Sediment Yield and Bank Erosion Assessment

Total Page:16

File Type:pdf, Size:1020Kb

Sediment Yield and Bank Erosion Assessment University of Ghana http://ugspace.ug.edu.gh SEDIMENT YIELD AND BANK EROSION ASSESSMENT OF PRA RIVER BASIN BY John Manyimadin Kusimi (10096985) This thesis is submitted to the University of Ghana, Legon in partial fulfilment of the requirement for the award of PhD Geography & Resource Development degree. June, 2014 University of Ghana http://ugspace.ug.edu.gh Declaration This thesis entitled “Sediment yield and bank erosion assessment of Pra River Basin” is entirely an original study that I conducted. With the exception of relevant literature and ideas of specific sources which have been duly referenced, the work has not been presented anywhere in part or whole for any award of a degree. ........................................................ John Manyimadin Kusimi (Student) (10096985) Date........................................... ............................................................ Dr. Emmanuel Morgan Attua Dept of Geography & Resource Dev’t University of Ghana, Legon (Principal supervisor) Date........................................... ........................................................ Prof Bruce Banoeng-Yakubo Department of Earth Science University of Ghana, Legon (Supervisor) Date........................................... ............................................................... Dr. Barnabas Amisigo Water Research Institute CSIR, Accra (Supervisor) Date........................................... i University of Ghana http://ugspace.ug.edu.gh DEDICATION This work is dedicated to my family for their immense support, prayers and contribution. ii University of Ghana http://ugspace.ug.edu.gh Acknowledgement I am grateful to God for bringing me this far in life and academia; to my supervisors: Dr. Emmanuel Morgan Attua, Dr. Barnabas Amisigo and Prof Bruce Banoeng-Yakubo for their support, suggestions, patience and making time off their busy schedules to supervise my work. The University of Ghana partially funded this thesis by awarding me a Faculty Development Grant which was very helpful in undertaking the field work and meeting the costs of field data analysis. I will like to express my gratitude to my brother Jonathan Kusimi, wife Mrs. Bertha Kusimi and Mr. Gabriel Appiah of Water Research Institute, CSIR – Accra for assisting me in my field data collection. I will wish to thank Water Research Institute, CSIR - Accra and Ecological Laboratory (ECOLAB) of the Dept of Geography & Resource Development, University of Ghana for providing field equipment and laboratory space to collect and analyze my field samples. The support of Mr. Prince Owusu of ECOLAB during my field data analyses is also acknowledged. Lastly, I wish to thank Mr. Gerald B. Yiran of the Dept of Geography & Resource Development, University of Ghana for always responding to my call anytime I was in need of assistance with respect to data processing and analysis on the modelling aspect of the thesis. iii University of Ghana http://ugspace.ug.edu.gh List of Tables Table Page Table 2.1: Examples of models for the derivation of R values................................... 34 Table 3.1: Discharge Rating Curves............................................................................ 42 Table 3.2: Annual suspended sediment load and specific suspended sediment yield for the monitored stations in the Pra River Basin................................................ 56 Table 3.3: Parameters for suspended sediment rating curves....................................... 57 Table 4.1: Mean 210Pb Concentration levels for stream sediment and potential source materials in Birim Basin........................................................................... 64 Table 4.2: Mean 210Pb Concentration levels for stream sediment and potential source materials in Pra Basin............................................................................... 64 Table 4.3: Mean 210Pb Concentration levels for stream sediment and potential source materials in Oda Basin............................................................................. 64 Table 4.4: Mean 210Pb Concentration levels for stream sediment and potential source materials in Offin Basin............................................................................ 64 Table 4.5: Contribution of bank material and surface soil sources to suspended sediment load in the various sub-catchments...................................................... 64 Table 5.1: Annual bank erosion or deposition rates at Anyinam................................. 75 Table 5.2: Annual bank erosion or deposition rates at Amuanda Praso....................... 75 Table 5.3: Annual bank erosion or deposition rates at Akim Oda.............................. 76 Table 5.4: Annual bank erosion or deposition rates at Brenase.................................. 