In this study, water samples from Miocene reservoirs, offshore Niger Delta, and seawater samples used for water injection were investigated in an attempt to examine the chemistry, evaluate the corrosion behaviour of steel, iron, and aluminium in different aqua media, and evaluate the scaling potentials of the oilfield produced waters (OFPW). Chemical analyses of the waters were determined; corrosion rate measurements were carried out by the weight loss method at room temperature while corrosion kinetics was carried out using conventional methods. Langelier saturation index (LSI), Ryznar stability index (RSI), Larson–Skold index (L–S), Puckorius scaling index (PSI), and aggressiveness index (AI) were evaluated for assessing the corrosiveness and scaling potential of the formation waters, using water quality data. The magnitude of corrosion of these metals was studied for an exposure period of 42 days. Chemical analysis revealed that the waters are slightly alkaline and generally classified as hard, saline water of the Na-Cl type based on its total dissolved solids (TDS). Produced water pH values range from 7.32 to 8.38. Results showed the likelihood of some of the water to form mild to severe scales based on the corrosivity indices, while the seawater samples are classified as ‘non-aggressive’ and ‘aggressive’. Steel has the highest corrosion rate with a value of 3.84 × 10−3 mg cm−2 h−1 compared to aluminium with the lowest rate of 0.37 × 10−3 mg cm−2 h−1. In most cases, the rate of corrosion of the metals followed the first-order rate constant in some of the samples, and the second-order in others within the first seven days. It was observed that the rate of corrosion follows this order: steel > iron > aluminium. The potential heavy and intolerable corrosion associated with the use of these seawater samples as injection waters is a potential risk that must be handled by adequate treatment.

  • An experimental study of corrosion and scaling potentials of produced water and seawater samples was carried out.

  • Water chemistry revealed that the produced waters are saline, dominantly of the Na-Cl type based on its TDS concentrations.

  • Five indices: Langelier saturation index (LSI), Ryznar stability index (RSI), Larson-Skold index (L-S index), Puckorius scaling index (PSI), and aggressiveness index (AI) were computed.

  • LSI is generally less than zero, in the water samples, indicating supersaturated water with scaling tendencies.

  • Corrosion rates of the metals beyond the first week generally followed first-order rate kinetics.

Graphical Abstract

Graphical Abstract

Formation waters occur naturally in association with crude oil and are referred to as oilfield produced water (OFPW) once it is separated from the oil for disposal. Since this water occurs naturally with the hydrocarbon fluids, they tend to generate certain problems in oilfield production operations. The large volume of OFPW, which the oil industry is currently contending with, makes the industry appear more like a water industry since it constitutes the largest waste stream on oilfield production facilities (OFPF) (Du et al. 2005). Due to the large volume of OFPW, it is often considered as injection water to enhance hydrocarbon recovery and maintain reservoir pressure, or may also be treated and disposed of into the environment. The former may trigger biogenic souring, corrosion and scaling, while the latter, if not properly treated, may cause bioaccumulation and transfer of potentially toxic elements (PTEs) in aquatic organisms, which would eventually affect the food chain (Konwar et al. 2021). OFPW contains low- and high-molecular-weight petroleum hydrocarbons (HCs), dispersed and dissolved oil, dissolved compounds, suspended solids, naturally occurring radioactive minerals (NORM), dissolved gases, and PTEs (Ozgun et al. 2013; Kpeglo et al. 2016).

Water corrosivity depends on many factors including pH, oxygen content, the presence of metabolizing bacteria, and its suspended solids, which tends to promote microbially assisted corrosion. Scales are inorganic deposits formed due to the precipitation of solids resulting from brines that are present in the oilfield reservoir and production system. The tendency of water to deposit insoluble and protective scales is a function of its corrosivity. Corrosion is the destruction or deterioration of materials due to its reaction with its environment and in an offshore setting, rusting, sweet corrosion, sour and microbiological corrosion are major concerns. Corrosion of metal surfaces is greatly influenced by their chemical composition, electronic properties, microstructure, and passive film properties (Das et al. 2009). Water saturated with CaCO3 tends to precipitate scale, which may protect against corrosion, which could also produce encrustation in water and injection wells. The degree of CaCO3 saturation has been used as an indicator of water corrosivity and scaling/encrustation tendency. Metals and their alloys are important materials used in pipeline production for oil fields. Experience and investigation of pipe failures suggest that corrosion of metals, both cast iron and steel, is the most predominant cause of pipe failures (Rajani et al. 1995; Mohebbi & Li 2011). In the last two decades, different studies have pointed out to the oil industry the advantages that aluminium alloys may present for tubular manufacturing compared to steel (Gelfgat et al. 2005; Osorio-Celestino et al. 2020). Since corrosion is linked to almost all pipe failures, it has become a global problem for all stakeholders, in particular engineers and asset managers of buried metal pipes (Goulter 1985; de Sena et al. 2012). The impact of corrosion cuts across so many sectors such as oil and gas, car assembling plants, chemical, electric power, medical and engineering industries (Parangusan et al. 2021). Nwanonenyi et al. (2020) reported the detrimental effects of metal corrosion in industries. Adequate measures that guarantee long-lasting materials must be put in place for efficient service delivery. Different approaches such as the application of native passive films on the surface and other corrosion inhibitory measures are being implemented to minimize corrosion in engineering sites. As is well appreciated, the consequence of pipe failures can be socially, economically, and environmentally catastrophic, resulting in massive disruption of daily life, considerable economic loss, widespread flooding, subsequent environmental pollution and even casualties and so forth (Hou et al. 2016). Corrosion generally occurs due to an electrochemical process that occurs in stages. The rates of corrosion also vary with time, depending on a complex interaction between the material, its environment and circumstances of exposure. In as much as the primary factors responsible for corrosion such as water and oxygen are present, the process is inevitable. The estimation is needed for engineers to be able to predict the lifespan of construction materials in industries. The cost of corrosion may run into billions of dollars every year. Due to the impact of corrosion on business economics, health safety and the environment, this study utilizes conventional water analysis, corrosion and scaling indices to ascertain the water stability conditions. Since aluminium, steel and iron are construction materials that show varying degrees of corrosion due to their physicochemical and electrochemical properties, these metals were used to measure corrosion rates in different formation water and seawater media under laboratory conditions.

