Omonona and Okogbue I.Pdf

Total Page:16

File Type:pdf, Size:1020Kb

Omonona and Okogbue I.Pdf GROUNDWATER POTENTIALS OF BASEMENT COMPLEX AREAS: CASE OF MOPA/AMURO AND EGBE AREAS, KOGI STATE, NIGERIA BY OMONONA, OLUFEMI VICTOR (PG/M.Sc/07/42520) DEPARTMENT OF GEOLOGY FACULTY OF PHYSICAL SCIENCES UNIVERSITY OF NIGERIA, NSUKKA NIGERIA JULY, 2010. GROUNDWATER POTENTIALS OF BASEMENT COMPLEX AREAS: CASE OF MOPA/AMURO AND EGBE AREAS, KOGI STATE, NIGERIA BY OMONONA, OLUFEMI VICTOR (PG/MSc/07/42520) A RESEARCH PROJECT SUBMITTED TO THE DEPARTMENT OF GEOLOGY, FACULTY OF PHYSICAL SCIENCES UNIVERSITY OF NIGERIA, NSUKKA IN PARTIAL FULFILLMENT OF THE REQUIREMENT FOR THE AWARD OF A MASTER OF SCIENCE IN HYDROGEOLOGY JULY, 2010. i CERTIFICATION Omonona, Olufemi Victor, a post graduate student in the Department of Geology with the registration number, PG/MS.c/07/42520 has satisfactorily completed the requirements for the course and research work for the degree of Master of Science in Hydrogeology. The work embodied in this project report is original and has not been submitted in part or full for any other degree or diploma of this or any other university. _______________________________ _________________ Prof C.O. Okogbue Date Project Supervisor ________________________________ _________________ Dr. A.W. Mode Date Ag. Head of Department _________________________________ ________________ External Examiner Date ii DECLARATION Omonona, Olufemi Victor, a post graduate student in the Department of Geology with the registration number, PG/MS.c/07/42520 has satisfactorily completed the requirements for the course and research work for the degree of Master of Science in Hydrogeology. The work embodied in this project report is original and has not been submitted in part or full for any other degree or diploma of this or any other university. ________________________________ ___________________ Date Supervisor _________________________________ __________________ Head of Department Date iii DEDICATION This piece of work is dedicated to the LORD GOD ALMIGHTY, who is my Life and Light. And also to the loving memory of my sister-in-Christ and friend, Oluwatosin Mosunmola Otitoju, whose lifestyle was challenging. iv ACKNOWLEDGEMENT I would like to thank my supervisor, Prof C.O. Okogbue, for accepting to take over the supervision of the work as soon as my former supervisor, Prof H.I. Ezeigbo proceeded to the life beyond in November, 2008. I am indeed very grateful for taking some time out of his very busy schedule to peruse the thesis. His criticisms, corrections and suggestions are clearly manifested in the quality of the work. The efforts of my late supervisor are worthy of mentioning. He spurred my interest in hydro-geophysics and encouraged me to pursue the topic despite my lack of what it entails in the first instance. To all members of staff of the Department of Geology, University of Nigeria, Nsukka, I appreciate you for providing a good working environment. Without this, it would have been difficult to complete this work. Many thanks to Mr. S. O Onwuka, whom I had sessions of beneficial discussions and he gave his time for a critical review of the manuscript. I am particularly grateful to Mr. Olawole J.F. and Mr. Kunle Rasaq of Lower River Niger Basin and Rural Water Development Authority, Ilorin, Kwara State for providing the primary vertical electrical sounding and borehole data for this work. I must not also forget to appreciate the moral and spiritual supports I received from members of the Graduate Student Fellowship and Christ Church Chapel, Sunday School Department, University of Nigeria, Nsukka. And also, to a host of friends too numerous to mention I say “Thank You All”. And to my parents; Revd E.A. and Mrs. J.A. Omonona, who were my first teachers. I am grateful for your lives; you believed in and encourage the education of your children. Finally, to my Lord and Saviour Jesus Christ, He is my life and light. He is the Living Water who bids each one of us to come and drink. Thank You Jesus! v ABSTRACT Investigations have been carried out for groundwater potentials, aquifer protective capacity and hydro-geochemical characteristics in Mopa/Amuro-Egbe Areas of Kogi State, Nigeria. The areas are underlain by the Nigeria Basement Complex consisting of PreCambrian rocks, made up of porphyroblatic granites, porphyritic granite, quartz granite, pegmatite, augen gneiss and migmatite gneiss. Static water level of 103 water wells were measured