76 Table 5.5: Annual bank erosion or deposition rates at Ejisu....................................... 76 Table5.6: Annual bank erosion or deposition rates at Adiembra................................ 77 iv University of Ghana http://ugspace.ug.edu.gh Table 6.1A: K Factor Values of the Soil types............................................................. 86 Table 6.1B: Soil erodibility classification.................................................................... 86 Table 6.2: Land Cover Types and Cover Management (C) factor values.................... 88 Table 6.3: Attributes of Landsat ETM+ 2008............................................................. 88 Table 6.4: Land cover co-efficient values................................................................... 90 Table 6.5: Statistics of the different sediment yield model variables......................... 100 Table 6.6: Estimates of sensitivity analysis of sediment yield for 12 mm event......... 101 Table 6.7: Estimates of sensitivity analysis of sediment yield for 12.5 mm event....... 101 List of Figures Figure Page Fig.1.1: Map of the Pra River Basin........................................................................... 14 Fig.3.1: Sediment Yield Sampling Stations................................................................ 40 Fig.3.2: Daily mean concentration of samples at Anwiankwanta.............................. 44 Fig.3.3: Daily mean concentration of samples at Brenase........................................... 44 Fig.3.4: Daily mean concentration of samples at Akim Oda....................................... 45 Fig.3.5: Daily mean concentration of samples at Adiembra....................................... 45 Fig.3.6: Daily mean concentration of samples at Twifo Praso.................................... 46 Fig.3.7: Daily mean concentration of samples at Assin Praso.................................... 46 Fig.3.8: Daily mean concentration of samples at Sekyere Heman.............................. 47 Fig.3.9: Mean monthly sediment load at Akim Oda................................................... 50 Fig.3.10: Mean monthly sediment load at Brenase..................................................... 50 Fig.3.11: Mean monthly sediment load at Anwiankwanta......................................... 51 v University of Ghana http://ugspace.ug.edu.gh Fig.3.12: Mean monthly sediment load at Adiembra.................................................. 51 Fig.3.13: Mean monthly sediment load at Twifo Praso.............................................. 52 Fig.3.14: Mean monthly sediment load at Assin Praso............................................... 52 Fig.3.15: Mean monthly sediment load at Sekyere Heman......................................... 53 Fig.3.16: Annual sediment yield. ............................................................................... 56 Fig.5.1: Particle size distribution curves of bank sediments....................................... 80 Fig.5.2: Eroded bank sediments.................................................................................. 82 Fig.6.1: Schematic chart of GIS applications to soil erosion mapping and the derivation of Sediment Delivery Ratio, SDR.............................................................. 84 Fig.6.2: Effective total rainfall erosivity (Re) factor map of 2008 for 12 mm............ 92 Fig.6.3: Effective total rainfall erosivity (Re) factor map of 2008 for 12.5 mm......... 92 Fig.6.4: The soil erodibility (K) map of the basin........................................................ 92 Fig.6.5: The length and slope (LS) map of the basin................................................... 92 Fig.6.6: Cover management factor (C) map derived from satellite image classification....................................................................................................... 93 Fig.6.7: Soil erosion potential map of the basin.......................................................... 93 Fig.6.8: Gross soil erosion map of 12 mm erosive event............................................ 95 Fig.6.9: Gross soil erosion map of 12.5 mm erosive event......................................... 95 Fig.6.10: Sediment delivery ratio map of the basin................................................... 95 Fig.6.11: Sediment yield map of 12 mm erosive event.............................................. 95 Fig.6.12: Sediment yield map of 12.5 mm erosive event........................................... 96 vi University of Ghana http://ugspace.ug.edu.gh List of Plates Plate Page Plata1.1a: Illegal gold mining along the bank of the Birim River at Kyebi................... 8 Plata1.1b: Illegal alluvial gold mining of the river bed and bank of the Ofin River at Adwumain..........................................................................................
