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HEAVY METAL DISTRIBUTION IN SEDIMENT OF AKPABUYO STREAM, CROSS RIVER BASIN SOUTHEASTERN NIGERIA

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ABSTRACT

Sediment samples were collected through the purposive sampling method from various streams in Akpabuyo L.G.A, ten sample location were selected. The concentration and areal distribution of selected metals (Fe, Zn, Mn, Cr, Ni, Co, Cu, Cd, Pb) in the sediments of Akpabuyo streams .Geo-accumulation index have been calculated to assess whether the concentrations observed represent background or contamination levels. It proves that the choice of the background plays an important role in the interpretation of the geo-chemical data. It is concluded that the selected streams in Akpabuyo is uncontaminated except a metal (Cd) which it i-geo value is 1 which means it is moderately/uncontaminated.

TABLE OF CONTENTS

ABSTRACT- – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – ii

LIST OF FIGURES – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – iii

LIST OF TABLES – – – — – – – – – – – – – – – – – – – – – – – – – – – – – – – – – iv

TABLE OF CONTENTS – – – – – – – – – – – – – – – – – – – – – – – – – – – – – – v

CHAPTER ONE

1.1 INTRODUCTION

1.2 AIMS AND OBJECTIVE

1.3 STUDY AREA

1.4 GEOLOGY OF THE STUDY AREA

CHAPTER TWO

2.1 LITERATURE REVIEW

CHAPTER THREE

3.1 MATERIALS

3.2 METHODOLOGY(FIELD)

3.3 LABORATORY METHODOLOGY

CHAPTER FOUR

4.1 RESULTS AND DISCUSSIONS

CHAPTER FIVE

5.1 SUMMARY AND CONCLUSION

REFERENCES

CHAPTER ONE

1.1 INTRODUCTION

Heavy metals pollution of aquatic ecosystem is becoming a potential global problem, pollution typically refers to chemicals or other substance in concentration greater than it would occur under natural conditions. Water pollution is the introduction by man of substances into the aquatic environment resulting from deleterious effect as harm to human health (FAO 1990).The presence of increased level of heavy metals in the aquatic environment has been of much concern for the past decades due to adverse effect of some metals on living organisms in food chains leading to man. Pollutants are the cause of major water quality degradation around the world. Several toxic metals which are important to the environment and human health have been detected in aquatic media. These toxic metals include the non-essential meals and are no importance to humans (Borgman and Norwood 2002).

Trace amount of heavy metals are always present in fresh water from terrigenous sources such as weathering of rocks resulting into geo-chemical recycling of heavy metal elements in these ecosystem. Trace elements may be immobilised within the stream sediments and could be involved in absorption, co-precipitation and complex formation. Sometimes they are co-adsorbed with other elements as oxides, hydroxides of Fe, Mn, or may occur in particulate form.

Heavy metal may enter into aquatic ecosystem from anthropogenic sources, such as industrial wastewater discharge, sewage wastewater, fossil fuel combustion, and atmospheric deposition. Trace element in stream sediment compartment can be used to reveal the history and intensity of local and regional pollution. In this work, the of stream sediment contamination was assess using geo-accumulation index.

1.2 AIMS AND OBJECTIVES

The main objectives of the current study area are:

To assess the extent and degree of metals, and the origin of these metals, using the geo-accumulation index of the metals.
To determine the total content of heavy metals in surface sediments of Akpabuyo.
To estimate the anthropogenic input and to assess the pollution status on the area.
1.3 STUDY AREA

The study area which is located in Akpabuyo, Cross River State lies between longitudes 80 22I 30II E – 80 30I 0II E and latitude 40 52I 30II N – 40 57I 30II N (fig 2). With an area of 126,4032 Square Km. Although many stream samples where collected but few was selscted for the heavy metal analysis. The various Locations in Akpabuyo which sediment samples were collected and used to carry out the analysis are Esuk Mbat stream(L1), Esuk Ekpo Eyo Stream(L2), Ikot Akwa Stream(L3), Dan Archibong Stream(L4), Itu Stream(L5), Ikot Ndarake Stream(L6), Asioha Stream(L7), Ikot Ekpo Ene Stream(L8), Ekpene Ikot Imo Stream(L9), Ikot Nakanda(L10), and their following coordinate shown respectively (table 1.3) . It originate from a hilly region and flows through several villages and farmland.

Map of Cross River State indicating the study area Akpabuyo(yellow arrow) Fig. 1

Fig. 2. Map of the study area and sample locations.

LOCATION NO.

LOCATION NAME

LATITUDE

LONGITUDE

1.

Esuk Mbat Stream

N 040 54I 40.3II

E 0080 23I 43.7

2.

Esuk Ekpo Eyo Stream

N 040 56I 55.8II

E 0080 23I 46.2II

3.

Ikot Akwa Stream

N 040 56I 30.6II

E 0080 27I 20.7II

5.

Dan Archibong Stream

N 040 56I 12.4II

E 0080 27I 35.5II

6.

Itu Stream

N 040 57I 19.9II

E 0080 28I 42.2II

7.

Ikot Ndarake Stream

N 040 56I 54.6II

E 0080 25I 46.3II

8.

