação do Eng.º Arrigo Querido, em Setembro de 2006. Praia, Setembro 2006 DEPARTAMENTO DE GEOCIÊNCIAS TRABALHO CIENTÍFICO APRESENTADO AO ISE PARA OBTENÇÃO DO GRAU DE LICENCIATURA EM GEOLOGIA-RAMO CIENTÍFICO ELABORADO POR, SANDRA MARIA MONIZ TAVARES, APROVADO PELOS MEMBROS DO JURI, FOI HOMOLOGADO PELO CONCELHO CIENTÍFICO PEDAGÓGICO, COMO REQUISITO PARCIAL À OBTENÇÃO DO GRAU DE LICENCIATURA EM GEOLOGIA – RAMO CIENTÍFICO. O JURI, _________________________________________ _________________________________________ _________________________________________ Praia, aos _____/_____/_____ DEDICATÓRIA Este trabalho é dedicado aos meus dois filhos, Sander Carlos Tavares Almeida e Alexander Tavares Almeida, ao meu marido Carlos António Mascarenhas Almeida e aos meus Pais. AGRADECIMENTOS Após um longo percurso desse trabalho gostaria de agradecer todos àqueles que de uma forma ou de outra contribuíram para o sucesso desse trabalho. Em primeiro lugar, agradeço a Deus, pela saúde, força e coragem para enfrentar as dificuldades deparadas ao longo da realização do trabalho. Gostaria de agradecer todos àqueles que contribuíram para que o mesmo atingisse a esse patamar. - Ao meu orientador, Eng. Arrigo Querido, um agradecimento especial, tanto na orientação como nos documentos facultados e correcção científica deste trabalho. - Ao Chefe do Departamento de Geociências Dr. Alberto da Mota Gomes um obrigado pela sugestão que me deu na escolha do Tema e do orientador; - Aos funcionários do INGRH, em especial o Dr.
    [Show full text]
  • Hydrogeology of Flowing Artesian Wells in Northwest Ohio
    Hydrogeology of Flowing Artesian Wells in Northwest Ohio By Curtis J Coe, CPG and Jim Raab Ohio Department of Natural Resources Division of Water Resources June 2016 Bulletin 48 Table of Contents 1.0 Introduction ........................................................................................................................... 1 1.1 Site Location and Setting .................................................................................................. 1 1.2 ODH Water Well Regulations for Flowing Artesian Wells ............................................. 3 1.3 Purpose and Scope of Work .............................................................................................. 3 2.0 Previous Work ....................................................................................................................... 4 2.1 Bedrock Hydrogeology ..................................................................................................... 4 2.2 Glacial Hydrogeolgy ......................................................................................................... 8 2.2.1 Williams Complex Aquifer ....................................................................................... 8 2.2.2 Williams End Moraine Aquifer ................................................................................. 8 2.2.3 Buried Valley Aquifers ............................................................................................ 13 2.2.4 Lake Maumee Lacustrine Aquifer ..........................................................................
    [Show full text]
  • Do You Drink It? 9-12
    DO YOU DRINK IT? 9-12 SUBJECTS: Science (Physical Science, Ecology, Earth Science), Social Studies (Geography) TIME: 2 class periods MATERIALS: 3-liter soda bottles aquarium gravel sand (coarse) pump from liquid dispenser blue, yellow & Red food coloring paper cups straws student sheets droppers scissors or razor blades markers OBJECTIVES The student will do the following: 1. Create an aquifer model. 2. Locate major U.S. aquifers. 3. Explain how a well works. 4. Examine a well’s relationship to the water table. 5. Apply principles of well placement. 6. Explain different ways that groundwater is contaminated. 4-37 BACKGROUND INFORMATION An aquifer is an underground layer of rock or soil that holds the water called groundwater. The word “aquifer” is derived from the Latin “aqua” meaning “water ,”and “ferre” meaning “to bring” or “to yield.” The ability of a geological formation to yield water depends on two factors - porosity and permeability. Porosity is determined by how much water the soil or rock can hold in the spaces between its particles. Permeability means how interconnected the spaces are so that water can flow freely between them. There are two types of aquifers. One is a confined aquifer, in which a water supply is sandwiched between two impermeable layers. These are sometimes called artesian aquifers because, when a well is drilled into this layer, the pressure may be so great that water will spurt to the surface without being pumped. This is an artesian well. The other type of aquifer is the unconfined aquifer, which has an impermeable layer under it but not above it.
