Review Article Volume 5 Issue 2
Department of Civil Engineering, Rivers State University, Nigeria
Correspondence: Itolima Ologhadien, Department of Civil Engineering, Rivers State University, Port Harcourt, Nigeria
Received: March 18, 2019 | Published: April 18, 2019
Citation: Ologhadien I. Developments in river bank protection schemes in the lower Niger delta basin. MOJ Civil Eng. 2019;5(2):58-67. DOI: 10.15406/mojce.2019.05.00150
This paper evaluates the performances of four revetment schemes at Sagbama, Otuokpoti, Sagbagreia and Opokuma/Opokuma in the lower Niger River Basin. The evaluation criteria are; reconnaissance survey, physical examination of revetment components, review of design calculations, and action photographs of defective components. The Sagbama and Otuokpoti schemes were designed for 2% annual exceedance probability (AEP) using Pilarcyzk 1990 equations and constructed in Profix mattress revetment. Edge failure occurred at Sagbama due to deflected river flow caused by an upstream depositional bar. The Sagbagreia scheme was constructed of rock – filled gabion mattress, in PVC coated twisted wire mesh. The entire revetment system was constructed inside the potential failure surface. Due to combined effects of reduced effective stresses, high pore pressure and poor drainage bank triggered deep – rotational failure 5years after construction. The Kolokuma/Opokuma revetment was constructed in anchored steel – sheet pile. The choice of anchored steel – sheet pile is incompatible with shore bathymetry resulting to insufficient embedment depth and eventual collapse. Only Sagbama and Otuokpoti schemes performed adequately for 30 and 25years respectively, thus attesting the suitability of Pilarczyk equation for revetment design. The assessment on impact of design on successful project implementation revealed that the non-engagement of design consultants with core competence in hydraulic/river engineering underpins the prevalence of faulty designs and widespread revetment failures being experienced in the region. Finally, this study recommends the need for river training and the establishment of hydro meteorological stations to forestall the dearth of data currently undermining river basin development initiatives.
Keywords: revetment, sinuosity, stability criterion, gabion, slope stability, Niger delta
In the Niger Delta, floodplains and maritime shore are used for human settlement and for economic development. These ecosystems are home to over 70 percent of the population, oil and gas installations but at the same time threatened by natural hazards of flooding and erosion. The scourge of flooding and erosion problems are exacerbated due to human settlements situated at the concave banks which are also the active zones of erosion processes. Concerns over the adverse impacts of river bank erosion on the socio economic development of the region has dominated political discourse for decades. Government commitment to flood and control in the Niger Delta dates back 1954 to 1961, when the Federal Government of Nigeria commissioned the NEDECO1 studies. These studies provided a concise description of the Niger Delta, river systems, guided in the selection of different flood and erosion protection options and navigation. Furthermore, the creation of the Niger Delta Development Board (NDDB) in 1966 demarcated Niger Delta as “Special Area” which deserves special consideration. Its major terms of reference were to submit schemes designed to promote the physical development of the Niger Delta together with cost estimates for implementation of such schemes. The NDDB was primarily an investigational body without executive powers to implement the designed schemes. In 1981, the Federal Government of Nigeria, through Niger Delta Basin Development Authority commissioned further studies of the Niger Delta with special emphasis on Flood and erosion Control and Improvement of Inland Waterways.1 This report provided detailed bathymetric and hydrographic data of the Nun and Forcados river system, sediment transport in rivers and long shore transport along the coast. The report presented plausible options to address the flood and erosion problems, and earmarked several prototype schemes for erosion and flood control, land reclamation and waterways improvement. Further the Federal Government of the Nigeria, through the Niger Delta Basin Development Authority also commissioned the Democratic People’s Republic (DPR) of Korea to investigate possible flood protection measures in the Nun and Forcados River Area.2 The Report focused on provision of hydro metrological data for the designs of flood controls schemes, economic development of the Basin and general improvement in the living standard of the people. The DPR Report1 recommendations for physical data acquisition towards development of a master plan. In 1981, the Rivers State Government commissioned Zinkcon International B.V. (Dutch) Company to undertake the design and construction of Flooding and Erosion Protection works for 16 towns and villages. The contract engagement commenced with the construction of two flooding and erosion prototype schemes at Otuokpoti and Sagbama towns. Sagbama town is situated on the left bank of Forcardos River, while Otuokpoti is situated also on the left bank of Ekole creek, a distributary of Nun River. The prototype schemes were the construction of composite revetment (profix materials system which offered combined advantages of reduced hydraulic loading and green solution for river bank protection. The remaining fourteen schemes were abandoned due to change of government and lack of political will to continue with the implementation. The development of flood and erosion problems in the Niger Delta gained impetus with the creation of Niger Delta Development Commission. So far, no fewer than 100 shore protection schemes had been sanctioned with No Single Success. It is against the backdrop of these failures that, this study is undertaken with the following objectives:
This paper is organized in the following sequence. The introductory section provides a review commissioned studies in chorological order. Section 2 begins with assessment of channel plan forms using channel sinuosity (S) and stability criterion (Scr) at critical erosion and flooding locations. Section 2 also provides the Description of the study area and hydrologic characteristics. Section 3 presents review of existing shore protection works in the Nun and Forcados river systems with assessment of their performances. Section 4, and then elaborate the design of revetment mattress option based on its successful performances in the Lower Niger River Basin over other options. Section 5, ends with conclusions and recommendations towards establishment of hydro meteorological stations, as solution to the dearth of stream flow data and to identify research gaps that would improve the planning and management of water resources in the basin.