Asioha Stream

N 040 55I 36.0II

E 0080 29I 43.9II

9.

Ikot Ekpo Ene Stream

N 040 53I 34.0II

E 0080 25I 46.0II

10.

Ekpene Ikot Umo Stream

N 040 54I 55.7II

E 0080 24I 19.8II

11.

Ikot Nakande Stream

N 040 52I 42II

E 0080 29I 29.0II

TABLE 1.3 Showing location names and their bearings.

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NameHEAVY METAL DISTRIBUTION IN SEDIMENT OF AKPABUYO STREAM, CROSS RIVER BASIN SOUTHEASTERN NIGERIA removeTHE GEOLOGY OF SOUTHERN AKOR AND ITS ENVIRONMENT removeEFFECTS OF SOIL EROSION ON SETTLEMENT removeResistivity methods used in horizontal and vertical discontinuities in the electrical properties of the ground water detection removeHEAVY METAL DISTRIBUTION IN SEDIMENT OF AKPABUYO STREAM, CROSS RIVER BASIN SOUTH EASTERN NIGERIA removeEFFECT OF LAND DISPUTE ON THE SOCIO-ECONOMIC ACTIVITIES remove
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Description
ContentABSTRACT Sediment samples were collected through the purposive sampling method from various streams in Akpabuyo L.G.A, ten sample location were selected. The concentration and areal distribution of selected metals (Fe, Zn, Mn, Cr, Ni, Co, Cu, Cd, Pb) in the sediments of Akpabuyo streams .Geo-accumulation index have been calculated to assess whether the concentrations observed represent background or contamination levels. It proves that the choice of the background plays an important role in the interpretation of the geo-chemical data. It is concluded that the selected streams in Akpabuyo is uncontaminated except a metal (Cd) which it i-geo value is 1 which means it is moderately/uncontaminated. TABLE OF CONTENTS ABSTRACT- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - ii LIST OF FIGURES - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - iii LIST OF TABLES - - - -- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - iv TABLE OF CONTENTS - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - v CHAPTER ONE 1.1 INTRODUCTION 1.2 AIMS AND OBJECTIVE 1.3 STUDY AREA 1.4 GEOLOGY OF THE STUDY AREA CHAPTER TWO 2.1 LITERATURE REVIEW CHAPTER THREE 3.1 MATERIALS 3.2 METHODOLOGY(FIELD) 3.3 LABORATORY METHODOLOGY CHAPTER FOUR 4.1 RESULTS AND DISCUSSIONS CHAPTER FIVE 5.1 SUMMARY AND CONCLUSION REFERENCES CHAPTER ONE 1.1 INTRODUCTION Heavy metals pollution of aquatic ecosystem is becoming a potential global problem, pollution typically refers to chemicals or other substance in concentration greater than it would occur under natural conditions. Water pollution is the introduction by man of substances into the aquatic environment resulting from deleterious effect as harm to human health (FAO 1990).The presence of increased level of heavy metals in the aquatic environment has been of much concern for the past decades due to adverse effect of some metals on living organisms in food chains leading to man. Pollutants are the cause of major water quality degradation around the world. Several toxic metals which are important to the environment and human health have been detected in aquatic media. These toxic metals include the non-essential meals and are no importance to humans (Borgman and Norwood 2002). Trace amount of heavy metals are always present in fresh water from terrigenous sources such as weathering of rocks resulting into geo-chemical recycling of heavy metal elements in these ecosystem. Trace elements may be immobilised within the stream sediments and could be involved in absorption, co-precipitation and complex formation. Sometimes they are co-adsorbed with other elements as oxides, hydroxides of Fe, Mn, or may occur in particulate form. Heavy metal may enter into aquatic ecosystem from anthropogenic sources, such as industrial wastewater discharge, sewage wastewater, fossil fuel combustion, and atmospheric deposition. Trace element in stream sediment compartment can be used to reveal the history and intensity of local and regional pollution. In this work, the of stream sediment contamination was assess using geo-accumulation index. 1.2 AIMS AND OBJECTIVES The main objectives of the current study area are: To assess the extent and degree of metals, and the origin of these metals, using the geo-accumulation index of the metals. To determine the total content of heavy metals in surface sediments of Akpabuyo. To estimate the anthropogenic input and to assess the pollution status on the area. 1.3 STUDY AREA The study area which is located in Akpabuyo, Cross River State lies between longitudes 80 22I 30II E – 80 30I 0II E and latitude 40 52I 30II N – 40 57I 30II N (fig 2). With an area of 126,4032 Square Km. Although many stream samples where collected but few was selscted for the heavy metal analysis. The various Locations in Akpabuyo which sediment samples were collected and used to carry out the analysis are Esuk Mbat stream(L1), Esuk Ekpo Eyo Stream(L2), Ikot Akwa Stream(L3), Dan Archibong Stream(L4), Itu Stream(L5), Ikot Ndarake Stream(L6), Asioha Stream(L7), Ikot Ekpo Ene Stream(L8), Ekpene Ikot Imo Stream(L9), Ikot Nakanda(L10), and their following coordinate shown respectively (table 1.3) . It originate from a hilly region and flows through several villages and farmland. Map of Cross River State indicating the study area Akpabuyo(yellow arrow) Fig. 1 Fig. 2. Map of the study area and sample locations. LOCATION NO. LOCATION NAME LATITUDE LONGITUDE 1. Esuk Mbat Stream N 040 54I 40.3II E 0080 23I 43.7 2. Esuk Ekpo Eyo Stream N 040 56I 55.8II E 0080 23I 46.2II 3. Ikot Akwa Stream N 040 56I 30.6II E 0080 27I 20.7II 5. Dan Archibong Stream N 040 56I 12.4II E 0080 27I 35.5II 6. Itu Stream N 040 57I 19.9II E 0080 28I 42.2II 7. Ikot Ndarake Stream N 040 56I 54.6II E 0080 25I 46.3II 8. Asioha Stream N 040 55I 36.0II E 0080 29I 43.9II 9. Ikot Ekpo Ene Stream N 040 53I 34.0II E 0080 25I 46.0II 10. Ekpene Ikot Umo Stream N 040 54I 55.7II E 0080 24I 19.8II 11. Ikot Nakande Stream N 040 52I 42II E 0080 29I 29.0II TABLE 1.3 Showing location names and their bearings.ABSTRACTS The study area is located within latitude 050 271 4611N and longitude 0080 431 46E, and the elevation of the place is 156m. The major rock types encountered in the