The need may arise to be able to simulate the migration of groundwater nanoparticles through the ground. Transportation velocities of nanoparticles are different from that of water and depend on many processes that occur during migration. Unstable nanoparticles, such as zero-valent iron nanoparticles, are especially slowed down by aggregation between them. The aggregation occurs when attracting forces outweigh repulsive forces between the particles. In the case of iron nanoparticles that are used for remediation, magnetic forces between particles contribute to attractive forces and nanoparticles aggregate rapidly. This paper describes the addition of attractive magnetic forces and repulsive electrostatic forces between particles (by ‘particle’, we mean both single nanoparticles and created aggregates) into a basic model of aggregation which is commonly used. This model is created on the basis of the flow of particles in the proximity of observed particles that gives the rate of aggregation of the observed particle. By using a limit distance that has been described in our previous work, the flow of particles around one particle is observed in larger spacing between the particles. Attractive magnetic forces between particles draw the particles into closer proximity and result in aggregation. This model fits more closely with rapid aggregation which occurs between magnetic nanoparticles.

Keywords

Magnetic nanoparticlesAggregationMass transport coefficientLimit distance

Background

There are a lot of types of nanoparticles and colloidal particles in groundwater [1]. Some of them are formed naturally, others are generated synthetically and put into the ground by humans. Not only is the reactivity of particles important, but also their migration properties are examined. For example, natural bentonite colloids are released as a consequence of bentonite disposal of radioactive wastes and could carry adsorbed radionuclides in groundwater through granite [2, 3]. Zero-valent iron nanoparticles are produced [4–6] and injected into the ground. Iron nanoparticles are able to migrate in groundwater through contaminated areas and remediate the polluted soils and water [7]. In the first case, the migration possibility is unwelcome. In the second case, the better the migration, the more effective of the remediation. That is why a simulation of the migration of nanoparticles might be desirable. To simulate the migration of nanoparticles, the coefficient of transport retardation of the nanoparticles is needed. The coefficient represents the possible reduction in the rate of nanoparticle migration compared with nanoparticles with similar properties. The number of nanoparticles with similar properties changes over time due to aggregation and it influences the results of the migration experiments. A dynamic model of aggregation has to be included in the simulation programme of nanoparticle transport in flowing water. That is why mass transport coefficients are needed. The coefficients represent the frequency of nanoparticle collisions [8, 9].

A commonly used model for mass transport coefficients [10, 11] in describing aggregation is based on the collisions among nanoparticles caused by heat fluctuation, the velocity gradient of the water in which the nanoparticles are suspended and the different velocities of sedimentation of nanoparticles of varying size. This model does not include the decrease in the rate of aggregation due to repulsive electrostatic forces which occurs due to the electric double layer which builds up on nanoparticle surfaces [12]. Further, in the case of magnetic nanoparticles, the aggregation rate is rapidly increased due to the attractive magnetic forces between nanoparticles [4, 13–16]. That is the reason why the model of aggregation has been expanded, enabling a more accurate model of aggregation of iron nanoparticles in water to be achieved. The paper describes the extension of the mass transport coefficients by the attractive magnetic forces and repulsive electrostatic forces between the nanoparticles.

Methods

A model of nanoparticle aggregation

Particles aggregate easily in groundwater. They create clumps of particles up to the size of several micrometres [15] that cohere and reduce the ability of particles to migrate through the pores on the ground. The aggregation of the particles is caused by processes that generally occur during particle migration. The reduction in mobility can be formulated by a rate of aggregation given by mass transport coefficients β (m^{3}s^{-1}) [9, 10]. The coefficients give a probability P_{ij} for the creation of an aggregate from particle i and particle j with concentrations n_{i}, n_{j} of particles i, j, respectively (Equation 1). Particle i means the aggregate is created from i elementary nanoparticles.

The coefficient (Equation 2) is given by the sum of mass transport coefficients of Brownian diffusion ${\beta}_{\text{ij}}^{1}$, velocity gradient ${\beta}_{\text{ij}}^{2}$ and sedimentation ${\beta}_{\text{ij}}^{3}$. The concept is adopted from [10].