Recommended publications
  • The Economics of the Atewa Forest Range, Ghana
    THE ECONOMICS OF THE ATEWA FOREST RANGE, GHANA Living water from the mountain Protecting Atewa water resources THE ECONOMICS OF THE ATEWA FOREST RANGE, GHANA Living water from the mountain Protecting Atewa water resources DISCLAIMER This report was commissioned by IUCN NL and A Rocha Ghana as part of the ‘Living Water from the mountain - Protecting Atewa water resources’ project. The study received support of the Forestry Commission, the Water Resource Commission and the NGO Coalition Against Mining Atewa (CONAMA) and financial assistance of the Dutch Ministry of Foreign Affairs as part of the Ghana – Netherlands WASH program. The findings, interpretations and conclusions expressed here are those of the authors and do not necessarily reflect the views of the Dutch Ministry of Foreign Affairs, IUCN NL, A Rocha Ghana, the Forestry Commission, the Water Resource Commission or the NGO Coalition Against Mining Atewa (CONAMA). Any errors are purely the responsibility of the authors. Not all economic values presented in this study are captured by market mechanisms or translated to financial streams; the values of ecosystem services calculated in this study should therefore not be interpreted as financial values. Economic values represent wellbeing of stakeholders and do not represent the financial return of an investment case. The study should not be used as the basis for investments or related actions and activities without obtaining specific professional advice. This publication may be reproduced in whole or in part and in any form for educational
    [Show full text]
  • The Pra Estuary Community-Based Fisheries Management Plan
    PRA ESTUARY COMMUNITY-BASED FISHERIES MANAGEMENT PLAN WESTERN REGION, GHANA MINISTRY OF FISHERIES AND AQUACULTURE DEVELOPMENT (MOFAD) FISHERIES COMMISSION ACKNOWLEDGEMENTS Much appreciation to the following institutions who contributed in diverse ways to the development of this plan; the Shama District Assembly, Fisheries Commission, Wildlife Division of the Forestry Commission, Environmental Protection Agency, University of Cape Coast’s Department of Fisheries and Aquatic Sciences and Friends of the Nation. The contributions of key traditional leaders including Nana Kwamina Wienu II and Nana Akosua Gyamfiaba II in the Shama Paramountcy is also very much appreciated. Fisherfolk, Traditional leaders and community members from all 11 communities along the Pra River provided a great deal of information to make this plan possible. Their contributions are hereby acknowledged. Theophilus Boachie-Yiadom of Friends of the Nation compiled this document with the assistance of Philip Prah, Wim C. Mullie, Kyei Kwadwo Yamoah and Eric Mawuko Atsiatorme. Brian Crawford of the University of Rhode Island’s Coastal Resources Center (URI-CRC) reviewed this document and his efforts are very much appreciated. This plan was developed with funding support from the USAID/Ghana Sustainable Fisheries Management Project implemented by the Coastal Resources Center at the University of Rhode Island. Friends of the Nation assisted the Fisheries Commission in the drafting of this plan through facilitation of community meetings. This document is dedicated to the late Emmanuel Ohene Marfo (formerly of Fisheries Commission – Western Region) who supported many field engagements and information sharing to make this plan a success. Citation: Ghana Ministry of Fisheries and Aquaculture Development and Fisheries Commission.