area include gneisses, quartzite, amphibolites and marbles. These are intruded by pegmatite, quartz vein and aplite. The latest metamorphic episode occurred during the Pan-African Orogeny (600 ± 15ma) and the deformation left a structural trend of NS and NE-SW on the rocks. The occurrence of NW-SE structural trend are also shown on some rocks indicating that the Pan-African event did not completely alter earlier structural imprints. The study area is highly forested, undulating in slope and is a characteristic of a tropical rain forest in the area. Chapter One: Introduction The geology of southern Akor and its environs lies within the Oban Massif, a component of the crystalline basement of Nigeria. The Nigeria crystalline basement in turn forms a part of the African crystalline basement and covers over 50% of the total land surface of Nigeria . The rock assemblages encountered and identified consists of mainly schists, gneisses, Amphibolite, Charnockite, Marble and Quartzites and pegmatite, Quartz vein and Aplite emerging as Igneous intrusive rocks. The area mapped and studied (Akor) is predominated by intrusive rocks and these rocks are very well exposed where the topographyis slopy along streams and river channels. Ekwueme et al (1992) proposed that charnockite rock's occur in both the eastern and western Oban Massif. The rocks occur as large coarse-grained, rounded and, massive bodies deformed together with the bounded gneisses. Ekwueme (1992) has shown that the diorities and charnockite are similar in composition and that the former may be retrogressive product of the latter. The occurrences of weathering and tectonic activities were observed to have greatly affected the exposed outcrop and such effects from wet season had deformed these outcrops to boulders with reference to their shapes and sizes. 1.1 Location and accessibility The area is located in the Eastern part of Akamkpa local Government area of theCross River State of Nigeria. It covers an estimated area of about 85sq.KM and constitutes part of the Oban Massif of the South-eastern Nigeria. The map area is largely made up of Ntebachot Akor. New Ntebeji and Ayip Eku all located in Akamkpa Local Government area of Cross River state. About 90 percent of the area is inaccessible due to thick vegetation, steep valleys and hilly terrains. The only access road across the area is the Calabar-Ekang Road while hunters tracks provide minimal access into the area.ABSTRACT This study examined the effects of soil erosion on settlement in Agbor, and its environs. It identifies the problems, conservation, strategies, control techniques and suggest proper management practices. The study adopts the survey research design in data collection through administration of 150 questionnaires to the respondents in Agbor coupled with direct field measurement of gully erosion effect on building structure in Agbor region. The data collected were analzed using PPMC and t-test statistical techniques. The PPMCC correlation value obtained for hypothesis 1 (0.935) is greater than the critical value (0.754) at 0.05 level of significance and the t-test calculated value (12.542) for hypothesis 2 is greater than t-critical value (3.182) at 0.05 level of significance. The PPMCC coefficient correlation value obtained for hypothesis 3 (6.235) is greater than the critical value (3.182) at 0.05 level of significance. This indicated that the hypotheses tested shows that there is a significant relationship between the effects of soil erosion and the level of settlement development in Agbor. Furthermore, hypothesis 2 shows that that there is a significant relationship between the causes of soil erosion and the factors responsible for the degradation of Agbor and its environs. The result of hypothesis 3 shows that soil erosion has significant effect on the settlement of Agbor. The implication is that soil erosion has resulted to the collapse of buildings and poor settlement structure in Agbor. This shows that, soil erosion has significant effect on the settlement of Agbor. The study recommended that government/private individuals should construct drainage, embankments and sand fill burrow pits. CHAPTER ONE 1.1 INTRODUCTION Soil erosion is a naturally occurring process whether it is by water, wind or ice, involves the actions of soil detachment, movement and deposition. It could be a slow process that continues relatively unnoticed or can occur at an alarming rate, causing serious loss of top soil (Jim, 2012). Loose soil, low organic matter, loss of soil structure, poor internal drainage, salination and soil acidity problems are other serious soil degradation conditions can accelerate the soil erosion process. Erosion is a natural process that is prompted by man-made human (anthropogenic) activities such as deforestation that involves the removal of vegetation, overgrazing, unmanaged construction of building and roads. Excessive erosion can produce ecosystem damage, loss of soil and receiving water sedimentation. The effect of soil erosion is sometimes linked to over population (Cohen, 2007). He further stated that erosion tends to remove topsoil at a faster rate than soil is accumulated in an area. This results in collapse of buildings, especially those of poor foundation. This affects settlement development by residents within the study area. However, increased soil erosion at a much faster rate than soil is accumulated materially or artificially is a recent problem due to mankind’s conservation which in action makes the land unprotected and vulnerable to degradation. Other natural causes are occurring adduced the rainfall with wind storms to make wreck havoc on the environment. This ugly effects occurs both in residential and agricultural/farming areas as well as the natural environment. The effects of soil erosion are found insitu (on-site) where the soil become detached), as well as off-site where the eroded soil is transported. Also, in form of the high rainfall, storms obviously cause deep gullies, but erosion due to smaller events can seem in form of sheets with no consequence, but in fact there is a cumulative effect on a long-term basis. 