at the peak of dry season, and the results used to generate hydraulic head data and hydraulic head map. A total of 81 vertical electrical soundings data were interpreted using curve-matching and computer aided techniques. Groundwater potential zones were delineated based on geology, hydro-geological and geo-electrical data. A total of 20 samples, three from boreholes and 17 from hand dug wells, were analyzed for their physiochemical properties with the intent of assessing their quality and characteristics. The static water level range between 0.01m and 10.16m. The hydraulic head map revealed two groundwater flow directions: northeastern and eastern. One main converging (collecting) zone and three diverging (radiating) zones were deciphered. The former coincides with areas of good groundwater potential zones and the latter low groundwater potential. The studies reveal three groundwater potential zones namely, high, medium and low. The result of the interpretation of the geophysical data shows that the area is characterized by variable subsurface layering ranging from two layers to five layers. Three distinct aquifer protective zones were identified namely moderate, poor and weak. The factors/processes which control the sources of elements in the groundwater include geologic/lithologic factor, contamination via weathering, agricultural drainage and bacteriological factors. Four hydro-geochemical facies (water types) were deduced from the − −2 −2 − Piper diagram. These include Na-K- HCO 3 , Ca-(Mg) - SO 4 , Ca-Mg-( SO 4 )- HCO 3 and −2 Na-K-( SO 4 ). The water quality was found to be good for all agricultural purposes. Water treatment may be required for some of the groundwater sources for drinking purposes because their elemental concentrations are above WHO (1993) guideline values. vi TABLE OF CONTENTS PAGES TITLE PAGE ii CERTIFICATION iii DECLARATION iv DEDICATION v ACKNOWLEDGEMENT vi ABSTRACT vii TABLE OF CONTENT viii LIST OF TABLES ix LIST OF FIGURES x LIST OF APPENDICES xi CHAPTER ONE: INTRODUCTION 1.1 Background Information 1 1.2 Location and Accessibility 1 1.3 Climate and Vegetation 2 1.4 Relief and Drainage 2 1.5 Aims and Objectives 2 1.6 Review of Previous Works 5 CHAPTER TWO: GEOLOGY AND HYDROGEOLOGY 2.1 Regional Geological Setting 9 2.2 Regional Hydrogeological Setting 14 2.3 Local Geology 15 2.4 Local Hydrogeology 15 CHAPTER THREE: METHODS OF STUDY 3.1 Geological Investigation 16 3.2 Geophysical Method 16 3.3 Hydro-geophysical Investigation 16 3.4 Data Analysis 20 vii CHAPTER FOUR: RESULTS AND DUSCUSSION 4.1 Local Geology and Groundwater Yield 23 4.2 Static Water Level and Hydraulic Head: Groundwater Flow Directions 23 4.3 Geo-electrical Characterization 28 4.4 Depth to Bedrock (Overburden Thickness) 31 4.5 Basement Relief 31 4.6 Evaluation of Aquifer Protective Capacity 38 4. 7 Groundwater Potentials Evaluation 42 4.8 Groundwater Quality and Hydro-geochemistry 44 4.9 Sources of Elements and the Controlling Processes 65 4.10 Hydro-Geochemical Facies 69 4.11 Stiff Pattern 73 CHAPTER FIVE: CONCLUSION 5.1 Conclusion and Recommendation 75 REFERENCES 78 APPENDICES 85 viii LIST OF TABLES Table1. Result of Borehole Yield and Static Water Level 24 Table 2 Static Water Level and Hydraulic Head 25 Table 3 Layer Resistivity, Thickness and Curve Types 29 Table 4 Longitudinal Conductance /Protective Capacity Rating 39 Table 5 Longitudinal Conductance and Aquifer Protective Capacity 40 Table 6 Aquifer potential as a Function of Weathered Layer Thickness and Resistivity 45 Table 7 Aquifer Potential as a Function of Depth to Bedrock and Bedrock Resistivity 46 Table 8 Physical and Biological Parameters 48 Table 9 Chemical Parameters 49 Table 10 Cations and Anions 50 Table11 Heavy Metals 52 Table 12 Hardness Classification of Water 55 Table13 Modified Richard Quality Classification of Irrigation Water 64 Table14 Suggested Limit for Magnesium Drinking Water for Livestock 64 Table 15 Guidelines for Levels of Toxic Substances in Live stocks Drinking Water 64 Table 16 Principal Component Analysis 66 Table 17 Correlation Matrix 67 ix LIST OF FIGURES 1 Location Map of the Study Area 3 2 Drainage Map of the Study Area 4 3 Geological Map of the Study Area 17 4 Sketch Diagram of Schlumberger Array 18 5 Base Map of the Study Area Showing the VES Locations 19 6 Base Map of the Study Area Showing the Pumping Test Locations 21 7 Base Map of the Study Area Showing Water Sampling locations 22 8 Static Water Level Map of the Study Area 