To manage a potential scaling problem, it is essential to know where and how much scale forms during oil and water production (Osorio-Celestino et al. 2020). Many studies have shown that PW has high TDS content, which is the major cause of scale formation and pipe clogging (Arthur & Bruce 2005; Merdhah & Yassin 2007; Al-Ghouti et al. 2019; Al-Samhan et al. 2020; Bolaji et al. 2021). The Niger Delta is a beehive of oil exploration and production (E & P) activities in Nigeria and the volume of OFPW is high. There is scant literature on the effect of OFPW on construction materials used in the area. The present study aims to elucidate the corrosion and scaling potential of these waters on iron, steel and aluminium. This work examines the chemical characteristics of the Freeman OFPW to evaluate the corrosion behaviour of steel, aluminium, and iron in the aqua media, and determine the scaling potentials and corrosion kinetics of the OFPW. This research will provide further information for engineers in ascertaining the integrity and predicting the lifespan of materials used in the construction of OFPF.

The study area is located in the production zone of the Freeman field in the southwestern part of the Niger Delta, about 120 km offshore on the continental slope, at water depths of about 950–1,200 m (Figure 1). The reservoirs are structurally and stratigraphically trapped mud-rich unconfined turbidite sands within the Akata-Agbada petroleum system, located in a mid-lower slope depositional setting and are of Lower–Upper Miocene age within the prograding siliciclastic system. The Tertiary section of the Niger Delta is divided into three formations: the Akata, Agbada and Benin Formations, the type sections which are described by Short & Stauble (1967) and summarized in many other papers (Weber & Daukoru 1975; Avbovbo 1978; Evamy et al. 1978; Ejedawe 1981; Whiteman 1982; Knox & Omatsola 1989; Doust & Omatsola 1990; Beka & Oti 1995; Bolaji 2020; Bolaji et al. 2021; and references cited therein).

Figure 1

Niger Delta concession map showing the study area (Bolaji 2020).

Figure 1

Niger Delta concession map showing the study area (Bolaji 2020).

Close modal

Water sources and experimental method

Nine (9) water samples were extracted (without adding a demulsifier) from produced fluids obtained from the Miocene reservoirs across the Freeman field (Figure 1). Raw (untreated) and treated seawater (injection water) samples were also collected close to the deepwater facility location. Chemical analyses were performed according to Standard Methods for the Examination of Water & Wastewater, SMEWW Standards for inorganic ions, which influence scaling, and corrosion. Corrosion rate measurements were carried out by the weight loss method at room temperature. The experiments were carried out at a room temperature of 29.85 °C (303 °K). A constant volume (70 ml) of the different water samples was placed in well-closed glass bottles and were left at room temperature for 20 min to achieve thermal equilibrium with the surrounding environment. The steel, iron and aluminium specimens were of dimensions 4 × 4 × 0.18 cm. A blank experiment was also conducted by placing the metals in distilled water. The clean, dried specimens were weighed (Wa, g) using a digital balance of 10−4 g accuracy and each specimen was inserted carefully in the studied sample waters. The total duration of the experiment was 42 days. The specimens were investigated after 7, 11, 14, 21, 28, 35 and 42 days of exposure. At each time interval, the specimens were removed from the studied solution, washed with double-distilled water, dried and mechanically polished with a 1,200 grade of emery paper, to remove all corrosion products and to obtain a smooth surface. Then the polished specimens were rinsed with ethanol and dried with air and finally weighed (Wb, g). The corrosion rates (CR) (mg cm−2 h−1) were calculated according to the following Equation (1):
(1)
where and are coupon weights (mg) measured before and after immersion in the water samples, A is the exposed area (cm−2) and t (h) is the exposure time. Each experiment was run twice and the average value was taken.

Water stability indices

In this study, five indices were used to identify the corrosiveness and scaling potentials of the formation water and seawater samples. These include Langelier saturation index (LSI), Ryznar stability index (RSI), Larson–Skold index (L–S index), Puckorius scaling index (PSI), and aggressiveness index (AI).

Langelier saturation index

The LSI, developed by Dr Langlier in 1936 is an equilibrium model derived from the theoretical concept of saturation which indicates the degree of saturation of water and its potential to precipitate calcium carbonate in a qualitative assessment (Olajire 2013). LSI considers the effects of calcium, total alkalinity, dissolved solids, and temperature to obtain pHs as regards their tendency to be in equilibrium with calcium carbonate. Calcium carbonate is just one of many minerals found in water and is one of the most important elements responsible for forming calcareous deposits. The LSI considers the effects of calcium, total alkalinity, TDS, and temperature to arrive at a computed pH shown as pHs in the formula. Once the pH is known you simply subtract it from the actual pH of the water and, if the result is positive, the water will be scaling and conversely, if the number is negative, the water will tend to dissolve calcium carbonate (McCaul 2008). After calculation of pHs, the value of LSI is defined as follows (Fazlzadehdavilb et al. 2009):
(2)
where, pH is actual pH of water and the pHs is the pH of water at calcium carbonate saturation condition (McCaul 2008). pHs is calculated with following equation:
(3)

Values of A, B, C and D are determined according to Piri et al. 2008; Table 1. Constant A is determined using the TDS table by taking the value that corresponds to the measured total filterable residue or the estimated TDS. Constant B takes into account the effect of temperature. Value C is obtained by the corresponding value to the calcium hardness (in mg/L CaCO3) of the sample. Value D is obtained from the hardness table by reading the measured value for total alkalinity (in mg/L CaCO3) of the sample (Piri et al. 2008; Fazlzadehdavilb et al. 2009).

