Mahmood M. S. Abdullaha, 
Hamad A. Al-Lohedana and 
Ayman M. Atta*ab
aSurfactants Research Chair, Chemistry Department, College of Science, King Saud University, Riyadh 11451, Saudi Arabia. E-mail: aatta@ksu.edu.sa; hlohedan@ksu.edu.sa; Mr.alhddad@gmail.com;  Fax: +966 114675998;   Tel: +966 561557975
bPetroleum Application Department, Egyptian Petroleum Research Institute, Nasr City 11727, Cairo, Egypt.  Fax: +20 222747433;   Tel: +20 222747917
First published on 15th June 2016
This work aims to apply modified asphaltene for capping of magnetite to form dispersed hydrophobic magnetic nanomaterials for environmental applications. In this respect, asphaltene was separated from heavy crude oil and functionalized by sulfonation in order to apply as a capping agent for magnetic materials to collect the heavy crude oil that was not easily collected or dispersed by using different oil spill control techniques. The coprecipitation method was used to prepare magnetite in the presence of sulfonated asphaltene as a capping agent. The magnetite nanomaterials were confirmed by thermogravimetric analysis, X-ray powder diffraction, transmittance electron microscopy and a vibrating sample magnetometer. Finally, sulfonated asphaltene magnetite nanomaterials were applied at different concentrations to collect a heavy crude oil spill after application of an external magnetic field as novel magnetic materials. They achieved remarkable oil spill collection efficiency with a reduction in the overall cost of the materials when compared with available techniques.
Magnetic fluids are advanced chemicals can be used to collect oil spills by applying an external magnetic field.16–18 The hydrophobic magnetic particles having strong magnetic properties are the main target to apply these materials to collect the oil spill.19 The disadvantages of these materials are caused from low dispersability of magnetic nanomaterials and collection of magnetic materials to reuse.20 In previous works,21–24 the hydrophobic magnetic nanomaterials were prepared and applied as a powder through spreading on the oil spill surface without applying toxic solvents or capping agents. In the present work, our aims are directed to separate asphaltene from heavy crude oil and modify its chemical structure in order to apply it as capping agents for magnetic nanoparticles. The formation of sulfonated asphaltene (SAS) is believed to serve as the nanoreactor to apply as a soft template because of its hydrophilic group (–SO3H) and the hydrophobic polycondensed aromatic, cycloparaffin and linear alkyl group assisting the formation of micelles and stabilizing colloids in an aqueous solution. It is expected that the particle size of magnetite can be controlled by the micelle “reactor” sizes.25 The advantage of this method is its offer to use cheap materials produced from crude oils to increase the dispersion of magnetic materials into crude oil. Moreover, it is expected that the performance of prepared magnetic nano-powder materials to collect the heavy crude oil will increase due to superior surface properties of the nanomaterials. The separation and reuse of these materials to collect the oil spill are another objective of the present work.
Asphaltene was sulfonated using a modified reported method26 as follows: 10 g of asphaltene was dissolved in 100 mL of dichloromethane and cooled to 10 °C using an ice bath. Oleum (10.5 g) was added dropwise under vigorous stirring for a period of 2 h. The reaction mixture was stirred for another 3 h at room temperature and extracted three times with n-hexane. The remaining solid was washed several times with acetone to produce sulfonated asphaltene (SAS).
The same procedure was repeated to prepare magnetite capped with SAS except KI was used as a reagent instead of Na2SO3.27 The dissolved weights of FeCl3·6H2O, KI and SAS are 5, 1.02 and 1.3 g, respectively. The produced magnetite can be designated as SAS-MPKI.
The crystal lattice structure and diffraction pattern of magnetite were analyzed by X-ray powder diffraction (XRD; BDX-3300 diffractometer using CuKα radiation of wavelength, λ = 1.5406 Å).
The magnetite and SAS contents were determined from thermogravimetric analysis (TGA; Shimadzu, DSC-60 and heating the samples from room temperature to 800 °C under N2 atmosphere at a heating rate of 10 °C min−1).
The surface morphology of magnetite was confirmed by high resolution transmission electron microscopy (HR-TEM; JEOL JEM-2100F).
The particle diameter and dispersity index were analyzed by dynamic light scattering (DLS; Zetasizer 3000HS; Malvern Instruments, Malvern, U.K.) with a 633 nm He–Ne laser using ethanol/water/(4/1) as the solvent. Zeta potentials of magnetite suspensions were evaluated at 25 °C using a zeta potential analyzer.