    [Show full text]
  • Water Levels in Major Artesian Aquifers of the New Jersey Coastal Plain, 1988
    WATER LEVELS IN MAJOR ARTESIAN AQUIFERS OF THE NEW JERSEY COASTAL PLAIN, 1988 By Robert Rosman, Pierre J. Lacombe, and Donald A. Storck U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 95-4060 Prepared in cooperation with the NEW JERSEY DEPARTMENT OF ENVIRONMENTAL PROTECTION West Trenton, New Jersey 1995 CONTENTS Page Abstract............................................................. 1 Introduction......................................................... 2 Purpose and scope............................................... 2 Study area...................................................... 2 Previous investigations......................................... 4 Well-numbering system........................................... 4 Methods of data collection...................................... 5 Description of data presented................................... 6 Acknowledgments................................................. 8 Hydrogeology of the Coastal Plain.................................... 8 Description of aquifers and confining units..................... 11 Location of freshwater/saltwater interface...................... 12 Water levels in artesian aquifers of the Coastal Plain............... 13 Cohansey aquifer in Cape May County............................. 13 Water levels............................................... 13 Water-level fluctuations................................... 13 Atlantic City 800-foot sand..................................... 14 Water levels............................................... 14 Water-level
    [Show full text]
  • Causes of Groundwater Depletion
    Number 63 Issue Paper February 2019 Aquifer Depletion and Potential Impacts on Long-term Irrigated Agricultural Productivity When developing policies that regulate groundwater systems that are being depleted, the potential consequences of groundwater depletion need to be fully assessed to determine the trade-offs that exist between the undesired impacts of groundwater depletion and whether these impacts outweigh the benefits associated with groundwater use. (Photo from Ed Hennigan/Shutterstock.) is even higher in arid and semi-arid ar- the Mississippi Embayment Aquifer ABSTRACT eas, where the only consistent source of (Mississippi River lowlands bordering Groundwater is the Earth’s most irrigation water is groundwater. In these Arkansas and Mississippi), aquifers in extracted raw material, with almost regions, however, the use of groundwa- southern Arizona, and smaller aquifers 1,000 cubic kilometers per year (800 ter typically far exceeds the rate at which in many western states. million acre-feet per year) of ground- it is naturally replenished, indicating The groundwater resource with the water pumped from aquifers around the that these critical groundwater resources greatest long-term depletion is the High world. Approximately 70% of ground- are being slowly depleted. Within the Plains (Ogallala) aquifer in the Great water withdrawals worldwide are used to United States, groundwater depletion has Plains Region of the United States, support agricultural production systems, occurred in many important agricultural where groundwater levels have declined and within the United States, about 71% production regions, including the Great by more than 50 meters (150 feet) of groundwater withdrawals are used for Plains Region (Nebraska, Colorado, in some areas.