26 9 Hydraulic Head Map of the Study Area 27 10 Frequency Distribution of observed Curve Types 30 11 Top Soil Thickness Map of the Study Area 32 12 Top Soil Resistivity Map of the Study Area 33 13 Weathered Layer Isopach Map of the Study Area 34 14 Weathered Layer Isorestivity Map of the Study Area 35 15 Overburden Map of the Study Area 36 16 Basement Relief Map of the Study Area 37 17 Aquifer Protective Capacity Rating 41 18 Aquifer Protective Capacity Map of the Study Area 43 19 Groundwater Potentials Map of the Study Area 47 20 Spatial Distribution of Arsenic in the Study Area 57 21 Spatial Distribution of Cadmium in the Study Area 59 22 Spatial Distribution of Chromium in the Study Area
Recommended publications
  • Effects of Wood Ash Biomass Application on Growth Indices and Chlorophyll Content of Maize and Lima Bean Intercrop
    Turkish Journal of Agriculture - Food Science and Technology, 5(6): 614-621, 2017 Turkish Journal of Agriculture - Food Science and Technology Available online, ISSN: 2148-127X www.agrifoodscience.com, Turkish Science and Technology Effects of Wood Ash Biomass Application on Growth Indices and Chlorophyll Content of Maize and Lima bean Intercrop Rasheedat Ajala,1 Moses Awodun1, Segun Oladele2* 1Department of Crop, Soil and Pest Management, Federal University of Technology Akure, Ondo State. Nigeria 2Department of Agronomy, Adekunle Ajasin University Akungba-Akoko, Ondo State Nigeria A R T I C L E I N F O A B S T R A C T Wood ash generated from wood industries have enormous potential which can be utilized Research Article due to its properties which influences soil chemistry and fertility status of tropical acidic soils. Field experiments were conducted on an acidic sandy loam alfisol to investigate the Received 24 November 2016 effects of wood ash on the growth indices and chlorophyll content of maize and lima Accepted 26 December 2016 beans intercrop during the late and early seasons of 2014 and 2015 at Akure in the rainforest zone of southwestern Nigeria. The treatments were 100% sole maize with ash, Keywords: 100% sole maize without ash, 75% maize + 25% lima beans with ash, 75% + 25% lima Maize-lima beans beans without ash, 50% maize + 50% lima beans with ash, 50% maize + 50% lima beans Intercrop without ash, 25% maize + 75% lima beans with ash and 25% maize + 75% lima beans Wood ash without ash. Wood ash was applied at 2.4kg/plot.
    [Show full text]
  • Necrophilia and Elite Politics: the Case of Nigeria Adebanwi, W
    Necrophilia and elite politics: the case of Nigeria Adebanwi, W. Citation Adebanwi, W. (2007). Necrophilia and elite politics: the case of Nigeria. Retrieved from https://hdl.handle.net/1887/11561 Version: Not Applicable (or Unknown) License: Downloaded from: https://hdl.handle.net/1887/11561 Note: To cite this publication please use the final published version (if applicable). African Studies Centre Leiden, The Netherlands Necrophilia and Elite Politics: The Case of Nigeria Wale Adebanwi ASC Working Paper 71 / 2007 African Studies Centre P.O. Box 9555 2300 RB Leiden The Netherlands Telephone +31-71-5273372 Fax +31-71-5273344 E-mail [email protected] Website http://www.ascleiden.nl © Wale Adebanwi, 2007 2 Abstract This work examines the political intrumentalization of culture and history as embodied in a ‘Big Man’, an Ur-agent that over-represents the cultural whole. I examine how the elites within a specific ethno-cultural group represent and re-present themselves as agents, using the specific instance of the ‘Cult of Awo (Obafemi Awolowo)’, the late politician regarded as the modern ‘avatar’ of the Yoruba. It focuses primarily on how the burial and the statue of the late leader were used to emphasize his centrality in Yoruba politics, by exploring ‘the form and meaning of the aura around a dead’ hero. The work examines the monumentalization of Awo, how his life and death are interpreted, and used to articulate Yoruba collective political vision and future - both materially and symbolically. While the death of Awo in 1987 provided a platform for a struggle by the elite associated with him to project themselves in his image as worthy successors – thereby creating internal struggles for supremacy – the controversy surrounding the destruction of his statue in 2003, happening at a point when those opposed to Awo were canvassing the ‘end of (the Awo) era’, also provides a context for examining the agency of Awo, in material and symbolic terms, in Yoruba politics.