Description of study area and hydrologic characteristics
The Niger River and Benue River forms a confluence at Lokoja and then flows Southwards into the vast Niger Delta covering approximately 30,000Km2. The River Niger bifurcates at Asamabiri into River Nun and River Forcados, which progressively spilt into several distributaries with no fewer than 30 outlets including estuaries into the Nigeria gulf of Guinue. A total of 250 Km3/yr of water discharges into the gulf of Guinea. Rainfall in the Niger Delta is typically 2700mm – 3000mm/year, while actual evaporation is about 1000mm/year.3 Table 1 shows the cross-sectional details of the rivers at the study stations while Figure 1 shows the study map.
S/N |
Stations |
River |
Dry Season water Surface Width (m) |
Bank full Width(m) |
Maxi Depth Dry season m) |
Depth flood season (m) |
Mean Flow Velocity m/s |
Bank Gradient |
Inflection radius (km) |
Inflection Length (km) |
1 |
Aboh |
Niger |
1110 |
3100 |
8.8 |
14.5 |
1.40 |
35o2’ |
3.45 |
12 |
2 |
Asambiri |
Niger |
1110 |
1600 |
8.10 |
13.8 |
1.36 |
50o11’ |
3.00 |
15 |
3 |
Kaiama |
Nun |
350 |
680 |
7.40 |
13.5 |
1.30 |
34o2’ |
3.00 |
11 |
4 |
Kolokuma/Opokuma |
Nun |
355 |
650 |
6.5 |
11.00 |
1.35 |
32o15’ |
7.5 |
8 |
5 |
Sagbagreia |
Nun |
355 |
660 |
6.3 |
10.9 |
1.30 |
33o20’ |
1.50 |
7 |
6 |
Sagbama |
Forcados |
500 |
700 |
4.0 |
11.30 |
1.45 |
29o53’ |
1.60 |
5.0 |
7 |
Otuokpoti |
Ekole Crk |
250 |
300 |
5.20 |
11.10 |
1.30 |
28o4’ |
1.75 |
8.0 |
8 |
Patani |
Forcados |
510 |
550 |
8.50 |
26.5 |
1.50 |
43o2’ |
2.0 |
10 |
Table 1 Cross-sectional detailed at study stations
Source: DPRK (1980, Nedeco – Haskoning (1980), NDES(2013).see locations (column 2) in Figure 1.
Survey of alluvial channel pattern in lower Niger River basin
Chang,4 and Deng & Singh5 investigated the mechanism and conditions for change in channel pattern, using theory and field data from 70 alluvial rivers having different chemical patterns. They recommended that river management and training works should help rivers achieve and maintain a sinuosity (s) close to 1.57 and a stability criteria Scr>0.2. Accordingly, the sinuosity and stability criterion parameters comprehensively reflects the stability of an alluvial river, thus Equations 1-3, defining S and Scr were applied to evaluate the channel pattern changes caused by changes in flow conditions at inflexion points where shore protection works are situated in the Lower Niger River Basin. Table 2 shows the computations of sinuosity and stability criteria at erosion locations.
S = Ls/Lm = 2pR/12B.……………………………… (1)
Where xo = morphologic coefficient, Scr = stability criterion, S = channel sinuosity, J = Channel slope; H is water depth and R = radius in any position of the thalweg.
The sinuosity was calculated as the ratio of the curvilinear length (along the curve) to distance (straight line) between the inflexion points.
……………………………………………. (3)
Consequently, Equation 1, 2 and 3 defining the Sinuosity (S) and Stability criterion (Scr.) have been used to assess the channel pattern and conditions of morphological changes at the concave banks and the results are shown in Table 2.