1.2 STUDY BACKGROUND Cohen (2007) stated that, the most serious consequence of soil erosion globally is the treat to long-term sustainability of agricultural productivity and hindrance to settlement development. This eventually leads to development of rugged terrain and collapse of buildings. The destructive impact of erosion is felt on developing countries such as Africa and Asia, and developed countries for which there is a huge environmental concern. Soil erosion results in the loss of soil fertility that makes the land barren that accumulate more than 25 million hectares of barren lands in the world and to desertification (Tutor Vista, 2013). High rainfall of short duration and torrential downpour results in flash floods that make rivers overflow their banks, destroy foundation and collapse buildings, washed away live stock and act as hindrance to settlement development (Adelye and Rustum, 2011). Also, it could damage bridges and causes a dam to overflow to submerging buildings, displace people from homes, with attendant loss of personal valuables and ongoing psychological fear and insecurity caused by such event (Bariweni, Tawari and Abowei, 2012). Like wind and water, coaster erosion is a natural process but can be exacerbated by human activities. Activities that can influence Agbor erosion of river droughts, include, mining of sand for construction purposes, building on the beach, to interfere natural movement of sand and impedes beach recovery, removal of vegetation from sand dunes, to destabilize protective barriers, from waves and currents. Erosion not only cause damages to the immediate area where it occurs but also have negative effects on the surrounding environment. Water erosion often destroys buildings, roads and fences and other type of structures, including bridges, cars, buildings, sewage systems, roadways and canals, etc. The economy can also be severely affected by flooding. Businesses may lose stock, patronage, data and productivity and cause disruption to utilities and transport infrastructure with knock-on effects to a wider area. Tourism, farming and livestock’s can equally be affected. The built environment may be damaged or destroyed as a result of erosion and flooding with high repair costs and long periods required for reinstatement. The public realm is often badly affected through damage and deposit of potentially large quantities river accumulated of debris. Land contamination may occur and spread during erosion. Individual properties and vital infrastructure may also be damaged or disrupted, communication, electricity and gas supplies can be interrupted, to wider communities if sub stations and transport are eroded. Road links, railways, canals, etc, may be blocked causing disruption to the wider transport network and accessibility and also result in severely disrupted local inhabitants settings, especially amongst those considered most vulnerable (Bariweni, Tawari and Abowei, 2012). This phenomenon is a common site in Agbor and its environs, posing direct threat to settlement development in the area and the destructions of building infrastructures in its surrounding rural areas. Cohen (2007) said that improved land use techniques such as terracing, of building and tree planting can limit erosion. It is against this background that this study is carried out to find lasting solution to curb the problems caused by soil erosion especially as it affects settlement in the study area. 1.3 STATEMENT OF RESEARCH PROBLEM Environmental hazards including erosion gave rise to lopsided concentration of vehicles in some of the roads thus making the roads, a place of great conflict between man and the environment. It has also been observed that improper planning in Agbor has resulted to in erosion, streets flooding, because in most areas, it was observed that settlements, buildings and other structures were built across River Plains and along flood water path as well as erosion sites and flood plains, thus obstructing the free flow of run-off result causing erosion. Soil erosion has posed a serious threat to Agbor and its environs, facing the problems resulting from erosion. During the wet or raised season, some areas are become inundated to uninhabitable and unmotorable. Local Government and individual in affected areas, have tried to control erosion problem without professional input by filling up the affected areas with gravel, building embankment, placing sand bags and planting trees. Erosion is now synonymous with disaster, dangers, despair, destruction, death and damage to economic properties. Environmental problems caused by urbanization, removal of the natural cover exposes the soil to the action of running water. This greatly reduces the fertility of the soil to cause development of monstrous soil gullies in the land. Though, there is no statistics data on the extent of soil erosion and fertility in degraded areas of Agbor, there is enough evidence to show that, the topsoil is increasingly depleted by soil erosion though outdated and unscientific practices. The impact of unchecked settlement development as a result of rapid urbanization has further aggravated the problem. Some of the natural factors which tends to increase soil erosion in Agbor include: soil type, soil slope and topography. The inherent low statues of soil has much impact on the effects of organic matter on soil properties. Soil is also lost when it is down slope, road network, commercial places, building which result from urbanization and other life and properties. It has been observed that the dual factors of topography and heavy rainfall affect the entire land area of Agbor. That is, most part of the region has been plagued and subjected to erosion which has resulted to menace to her inhabitants. A lot of studies have been carried out by scholars on the causes of erosion and this research will therefore focus on the effects and solution to soil erosion on settlement in Agbor and its environs. 