In the case of small nanoparticles, temperature fluctuation of particles has a significant effect on particle aggregation [17]. Brownian diffusion causes a random movement of the particles and it facilitates aggregation. The mass transport coefficient for the Brownian diffusion [10] is

where k_{B}stands for Boltzmann constant, T denotes the absolute temperature, η is the viscosity of the medium, and d_{i}is the diameter of the particle i.

Another process causing aggregation is the drifting of nanoparticles in water. Water flowing through a pore of soil has a velocity profile. In the middle of the pore, the velocity of water is highest. Since the particles have different velocities, according to their location in the flow, the particles can move close together and create an aggregate. The mass transport coefficient for the velocity gradients of particles [10] is

where G is the average velocity gradient in a pore.

Particles settle due to gravitational forces. The velocity of the sedimentation varies for different aggregates depending on their size, so particles can move closer together and aggregate. The mass transport coefficient for the sedimentation [10] is

where g is the acceleration due to gravity, ϱ is the density of the medium, and ϱ pis the density of the aggregating particles.

The magnetic properties of nanoparticles

Because of the composition of nanoparticles, every nanoparticle has a non-zero vector of magnetization. According to [15], TODA iron nanoparticles produced by the Japanese company Toda Kogyo Corp. (Hiroshima, Japan) [5], with diameter of 40 nm have saturation magnetization 570 kA/m. This is the value for a substance composed of nanoparticles containing 14.3% of Fe^{0} and 85.7% of Fe_{3}O_{4}. We use these data for our model. Therefore, we assume the same size magnetization vector for all nanoparticles.

Our model of a magnetic field around an iron nanoparticle is based on the model of the magnetic field around a magnet described in [18]. The electromagnetic potential in the point r near a permanent magnet of volume V is equal to

where M is the magnetization vector at the point dV, the vector R is the difference between source of the magnetic field dV and the point r, R is the length of R.

The intensity of the magnetic field H can be subsequently computed as

Finally, the magnetic force between the source of the intensity of magnetic field H and a permanent magnet of volume $\stackrel{~}{V}$ with a magnetization vector M_{0} at the point r is equal to

In our previous work [19], the scalar potential of the magnetic field around one homogeneous spherical iron nanoparticle with radius a located at the point (0,0,0) was derived as follows:

where a is the radius of the nanoparticle, and (x_{1},x_{2},x_{3}) are the coordinates of the point r. Here, the direction of the magnetization vector M is set towards x_{3}, and M is the magnitude of the vector M.

From Equations 7 and 8, the analytical computation of the magnetic force between two iron nanoparticles can be obtained. Since nanoparticles aggregate, the magnetic force between aggregates must be derived. One aggregate can be composed of millions of nanoparticles. It would be time-consuming and very difficult to analytically compute all these forces. As a consequence, the forces are computed numerically, either as a sum of the magnetic forces between every nanoparticle in one aggregate with every nanoparticle in the second aggregate

where $\stackrel{~}{V}=\frac{4}{3}\Pi {a}^{3}$ is the volume of a nanoparticle, r_{2j} is the location of the centre of the j-th nanoparticle in the second aggregate, M_{2j} is the magnetization vector of the j-th nanoparticle in the second aggregate, M_{1A} and M_{2A} are the averaged magnetization vectors (Equation 12) of the first and the second aggregate respectively, and ${V}_{2}=\sqrt[3]{{n}_{2}}a$ is the volume of the second aggregate.

The averaged aggregate is a big homogeneous particle with its direction of magnetization vectors M_{A} which is computed as a vector sum of the magnetization vectors of all nanoparticles in the aggregate M_{A} and computed as an average of the sizes of all nanoparticles divided by the number of nanoparticles in the aggregate n.

When particles aggregate due to magnetic forces, the rate of aggregation depends on the magnetization vectors of the aggregating particles and on the distance between the particles. The rate of aggregation changes with the changing number of nanoparticles within the aggregates, that is, the changing scale of the structure by order. The model which has been chosen for the structure of an aggregate is a sphere with randomly located nanoparticles within the aggregate, either with random directions of magnetization vectors for every nanoparticle; or with the same direction of magnetization vectors for all nanoparticles in the aggregate. Aggregate structures were assessed in previous work [21]. A more accurate assessment of the most probable structure of an aggregate was performed for this paper in section ‘The structure of an aggregate based on interaction energy’.