Table 1

Summary of the computed indices for the studied water samples

Sample IDpHTDSTemp (°C)Ca2+Mg2+Na+ + K+T.AlkABCDpHs
B-01 7.68 22,246.00 25 545.09 349.92 13,389.13 1,160.00 0.335 2.088 2.336 3.064 6.322 
B-14 7.32 23,984.00 25 657.32 233.28 7,797.67 1,040.00 0.338 2.088 2.418 3.017 6.291 
B-24a 7.73 14,617.00 25 416.83 330.48 3,787.87 1,440.00 0.316 2.088 2.220 3.158 6.326 
B-24b 7.75 14,537.00 25 601.20 121.50 3,619.80 1,200.00 0.316 2.088 2.379 3.079 6.246 
B-30 8.00 31,761.00 25 561.12 1,117.80 10,907.67 760.00 0.350 2.088 2.349 2.881 6.509 
B-35 7.60 23,568.00 25 432.86 806.76 8,021.33 920.00 0.337 2.088 2.236 2.964 6.525 
B-51a 7.93 28,430.00 25 737.47 330.48 7,673.60 1,760.00 0.345 2.088 2.468 3.246 6.020 
B-51b 8.38 17,671.43 25 368.74 797.04 4,504.00 1,160.00 0.325 2.088 2.167 3.064 6.482 
P-05 7.88 24,043.00 25 689.38 408.24 7,784.07 1,240.00 0.338 2.088 2.438 3.093 6.195 
SWR 7.76 36,184.00 25 426.45 1,240.27 10,261.00 360.00 0.356 2.088 2.230 2.556 6.958 
SWT 6.63 34,658.00 25 391.18 1,281.10 9,174.00 178.00 0.354 2.088 2.192 2.250 7.299 
Sample IDLSIRSIClL–S IndexpHeqPSIAIT. Hardness
B-01 1.36 4.964 12,043.30 600.00 696.00 1,415.20 5.989 9.069 3.575 13.481 2800.00  
B-14 1.03 5.263 12,956.49 1,100.00 624.00 1,268.80 7.426 9.022 3.561 13.155 2600.00  
B-24a 1.40 4.923 7,693.72 400.00 864.00 1,756.80 3.088 9.163 3.490 13.508 2400.00  
B-24b 1.50 4.743 7,211.32 500.00 720.00 1,464.00 3.531 9.084 3.408 13.608 2000.00  
B-30 1.49 5.017 18,761.21 2,000.00 456.00 927.20 15.010 8.886 4.131 13.630 6000.00  
B-35 1.07 5.451 13,313.82 1,000.00 552.00 1,122.40 8.549 8.969 4.082 13.200 4400.00  
B-51a 1.91 4.111 15,672.24 1,300.00 1,056.00 2,147.20 5.299 9.251 2.790 14.043 3200.00  
B-51b 1.90 4.584 9,712.67 400.00 696.00 1,415.20 4.790 9.069 3.894 14.011 4200.00  
P-05 1.69 4.509 13,480.58 600.00 744.00 1,512.80 6.239 9.098 3.291 13.812 3400.00  
SWR 0.80 6.156 21,071.83 2,450.00 216.00 439.20 35.900 8.561 5.355 12.946 6168.00  
SWT −0.67 7.969 21,278.29 2,300.00 106.80 217.16 72.781 8.255 6.344 11.473 6248.00  
Sample IDpHTDSTemp (°C)Ca2+Mg2+Na+ + K+T.AlkABCDpHs
B-01 7.68 22,246.00 25 545.09 349.92 13,389.13 1,160.00 0.335 2.088 2.336 3.064 6.322 
B-14 7.32 23,984.00 25 657.32 233.28 7,797.67 1,040.00 0.338 2.088 2.418 3.017 6.291 
B-24a 7.73 14,617.00 25 416.83 330.48 3,787.87 1,440.00 0.316 2.088 2.220 3.158 6.326 
B-24b 7.75 14,537.00 25 601.20 121.50 3,619.80 1,200.00 0.316 2.088 2.379 3.079 6.246 
B-30 8.00 31,761.00 25 561.12 1,117.80 10,907.67 760.00 0.350 2.088 2.349 2.881 6.509 
B-35 7.60 23,568.00 25 432.86 806.76 8,021.33 920.00 0.337 2.088 2.236 2.964 6.525 
B-51a 7.93 28,430.00 25 737.47 330.48 7,673.60 1,760.00 0.345 2.088 2.468 3.246 6.020 
B-51b 8.38 17,671.43 25 368.74 797.04 4,504.00 1,160.00 0.325 2.088 2.167 3.064 6.482 
P-05 7.88 24,043.00 25 689.38 408.24 7,784.07 1,240.00 0.338 2.088 2.438 3.093 6.195 
SWR 7.76 36,184.00 25 426.45 1,240.27 10,261.00 360.00 0.356 2.088 2.230 2.556 6.958 
SWT 6.63 34,658.00 25 391.18 1,281.10 9,174.00 178.00 0.354 2.088 2.192 2.250 7.299 
Sample IDLSIRSIClL–S IndexpHeqPSIAIT. Hardness
B-01 1.36 4.964 12,043.30 600.00 696.00 1,415.20 5.989 9.069 3.575 13.481 2800.00  
B-14 1.03 5.263 12,956.49 1,100.00 624.00 1,268.80 7.426 9.022 3.561 13.155 2600.00  
B-24a 1.40 4.923 7,693.72 400.00 864.00 1,756.80 3.088 9.163 3.490 13.508 2400.00  
B-24b 1.50 4.743 7,211.32 500.00 720.00 1,464.00 3.531 9.084 3.408 13.608 2000.00  
B-30 1.49 5.017 18,761.21 2,000.00 456.00 927.20 15.010 8.886 4.131 13.630 6000.00  
B-35 1.07 5.451 13,313.82 1,000.00 552.00 1,122.40 8.549 8.969 4.082 13.200 4400.00  
B-51a 1.91 4.111 15,672.24 1,300.00 1,056.00 2,147.20 5.299 9.251 2.790 14.043 3200.00  
B-51b 1.90 4.584 9,712.67 400.00 696.00 1,415.20 4.790 9.069 3.894 14.011 4200.00  
P-05 1.69 4.509 13,480.58 600.00 744.00 1,512.80 6.239 9.098 3.291 13.812 3400.00  
SWR 0.80 6.156 21,071.83 2,450.00 216.00 439.20 35.900 8.561 5.355 12.946 6168.00  
SWT −0.67 7.969 21,278.29 2,300.00 106.80 217.16 72.781 8.255 6.344 11.473 6248.00  

Ryznar stability index

John Ryznar developed the Ryznar stability index (RSI) in 1944 as a modification to LSI, when he realized the possibility for both low and high hardness water to have the same LSI values. By reversing the placement of pH and pHs in the formula, the result of RSI always will be a positive number. The RSI always will be a positive number. The pHs for the RSI is determined via the actual pH as well as the concentration of the calcium and bicarbonate ions, TDS and temperature. An RSI less than 5 should be scaling whereas an RSI above 7 will produce little if any scale (McCaul 2008). The value of RSI is evaluated as follows:
(4)
where, pH is the measured water pH, and pHs is the pH at saturation in calcite or calcium carbonate.