    [Show full text]
  • Water Resources and Environmental Management in Ghana
    Journal of the Faculty of Environmental Science and Technology, Okayama University Vo1.9, No.I. pp.87-98. February 2004 Water Resources and Environmental Management in Ghana Kwabena KANKAM-YEBOAH*, Philip GYAU-BOAKYE**, Makoto NISHIGAKI*** and Mitsuru KOMATSU*** (Received December 3, 2003) Three principal river basins are found in Ghana and the Volta River Basin is the major one, covering about three-quarters of Ghana. The basin is shared with Mali, Burkina Faso, Cote d'lvoire, Togo and Benin. Water from the Volta River Basin is used for drinking water supply, generating hydro-electric power, irrigation, inland fisheries and lake transport. The sustainable management of the Volta River Basin is thus of great importance. Land use activities in the basin are thus closely monitored not only in Ghana, but also in the other riparian countries as well. This paper presents information and data on the water resources and environmental management of the Volta River Basin in Ghana. Key words: water resources, environmental management, Volta River Basin, Ghana, water utilization 1 INTRODUCTION both the forest and savannah zones since the early 1970s (Opoku-Ankomah and Amisigo, 1998; Paturel, et al. Ghana is covered by three main river basins. These 1997; Aka, et al. 1996). The mean annual temperatures are the Volta, South-Western and the Coastal Basins. The vary between 24.4 DC and 28.1 DC. Gyau-Boakye and Volta River Basin (Fig. 1) covers about 70 % of the total Tumbulto (2000) have observed that the mean annual surface area of the country and it is shared by six West temperature in the basin has increased by 1 DC between Africa countries, namely; Ghana, Mali, Burkina Faso, 1945 and 1993.
    [Show full text]
  • Paper 5 Ppoint Presentation
    COMMUNITIES AND SMALL SCALE MINING (CASM) 3 RD AGM AND LEARNING EVENT-ELMINA, GHANA SEPTEMBER 8th-10 th 2003 PRESENTATION BY PRECIOUS MINERALS MARKETING COMPANY LTD TOPIC: THE IMPORTANCE OF MARKETING IN SMALL SCALE MINING REGULARIZATION PROCESS IN GHANA FORMAT OF PRESENTATION • DEFINITION • NATURE • CHARACTERISTICS • HISTORICAL PERSPECTIVE - GOLD - DIAMOND • EARLY DISPOSAL BY WINNERS - DIAMOND - GOLD • ROLE OF PMMC • MARKETING OF SMALL SCALE MINERS’ WINNINGS - INTRODUCTION - DIAMOND - GOLD • CONCLUSION 1 • DEFINITION Small scale mining • Is also called artisanal mining • It involves alluvial mining operations (alluvial gold) from uncertain reserves . • It is a process where peasant miners pan for gold along the banks and the beds of rivers and streams • May involve mining deep down to gold bearing rocks (lode gold) and diamondiferous gravels. NATURE Small scale mining is: • Driven by the get rich quick mentality of transient youth. • Family- oriented analogous to subsistence farming • Largely poverty driven activity • Generally labour intensive • Widespread and prevalent in many of the world’s poorest countries in Africa and South America. CHARACTERISTICS Small scale mining is characterized by • The absence or low degree of mechanization, explosives and chemicals. • Low safety standards • Poorly trained personnel • High production waste due to low recovery • Inadequate capital • High exposure to risk and health hazards • Some illegality due to refusal to acquire mining rights and excessive trespassing • Very little consideration for environmental issues 2 HISTORICAL PERSPECTIVE GOLD • Ghana formerly Gold Coast had been associated with gold several years before arrival of Europeans. • Gold used as ornaments by Chiefs and the wealthy for barter and as a treasure in ancient kingdoms and pre-colonial Arab trading.
    [Show full text]
  • Ecology and Development Series No. 67, 2009
    Ecology and Development Series No. 67, 2009 Editor-in-Chief: Paul L.G.Vlek Editors: Manfred Denich Christopher Martius Ahmad Manschadi Janos Bogardi Adelina Maria Mensah The influence of land-use activities on nutrient inputs into upland catchment streams, Ghana Life is simple. Man complicates it when he doesn’t follow the simple pathways that govern. An honorable intension is the beginning; persistent questioning, the direction; and inner guidance, the key. Then man works with life to create magnificence. - Adelina Mensah, July 17 2008 - To my parents, for giving me the opportunity to create ABSTRACT In Ghana, increasing agricultural productivity is seen as an essential component of most development programs. The main objective of this study was to assess the implications of increased land-use activities on in-stream nutrients and impacts on the quality of water for domestic use and on aquatic ecosystem health. To guide the evaluation of the land-water interlinkages, the conceptual structure defined by the DPCER (Driving forces-Pressure- Chemical state-Ecological state-Response) framework was used, which is an adapted version of the traditional DPSIR (Driving forces-Pressure-State-Impact-Response) model. The study compares three small upland sub-catchments in the same geo-morphologic Ofin Basin of the Ahafo-Ano South District. Based on the percentage cover of natural land to agricultural land, the catchments were categorized as low (Nyamebekyere), medium (Dunyankwanta), and high (Attakrom) land-use intensities. With simple mathematical tools and selected indicators, the performance of each link within the DPCER framework was evaluated, and with the comparison of each set of indicators between catchments, changes as a function of land-use intensity were assessed.