Contact angle measurements between magnetite dispersions in ethanol and crude oil were determined using the sessile drop technique drop shape analyser (model DSA-100). The crude oil layer with a thickness of 1 cm was spread on a glass plate and the drop of dispersed magnetite ethanol solution contacted the crude oil layer to measure the advancing and receding contact angles.
The magnetic parameters of the prepared magnetite were determined at room temperature using vibrating sample magnetometer (VSM; LDJ9600 in a field of 20![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) 000 Oe).
000 Oe).
![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) :
:![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) 25 to 1
25 to 1![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) :
:![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) 1 after mixing with a 1 cm deep vortex obtained by slow stirring for 1 minute. The dispersed crude oil spill stood for 5 min and a permanent magnet of Nd–Fe–B (4300 Gauss) was applied to collect the crude oil layer from the water surfaces. The remained oil volume was extracted by chloroform and determined after evaporation of chloroform using a rotary evaporator. The efficiency for collection of crude oil can be calculated as: CE (%) = (volume of removed oil/volume of original spill) × 100%. The magnetite powders were separated by dilution of the separated oil and using an external magnetic field and reused three times.
1 after mixing with a 1 cm deep vortex obtained by slow stirring for 1 minute. The dispersed crude oil spill stood for 5 min and a permanent magnet of Nd–Fe–B (4300 Gauss) was applied to collect the crude oil layer from the water surfaces. The remained oil volume was extracted by chloroform and determined after evaporation of chloroform using a rotary evaporator. The efficiency for collection of crude oil can be calculated as: CE (%) = (volume of removed oil/volume of original spill) × 100%. The magnetite powders were separated by dilution of the separated oil and using an external magnetic field and reused three times.
The chemical structure of sulfonated asphaltene was confirmed from the FTIR spectrum that is represented in Fig. 1a. It was noticed that the spectrum of asphaltene (Fig. 1a) is similar to data reported previously for asphaltene32 except the appearance of a new band observed at 1074 cm−1 (S![[double bond, length as m-dash]](https://www.rsc.org/images/entities/char_e001.gif) O stretching vibration) which confirms the sulfonation of asphaltene. The presence of aromatic groups was confirmed by the appearance of bands at 3095, 1602 and 860, 800, 750 cm−1 which was attributed to
O stretching vibration) which confirms the sulfonation of asphaltene. The presence of aromatic groups was confirmed by the appearance of bands at 3095, 1602 and 860, 800, 750 cm−1 which was attributed to ![[double bond, length as m-dash]](https://www.rsc.org/images/entities/char_e001.gif) CH stretching, C
CH stretching, C![[double bond, length as m-dash]](https://www.rsc.org/images/entities/char_e001.gif) C stretching and aromatic out of plane bending vibrations, respectively. The presence of CH2 cyclic and CH3 aliphatic is confirmed from bands at 2950, 2850, 1450 and 1375 cm−1 that referred to aliphatic CH stretching and bending vibrations. The polar functionalities of asphaltene were confirmed by the appearance of stretching vibrations of –OH and/or –NH at 3450 cm−1; and stretching vibrations of C
C stretching and aromatic out of plane bending vibrations, respectively. The presence of CH2 cyclic and CH3 aliphatic is confirmed from bands at 2950, 2850, 1450 and 1375 cm−1 that referred to aliphatic CH stretching and bending vibrations. The polar functionalities of asphaltene were confirmed by the appearance of stretching vibrations of –OH and/or –NH at 3450 cm−1; and stretching vibrations of C![[double bond, length as m-dash]](https://www.rsc.org/images/entities/char_e001.gif) O or C
O or C![[double bond, length as m-dash]](https://www.rsc.org/images/entities/char_e001.gif) N in heterocyclic rings at 17
N in heterocyclic rings at 17![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) 010 cm−1.
010 cm−1.
The magnetite can be formed under oxidizing and reducing conditions using KI or Na2SO3 as illustrated in eqn (1) and (2):21,27
| 3Fe3+ + I− → 2Fe3+ + Fe2+ + ½I2 | (1) | 
| 6Fe3+ + SO32− + ½O2 → 4Fe3+ + 2Fe2+ + SO42− | (2) | 
Ferric chloride was oxidized to ferrous and ferric cations (Fe2+ and Fe3+) which hydrolyzed in basic conditions to form magnetite. The mechanism for preparation and capping of magnetite nanoparticles is illustrated in Scheme 1.