Larson–Skold index

The LSI index describes the corrosivity of water towards mild steel. The index is based upon an evaluation of in situ corrosion of mild steel. The index is the ratio of equivalents per million (epm) of sulphate () and () to the epm of alkalinity in the form of bicarbonate plus carbonate.
(5)

This index has been correlated to observed corrosion rates and the type of attack. The L-S index might be interpreted by the following guidelines: index < <0.8, chlorides and sulphates probably will not interfere with natural film formation 0.8 < <index < <1.2, chlorides and sulphates may interfere with natural film forming. Higher than desired corrosion rates might be anticipated. Index > >1.2, the tendency towards high corrosion rates of a local type should be expected as the index increases.

Puckorius scaling index

Paul Puckorius developed the PSI which accounts for two additional variables that the indices do not – the buffering capacity of water and the maximum quantity of precipitate that brings water to equilibrium. Therefore, the PSI uses an equilibrium pH to account for the buffering capacity of water and the maximum quantity of precipitate that brings water to equilibrium. Therefore, the PSI uses an equilibrium PH rather than the actual pH to account for the buffering effect (McCaul 2008). The equilibrium pH is determined as:
(6)
The numbers resulting from Equation (6) are the same as the RSI so a value less than 5 will be scaling and a number greater than 7 will result in little if any scaling. PSI is calculated as follows (McCaul 2008):
(7)

Aggressiveness index (AI)

The AI was developed for asbestos cement pipes with water temperatures ranging from 4 to 27 °C (40–80 °F). The AI is calculated as a function of pH, calcium concentration, and alkalinity. Waters with AI less than 10 are considered highly aggressive; AI between 10 and 12 is considered mildly aggressive; AI greater than 12 is considered non-corrosive and depositing (McCaul 2008). The AI is calculated as follows (Fazlzadehdavilb et al. 2009):
(8)
where A is the total alkalinity in mg/L as CaCO3 and H is the calcium hardness (in mg/L CaCO3).

Physicochemical characteristics

Analytical results of the measured physicochemical parameters are presented in Table 2. Produced water pH values range from 7.32 to 8.38, slightly alkaline to alkaline in nature, while those obtained for the raw seawater (SWR) and treated seawater (SWT) are 7.76 and 6.63 respectively. pH value less than 4 encourages corrosion as protective oxide film dissolves, while solutions with pH values between 4 and 10 have little effect on corrosion. Higher values above 10 make the metals passive, thereby reducing corrosion. Total alkalinity (T. Alk) ranges between 760 and 1,760 mg/L for formation water samples, while 178 and 360 mg/L were obtained for SWR and SWT samples respectively. The mean Total Hardness (TH) concentration of 3,444.44 mg/L for the formation water samples indicate the presence of more magnesium rather than calcium, while TH in seawater samples slightly exceeds the peak value of 6,000 mg/L obtained for the formation waters. Chloride, bicarbonate, and sulphate are the dominant anions, with an average of 12, 316.15 mg/L, 1,447.73 mg/L, and 877.78 mg/L respectively. Sodium and calcium on the other hand predominate the cations, averaging 7,426.79 mg/L and 556.67 mg/L respectively. Total dissolved solids (TDS) for the produced water samples ranges between 14,537 and 31,761 mg/L (Av. 22,317.49 mg/L), while 36,184 mg/L and 34,658 mg/L were obtained for the SWR and SWT samples. The analyses revealed that the principal hydrochemical is Na-K-SO4-Cl where the chemical properties of the waters are dominated by alkali elements. The water chemistry revealed that the formation waters are generally hard, saline water, dominantly of the Na-Cl type based on its TDS concentrations (Sawyer et al. 1994; Bolaji et al. 2021).

Table 2

Water chemistry results for the studied water samples

S/NParameterUnitMin.Max.MeanMedianStd Dev.
pH °C 6.63 8.35 7.70 7.75 0.44 
Eh mV −0.07 0.04 −0.03 −0.04 0.03 
EC mS/cm 19.39 59.55 35.75 32.98 13.65 
Ca2+ mg/L 368.74 737.47 529.79 545.09 130.06 
Mg2+ mg/L 121.50 1,281.10 637.90 408.24 426.12 
Na+ mg/L 3,576.33 13,328.00 7,811.06 7,742.67 3,026.14 
K+ mg/L 38.93 194.00 90.77 61.13 53.35 
Fe mg/L 5.73 268.00 53.37 12.93 94.15 
 mg/L 0.60 3.00 1.79 1.80 0.93 
10 Cl mg/L 7,211.32 21,278.29 13,926.86 13,313.82 4,881.45 
11  mg/L 400.00 2,450.00 1,150.00 1,000.00 770.39 
12  mg/L 217.16 2,147.20 1,244.18 1,415.20 554.61 
13  mg/L 6.10 19.10 12.91 12.70 5.24 
14 TH mg/L 2,000.00 6,248.00 3,946.91 3,400.00 1,577.43 
15 TA mg/L 178.00 1,760.00 1,019.82 1,160.00 454.60 
16 TDS mg/L 14,537.00 36,184.00 24,699.95 23,984.00 7,466.03 
17 Salinity  13.03 38.44 25.16 24.05 8.82 
S/NParameterUnitMin.Max.MeanMedianStd Dev.
pH °C 6.63 8.35 7.70 7.75 0.44 
Eh mV −0.07 0.04 −0.03 −0.04 0.03 
EC mS/cm 19.39 59.55 35.75 32.98 13.65 
Ca2+ mg/L 368.74 737.47 529.79 545.09 130.06 
Mg2+ mg/L 121.50 1,281.10 637.90 408.24 426.12 
Na+ mg/L 3,576.33 13,328.00 7,811.06 7,742.67 3,026.14 
K+ mg/L 38.93 194.00 90.77 61.13 53.35 
Fe mg/L 5.73 268.00 53.37 12.93 94.15 
 mg/L 0.60 3.00 1.79 1.80 0.93 
10 Cl mg/L 7,211.32 21,278.29 13,926.86 13,313.82 4,881.45 
11  mg/L 400.00 2,450.00 1,150.00 1,000.00 770.39 
12  mg/L 217.16 2,147.20 1,244.18 1,415.20 554.61 
13  mg/L 6.10 19.10 12.91 12.70 5.24 
14 TH mg/L 2,000.00 6,248.00 3,946.91 3,400.00 1,577.43 
15 TA mg/L 178.00 1,760.00 1,019.82 1,160.00 454.60 
16 TDS mg/L 14,537.00 36,184.00 24,699.95 23,984.00 7,466.03 
17 Salinity  13.03 38.44 25.16 24.05 8.82 