    [Show full text]
  • Ghana: Floods
    Disaster relief emergency fund (DREF) Ghana: Floods DREF operation n° MDRGH004 GLIDE n° FL-2011-000106-GHA 19 August, 2011 The International Federation of Red Cross and Red Crescent (IFRC) Disaster Relief Emergency Fund (DREF) is a source of un-earmarked money created by the Federation in 1985 to ensure that immediate financial support is available for Red Cross and Red Crescent emergency response. The DREF is a vital part of the International Federation’s disaster response system and increases the ability of National Societies to respond to disasters. CHF 91,510 has been allocated from the IFRC’s Disaster Relief Emergency Fund (DREF) to support the Ghana Red Cross Society in delivering immediate assistance to some 2,500 beneficiaries Un-earmarked funds to repay DREF are encouraged. Summary: A 10-hour torrential rainfall in Ghana on 20 July, 2011 and the overflow of the Birim River in the Eastern Region have caused heavy flooding in some parts of the country. One Hundred and Thirty communities in 15 districts of the Eastern and Volta Regions were the most affected with 1,875 houses damaged. Nine lives were lost to the floods. Some 872 acres of farmlands have been submerged with crops washed away while some bridges have also Many of the affected persons were trapped with their houses been damaged by the floods, thereby making submerged while vehicular movement was disrupted by flood water/photo GRCS movement of people and goods difficult. Over 45,000 persons have been displaced in 4 regions of Ghana, namely Eastern, Volta, Ashanti and Central –with the Eastern and Volta being the most affected (36,517 persons).
    [Show full text]
  • Biochemistry of Mercury in an Impacted Gold Mining Tropical
    BIOGEOCHEMISTRY OF MERCURY IN AN IMPACTED GOLD MINING TROPICAL AQUATIC SYSTEM: THE PRA RIVER BASIN IN SOUTHWESTERN GHANA By AUGUSTINE KWAME DONKOR A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 2005 Copyright 2005 by Augustine Kwame Donkor TO MY LORD BE THE GLORY ACKNOWLEDGMENTS I am most grateful to the Most High God for seeing me through this program. I am very much indebted to my advisor Dr. Jean-Claude Bonzongo under whose guidance and advice I undertook this project. His invaluable ideas and wisdom he shared gave me the needed inspiration to complete this research. He will always be remembered for his support, love, concern and close cooperation. My warmest thanks also go to my supervisory committee members, Dr. Joseph Delfino, Dr. Thomas Crisman and Dr. James Winefordner (Chemistry Department) who carefully read the manuscript and made many useful suggestions. Their outstanding efforts brought this dissertation to a reality. I wish to express my profound gratitude to Dr. Vincent Nartey (Chemistry Department) University of Ghana, Accra-Ghana, for his key role in the sampling and transporting of samples to USA. His understanding, close cooperation, encouragement and moral support “kept me going and the completion of this research”. I am also thankful for the services of his student, Mr. Dennis Adotey. My sincere thanks to Dr. Benjamin Smith (Chemistry Department); his services and assistance in diverse ways will not be forgotten. I would also like to thank all my colleagues in the department especially those in Dr.
