Dimension of Major Gullies in Edo State, Nigeria

Travail de Recherche , 2017 , 16 Pages , Note: A

Sciences de la Terre / Géographie - Géographie physique, Géomorphologie, Ecologie

The issue of gully erosion is of major concern in Nigeria. The study was carried out in Edo state, Southern Nigeria. Edo State was chosen as the study area due to the fact that the magnitude of gully erosion has resulted in loss of lives and properties, destruction of arable lands and wastage of large areas of usable land. In the study, effort was made to identify the major gully sites in the area and the length, depth and width of the gullies were determined through direct field measurement with the help of research assistants using simple survey equipments (measuring tape, Camera and 3percent accuracy Global Positioning System (GPS). The results revealed that dimension of major gullies in the area are large and the gullies are fully developed

Abstract

The issue of gully erosion is of major concern in Nigeria. The study was carried out in Edo state, Southern Nigeria. Edo State was chosen as the study area due to the fact that the magnitude of gully erosion has resulted in loss of lives and properties, destruction of arable lands and wastage of large areas of usable land. In the study, effort was made to identify the major gully sites in the area and the length, depth and width of the gullies were determined through direct field measurement with the help of research assistants using simple survey equipments (measuring tape, Camera and 3percent accuracy Global Positioning System (GPS). The results revealed that dimension of major gullies in the area are large and the gullies are fully developed

Key words: gully, erosion, dimension, length, depth, width

INTRODUCTION

Gully erosion is the removal of soil and soft rock as a result of concentrated runoff that forms a deep channel. Poesen, Nachtergaele, Verstraetena, Valentin (2003) defined gully erosion as the erosion process whereby runoff water accumulates and often recurs in narrow channels and, over short periods, removes the soil from this narrow area to considerable depths. According to Amangabara (2012), gully erosion is the terminal phase of a four-stage erosion process involving splash, sheet, rill, and gully. The process begins by water falling as raindrops and flowing on the soil surface.

Splash erosion results when the force of raindrops falling on bare or sparsely vegetated soil detaches soil particles. Radoane, Ionita and Radoane (1995), observed that gullies are important part of soil erosion process and their occurrence and development may cause serious problems to a region's economy. Gully is normally formed on very steep land, where water running downhill cuts a channel deep into the soil. Gobena (2003) defined gullies as steep-sided eroding watercourses that are subject to ephemeral flash flood during rainstorms. It also occurred where there is a sudden fall. According to Eseigbe and Ojeifo (2012), gully erosion is a serious form of soil degradation often involving an initial incision in to the subsurface, by concentrated runoff along lines or zones of weakness such as tension and desiccation fractures. These narrow incisions are subsequently widened and elongated by sidewall processes and headward erosion. Aderemi and Iyamu (2013) observed that gullies may also be initiated at the local base level streams and rivers by the combined effects of seepage forces, subterranean erosion and liquefaction. Gullies of this type develop into gigantic negative relief features by progressive liquefaction, flowage, progressive tension fracturing, slumping and landslides. Gully erosion is essentially a slope failure phenomenon operating under the influence of hydrodynamic, gravitational and body forces. Slope failure can also proceed through flowage, sliding and slumping, and toppling. Ekpenyong (2013), observed that the rates of these failures which culminate to gully advance and lateral expansion are more during periods of heavy precipitation.

The control of gully erosion has not been given adequate attention because gully processes are difficult to study and in some cases, the right control measures are not applied. Poesen, Nachtergaele, Verstraetena, Valentin (2003) observed that no systematic compilation of length, width, depth of the different types of gullies and their controlling factors in a wide range of environments has been made. Such quantitative data is needed for application of effective. This prompted the researcher to carry out this study on dimension of major gullies in the area because providing such information is valuable for designing effective control for the eroded sites.

STUDY AREA DESCRIPTION

Edo State is located in the South-South Zone of Nigeria. Its capital town is Benin-city. The State was created in 1991 out of the old Bendel state and its geographical coordinates are Latitudes 05° 44′ to 07° 34′ N and longitude 05° 04′ and 06° 45′ E. It has a land mass of 19,794km square and it is bordered by Kogi State to the north, Delta State to the East and South and Ondo State to the West.