Water quality indices

The LSI determined for the produced water samples ranged from −0.67 to 1.91. Except for the treated seawater (SWT) sample, LSI was generally greater than zero, indicating super saturated water with scaling tendencies (Figure 2). Based on this index, SWT is not saturated and has no corroding tendency, hence, it is considered suitable as injection water. However, the remaining PW samples are generally supersaturated with respect to CaCO3 and may form scale. Although water temperature has a positive effect on LSI, i.e. as water temperature increases, LSI becomes more positive. In this study, LSI values revealed that the majority of the PW are supersaturated with respect to CaCO3 and scale forming may occur on the pipelines, thereby restricting the free flow of HC fluids. Undersaturated waters (e.g. SWT) changes the chemical equilibrium of CaCO3, favouring the dissolution of protective coatings in pipelines and equipment (DeMartini 1938).

Figure 2

Computed LSI for the studied water samples.

Figure 2

Computed LSI for the studied water samples.

Close modal

Ryznar saturation index ranges between 4.1 and 5.5 for PW samples and 6.2–8.0 for SW samples (Figure 3). RSI less than 5.5 indicate heavy scale formation while values greater than 8.5 indicates that the water is aggressive, that is such water actively seeks to gain minerals and metals which results in the corrosion of iron and copper surfaces and causes dissolving concrete and stone surfaces (Konwar et al. 2021). The Freeman PW samples show rigorous scaling tendency based on the RSI. SWR is balanced with no scaling and corrosive tendency, while SWT has a corrosive tendency. The SWT which show a seemingly neutral has the highest RSI value.

Figure 3

RSI computed for the studied water samples.

Figure 3

RSI computed for the studied water samples.

Close modal

L–S index is generally greater than 1.2 indicating that high rates of localized corrosion can be expected in all the studied water samples (Figure 4). PSI values in the OFPW samples range from 2.79 to 6.34. PSI values generally suggest that scaling is likely to occur in the PW and SWR samples, while SWT shows little scaling and corrosive tendency (Figure 5). AI range from 11.47 to 14.04 (Figure 6). According to the AI, produced water and SWR samples are non-aggressive with the ability for scale formation, while SWT is moderately corrosive and aggressive.

Figure 4

L–S index computed for the studied water samples.

Figure 4

L–S index computed for the studied water samples.

Close modal
Figure 5

Computed PSI for the studied water samples.

Figure 5

Computed PSI for the studied water samples.

Close modal
Figure 6

AI Computed for the studied water samples.

Figure 6

AI Computed for the studied water samples.

Close modal

Corrosion rates

Steel has the highest CR in B-25b with value 3.84 × 10−3 mg cm−2 h−1, while the least value was 1.49 × 10−3 mg cm−2 h−1 in B-51a (Table 3). Iron has the highest CR in B-30 with a value of 3.29 × 10−3 mg cm−2 h−1 while the least value was 1.24 × 10−3 mg cm−2 h−1 in SWT. The highest and least CR were 2.48 × 10−3 mg cm−2 h−1 in SWR and 0.37 × 10−3 mg cm−2 h−1 in B-24a for aluminium. The highest CR was observed in steel with a value of 3.84 × 10−3 mg cm−2 h−1, while the least CR occurred in aluminium with a value of 0.37 × 10−3 mg cm−2 h−1. The corrosion suffered by iron plates is of the general type (uniform attack). The corrosion rate of iron varied from month to month. Iron has the highest CR in all the water samples except B-25b, B-14, B-01 and SWT where steel CR was higher. The corrosion suffered by steel plates was mainly of a general type attack. Aluminium has the least CR in all the water samples compared to other metals investigated. It is a very reactive metal but mild to corrosion. Of all metals investigated by Natesan et al. (2006), aluminium was also the least corroded. No significant attack was observed on aluminium panels. Corrosion observed in B-01 was due to atmospheric gases and water which aids the corrosion process. An increase in salt content (salinity) also increases the rate of corrosion.