In this respect, the Fe2+ and Fe3+ that were produced from the reaction of ferric chloride with KI or Na2SO3 interacted with sulfonated asphaltene as described in the experimental section. The capped iron cations were hydrolyzed with ammonia solution at pH 10 to form capped magnetite iron oxide. Magnetite can interact with sulfonated asphaltene by complexation with sulfonate groups and hetero nitrogen, oxygen or sulfur groups of asphaltene moieties. It was expected that sulfonated asphaltene can form a physical cap with magnetite by hydrogen bond forces, polarity induction forces, and electrostatic attractions between the magnetite and sulfonated asphaltene molecules.31
![[double bond, length as m-dash]](https://www.rsc.org/images/entities/char_e001.gif) O stretching which elucidated the functionalization of magnetite nanoparticles with the sulfonate, carboxylic or hydroxyl groups of sulfonated asphaltene as illustrated in Scheme 1. The low intensity of SAS of magnetite prepared by the KI method (Fig. 1b) indicates that the concentration of the magnetite content was increased more than SAS. The higher intensity of the band at 3450 cm−1 (Fig. 1c) indicated an increase of the hydroxyl group content in the case of the magnetite of SAS-MPNS more than that of SAS-MPKI. This observation confirms that the magnetite surfaces were modified with hydroxyl groups in the case of magnetite of SAS-MPNS more than that of SAS-MPKI.21,27 The shift of the C
O stretching which elucidated the functionalization of magnetite nanoparticles with the sulfonate, carboxylic or hydroxyl groups of sulfonated asphaltene as illustrated in Scheme 1. The low intensity of SAS of magnetite prepared by the KI method (Fig. 1b) indicates that the concentration of the magnetite content was increased more than SAS. The higher intensity of the band at 3450 cm−1 (Fig. 1c) indicated an increase of the hydroxyl group content in the case of the magnetite of SAS-MPNS more than that of SAS-MPKI. This observation confirms that the magnetite surfaces were modified with hydroxyl groups in the case of magnetite of SAS-MPNS more than that of SAS-MPKI.21,27 The shift of the C![[double bond, length as m-dash]](https://www.rsc.org/images/entities/char_e001.gif) O and S
O and S![[double bond, length as m-dash]](https://www.rsc.org/images/entities/char_e001.gif) O vibration (symmetric stretching) to a broad intense band confirms the chemisorption between Fe–O and sulfonated asphaltene.33 It was also noticed that the intensity of sulfonated asphaltene bands was highly increased for magnetite formed from the reaction of FeCl3 with Na2SO3 (Fig. 1b and c) more than that formed from the reaction with the KI reagent. This observation confirms that more magnetite nanoparticles were capped in the presence of KI than that of Na2SO3. This means that KI is more effective in the redox reaction that produces ferric and ferrous cations than Na2SO3 as illustrated in eqn (1) and (2) which was confirmed from the high yield of magnetite that was produced by using KI in previous works.21,22,27
O vibration (symmetric stretching) to a broad intense band confirms the chemisorption between Fe–O and sulfonated asphaltene.33 It was also noticed that the intensity of sulfonated asphaltene bands was highly increased for magnetite formed from the reaction of FeCl3 with Na2SO3 (Fig. 1b and c) more than that formed from the reaction with the KI reagent. This observation confirms that more magnetite nanoparticles were capped in the presence of KI than that of Na2SO3. This means that KI is more effective in the redox reaction that produces ferric and ferrous cations than Na2SO3 as illustrated in eqn (1) and (2) which was confirmed from the high yield of magnetite that was produced by using KI in previous works.21,22,27
XRD diffractograms of magnetite nanoparticles capped with sulfonated asphaltene are illustrated in Fig. 2a and b. The diffraction patterns confirm the presence of magnetite without contamination of other iron oxides. There are characteristic peaks at 2θ = 30.17°, 35.53°, 43.16°, 53.51°, 57.27°, 62.77°, and 73.79° confirming peaks for Fe3O4 marked by their indices (220), (311), (400), (422), (511), (440), and (622) as confirmed with the database in the Joint Committee on Powder Diffraction Standards (JCPDS) file (PDF no. 65-3107). The presence of sulfonated asphaltene was elucidated from the appearance of broad diffraction peaks at about 2θ = 20° that confirms the capping of magnetite with amorphous sulfonated asphaltene without distortion of magnetite crystals due to functionalization of magnetite with reactive functional groups of sulfonated asphaltene.34 It can also be observed that the presence of a broad intense peak at 35.53° confirms the formation of magnetite nanospheres due to capping with sulfonated asphaltene.35
The concentration of magnetite encapsulated into asphaltene colloid nanoparticles can be determined from TGA as illustrated from thermograms represented in Fig. 3a and b. It was previously reported36 that magnetite lost approximately 8% (wt%) from its weight due to the presence of bound water and functionalization of magnetite surfaces with hydroxyl groups. In the present work, it was found from Fig. 3a and b that magnetite nanoparticles lost 4 and 8 wt%, at a temperature ranging from 80 to 150 °C, from their initial weights when KI and Na2SO3 were used to form magnetite. This observation indicates that more hydroxyl groups were functionalized on the magnetite surfaces when Na2SO3 was used to form magnetite as confirmed from the FTIR spectrum (Fig. 1b and c). Moreover, the surface of magnetite can be easily encapsulated with sulfonated asphaltene when KI was used to form magnetite nanoparticles. The asphaltene begins to degrade at 300 °C (Fig. 3a and b) followed by a significant weight loss between 450 °C and 550 °C. The thermal degradation and pyrolysis of asphaltene are similar to the data reported for modification of asphaltene.37 The magnetite content, determined at 800 °C, are 68.5 and 48% when KI and Na2SO3 reagents are used to form magnetite nanoparticles, respectively. This means that the magnetite content increased inside sulfonated asphaltene when their surfaces contain less hydroxyl groups on their surfaces. These data confirmed from the results obtained from FTIR analysis (Fig. 1a–c).