S/N |
R reach |
River |
n |
|
B |
Ɛo |
Scr |
S |
Depth |
J |
ÖƐo |
1 |
Aboh |
Niger |
0.041 |
|
1135 |
8.967866 |
0.066011 |
0.1506 |
14.5 |
0.000077 |
2.91506 |
2 |
Asamabiri |
Niger |
0.035 |
|
1300 |
11.51933 |
0.050869 |
0.1047 |
12.4 |
0.000069 |
3.394013 |
3 |
Kiama |
Nun |
0.03 |
|
425 |
5.030068 |
0.066903 |
0.1428 |
13.1 |
0.000072 |
2.242781 |
4 |
KOl/Opok |
Nun |
0.036 |
|
550 |
6.909174 |
0.066607 |
0.4909 |
11.4 |
0.000072 |
2.628531 |
5 |
Sagbagrea |
Nun |
0.029 |
|
556 |
7.085553 |
0.055506 |
0.1122 |
11.2 |
0.000068 |
2.66187 |
6 |
Sagbama |
Forcados |
0.028 |
|
520 |
6.704955 |
0.055391 |
0.1676 |
11.3 |
0.000068 |
2.589393 |
7 |
Otuokpoti |
E. Creek |
0.31 |
|
300 |
5.508585 |
0.066805 |
0.1146 |
9.4 |
0.000062 |
2.347037 |
8 |
Patani |
Forcados |
0.026 |
|
510 |
2.820932 |
0.461555 |
0.1047 |
26.5 |
0.000068 |
1.679563 |
Table 2 Channel pattern changes evaluated with sinuosity and stability criteria
Where S: Channel Sinuosity; Scr: Stability criterion; B: Bankfull channel width; Average flow depth: roughness coefficient
The towns and villages in the lower Niger River Basin are clustered around the concave banks of the Nun and Forcados river systems. The concave banks have physiographic advantage that they are at higher elevation than the back swamps, thus less prone to flooding, but at the same time, they are zones of severe bank erosion. It is therefore, of a great importance to scientifically characterize the inflection points in terms of their stability criterion and sinuosity.
The channel sinuosity (S) varies between 0.1047 and 0.491 while the stability criterion (Scr) was generally less than 0.1 except at Patani station. Deng & Singh,5 reported that the closer the channel sinuosity of an alluvial river is to 1.57 and stability criteria greater than 0.20. The failure of the concave banks to meet the stability criteria is indicative of channel instability, erosion and channel migration and in general morphological problems at those locations.
Review of existing shore protection works
A revetment is a slope engineered shore protection structure designed to protect and stabilize an eroding shoreline against erosion by currents and wave actions. The types of revetment commonly used for river bank and shore protection and stabilization may be found in standard tests.6−8 In order to evaluate the performance of the existing shore protection schemes, a reconnaissance survey, and physical examination of the components of each revetment scheme and action photographs were taken. Structural failure of the revetment may be attributed to any of the three fundamental mechanisms or induced by any combination of the following;
The various components elements of the revetment structure are listed in Table 2 to enable a component by component evaluation performance evaluation of each scheme (Table 3).
S/N |
Revetment Components |
||||||||||
Location |
River |
Revetment |
Armour Layer |
Filter Layer |
Subsoil Condition |
Crest |
Toe |
Edge Detail |
Year |
Remarks |
|
2 |
Otuokpoti |
Ekole Creek |
Proefix Mattress |
As a Sagbama |
Ditto |
Ditto |
Ditto |
Ditto |
Ditto |
1982 |
Profix mattress performed adequately for about 25 years and failed due to inadequate edge protection |
3 |
Sagbagreia |
Nun |
Gabion mattress constructed of gabion mattress, rock-filled in PVC coated wire mesh with stone sizes; 200 –250mm |
High pour water pressure with high hydrostatic pressure gradient during flood recession. Reduce effective stresses in the bank trigger deep-seated rotational failure (plates 1 and 2). Also increased unit weight caused by infiltrating water into the banks |
Description of Filter Integrity and failure |
Poor compaction of slope before laying gabion mattress. |
Surface drainage infiltrating into the bank through cracks caused by increase water weight of the bank material and poor pressure built-up trigger crest failure. |
Poor anchorage and failure |
Inadequate edge protection and failure |
2005 |
Failure caused by underground water drainage infiltration into cracks and high pore pressured gradients during flood recession. Gabbon mattress failed 5 years after construction |
4 |
Okokuma Kolokuma |
Nun |
Anchored steel-sheet piles |
Wrong choice of revetment, steel-sheet pile option not compatible with site bathymetry, caused restricted access to the river and berthing of canoes. |
|
Insufficient embedmen depth and collapse during flood conditions. |
Table 3 Evaluation of existing shore protection works
Armour layer: outer layer of a revetment; Gabion: rectangular or tubular basket made from steel; Geotextile: permeable synthetic fabric; Revetment: a bank protection system with no slope retention capability; Scour: local removal of soil particle by hydraulic forces.