Table 3

Cumulative corrosion rate (mg·cm−2 h−1)

S/NSample IDCR steel × 10−3CR iron × 10−3CR aluminium × 10−3
B-01 3.16 1.30 0.68 
B-14 2.60 2.11 0.74 
B-24a 1.92 2.48 0.37 
B-25b 3.84 2.36 0.49 
B-30 2.48 3.29 0.99 
B-35 2.23 3.28 0.99 
B-51a 1.49 2.11 0.74 
B-51b 1.79 1.98 1.05 
P-05 1.86 2.67 1.36 
10 SWR 2.66 2.73 2.48 
11 SWT 2.54 1.24 0.74 
S/NSample IDCR steel × 10−3CR iron × 10−3CR aluminium × 10−3
B-01 3.16 1.30 0.68 
B-14 2.60 2.11 0.74 
B-24a 1.92 2.48 0.37 
B-25b 3.84 2.36 0.49 
B-30 2.48 3.29 0.99 
B-35 2.23 3.28 0.99 
B-51a 1.49 2.11 0.74 
B-51b 1.79 1.98 1.05 
P-05 1.86 2.67 1.36 
10 SWR 2.66 2.73 2.48 
11 SWT 2.54 1.24 0.74 

Kinetics of steel, iron and aluminium corrosion in water samples

The kinetics study was investigated at 29.85 °C (303 °K) by fitting the corrosion data into different rate laws (Table 4). Coefficients of determination (R2) were used to determine the best rate law for the corrosion process. The rate laws considered were:
(9)
(10)
where Wo is the initial weight of iron, Wt is the weight loss of iron at time t and k is the rate constant. Previous studies have shown that the rate of corrosion is not constant with respect to time and this can be attributed to complex reaction chemistry, the reactivity of the corrosive medium, adsorption, coating on the metal surface and variations in environmental conditions. Based on results obtained for the first-order (Figures 7 and 8) and second-order (Figures 9 and 10) kinetics, the model with the highest R2 was chosen as the best fit for the study. By far, most of the results fit into first-order kinetics. The plot of In Wt against t was linear and shows a higher R2 value for all water samples used for steel corrosion study except B-51b. The plot of 1/Wt against t for steel in B-51b has a higher R2 value confirming the second-order reaction model. This result is similar to a study conducted by Aljbour (2016), which indicates a second-order reaction model for steel in various concentrations of HCl solutions. The highest R2 value confirms the first-order reaction model for iron in all the water samples investigated. Research conducted by Patil & Sharma (2011) also reveals a first-order reaction model for iron in different concentrations of HCl solutions. In almost all the water samples, aluminium fits into the first-order reaction model with R2 close or higher than 0.9, the only exception is for the B-24b water sample showing a higher R2 value confirming the second-order kinetic model.
Table 4

First-order and second-order kinetics data

Sample IDSteel
Iron
Aluminium
First order (r2)Second order (r2)First order (r2)Second order (r2)First order (r2)Second order (r2)
B-01 0.6543 0.5674 0.3826 0.3549 0.7413 0.6814 
B-14 0.5835 0.5043 0.7665 0.6851 0.9572 0.9473 
B-24a 0.4474 0.307 0.5044 0.3913 0.1541 0.808 
B-24b 0.5156 0.4594 0.5819 0.4887 0.9088 0.798 
B-30 0.7181 0.6731 0.6514 0.5209 0.6826 0.6144 
B-35 0.6237 0.5691 0.8252 0.7827 0.8829 0.8211 
B-51a 0.716 0.5393 0.748 0.6713 0.7606 0.7216 
B-51b 0.4681 0.5417 0.639 0.5417 0.767 0.6194 
P-05 0.742 0.7111 0.9366 0.9004 0.8717 0.7564 
SWR 0.5505 0.543 0.6079 0.5243 0.7546 0.7197 
SWT 0.4425 0.366 0.565 0.4038 0.6484 0.5197 
Sample IDSteel
Iron
Aluminium
First order (r2)Second order (r2)First order (r2)Second order (r2)First order (r2)Second order (r2)
B-01 0.6543 0.5674 0.3826 0.3549 0.7413 0.6814 
B-14 0.5835 0.5043 0.7665 0.6851 0.9572 0.9473 
B-24a 0.4474 0.307 0.5044 0.3913 0.1541 0.808 
B-24b 0.5156 0.4594 0.5819 0.4887 0.9088 0.798 
B-30 0.7181 0.6731 0.6514 0.5209 0.6826 0.6144 
B-35 0.6237 0.5691 0.8252 0.7827 0.8829 0.8211 
B-51a 0.716 0.5393 0.748 0.6713 0.7606 0.7216 
B-51b 0.4681 0.5417 0.639 0.5417 0.767 0.6194 
P-05 0.742 0.7111 0.9366 0.9004 0.8717 0.7564 
SWR 0.5505 0.543 0.6079 0.5243 0.7546 0.7197 
SWT 0.4425 0.366 0.565 0.4038 0.6484 0.5197 
Figure 7

First-order corrosion kinetic for the studied water samples (a) B-01, (b) B-14, (c) B-24a, (d) B-24b, (e) B-30, and (f) B-35.

Figure 7

First-order corrosion kinetic for the studied water samples (a) B-01, (b) B-14, (c) B-24a, (d) B-24b, (e) B-30, and (f) B-35.

Close modal
Figure 8

First-order corrosion kinetics for the studied water samples: (a) B-51a, (b) B-51b, (c) P-05, (d) SWR, and (e) SWT.

Figure 8

First-order corrosion kinetics for the studied water samples: (a) B-51a, (b) B-51b, (c) P-05, (d) SWR, and (e) SWT.

Close modal
Figure 9

Second-order corrosion kinetics for the studied water samples (a) B-01, (b) B-14, (c) B-24a, (d) B-24b, (e) B-30, and (f) B-35.

Figure 9

Second-order corrosion kinetics for the studied water samples (a) B-01, (b) B-14, (c) B-24a, (d) B-24b, (e) B-30, and (f) B-35.

Close modal
Figure 10

Second-order corrosion kinetics for the studied water samples (a) B-51a, (b) B-51b, (c) P-05, (d) SWR, and (e) SWT.

Figure 10

Second-order corrosion kinetics for the studied water samples (a) B-51a, (b) B-51b, (c) P-05, (d) SWR, and (e) SWT.