    [Show full text]
  • Evaluation of Fertility Status of Soils of Yagba West Local Government Area of Kogi State
    Journal of Agricultural Science and Engineering Vol. 2, No. 3, 2016, pp. 18-23 http://www.aiscience.org/journal/jase ISSN: 2381-6821 (Print); ISSN: 2381-6848 (Online) Evaluation of Fertility Status of Soils of Yagba West Local Government Area of Kogi State Amhakhian Sunday Okhonfoh *, Oyelude Ifelola, AINA Oluseyi Abel Department of Soil and Environmental Management, Faculty of Agriculture, Kogi State University, Anyigba, Nigeria Abstract The study was conducted to evaluate the current soil fertility status of different farmlands in Yagba West Local Government area of Kogi state. A total of 24 samples were taken from two districts at a depth of 0-15cm and 15-30cm from each ward. The samples were analyzed each for their Physio-chemical properties. The results obtained showed that particle size distribution ranged from loamy sand (LS) to sandy loam (SL). The pH of the area were within 5.0-6.54, a pH range suitable for most agricultural crops, while EC of the soils ranges from 0.10-0.60µmhos/cm. Available phosphorus (P) in the soil ranged from 2.26-20.42mg/kg with a mean value of 8.02mg/kg at depth of 0.15cm and 1.23-14.2mg/kg with a mean value of 5.66mg/kg at depth of 15-30cm, which is below the critical value of 15ppm. Total nitrogen and organic carbon fell below their critical values of 0.78% and 0.64% respectively. Exchangeable cations (Ca, Mg, K, Na) gave mean values of 3.21, 1.14, 1.38 and 0.64Cmol/kg respectively of Ca, Mg, K and Na.
    [Show full text]
  • The Contributions of Chief Obafemi Awolowo to the Growth and the Development of Nigeria During First Republic
    Annals of Reviews and Research Review Article Ann Rev Resear Volume 4 Issue 4 - March 2019 Copyright © All rights are reserved by Buhari LO The Contributions of Chief Obafemi Awolowo to the Growth and the Development of Nigeria During First Republic Buhari LO* Department of History and International Studies, Ekiti State University, Ado-Ekiti, Nigeria Submission: October 11, 2018; Published: March 11, 2019 *Corresponding author: Buhari LO, Department of History and International Studies, Ekiti State University, Ado-Ekiti, Nigeria Abstract This study examines the personality of Chief Obafemi Awolowo in the making of Nigerian nation in the First Republic. The study found out keythat playerChief Obafemi in the intra-party Awolowo waspower a Nigerian tussle that nationalist erupted and in 1962 statesman that led who to playeddisturbances a significant in Western role in Region Nigeria’s House independence of Assembly. movement Also, the during study examinesFirst and Secondmajor challenges Republics. faced The studyby Chief notes Obafemi that Chief Awolowo Obafemi and Awolowohow he eventually was thrice became a major the contender Federal Commissioner for Nigeria’s highestof Finance office. and He the was Vice a Chairman of the Federal Executive Council in 1966. The study employs primary and secondary source materials including books, journal articles and other scholarly publications to interrogate the study. It concludes that Awolowo was responsible for much of the progressive social legislation that made Nigeria a modern nation today. Keywords: Nigeria; Obafemi Awolowo; Economy; Nation; Politics Introdution a modernist Yoruba political project in an emergent Nigerian The Yoruba speaking people are found not only in the post-colonial nation-state after decolonization process in the Western Region Nigeria but also in other parts of West Africa (Dahomey and Togo, and as far as Brazil and Cuba).
    [Show full text]