1.4 AIM AND OBJECTIVES The aim of this research work is to examine the effects of soil erosion on settlement in Agbor, and its environs. Specifically, the following objectives will be addressed; To examine the factors responsible for the high erosion degradation in the study area. To identify the causes of soil erosion in the study area. To examine the extent to which the Agbor environment has been degraded by soil erosion. To examine the effects of soil erosion on settlement in Agbor and its environs. To identify the problem, conservation, strategies control techniques and suggest proper management practices, To recommend measures to prevent or ameliorate to help eradicate soil erosion in Agbor and its environ. Furthermore, for the purpose of this study, the researcher will determine soil erosion problems in Agbor which will go a long way to address the socio-economic welfare of the people. 1.5 RESEARCH QUESTIONS The following questions were drawn to guide this research in the study area; What are the immediate and remote causes of soil erosion in the study area? What are the major factors responsible for environmental degradation in the study area? To what extent has Agbor environment been degraded by soil erosion? What are the effects of soil erosion on settlement in Agbor and its environs? What are the possible solution to address the problems of soil erosion and its adverse effect on settlement in Agbor and its environ? 1.6 HYPOTHESES The following hypotheses have been formulated for this study; There is no significant relationship between the effects of soil erosion and the level of settlement development in Agbor. There is no significant relationship between the causes of soil erosion and the factors responsible for the degradation of Agbor and its environs. Soil erosion has no significant effect on the settlement of Agbor. 1.7 SIGNIFICANCE OF THE STUDY There is a great need to examine the effects of soil erosion on settlement in Agbor, Delta State-Nigeria. This study will help to know if there is any significant relationship between the effects of soil erosion and the level of settlement development in the study area. The researcher is interested whether soil erosion has significant effect on the settlement of Agbor. The study will also look at the factors responsible for the degradation of the natural environment especially in Agbor, Delta State. This research work will cover the entire of Agbor and it’s to look intensely at the effects of erosion on buildings. It would offer suggestion(s) on the causes of soil erosion and its advance effect on settlement development. Therefore, the research work will unfold the deteriorating effects of soil erosion on settlement development and other related land use in Agbor. It will educate the general public on the various causes of soil erosion in the area and proffer solution to combat the soil erosion problem(s) on settlement development in the study area. This study gives us information about the effects of soil erosion on settlement in Agbor, Delta State-Nigeria as well as to proffer solution(s) to problems of soil erosion and its adverse effect on the settlement of Agbor, Delta State. This opens new horizons for new researchers. The findings of the research are helpful for the policy makers to introduce some new strategies for the betterment of the society. However, the findings will also provide useful background information to future research in the contribution of geography towards nation’s buildings. This work is expected to guide geographers, geologists, pedologists, geomorphologists, environmentalists, agriculturists, builders, engineers, surveyors, educationists, academicians, experienced soil analysts, etc., and all those whose field of study is associated with solving soil erosion issues to gain understanding of how soil erosion affects settlement development and control measures and mitigation strategies and management techniques can help to advert the enormous problems of environmental degradation especially those caused by soil erosion. Finally, the study is also carried out to enlighten the entire people of Agbor and Delta State on the need to establish a good and favorable condition to enhance better living among the urban and rural dwellers. 1.8 STUDY AREA Agbor is located in the Niger Delta Region of Nigeria and lies in the South-South geo-political zone of Nigeria. The dialect belongs to the Igbo group (Williamson, 1986). Agbor came from the word “Gbon” meaning “develop” or “rise”. 1.8.1 Location and Size Agbor lies between the geographical co-ordinate of latitudes 060 051N to 060 161N of the equator and longitudes 060 051E to 060 091 E of the Greenwich Meridian. Agbor is one of the major towns in Delta State and located in Ika south Local Government Area of Delta State. The neighborhoods of Agbor includes; Boji-Boji Agbor, Emuhu, Ekuku Agbor, Agbor Nta, Alihami, Alisemen, Alifekede, Alizomor, etc.Chapter One: Introduction The resistivity method is used in the study of the horizontal and vertical discontinuities in the electrical properties of the ground and also in the detection of three dimensional bodies of anomalous electrical conductivity. In the study of ground water movement in obubra area, the the resistivity method commonly employed are the electrical resistivity method. Electrical resistivity method is one of the most useful techniques in groundwater geophysical exploration, because the resistivity of rocks is sensitive to its ionic content (Alile, et al., 2011). The method allows a quantitative result to be obtained by using a controlled source of specific dimensions. Records show that the depths of aquifers differ from place to place because of variation in geo-thermal and geo-structural occurrence (Okwueze, 1996). Therefore, the need to study the area for groundwater potential especially in terms of determining the flow direction is a prerequisite for portable ground water exploration and exploitation in this area. 1.1 Location And Geology Of The Area The study area lies between latitudes 50 15′ and 60 15′N and longitudes 70 45′ and 80 45′E. It is located within the sub-equatorial climatic region of Nigeria with a total annual rainfall of more than 300 to 