Close modal

Chemical analysis revealed that the studied formation water and seawater samples are slightly alkaline and generally classified as hard, saline water based on its TDS. The waters are of the Na-Cl type with Na-K-SO4-Cl as the principal hydrochemical facies. Based on the computation of the different corrosivity indices, there is a likelihood of some of the water to form mild to severe scales, while the seawater samples are classified as ‘non-aggressive’ and ‘aggressive’. In most cases, the rate of corrosion of the metals followed the first-order rate constant in some of the samples, and second-order in others within the first seven days. It was observed that the rate of corrosion follows this order: steel > iron > aluminium. The potential heavy and intolerable corrosion associated with the use of these seawater samples as injection waters is a potential risk that must be handled by adequate treatment. A comprehensive analysis of steel, iron and aluminium corrosion in oilfield waters was presented in this paper. From the results available it has been established that aluminium was the least corroded while the iron was the most corroded. It can be concluded that the results of cumulative corrosion rate and kinetics study presented in the paper can contribute to the body of knowledge of corrosion behaviour of the metals and aid in the prediction of long-term properties of the metals in construction. This knowledge can enable a more accurate prediction of failures of metal pipes.

The authors wish to appreciate Shell Nigeria for providing fluid samples for this study. Comments from anonymous reviewers, which greatly improved the quality of this work are gratefully acknowledged.

All relevant data are included in the paper or its Supplementary Information.

The authors declare there is no conflict.