    [Show full text]
  • PLATAFORMA DAS ONG's DE CABO VERDE ONG's E/OU
    PLATAFORMA DAS ONG’S DE CABO VERDE ONG’s E/OU ASSOCIAÇÕES CABOVERDIANAS MEMBROS DA PLATAFORMA Praia, Novembro / 2011 ILHA DE SANTIAGO – CONCELHO DA PRAIA ZONA NOME LOCALIZAÇÃO DA SEDE DOMÍNIO DE ACTIVIDADE GEOGRÁFICA 1- PLURAL - Associação para a Promoção da Família, Praia - Tel: 2611506 / Fax: 2614503 Promoção da Família, da Mulher e da Cabo Verde da Mulher e da Criança C.P. 174 – A Criança 2- ADAD - Associação para a Defesa do Ambiente e Praia - Tel: 2612650 / Telm: 9918555 Meio Ambiente Cabo Verde Desenvolvimento Fax: 2622705 3- Associação dos Deficientes Visuais de Cabo Verde Praia - Tel: 2622010 / 2647378 Apoio aos Deficientes Visuais Cabo Verde C.P. 6 4- AECV - Associação dos Escuteiros de Cabo Verde Praia - Tel: 2614417 / 9939243 Escutismo Cabo Verde Fax: 615654 - C.P. 817 5- MORABI - Associação de Apoio à Auto-Promoção da Praia - Tel: 2621775 / Fax: 2621722 Promoção da Mulher Cabo Verde Mulher no Desenvolvimento C.P. 568 6- LAB - Liga dos Amigos do Brasil Praia - Brasil - Tel: 2623434 Desenvolvimento Comunitário Brasil - Achada de Stº C.P. 568 António 7- Associação para o Desenvolvimento de S. Francisco S. Francisco - Tel: 2611668 / 2631104 Desenvolvimento Comunitário S. Francisco C.P. 351-C 8- Liga Nazarena de Solidariedade Praia - Tel: 2614556 / 2612587 Formação profissional / criação de centros Cabo Verde Fax: 2611824 – C.P. 5 infantis e juvenis 9- CITI-HABITAT - Centro de Investigação de Praia - Tel: 2644008 / Fax: 2643968 Desenvolvimento sócio-económico de Cabo Verde Tecnologias Intermédias para o Habitat C.P. 132-C grupos desfavorecidos 10- ACD - Associação Cabo-verdiana de Deficientes Praia - Tel: 2628682 / Fax: 2628684 Apoio aos Deficientes Cabo Verde [email protected] 11- Associação para o Desenvolvimento de Achada Praia - Tel: 2631280 Desenvolvimento Comunitário de Achada Achada Eugénio Lima Eugénio Lima C.P.
    [Show full text]
  • Flowing Artesian Wells
    Flowing Artesian Wells Water Stewardship Information Series Table of Contents What’s the difference between a flowing artesian well Are there specific actions to avoid when flowing artesian and an artesian well? . 1 conditions are present? . 6 Why do wells flow? . 1 How can flowing artesian well be constructed in bedrock aquifers? . 7 Why is stopping or controlling artesian flow important? . 2 How can flowing artesian well be constructed in How can flowing artesian conditions be determined unconsolidated aquifers? . 7 before drilling? . 2 What should be done if flowing artesian conditions are What are the provincial regulatory requirements for suddenly encountered? . 7 controlling or stopping artesian flow? . 2 What are the key factors in completing and equipping What does it mean to “control” artesian flow from a well? . 3 a flowing artesian well? . 8 Will a flowing artesian well dry up if the flow is stopped How is the pressure or static water level for a flowing or controlled? . 3 artesian well measured? . 8 Are there any water quality concerns with flowing How should flowing artesian wells be closed? . 8 artesian wells? . 3 How is a flowing artesian well disinfected? . 9 Are there any other concerns with flowing artesian wells? . 3 Further Information . 9 What can be done with an existing flowing well? . 4 What if the flow is needed, for example, to increase the baseflow of a creek or stream? . 4 Are there some general guidelines for constructing a flowing artesian well? . 4 What are the key issues to be aware of when drilling a flowing artesian well? . 5 This booklet contains general information on flowing artesian wells for well drillers, groundwater consultants and well owners Hydrostatic head (or confining pressure) is the vertical in British Columbia .