The geology of the study area reveals that the entire area is underlain by sedimentary rocks. It consists of the crystalline basement rocks in the hilly and dissected zone in the north followed southwards by residual lateritic soils of the well drained dry lands at Auchi, Agbede and Afuze. Aderemi and Iyamu (2013) observed the area is underlain by sedentary rock of the Pleistocene age often referred to as the Benin formations. The sedimentary rock contains about 90 percent of sandstone and shale intercalation. It consists of over 90% sandstone, clay, shale and lignite coarse fine grained in some areas. The nature of the underlying geology contributes significantly to the origin and spread of gullies Afegbua, Uwazuruonye and Jafaru (2016). The relief of the area is mainly characterized by swamping creeks and dissected plateau such as the Esan Plateau, Orle valley and the dissected uplands of Akoko-Edo Local Government Area. According to Aderemi and Iyamu (2013), there are six types of physical features which constitute the landscape of the area. Sandy coastal plain and alluvium clay are found in the Benin lowlands area with some hills in the east. Slopes are tilled in the southwest direction. River Osse, River Orihionmwon and lkpoba are the major drain in the area. With the exception of River Osse that has a wide flood plain, Eseigbe and Ojeifo (2012), observed that other rivers in the area are characterised by steeply incised valleys in their upper courses and they become broad as they enter River Ethiope in Delta State. According to Eseigbe and Ojeifo (2012), the state has land mass that is relatively flat terrain in the southern part with an average height above the sea level of about 500metres except towards the northern axis where the Northern and Esan plateaus range from 183 metres at the Kukuruku Hills and 672 metres at the Somorika Hills.

The climate of the study area is humid sub-tropical indicating that it is basically within the tropical rain forest zone dominated by broadleaved trees that form dense layered stands which usually are above 50m (165 ft) in height. It is typically tropical with two major seasons- the wet and the dry seasons. Ikhile (2015), highlight that the seasons correspond to the periods of dominance of the wet tropical continental air masses and the seasonal distribution of rainfall follows the direction of the Inter-Tropical Divergence (ITD) which varies almost proportionally with distance from the coast. The temperatures across the state is relatively high with a very narrow varies in seasonal and diurnal ranges 22-36 range with an average annual rainfall of about between 2000mm-2500mm. The wet season comes between April and November and the dry season between December and March. According to Onakerhoraye (1995), there is a marked dry season, with duration of increases from three months in south, northwards, while the rainy period decreases inland from nine months in the south to five months in the northeast. The vegetation zones of Edo State coincide with the political zones in the state. Edo South is in the moist rainforest, Edo Central in the dry rainforest and derived savanna and Edo North is characterized with derived savanna and southern guinea savanna. The area is also characterized by few scattered rainforests, wooded shrub lands and farmlands. Adekunle, Olagoke and Ogundare (2013), observe that the trees could be seen to be green throughout the year because they retain their leaves all through the year. This is because the temperature and precipitation are sufficiently high for continuous growth. The state is blessed with abundant natural resources. Virtually all species of hardwood can be found – high quality timber is produced from most local government areas of the State.

The state consists of eighteen Local Government Areas which include Akoko-Edo, Egor, Esan Central, Esan North-East, Esan South-East, Esan West, Etsako Central, Etsako East, Etsako West, Igueben, Ikpoba-Okha, Oredo, Orhionmwon, Ovia North-West, Ovia South-West, Owan East, Owan West and Uhunmwonde. Major towns in the State include Benin City (the State Capital), Abudu, Ekpoma, Uromi, Auchi, and Sabongida-Ora. Generally, Edo State is traditionally known for agriculture, trade and deep historical virtues. The residents are traders and farmers whose activities are closely tied to the land. A lot of residential structures are within the gully strip, Edo State Strategic Health Development Plan (2010-2015). Due to their proximity to the gully, some of these structures have been marked as danger zones by the Edo State Ministry of Land, Housing and Survey. According to the State Strategic Health Development Plan (2010-2015) 70% of the landmass is cultivated for agricultural production as a means of livelihood with an average of about 2.345 million persons in the State directly or indirectly engage in agricultural activities. Major ethnic groups in the state are the Binis, the Esan, Ora, Etsakos, Owans, Akoko, Igarra and Afemai. The Binis occupy the southern part of the state, Esan and Ora occupy the central part and Afemai, Igarra and Akoko in the northern area. According to National Population Commission (2006) Edo State has a total population of 3,218,332.