    [Show full text]
  • Kwahu South District
    KWAHU SOUTH DISTRICT Copyright © 2014 Ghana Statistical Service ii PREFACE AND ACKNOWLEDGEMENT No meaningful developmental activity can be undertaken without taking into account the characteristics of the population for whom the activity is targeted. The size of the population and its spatial distribution, growth and change over time, in addition to its socio-economic characteristics are all important in development planning. A population census is the most important source of data on the size, composition, growth and distribution of a country’s population at the national and sub-national levels. Data from the 2010 Population and Housing Census (PHC) will serve as reference for equitable distribution of national resources and government services, including the allocation of government funds among various regions, districts and other sub-national populations to education, health and other social services. The Ghana Statistical Service (GSS) is delighted to provide data users, especially the Metropolitan, Municipal and District Assemblies, with district-level analytical reports based on the 2010 PHC data to facilitate their planning and decision-making. The District Analytical Report for the Kwahu South District is one of the 216 district census reports aimed at making data available to planners and decision makers at the district level. In addition to presenting the district profile, the report discusses the social and economic dimensions of demographic variables and their implications for policy formulation, planning and interventions. The conclusions and recommendations drawn from the district report are expected to serve as a basis for improving the quality of life of Ghanaians through evidence- based decision-making, monitoring and evaluation of developmental goals and intervention programmes.
    [Show full text]
  • Ghana Water Resources Profile Overview Ghana Has Abundant Water Resources and Is Not Considered Water Stressed Overall
    WATER RESOURCES PROFILE SERIES The Water Resources Profile Series synthesizes information on water resources, water quality, the water-related dimen- sions of climate change, and water governance and provides an overview of the most critical water resources challenges and stress factors within USAID Water for the World Act High Priority Countries. The profile includes: a summary of avail- able surface and groundwater resources; analysis of surface and groundwater availability and quality challenges related to water and land use practices; discussion of climate change risks; and synthesis of governance issues affecting water resources management institutions and service providers. Ghana Water Resources Profile Overview Ghana has abundant water resources and is not considered water stressed overall. The total volume of freshwater withdrawn by major economic sectors amounts to 6.3 percent of its total resource endowment, which is lower than the water stress benchmark.i Total renewable water resources per person of 1,949 m3 is also above the Falkenmark Indexii threshold for water stress. However, water availability is influenced by management decisions and abstractions from upper-basin countries as almost half of its freshwater originates outside the country. The Volta Basin covers most of the country and is critical to hydroelectric generation, agriculture, and fisheries. However, water availability for hydropower generation and agriculture is vulnerable to drought and depends on upper basin dam releases and abstractions in Burkina Faso. Flood risks are amplified by uncoordinated floodgate releases from upstream dams. Transboundary cooperation is needed to reconcile basin development plans and address flood mitigation and drought contingencies in the Volta Basin. Informal gold mining, logging, and the expanding cocoa sector are increasing flood risks, erosion, and sedimentation in the Southwestern and Coastal Basins.
    [Show full text]
  • Soil Erosion and Sediment Yield Modelling in the Pra River Basin of Ghana Using the Revised Universal Soil Loss Equation (RUSLE)
    Soil Erosion and Sediment Yield Modelling in the Pra River Basin of Ghana using the Revised Universal Soil Loss Equation (RUSLE) John Manyimadin Kusimi1 Gerald A. B. Yiran2 Emmanuel Morgan Attua3 Abstract There has been an upsurge of uncontrolled land use activities in the Pra River Basin in Ghana which are likely to promote surface soil erosion into the fluvial sediment transport system of the basin. The revised universal soil loss equation (RUSLE) was integrated with Geographic Information System (GIS) to model the spatial patterns in soil erosion and sediment yield in 2008 within the catchment. Parameters of the model were formatted as raster layers and multiplied using the raster calculator module in ArcGIS to produce a soil erosion map. The concept of sediment delivery ratio (SDR) was used to determine the annual sediment yield of the catchment by integrating a raster SDR layer with that of the soil erosion map. Predicted soil loss and sediment yield were found to be low due to good soil protective cover by vegetation and tree crops as well as a low relief of the physical landscape. Though, the elements and processes prevailing in the basin in 2008 result in low surface soil erosion and sediment yield, this condition could degenerate into very severe surface soil erosion if the current state of land degradation, particularly small scale mining (galamsey) activities are allowed to continue. Keywords: Geographic information system; Pra River; revised universal soil loss equation; sediment delivery ratio; soil erosion modelling; sediment yield modelling. All Authors are based in the Department of Geography and Resource Development, University of Ghana 1Tel: 2 3 +233302500394 Email: [email protected] Tel: +233302500394 Email: [email protected] Tel: +233302500394 Email: [email protected] Ghana Journal of Geography Vol.