400cm. Temperature ranged from 250C to 280C. The area experiences two seasons, these are the wet season which lasts from April to September with a peak in June and July while the dry seasons lasts from October to March (Iloeje,1991). The study area is underlain by two major lithologic units: Crystalline basement and Cretaceous sediments. The crystalline basement rocks occupy the extreme south of the study area. Also, there are intermediate rocks scatteredin patches around Obubra, Iyamayong, Iyamitet, Ikom, Nkpani and Usumutong. The Cretaceous sediments cover about 90% of the study area. Asu River Group is the basal and oldest recorded sediment in the study area. It is dominated by bluish gray/black to olivine brown shale and sandy shale, fine - grained micaceouscalcareous sandstone and siltstone with limestone lenses. The shale is often carbonaceous and pyritic which indicates that the sediments were deposited under a poorly oxygenated shallow water environment of restricted circulation, an indication of low energy environment (Petters et al., 1987). In general, Southern Obubra lies within the Cross River plain and the clastic beds in the study area can be ascribed to the Ezillo Formation. The Ezillo Formation comprises mostly dark gray shales with fine sandstone and siltstone intercalations in the lower part, and an upper unit that is highly bioturbated, fine medium sandstone, similar to the sandstone of the Amaseri Formation. The Ezillo Formation between Appiapum and Ikom was deposited in a deltaic coastal plain, in brackish marshes and inter-distributary bays (Barth, et al., 1995). A major river (Cross River) exists in the study area into which minor streams empty their loads. The elevation of the study area ranged from 14 to 170m above sea level. The relief is characterized by undulations running at undefined direction and variably demarcating the very lowland areas from moderate relief landmarks. The occurrence of the low plains is occasionally broken by inselbergs of granite and basalts in the southern portion of the study area. In the sediment filled portions, the low plains are occasionally broken by flat -topped hills of sandstone ridges and igneous intrusive with highly ferroginized sandstones with gravels resulting from uplifts. The area is drained by the Cross River with major tributaries like, Udip, Ukong, Lakpoi, Okwo, and Okpon rivers. These rivers form a network of dendritic drainage systemABSTRACT Sediment samples were collected through the purpose sampling method from various streams in Akpabuyo L.G.A, ten sample location were selected. The concentration and areal distribution of selected metals (Fe, Zn, Mn, Cr, Ni, Co, Cu, Cd, Pb) in the sediments of Akpabuyo streams .Geo-accumulation index have been calculated to assess whether the concentrations observed represent background or contamination levels. It proves that the choice of the background plays an important role in the interpretation of the geo-chemical data. It is concluded that the selected streams in Akpabuyo is uncontaminated except a metal (Cd) which it i-geo value is 1 which means it is moderately/uncontaminated. TABLE OF CONTENTS ABSTRACT- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - ii LIST OF FIGURES - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - iii LIST OF TABLES - - - -- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - iv TABLE OF CONTENTS - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - v CHAPTER ONE 1.1 INTRODUCTION 1.2 AIMS AND OBJECTIVE 1.3 STUDY AREA 1.4 GEOLOGY OF THE STUDY AREA CHAPTER TWO 2.1 LITERATURE REVIEW CHAPTER THREE 3.1 MATERIALS 3.2 METHODOLOGY(FIELD) 3.3 LABORATORY METHODOLOGY CHAPTER FOUR 4.1 RESULTS AND DISCUSSIONS CHAPTER FIVE 5.1 SUMMARY AND CONCLUSION REFERENCES CHAPTER ONE 1.1 INTRODUCTION Heavy metals pollution of aquatic ecosystem is becoming a potential global problem, pollution typically refers to chemicals or other substance in concentration greater than it would occur under natural conditions. Water pollution is the introduction by man of substances into the aquatic environment resulting from deleterious effect as harm to human health (FAO 1990).The presence of increased level of heavy metals in the aquatic environment has been of much concern for the past decades due to adverse effect of some metals on living organisms in food chains leading to man. Pollutants are the cause of major water quality degradation around the world. Several toxic metals which are important to the environment and human health have been detected in aquatic media. These toxic metals include the non-essential meals and are no importance to humans (Borgman and Norwood 2002). Trace amount of heavy metals are always present in fresh water from terrigenous sources such as weathering of rocks resulting into geo-chemical recycling of heavy metal elements in these ecosystem. Trace elements may be immobilised within the stream sediments and could be involved in absorption, co-precipitation and complex formation. Sometimes they are co-adsorbed with other elements as oxides, hydroxides of Fe, Mn, or may occur in particulate form. Heavy metal may enter into aquatic ecosystem from anthropogenic sources, such as industrial wastewater discharge, sewage wastewater, fossil fuel combustion, and atmospheric deposition. Trace element in stream sediment compartment can be used to reveal the history and intensity of local and regional pollution. In this work, the of stream sediment contamination was assess using geo-accumulation index. 1.2 AIMS AND OBJECTIVES The main objectives of the current study area are: 1. To assess the extent and degree of metals, and the origin of these metals, using the geo-accumulation index of the metals. 2. To determine the total content of heavy metals in surface sediments of Akpabuyo. 