The demographic features of the area are typical of states in Southern part of Nigeria, growing rapidly with the population overstretching the weak social services. With the figure of 2006 Population and Housing Census, the state has population of 3,218,332 and an average population density for the state is about109 persons per sq. km, which is above the national average of about 96 persons per sq. km. According to the State Strategic Health Development Plan (2010-2015), the total population figures have been projected to over 3.4 million people. Most people in the area engaged in food crops cultivation. The main food crops cultivated include yam, cassava, maize and rice in the Benin lowlands and on the Esan plateau. There is also rice cultivation in the flood plains of the River Niger at Agenebode and Illushi. Tree crops such as rubber and oil palm are also cultivated in the Benin lowlands and Esan Plateau and cocoa in Owan, Etsako and Akoko Edo. The major environmental and ecological problems associated with Edo State are waste management, pollution and sanitation, forest depletion, flooding and erosion of the surface of the soil. Land degradation due to flooding and erosion ranked first and second in the objective ranking of environmental problems in the state. (Edo State Strategic Health Development Plan 2010-2015).

The magnitude of devastation as a result of flooding and erosion has resulted in loss of lives and properties, destruction of arable lands and wastage of large areas of usable lands. The State Strategic Health Development Plan also suggested need for re-afforestation, regulated construction and provision of drainage facilities in urban areas as well as attitudinal change on the part of the people.

METHODOLOGY

Direct field observation and measurement of gully length, depth and width was done with the help of research assistants using simple survey equipments (measuring tape, Camera and 3percent accuracy Global Positioning System (GPS). The numbers of gullies chosen for the study were determined using the Taro Yamane formula. [illustration not visible in this excerpt]Equation 1

Where

n = sample size

N = total number of gullies in the state

e = is the margin of error assumed (0.05)

1 = is the theoretical constant

The formula was chosen because it has 95% confidence level and the total number of gullies in the study area is within ranges of hundred which fit into the basic assumption of the formula.

illustration not visible in this excerpt

Basic Assumption

If the population is a few hundreds, a 40% sample will do, if many hundreds, a 20% sample will do. If a few thousands, a 10% sample and if several thousands, a 5% or fewer sample will do (Singh and Masuku, 2014)

illustration not visible in this excerpt

The random sampling technique was used in selecting the 16 gullies sites across the study area.

RESULTS AND DISCUSSION

The mean depths of gullies in Edo North ranges between 6.5m in Egelessor to 26m recorded in Gaz Momoh. The mean width of gullies in the area ranges from 12.6m in Ikabigbo to 45m in Jatu Road and the mean length of gullies in the area is1009.6m. Range of gullies lengths in Edo North is 2045.8m, Range of depths is 19.5m and Range of widths is 86.6. This indicates that gullies in the area are large and fully developed.

Mean depth of gullies in Edo South ranges from 4m at Ogiso to 45m in Queen Eden. The mean width is between 5m at Ogiso to 45m in Ikoba Slope and mean of length in area is 695.5m. Range of gullies lengths in Edo South is 1016.8m, Range of depths is 41m and Range of widths is 40.7m.

The mean depth of gullies in Edo Central ranges from 4.2m at Uromi to 15.3m at Ewu. The mean width is 4.8m at Ewohimi to 20.6m in Ewu and the mean length in the area is 439.9m. Range of gullies lengths in Edo Central is 976m, Range of depths is 11.1m and Range of widths is 15.8m.

The mean length of all gullies sampled is 678.14m, the mean width of all gullies sampled is 17.33m and the mean depth of all gullies sampled is 12.24m. The standard deviation (s) of length of all gullies sampled is 636.24m, the standard deviation (s) of mean width of all gullies sampled is 12.92m and the standard deviation (s) of mean depth of all gullies sampled is 10.48.