The particle size diameter and their distribution were determined from DLS measurements as represented in Fig. 5a–c. The data showed that the sulfonated asphaltene was dispersed in water as a colloid with an average diameter of 1075 nm and polydispersity index (PDI) of 0.377. The magnetites coated with sulfonated asphaltene have considerably larger diameters than that determined from TEM data which referred to the inclusion of regions of agglomerations. It was also noticed that the PDI increased with the formation of magnetite nanoparticles using Na2SO3 instead of the KI reagent. Moreover, the size of agglomerates decreased for magnetite capped with sulfonated asphaltene in the presence of KI as the reagent to form magnetite nanoparticles. It was previously reported that poor control of shape and particle size distribution are drawbacks of magnetite nanoparticles prepared using the aqueous coprecipitation method.40 The distribution width is still in an acceptable range in this work when compared with reported coprecipitation methods. The zeta potential measurements represented in Fig. 6a and b confirm the more negative values for the zeta potential of magnetite prepared in the presence of KI than that prepared in the presence of Na2SO3. The zeta potential of magnetite prepared in the presence of KI and in the presence of Na2SO3 are −7.37 and −20.26 respectively which confirms the high content of SAS-MPNS more than that prepared in the presence of KI as confirmed from FTIR and TGA data.
Magnetic properties of iron oxide nanoparticles are important parameters that affect their environment applications. In this respect, there are three different parameters based on saturation magnetization (Ms), coercive force (Hc) and magnetic remanence (Mr) used to determine the magnetic properties of particles. The Ms, Hc and Mr reflect the magnetizability of magnetic materials, the ability of magnetic particles to retain magnetization and the remaining magnetization of magnetic materials after removing an external magnetic field. These parameters were determined from the magnetic hysteresis loop which characterizes the response ability (magnetization, M) of magnetic materials to an external magnetic field (denoted by the magnetic field strength, H). In this work, the magnetic hysteresis loop of SAS-MPs was measured at room temperature by a vibrating sampling magnetometer (VSM) and represented in Fig. 7a and b. Moreover, the Ms, Hc, Mr and squareness ratio (Mr/Ms) values of SAS-MPs were determined and listed in Table 1. The data represented in Fig. 7 and Table 1 showed that SAS-MPs have low Ms values compared to bulk magnetite values that ranged from 75 to 92 emu g−1.41 The magnetization curve confirms the low values of Hc, Mr and the squareness ratio (Mr/Ms) which indicates the absence of remanence or coercivity at room temperature, and suggests the superparamagnetic characteristics of the prepared samples. It can also be observed that the Ms values of SAS-MPs were decreased by increasing the content of SAS capped on Fe3O4 nanoparticles. This means that the higher concentration of magnetite increases the Ms value and reduces the interparticle spacing due to the presence of more intense interactions between particles.42 It was also reported that the magnetic materials have superparamagnetic behaviour when their size decreases below the critical value, generally around 20 nm.42 In this work, although the formed magnetite nanoclusters have sizes above 20 nm as determined from DLS measurements (Fig. 5) the particles showed superparamagnetic rather than ferromagnetic characteristics. This can be attributed to the formation of nano-chain clusters that resist the transition from superparamagnetism to ferromagnetism.43,44 The superparamagnetism of the prepared SAS-MPs supports the application of these materials as oil spill collectors after dispersion in an oil layer followed by application of an external magnetic field.