3. To estimate the anthropogenic input and to assess the pollution status on the area. 1.3 STUDY AREA The study area which is located in Akpabuyo, Cross River State lies between longitudes 80 22I 30II E – 80 30I 0II E and latitude 40 52I 30II N – 40 57I 30II N (fig 2). With an area of 126,4032 Square Km. Although many stream samples where collected but few was selscted for the heavy metal analysis. The various Locations in Akpabuyo which sediment samples were collected and used to carry out the analysis are Esuk Mbat stream(L1), Esuk Ekpo Eyo Stream(L2), Ikot Akwa Stream(L3), Dan Archibong Stream(L4), Itu Stream(L5), Ikot Ndarake Stream(L6), Asioha Stream(L7), Ikot Ekpo Ene Stream(L8), Ekpene Ikot Imo Stream(L9), Ikot Nakanda(L10), and their following coordinate shown respectively (table 1.3) . It originate from a hilly region and flows through several villages and farmlandCHAPTER ONE INTRODUCTION 1.1 Background of the Study Land is the basis for every form of physical development and constitutes the primary medium for food production, for the provision of sheets and utilities, for the manufacture of goods and the establishment of institutions to support the basic needs of modern communities (Lanus ad Olufemi 2006). Ukaejiofor (2009) posited that land at the heart of social, political and economic life of the most African countries. He stressed further that, it is the key factor for economic growth and development of every nation and the foundation for shelter in the urban areas as well as the source of livelihood in the rural areas. Therefore, it is an indisputable source of employment and wealth (Idoma and Muhammed, 2014). In recent times, the struggle for available land resource has often resulted to land disputes and conflicts. A land dispute is a disagreement over the possession/control of land between two or more terrestial entities or over the possession or control of land, usually between a new state and the occupying power (Afzalur, 2010). Robert (2012) asserted that land disputes are often related to the possession of natural resources such as rivers, fertile farmland, mineral or oil resources although the disputes can also be driven by culture, religion and ethnic nationalism. Land disputes result often from vague and unclear language in a treaty that set up the original boundary. According to Afzalur (2010) land disputes are a major cause of wars and terorism as states often try to assert their sovereignty over a territory through invasion, and non-state entities try to influence the actions of politicians through terrorism. International law does not support the use of force by one state to annex the territory of another state. Deininger and Castagnini (2004) observed that widows are mostly affected by land conflicts and are the worst hit of land disputes. Studies have shown that female-headed households and widows are particularly affected and that the enactment of the 1990 Land Use Act has failed to reduce the number of pending land conflicts. The government of Nigeria has suggested amending the above said Land Use Act in a bid to resolve the ever emerging land conflicts between the Land lords and the sitting tenants. This suggests that, especially in Africa, attention to land-related conflicts and exploration of ways to prevent and speedily resolve them would be an important area for policy as well as research. Land is a treasured resource for development in every respect and at all levels especially in the sub Saharan regions, and it has become a source of conflict (Afzalur, 2010). Evidence shows that the highest numbers of cases registered by Local Council Courts from village level to sub-county level are land related (Michael, 1992). According to interactions with the Local Council members in Warri South-West L.G.A of Delta State, these cases range from unclear boundaries, grabbing, disputes of inheritance to deceased property, sell of “air” (land that is not there) and forceful eviction of sitting tenants by the land lords like those in Warri Estates. In Nigeria, over 80% of its population practice agriculture and these depend on land, this is also the case in Warri South-West L.G.A of Delta State especially in the Ogbe-Ijaw sub-region unlike in Warri Metropolis which is predominately an Urban Place. What should be observed in this region is that land is limited due to the high population that has lead to land fragmentation. This has in turn hindered the socio-economic development of the region due to the various land disputes resulting from the scarcity of land resources in Ogbe-Ijaw community. Studies (such as Michael, 1992; Lanus ad Olufemi 2006; Ukaejiofor, 2009; Afzalur, 2010; Robert, 2012) have shown that there is no sufficient empirical data to show the effect of land dispute on the socio-economic activities in Ogbe-Ijaw, Warri South-West L.G.A of Delta State and as such there is no basis where land disputes can be handled. Little attention has actually been devoted to the study of land disputes despite evidence on increasing incidences of such disputes. It is therefore; against this background that the researcher will investigate the effect of land dispute on the socio-economic activities in Ogbe-Ijaw community, Warri South-West L.G.A of Delta State. 1.2 Statement of the Problem The major problem associated with land dispute is the loss of lives and valuable properties. Land disputes often occur between individuals, groups and organizations. Land dispute in recent times have caused more damage and harm than good to the modern day society (Ukaejiofor, 2009). Land dispute often hinder the socio-economic activities of most urban and rural dwellers leading to economic hardship, poverty, health problems, food scarcity, low standard of living, among others. This is evidence that the problems emanating from land disputes are enormous. It has been discovered in repeated studies that land disputes often results to death and serious injury during conflict battles especially in situations where it is communal disputes or territorial conflicts (Fischer, 2012). It has been observed that the number of land cases in most Nigerian towns, villages and cities has sometimes led to war which has displaced citizens from their natural habitats thereby hindering their socio-economic activities and day-to-day business activities in the areas (Robert, 2012). Presently, parties have still not come to terms on how to resolve land disputes especially