Table 5.1 Dimensions of Major Gullies in Edo North

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Source: Field Work 2017

Abbildung in dieser Leseprobe nicht enthalten Google Earth Map Showing Locations of Major Gullies in Edo North

Abbildung in dieser Leseprobe nicht enthalten Photo of Jatu Road Gully in Edo North Showing Speed Breakers as Control Measure

Dimensions of Major Gullies in Edo South

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Source: Field Work 2017

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Google Earth Map Showing Locations of Major Gullies in Edo South

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Photo of Ikpoba Slope Gully in Edo South Threatening the Highway

Dimensions of Major Gullies in Edo Central

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Source: Field Work 2017

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Google Earth Map Showing Locations of Major Gullies in Edo Central

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Photo of Ewu Gully Erosion Site Edo Central

DISCUSSION OF RESULTS

Results from field measurements of gullies dimension in the study indicate that the major gullies are large and fully developed. This collaborated with Okonofua and Uwadia (2013) that the average depth, top width, bottom width and the length of the gully in University of Benin are 10.2m, 18m, 14m and 1.1km respectively. It also collaborated with observation of Mallam, Iguisi and Tasi’u (2016) that the length, depth and widths of gullies in Kano metropolis have significantly increased in the last 10 years.

CONCLUSIONS

In many of the identified gully erosion sites, the magnitude of devastation have resulted in loss of lives and properties, destruction of arable lands and wastage of large areas of usable lands. The seriousness of deep erosion gullies in the study area is advancing at alarming rates. The sites now have adverse effects on the environment and socio-economic life of the citizenry of the State. Major gullies in the study area continue to expand at an alarming rate and this has increased the vulnerability of the entire area to intensified gully erosion. Although there are some control measures currently in place such as the Nigeria Erosion and Watershed Management Project of 2012 which only covered three sites and some local effort in other sites but they are not effective to address the extent of gully erosion menace in the area.

REFERENCES

Adekunle V.A.J, Olagoke A.O. And Ogundare L.F (2013), Logging Impacts in Tropical Lowland Humid Forest on Tree Species Diversity and Environmental Conservation Applied Ecology and Environmental Research 11(3): 491-511.

Aderemi, A. and Iyamu F. (2013), Risk Assessment Analysis of Accelerated Gully Erosion in Ikpoba Okha Local Government Area of Edo State . Nigeria Environment and Natural Resources Research, Canadian Center of Science and Education; 3(1) Pg 68-76.

Afegbua, U. K., Uwazuruonye J., and Jafaru B., (2016), Investigating the Causes and Impacts of Gully Erosion in Auchi, Nigeria. Journal of Geography, Environment and Earth Science International SCIENCEDOMAIN international 4(4): 1-13, www.sciencedomain.org

Amangabara, G. T. (2012), Analysis of Selected Failed Gully Erosion Control Works in Imo State. Special Publication of the Nigerian Association of Hydrological Sciences Nigeria Pages 279-286.

Edo State Government (2010), Strategic Health Development Plan (2010-2015). Edo State Ministry of Health

Ekpenyong, R. E., (2013), An Assessment of Land Cover Change and Erosion risk in Akwa Ibom State of Nigeria using the Coordination of information on the Environment (CORINE) methodology. Greener Journal of Physical Sciences \ 3(3), pages 076-089

Eseigbe, J. O., and Ojeifo M. O., (2012), Aspects of Gully Erosion in Benin City Edo State, Nigeria. Research on Humanities and Social Sciences 2(7).

Gobena Y.J. (2003), Soil Erosion Assessment Using Remotely Sensed Data and Ancillary Data in the Desert of Tabernas Southeast Spain. International Institute for Geo-Information Science and Earth Observation Enschede, Netherlands

Ikhile, C.I., (2015), Climate change and erosion activities in Benin-Owena River Basin, South West Nigeria. Journal of Geography and Regional Planning pp 99-110.

Onokerhoraye, A. G., (1995), Urbanization and Environment in Nigeria: Implications for Sustainable Development. The Benin Social Science Series for Africa. Benin City: University of Benin.

Poesen J, Nachtergaele J, Verstraeten G, and Valentin C (2003), Gully erosion and environmental change: importance and research needs. Laboratory for Experimental Geomorphology, K.U. Leuven,

Belgium, Catena 50 91– 133 www.elsevier.com/locate/catena

Radoane M, Ionita I, and Radoane N., (1995), Gully distribution and development in Moldavia, Romania. Stejarul Research Station, Piatra Neamt, Romania ELSEVIER Catena 24(127-146)

• Université: University Of Abuja
• Note: A
• Auteur: Augustine Osayande (Auteur)
• Année de publication: 2017
• Pages: 16
• N° de catalogue: V381321
• ISBN (ebook): 9783668659452
• Langue: anglais
• mots-clé: dimension, major, gullies, state, nigeria