    [Show full text]
  • Groundwater Modeling of the Withdrawal
    DOI: 10.7343/as-2018-333 Paper Groundwater modeling of the withdrawal sustainability of Cannara artesian aquifer (Umbria, Italy) Modellazione delle acque sotterranee e prelievo sostenibile dall’acquifero artesiano di Cannara (Umbria) Giovanni Pietro Beretta, Monica Avanzini, Tomaso Marangoni, Marino Burini, Giacomo Schirò, Jacopo Terrenghi, Gaetano Vacca Riassunto: L’acquifero di Cannara (Umbria, Italia) è noto da oltre un Abstract: The Cannara aquifer (Umbria, Italy) has been known for more secolo ed è uno dei principali punti di approvvigionamento di acqua than a century, and is one of the main drinking water supplies in the Umbria potabile nella Regione Umbria. All’inizio veniva utilizzato per scopi Region. In the beginning it was used for irrigation purposes, since this area was irrigui, poiché quest’area era prevalentemente agricola fino agli anni mainly agricultural up to the 1960s. The groundwater—exploited by Umbra ‘60. Le acque sotterranee, sfruttate da Umbra Acque S.p.A. (Società che Acque S.p.A. (a Company supplying drinking water)—is 150 m under ground fornisce l’acqua potabile), sono a 150 m al di sotto il livello del suolo e level and is contained in a porous confined aquifer, which originally had arte- sono contenute in un acquifero poroso confinato, che in origine aveva sian characteristics. Exploitation of 200–300 l/s with nine wells caused a re- caratteristiche artesiane. Lo sfruttamento di 200-300 l/s con nove pozzi duction of piezometric level, maintaining the confined aquifer conditions, except ha causato una riduzione del livello piezometrico, mantenendo le con- for a very short period during which the aquifer was depressurised by drought, dizioni di acquifero confinato, ad eccezione di un periodo molto breve and for increase of emergency withdrawals replacing other water supplies (from durante il quale la falda è stata depressurizzata in seguito alla siccità e springs) for drinking purposes.
    [Show full text]
  • Cabo Verde): Análise E Proposta Para O Seu Desenvolvimento Sustentado
    O sistema de pastoreio transumante no planalto do Tarrafal de Santiago (Cabo Verde): análise e proposta para o seu desenvolvimento sustentado. LEININE JÚNIOR DA VEIGA TAVARES Dissertação apresentada à Escola Superior Agrária de Bragança para obtenção do Grau de Mestre em Gestão de Recursos Florestais Orientado: Professora Doutora Marina Maria Meca Ferreira de Castro Co-Orientador: Professor Doutor José Manuel Correia dos Santos Ferreira de Castro Bragança Novembro, 2017 DEDICATÓRIA À minha família iv AGRADECIMENTOS Em primeiro lugar, agradeço a Deus e a minha família, por me possibilitar e triunfar mais uma etapa da minha vida. Os meus sinceros agradecimentos a todas as pessoas e instituições que de uma forma ou outra mostraram apreço e consideração por esta investigação. Agradeço a todos os meus professores do Mestrado em Gestão de Recursos Florestais pelos ensinamentos, acompanhamento e disponibilidade demonstrada. Aos meus amigos e colegas em Cabo Verde pelo apoio demonstrado na facilitação dos dados e documentos. Aos meus colegas de curso e amigos, pela amizade e apoio dado ao longo destes anos, um grande obrigado pelos momentos que passamos juntos. Os meus agradecimentos á Delegação do Ministério do Desenvolvimento Rural do Tarrafal (MDR), DGASP ao Instituto Nacional de Estatística (INE) e à Camara Municipal do Tarrafal (CMT). Aos meus orientadores a Professora Doutora Marina Castro e o Professor Doutor José Castro, um especial agradecimento pela orientação e os ensinamentos. Finalmente, uma enorme palavra de apreço e gratidão a todos os pastores que contribuíram de forma decisiva para a concretização deste trabalho e dedico este passo na minha vida académica de aprendizagem á minha família.
    [Show full text]