| Sample | Ms (emu g−1) | Mr (emu g−1) | Mr/Ms | Hc (Oersted; Oe) | 
|---|---|---|---|---|
| SAS-MPKI | 58.3 | 0.0085 | 0.00014 | 3.469 | 
| SAS-MPNS | 43.2 | 0.0170 | 0.00039 | 5.17 | 
| Sample | Contact angle of crude oil dispersion | Contact angle of ethanol dispersion | CE% at different ratios | |||
|---|---|---|---|---|---|---|
| 1 | 10 | 25 | 50 | |||
| SAS-MPKI | 98 ± 4 | 18.5 ± 3 | 92 | 90 | 88 | 80 | 
| SAS-MPNS | 110 ± 3 | 29.3 ± 2 | 98 | 94 | 90 | 85 | 
The crude oil collection efficiency (CE%) of SAS-MPNS and SAS-MPKI as oil spill collectors for Arabian heavy crude oil at different magnetic materials to crude oil ratios (1![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) :
:![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) 1 to 1
1 to 1![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) :
:![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) 50) was determined and listed in Table 2. The photos of oil spill collection by applying an external magnetic field are represented in Fig. 9. The data listed in Table 2 indicate that the best magnetite to crude oil ratio of 1
50) was determined and listed in Table 2. The photos of oil spill collection by applying an external magnetic field are represented in Fig. 9. The data listed in Table 2 indicate that the best magnetite to crude oil ratio of 1![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) :
:![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) 25 succeeded to remove 90% of crude oil, which means that each gram of SAS-MPNS and SAS-MPKI is able to remove around 22.5 g of the heavy crude oil from the water. This value is very high when compared with the maghemite composite which collects 10 g of crude oil per g of magnetic materials.22–24,45 These results indicate also that the increase of the magnetite oil ratio to 1
25 succeeded to remove 90% of crude oil, which means that each gram of SAS-MPNS and SAS-MPKI is able to remove around 22.5 g of the heavy crude oil from the water. This value is very high when compared with the maghemite composite which collects 10 g of crude oil per g of magnetic materials.22–24,45 These results indicate also that the increase of the magnetite oil ratio to 1![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) :
:![[thin space (1/6-em)]](https://www.rsc.org/images/entities/char_2009.gif) 1 was not effective to collect crude oil due to aggregation of magnetite clusters that affect the magnetic attraction between the magnetic particles and the magnet. It was also found that the presence of asphaltene and magnetite in SAS-MPNS and SAS-MPKI increases the removal efficiency of the oil from the water due to the larger dispersion of the prepared materials in heavy crude oil. The high dispersion of magnetite and the larger magnetic attraction of SAS-MPNS and SAS-MPKI are responsible for the formation of a strongly bonded network, which acts as a trap for crude oil. Therefore, the oil removal collection efficiency can be improved by increasing the hydrophobicity of magnetite nanomaterials.
1 was not effective to collect crude oil due to aggregation of magnetite clusters that affect the magnetic attraction between the magnetic particles and the magnet. It was also found that the presence of asphaltene and magnetite in SAS-MPNS and SAS-MPKI increases the removal efficiency of the oil from the water due to the larger dispersion of the prepared materials in heavy crude oil. The high dispersion of magnetite and the larger magnetic attraction of SAS-MPNS and SAS-MPKI are responsible for the formation of a strongly bonded network, which acts as a trap for crude oil. Therefore, the oil removal collection efficiency can be improved by increasing the hydrophobicity of magnetite nanomaterials.
|  | ||
| Fig. 9 Oil collector photos of SAS-MPKI (a) blank crude oil, (b) application of magnetic material and (c) collection of oil by an external magnetic field. | ||
Finally the feasibility study showed that the cost for preparing 1 kg of magnetic materials based on SAS-MPNS was 2 US $ including the material and production costs (25% from material cost). Moreover, the yield on a semi-pilot scale was 95%. This mean that the cost for collection of 1 crude oil barrel was 12 US $ based on CE% of the effective magnetic material crude oil ratio (25 as listed in Table 2). Moreover, depending on the thickness of crude oil, the total volume of crude oil can be estimated, and it was found that 1 kg of magnetic materials can recover 60 m3 of crude oil spill with a thickness of 1 cm. The application of the magnetic material to collect the crude oil spill has great advantages over other methods to clean-up the oil spill in which the crude oil was collected and reused without loss in water through the use of oil spill dispersants that pollute the water. Moreover, the recovery of magnetic materials and using a predominant external magnet requires more research work to apply these materials in offshore and onshore oil spill fields.
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