The electrostatic properties of nanoparticles

In an electrolyte, a surface charge builds up on the nanoparticle surface. The surface charge depends on its zeta potential (see e.g. [22]) which is measurable. The zeta potential strongly depends on the pH of the water. The results of this dependence were measured using the Malvern ZetaSizer (Malvern Instruments Inc, Malvern, Worcestershire, UK) as published in [19]. From the zeta potential, the surface potential can be computed, based on the electrical double layer [23, 24]

where σ is the surface charge density of the particle, c is the molar electrolyte concentration, R_{g} is the molar gas constant, F is Faraday’s constant, Z is the charge number and ζ is the electrostatic potential. The electrostatic force between two particles is equal to

where D is the distance between the particles i and j. The electrostatic forces repel nanoparticles with the same polarity and cause a reduction in the rate of aggregation. Inclusion of the dependence is done in section ‘The inclusion of the limit distance into mass transport coefficients’.

The limit distance

The effect of magnetic forces on the rate of aggregation was assessed by one parameter - the limit distance L_{D}. This dimension expresses the range of magnetic forces between particles. The definition of this parameter is as follows: this is the distance from centre of an aggregate up to which attractive magnetic forces cause the aggregation between the aggregate and a particle placed in this range. Hence, in a range larger than the limit distance, other forces outweigh the magnetic forces (Figure 1). The limit distance L_{D} can be defined as the distance of the point in which gravitation F_{g} and magnetic forces F_{mg} effecting on the aggregate are equal

The magnetic force between two single domain magnetic nanoparticles falls by the power of 4. In the case of aggregates, the fall depends on the structure of the aggregates and iteration of limit distance computation is needed [20].

When including electrostatic forces, we define the limit distance as the distance where the repulsive magnetic forces is equal to the sum of attractive forces F_{mg} and F_{C}. As the effect of electrostatic forces falls by the power of 2, electrostatic forces can be included into the equilibrium of force in the following way [20]

The values of magnetization vector and surface charge were selected as follows: M=570 kA/m; σ=2.5×10^{−5} C/m^{2}. We used these selected values for all the computations of the interaction energies and mass transport coefficients.

Simulation software

All the computations of magnetic forces, limit distance, electrostatic forces and mass transport coefficients were performed using Matlab R2009a software (MathWorks Inc, Natick, MA, USA). The computation was carried out for different sizes of aggregates i and j, mostly varying in the order of the number of nanoparticles that the aggregates were composed of. The magnetic forces between two aggregates were computed either by summation of the magnetic force between every nanoparticle in the first aggregate and every nanoparticle in the second aggregate (when the ratio L_{D}/R_{0} expresses distance between the aggregates was lower than 15 [20]), or by the averaging of the first and second aggregates. Values for the magnetization vector and surface charge were selected in the following way: M=570 kA/m; σ=2.5×10^{−5} C/m^{2}. For the velocity gradient, we chose the dimensionless value 50. We used these selected values for all the computations of the interaction energies and mass transport coefficients.

Results and discussion

The structure of an aggregate based on interaction energy

To assess the most probable structures of aggregates, one can compute an interaction energy E between the nanoparticles which make up the aggregate, according to [25]

$E=-\mathbf{m}\xb7\mathbf{B}.$

(20)

This is the potential energy of the magnetic moment m in the externally produced magnetic field B. Again, we assume the same magnetization vectors for all nanoparticles in the aggregates with value 570 kA/m [15]. Positive interaction energy means repulsion of the magnetic moment from the magnetic field of another magnetic moment; negative interaction energy means attraction of the dipoles. By summation of the interaction energies between every two nanoparticles in an aggregate, one can deduct the probability of stability of the different structures of the aggregates (the higher the negative interaction energy, the higher the probability of the structure of the aggregate).