between villages, towns and cities. Communal conflicts still dominate the southern parts of Nigeria since the discovery of oil in the Niger Delta Region. The need for arable land has also increased over the years giving room for conflict issues and land disputes. No matter the effort made by the federal, state and local government to resolve land disputes between villages, towns, and cities, land disputes is still common in these areas especially among the villagers who see land possession as wealth and inheritance (Fischer and Ferlie, 2013). It is no doubt today that, the problems associated with land disputes could hinder the socio-economic activities and well-being of most urban and rural dwellers of Ogbe-Ijaw community and its environs. The socio-economic activities of the people in Ogbe-Ijaw community which ranges from primary activities (farming, agriculture, fishing, etc), secondary activities (trading, business, artesian, etc) to tertiary activities (banking, industries, factories, etc) have been seriously hindered by land disputes. Businesses are often shut down during crisis, war and conflicts resulting from land disputes. This often leads to loss of perishable goods, increase in food prices, high cost of living, unstable society, loss of infrastructural facilities, damage to available community services and basic/social facilities and poor infrastructural development. Evidences have shown that land dispute has a direct effect on the socio-economic activities of the Ogbe-Ijaw people. Studies also shown that not much effort have been directed towards examining these effects land dispute has on the socio-economic activities of the Ogbe-Ijaw people especially on finding possible ways to address these problems. It has also been discovered that there is dealt in literature on the effect of land dispute on the socio-economic activities in Ogbe-Ijaw community. This study therefore seeks to fill this gap which previous studies have failed to cover and thereafter address the aforementioned problems which necessitated this study. 1.3 Aim and Objectives of the Study The aim of this study is to examine the effect of land dispute on the socio-economic activities in Ogbe-Ijaw community, Warri South-West L.G.A of Delta State. In order to achieve the above stated aim, the following objectives were designed to guide the study. They include to: identify the socio-economic activities in the area; identify the causes of land disputes in the study area; examine the consequent effect of land dispute on the socio-economic activities of the people in Ogbe-Ijaw community; examine the problems associated with land dispute in the study area; find possible solutions to the problems associated with land dispute in Ogbe-Ijaw community. 1.4 Research Questions The following research questions were raised to guide the study; What are the socio-economic activities in Ogbe-Ijaw community? What are the causes of land disputes in Ogbe-Ijaw community? What are the effects of land dispute on the socio-economic activities of the people in Ogbe-Ijaw community? What are the problems associated with land dispute in Ogbe-Ijaw community? Are there possible solutions to the problems associated with land dispute in Ogbe-Ijaw community? 1.5 Research Hypothesis The following hypothesis stated in the null and alternative form will be tested in this study; H0: Land dispute has no significant effect on the socio-economic activities in Ogbe-Ijaw community. H1: Land dispute has a significant effect on the socio-economic activities in Ogbe-Ijaw community. 1.6 Significance of the Study The study is intended to establish how land disputes have affected the socio-economic activities in Ogbe-Ijaw community, Warri South-West L.G.A of Delta State. It may also enhance and build a body of knowledge on the causes of land disputes and the consequent effects of land disputes on the socio-economic activities in the study area. This study will also help to unfold the numerous problems associated with land disputes as well as suggesting possible ways to solve such problems. Besides these the Research is a partial fulfillment leading to the Award of Bachelor of Science Degree in Geography and Regional Planning and opening up for further future research undertakings. 1.7 Scope and Limitation of the study This study is restricted to assessing the effects of the land disputes on the socio-economic activities in Ogbe-Ijaw community, Warri South-West L.G.A of Delta State with particular emphasis on the causes of land disputes, consequences and how it has affected the socio-economic activities in Ogbe-Ijaw community. It will be limited to the period of one academic year, as delimitation to the scope of study for better management and during this period many land disputes will be experienced. This period is optimal to have a clear picture of the land disputes in Ogbe-Ijaw community. The study will be carried out in the various quarters that make up Ogbe-Ijaw community comprising of urban and rural areas. This study is also limited by inadequate finance, time, unavailability of resource materials, language and communication barrier. 1.8 STUDY AREA Ogbe-Ijaw is an ancient community in the Niger Delta coast of Nigeria. Ogbe-Ijaw is well known to be one of the Ijaw communities in Nigeria. Ogbe-Ijaw community is the administrative headquarter of Warri-South-West Local Government Area of Delta State. 1.8.1 Location and Size Ogbe-Ijaw lies within latitude 50521N and 50451N of the equator and longitude 50751E and 50311E of the Greenwich meridian. From West to South, the area is wrapped by the Forcadoes on the west, Warri South L.G.A on the east, Burutu L.G.A on the South and Warri North L.G.A on the north. Ogbe-Ijaw has an estimated population of over 116,000 people (NPC, 2006). The location and size of the study area is such that favours oil exploitation activities and man has through his various human and anthropogenic activities (resources exploitation) destroyed the natural environment. This has given rise for various land disputes in the community.
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