Al-Ghouti
M. A.
,
Al-Kaabi
M.
,
Ashfaq
M.
&
Da'na
D. A.
2019
Produced water characteristics, treatment and re-use: a review
.
Journal of Water Process Engineering
28
,
222
239
.
https://doi.org/10.1016/j.jwpe.2019.02.001
.
Aljbour
S. H.
2016
Modeling of corrosion kinetics of mild steel in hydrochloric acid in the presence and absence of a drug inhibitor
.
Portugaliae Electrochimica Acta
34
(
6
),
407
416
.
http://dx.doi.org/10.4152/pea.201606407
.
Al-Samhan
A.
,
Alanezi
K.
,
Al-Fadhli
J.
,
Al-Attar
F.
,
Mukadam
S.
&
George
J.
2020
Evaluating scale deposition and scale tendency of effluent water mix with seawater for compatible injection water
.
Journal of Petroleum Exploration and Production Technology
10
,
2105
2111
.
https://doi.org/10.1007/s13202-020-00849-w
.
Arthur
J.
&
Bruce
G.
2005
Technical Summary of oil and gas Produced Water Treatment Technologies
.
All Consulting, LLC
,
Tulsa
.
Avbovbo
A. A.
1978
Tertiary lithostratigraphy of the Niger delta
.
AAPG Bulletin
62
,
295
300
.
Beka
F. T.
,
Oti
M. N.
1995
The Distal Offshore Niger Delta: frontier prospects of a mature petroleum province
. In:
Geology of Deltas
(
Oti
M. N.
&
Postma
G.
, eds).
A.A. Balkema
,
Rotterdam
, pp.
237
241
.
Bolaji
T. A.
2020
Reservoir Souring Possibilities in Freeman Oilfield, Niger Delta: Insights from Mineralogy, Diagenesis and Water Chemistry
.
Unpublished Ph.D. Dissertation
,
University of Port Harcourt
,
Nigeria
.
Bolaji
T. A.
,
Oti
M. N.
,
Onyekonwu
M. O.
,
Bamidele
T.
,
Osuagwu
M.
,
Chiejina
L.
&
Elendu
P.
2021
Preliminary geochemical characterization of saline formation water from Miocene Reservoirs, Offshore, Niger Delta
.
Heliyon
7
(
2
),
e06281
.
https://doi.org/10.1016/j.heliyon.2021.e06281
.
Das
N. K.
,
Suzuki
K.
,
Ogawa
K.
&
Shoji
T.
2009
Early stage SCC initiation analysis of FCC Fe–Cr–Ni ternary alloy at 288 °C: a quantum chemical molecular dynamics approach
.
Corrosion Science
51
(
4
),
908
913
.
https://doi.org/10.1016/j.corsci.2009.01.005
.
DeMartini
F. E.
1938
Corrosion and the Langelier calcium carbonate saturation index
.
Journal (American Water Works Association)
30
(
1
),
85
111
.
de Sena
R. A.
,
Bastos
I. N.
&
Platt
G. M.
2012
Theoretical and experimental aspects of the corrosivity of simulated soil solutions
.
ISRN Chemical Engineering
2012
.
Article ID 103715. https://doi.org/10.5402/2012/103715
.
Doust
H.
,
Omatsola
E.
1990
Niger Delta in divergent/passive margin basins
. In:
AAPG Memoir 48
(
Edwards
J. D.
&
Santogrossi
P. A.
, eds).
American Association of Petroleum Geologists, Tulsa
, pp.
201
238
.
Du
Y.
,
Guan
L.
&
Liang
H.
2005
Advances of produced water management
. In
Canadian International Petroleum Conference
,
Petroleum Society of Canada
.
https://doi.org/10.2118/2005-060
.
Ejedawe
J. E.
1981
Patterns of incidence of oil reserves in Niger Delta Basin
.
American Association of Petroleum Geologists Bulletin
65
,
1574
1585
.
Evamy
B. D.
,
Haremboure
J.
,
Kamerling
P.
,
Knapp
W.
,
Molloy
F. A.
&
Rowlands
P. H.
1978
Hydrocarbon habitat of Tertiary Niger Delta
.
American Association of Petroleum Geologists Bulletin
62
,
1
39
.
Fazlzadehdavilb
D. M.
,
Norouzi
M.
,
Mazloomi
S.
,
Amarluie
A.
,
Tardast
A.
&
Karamitabar
Y.
2009
Survey of corrosion and scaling potentials of produced water from Ilam water treatment plant
.
World Applied Sciences Journal
7
(
Special Issue of Applied Math
).
Gelfgat
M. Y.
,
Basovich
V. S.
&
Adelman
A. J.
2005
Aluminium alloy tubulatrs for oil and gas industry
. In
SPE Annual Technical Conference and Exhibition
,
Society of Petroleum Engineers
,
Dallas, Texas
, pp.
1
11
.
Goulter
C.
1985
An analysis of pipe breakage in urban water distribution networks
.
Canadian Journal of Civil Engineering
12
(
2
),
286
293
.
Hou
Y.
,
Lei
D.
,
Li
S.
,
Yang
W.
&
Li
C.
2016
Experimental investigation on corrosion effect on mechanical properties of buried metal pipes
.
International Journal of Corrosion
.
https://doi.org/10.1155/2016/5808372
.
Knox
G. J.
,
Omatsola
E. M.
1989
Development of the Cenozoic Niger Delta in terms of the ‘Escalator Regression’ model and impact on hydrocarbon distribution
. In:
Proceedings of the KNGMG Symposium Coastal Lowlands, Geology and Geotechnology, The Hague, 1987
(
van der Linden
W. J. M.
,
Cloetingh
S. A. P. L.
,
Kaasschieter
J. P. K.
,
van der Graf
W. J. E.
,
Vandenberglie
J.
&
van der Gun
J. A. M.
, eds).
Kluwer Academic
,
Dordrecht
, pp.
181
202
.
Konwar
D.
,
Gogoil
S. B.
&
Gogoi
T. J.
2021
Evaluation of the corrosion and scaling potentials of oilfield produced water of the Upper Assam Basin
. In:
Advances in Petroleum Technology
(
Gogoi
S. B.
, ed.).
Jenny Stanford Publishing Pte. Ltd.
,
Singapore
, p.
505
.
Kpeglo
D. O.
,
Mantero
J.
,
Darko
E. O.
,
Emi-Reynolds
G.
,
Faanu
A.
,
Manjón
G.
,
Vioque
I.
,
Akaho
E. H. K.
&
Garcia-Tenorio
R.
2016
Radiochemical characterization of produced water from two production offshore oilfields in Ghana
.
Journal of Environmental Radioactivity
152
,
35
45
.
http://dx.doi.org/10.1016/j.jenvrad.2015.10.026
.
McCaul
C.
2008
Stress corrosion cracking
.
Materials Newsletter
7
(
4
).
Merdhah
A.
&
Yassin
A.
2007
Scale formation in oil reservoir during water injection of high-salinity formation water
.
Journal of Applied Sciences
7
(
21
),
3198
3207
.
https://dx.doi.org/10.3923/jas.2007.3198.3207
.
Mohebbi
H.
&
Li
C. Q.
2011
Experimental investigation on corrosion of cast iron pipes
.
International Journal of Corrosion
2011
.
Article ID506501. https://doi.org/10.1155/2011/506501
.
Natesan
M.
,
Venkatachari
G.
&
Palaniswamy
N.
2006
Kinetics of atmospheric corrosion of mild steel, zinc, galvanised iron and aluminium at 10 exposure stations in India
.
Corrosion Science
48
,
3584
3608
.
http://dx.doi.org/10.1016/j.corsci.2006.02.006
.
Nwanonenyi
S.
,
Obasi
M.
,
Obidiegwu
H.
&
Chukwujike
I.
2020
Anticorrosion response of polymer mixture on mild steel in hydrochloric acid environment
.
Emergent Materials
3
(
5
),
663
673
.
Olajire
A. A.
2013
Fundamentals of Oilfield Chemistry for Professionals in Petroleum and Energy Industries
.
Akmos Environmental Consult
,
Ogbomosho
,
Nigeria
, p.
560
.
Osorio-Celestino
G. R.
,
Hernandez
M.
,
Solis-Ibarra
D.
,
Tehuacanero-Cuapa
S.
,
Rodriguez-Gomez
A.
&
Gomora-Figueroa
P.
2020
Influence of calcium scalling on corrosion behavior of steel and aluminum alloys
.
ACS Omega
5
,
17304
17313
.
https://dx.doi.org/10.1021/acsomega.0c01538
.
Ozgun
H.
,
Ersahin
M. E.
,
Erdem
S.
,
Atay
B.
,
Sayili
S.
,
Eren
E.
,
Hoshan
P.
,
Atay
D.
,
Altinbas
M.
,
Kinaci
C.
&
Koyuncu
I.
2013
Comparative evaluation for characterization of produced water generated from oil, gas, and oil-gas production fields
.
Clean-Soil, Air, Water
41
(
12
),
1175
1182
.
https://doi.org/10.1002/clen.201200204
.
Parangusan
H.
,
Bhadra1
J.
&
Al-Thani
N.
2021
A review of passivity breakdown on metal surfaces: influence of chloride and sulfide-ion concentrations, temperature, and pH
.
Emergent Materials
4
,
1187
1203
.
https://doi.org/10.1007/s42247-021-00194-6
.
Patil
D. B.
&
Sharma
A. R.
2011
Study on the corrosion kinetics of iron in acid and base medium
.
E-Journal of Chemistry
8
(
1
),
358
362
.
http://dx.doi.org/10.1155/2011/294792
.
Piri
E. R.
,
Shams
G.
,
Shahmansouri
M.
&
Farzadkia
M.
2008
Survey of corrosion and scaling potential in drinking water of distribution system of Khoramabad city with corrosion indices
.
Quarterly Newsletter
10
(
3
).
https://dx.doi.org/10.5681 %2Fhpp.2012.013
.
Rajani
B.
,
McDonald
S.
&
Felio
G.
1995
Water Mains Break Data on Different Pipe Materials for 1992 and 1993. Report A-7019.1
.
National Research Council of Canada
,
Ottawa
,
Canada
.
Sawyer
C. L.
,
McCarthy
P. L.
&
Parkin
G. F.
1994
Chemistry for Environmental Engineering
, 4th edn.
McGraw-Hill Book Company
, New York, p.
545
.
Short
K. C.
&
Stauble
A. J.
1967
Outline of geology of Niger Delta
.
American Association of Petroleum Geologists Bulletin
51
,
761
779
.
Weber
K. J.
&
Daukoru
E. M.
1975
Petroleum geological aspects of the Niger Delta Nigeria
.
Journal of Mineral Geology
12
,
9
32
.
Whiteman
A.
1982
Nigeria: Its Petroleum Geology, Resources, and Potential
, Vols.
1 and 2
.
Graham and Trotman
,
London
.
This is an Open Access article distributed under the terms of the Creative Commons Attribution Licence (CC BY 4.0), which permits copying, adaptation and redistribution, provided the original work is properly cited (http://creativecommons.org/licenses/by/4.0/).