Abbreviation/Notation ASCE, America Society of Civil Engineers; ICE, Institution of Civil Engineers, London; EoI, Expression of Interest; Scr, Stability criterion; S, Channel sinuosity; NDES,: Niger Delta Environmental Survey; J, Channel slope; o, Morphologic coefficient.
Performance evaluation of the four schemes
The main factors controlling dictate the choice of revetment may be classified under:
Other factors such as flexibility and permeability are related to the ability of the revetment structure to transfer pressure forces to and fro the river bank. Considering columns 8 and 10 in Table 1), that the banks are very steep and slopes greater than 34o degrees with moderate to very heavy hydraulic loading and low permeabilities. Consequently, the sheet-pile revetment option adopted for Opokuma/Kolokuma shore protection is in-appropriate. Sheet-piles are available in standard length of 39ft (≈13m), given the existing bank heights, they were not driven to the required embedment depth. The result was failure and collapse under flood conditions (Plate 1−3). Furthermore, sheet-piles offer restricted access to the foreshore and have adverse effect on the community lifestyle.
The Sagbagreia scheme was constructed of box gabions (Maccaferri Gabions). The gabion protection was laid on non-woven geotexile filter fabrics. The main problems with this scheme are:
The Otuokpoti and Sagbama flood and erosion protection works were constructed of profix mattress, the armour layer, granular and geotextile filter comprised the profix mattress system. The profix mattress system failed due to instability of the subsoil which generated localized slipe failure around the middle portion of the armour layers while the toe and crest components of the revetment system are in-tack and performing adequately. In summary, combining the lessons from the performance of the above schemes with physical understanding of the problem; a gabion mattress or cable block revetment be an excellent choice for the lower Niger River Basin and particularly the Niger Delta with regard to the very heavy hydraulic loading, bank slopes, flexibility and accessibility to the foreshore.
Discussion and development of appropriate shore protection scheme
The better performing schemed of Otuokpoti and Sagbama were designed using the Pilarczyk’s equation9 which failed 30 years after completion and also survived the 2012 centinary flood with a discharge of about 30,000m3/sec. Pilarczyk’s equation have been recommended for design of riprap, cabled concrete block, box gabions and asphalt mattresses while Hemphill & Bramley,10 is recommended for riprap, loose or interlocking concrete blocks and gabion mattresses.8 In view of the poor designs, failed installations with concomitant financial wastage characterizing the development of the shore protection works in the Lower Niger River Basin. The flowcharts for both preliminary and detailed design respectively adopted from Escarameia8 are presented to guide prospective designers. Figures 2 &3 shows typical flowchart for preliminary and final design stages respectively.
The causes of failure of the investigated schemes call for special attention in some critical aspects of the design process namely:
Impact of design on successful project implementation
Quality design is a sina-quo-non for successful implementation of the construction phase. Quality in construction is defined as conformance with requirement, as defined by the owner, designer, contractor, and the regulatory agencies.14 The objective of achieving these requirements rests with the design and constructions. Farooq15 enumerated the triple tasks of any consulting organization as follows
These findings were evaluated against recent Expression of Interest (EoI) adverts for prospective consultants by government agencies for design of infrastructure in the Niger Delta Basin. Conversely, it was observed that core competence in River/hydraulic engineering is not a criterion in the selection of design consultants on river basin development projects. The neglect of core competence underpins the prevalence of faulty designs and attendant project failures being observed in the Niger Delta Basin.
This paper assessed the mechanism of channel pattern change and found that the observed that prevailing patterns in the Lower Niger River Basin agreed with a stability criterion proposed by Deng & Sing.5 Further, this paper evaluated the performances of existing shore protection schemes to underpin the best scheme in terms of durability. This study found that the best performed schemes were those of Otuokpoti and Sagbama, designed using Pilarczyk’s equations. The scheme at Sagbagreia failed due to absence drainage, pour water pressure development behind the geotextile and gabion mattress which generated rotational slope failures. The steel-sheet pile revetment adopted for Opokuma/Kolokuma is inappropriate, inview of the prevailing river bank geometry. The use of Pilarczyk equations involves several uncertainties, therefore, experimental verification and further improvement of design methods through research studies is recommended. Designers should pay special attention to
There is a tripartite nexus between mathematical, hydraulic modeling and water resource development. Both water resources development and management is strongly dependent on the availability of data, yet data collection and hydrometric measurement are less appreciated.17 In the Lower Niger River Basin, there is no functional hydrological station. Consequently, water resources planning and management is mission impossible unless the dearth of data is addressed. Accordingly, no meaningful designs can be executed in the Niger Delta and Lower Niger River Basin in the face of current-data problems. Finally, I wish to make the following recommendation:
None.
The author declares there is no conflict of interest.
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