    [Show full text]
  • EVANS ASAMOAH THESIS.Pdf
    KWAME NKRUMAH UNIVERSITY OF SCIENCE AND TECHNOLOGY, KUMASI, GHANA THE IMPACT OF SMALL SCALE GOLD MINING ACTIVITIES ON THE WATER QUALITY OF RIVER BIRIM IN THE KIBI TRADITIONAL AREA EVANS ASAMOAH (B.ED SCIENCE) JUNE, 2012 KWAME NKRUMAH UNIVERSITY OF SCIENCE AND TECHNOLOGY, KUMASI, GHANA THE IMPACT OF SMALL SCALE GOLD MINING ACTIVITIES ON THE WATER QUALITY OF RIVER BIRIM IN THE KIBI TRADITIONAL AREA BY EVANS ASAMOAH (B.ED SCIENCE) A THESIS SUBMITTED TO THE DEPARTMENT OF THEORETICAL AND APPLIED BIOLOGY, KWAME NKRUMAH UNIVERSITY OF SCIENCE AND TECHNOLOGY (KNUST), KUMASI, IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE IN ENVIRONMENTAL SCIENCE. JUNE, 2012 DECLARATION Candidate’s Declaration I hereby declare that this work presented to the Department of Theoretical and Applied Biology in partial fulfillment for the award of MSc. Degree, is a true account of my own work except where particularly all sources of information have been acknowledged by means of reference. Candidate’s signature…………………………………. Date…………………… Name: Evans Asamoah (STUDENT) Signature…………………………………. Date………………… Prof. B.W.L. Lawson (SUPERVISOR) Signature…………………………………. Date………………… Rev. Stephen Akyeampong (HEAD OF DEPARTMENT) ii ABSTRACT The study of the impact of small scale gold mining activities on the water quality of river Birim in the Kibi Traditional Area was carried out at the four sampling sites along the river profile. Water and sediment samples of the River were analyzed for various parameters and compared with Ghana Environmental Protection Agency (GEPA) and World Health Organization (WHO) permissible guidelines for drinking water. The water quality parameters included pH, Electrical Conductivity (EC), Total Dissolved Solids (TDS), Total Suspended Solids (TSS), Dissolved Oxygen (DO) and True Colour.
    [Show full text]
  • Alluvial Diamond Resource Potential and Production Capacity Assessment of Ghana
    Prepared in cooperation with the Geological Survey Department, Minerals Commission, and Precious Minerals Marketing Company of Ghana under the auspices of the U.S. Department of State Alluvial Diamond Resource Potential and Production Capacity Assessment of Ghana Scientific Investigations Report 2010–5045 U.S. Department of the Interior U.S. Geological Survey Cover. The Bonsa River flowing west-northwest from the village of Bonsa, March 2009. Alluvial Diamond Resource Potential and Production Capacity Assessment of Ghana By Peter G. Chirico, Katherine C. Malpeli, Solomon Anum, and Emily C. Phillips Large alluvial diamond mining site at alluvial flat in Wenchi, March 2009 Prepared in cooperation with the Geological Survey Department, Minerals Commission, and Precious Minerals Marketing Company of Ghana under the auspices of the U.S. Department of State Scientific Investigations Report 2010–5045 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2010 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report.
    [Show full text]