The results of interaction energies are shown in Figure 2. The computed interaction energies are displayed for different structures of aggregates (according to the schemes: Figures 3, 4, 5, 6). The Figure 2 is shown using a logarithmic scale. The exact values of interaction energies for different structures of aggregate (Figures 3, 4, 5, 6) and the different numbers of nanoparticles making up the aggregates are in Table 1. Not the absolute values but the comparison between the values of the different structures is relevant. According to Figure 2, the most probable structure of aggregates for the small aggregates are chains and for the bigger aggregates, spherical clusters with the same direction of magnetization vectors of the nanoparticles which make up the aggregate.

Table 1

Interaction energies of different structures of aggregates

Number of nanoparticles [1]

Structure

Energy/μ (eV)

2

Chain

273

3

Chain

588

8

Cube

903

8

Sphere

1,449

8

Circle

2,184

8

Chain

2,688

27

Chain

3,780

27

Sphere

8,400

29

Cube

8,400

343

Cube

56,700

343

Chain

109,200

343

Sphere

184,800

Computed interaction energies divided by the permittivity constant for different structures of aggregates (according to the diagrams in Figures 3, 4,5,6) and for different numbers of nanoparticles within the aggregates.

In their research, Phenrat et al. [15], aggregates of nanoscale zero-valent iron particles were measured using dynamic light scattering, optical microscopy and sedimentation measurements. According to their results, firstly, the nanoparticles created clusters and subsequently, these aggregates assemble themselves into fractal, chain-like clusters. We presume that it was because of the high concentration of nanoparticles that they used, and the very fast aggregation, first into chains and then into clusters, which lead to the measurement of only larger clusters in [15]. Our presumption that with larger numbers of nanoparticles, spherical cluster is created which leads to the supposition that at very high concentrations of particles, spherically structured aggregates only attach to each other, without changing their structure. This corresponds to the observations of Phenrat et al. [15]: in high concentrations, first nanoparticles aggregate into clusters, then the created clusters aggregate into pairs or triplets, and finally into chain-like fractal aggregates.

The inclusion of the limit distance into mass transport coefficients

The basic model of aggregation as given in the section, ‘A model of nanoparticle aggregation’, indicates the rate of aggregation caused by the collision of particles (in proximity, attractive forces outweigh the repulsive ones). We established a limit distance in which attractive forces outweigh the repulsive ones. The magnetic forces attract particles closer to each other and then they aggregate due to attractive van der Waals forces.

Mass transport coefficients (in Equations 3, 4, and 5) were derived on the basis of the flux of nanoparticles through an observed volume or circular area around a particle. The area had a radius equal to sum of the radii of both particles. That means that the particles collide and aggregate. According to our supposition, the particles do not have to be in proximity to aggregate when attractive magnetic forces are acting between them. Therefore, the mass transport coefficients are computed as flux through the spherical or circular area around a particle with a diameter equal to the limit distance:

where ${\beta}_{\text{ij}}^{1,\text{mg}}$, ${\beta}_{\text{ij}}^{2,\text{mg}}$, and ${\beta}_{\text{ij}}^{3,\text{mg}}$, stand for the mass transport coefficient of Brownian motion, the velocity gradient, and sedimentation respectively, with the inclusion of magnetic forces between particles. The results of this change in mass transport coefficients are discussed in the next section - ‘A comparison of the rate of aggregation with and without the effect of electrostatic and magnetic forces’.

A comparison of the rate of aggregation with and without the effect of electrostatic and magnetic forces

The comparison was carried out using an extreme case with a spherical aggregate structure with the same direction of magnetization vectors of all nanoparticles within the aggregates. The aggregation is highest in this case because attractive magnetic forces attract the aggregates and the rate of aggregation is significantly higher (Figure 7). Table 2 contains a comparison of mass transport coefficients computed by primary model, mass transport coefficients computed in distance L_{D}including magnetic forces and mass transport coefficients computed in distance L_{D}including both magnetic and electrostatic forces. The computation of L_{D}was performed by averaging the magnetic forces for particles with ratio L_{D}/R_{0} higher than 15; otherwise, the computation of magnetic forces was done accurately by summation (for more information see [20]). The values in Table 2 are computed with values M=570 kA/m; σ=2.5·10^{−5} C/m^{2}; G=50. According to the results in Table 2 for the chosen values of variables, the attractive magnetic forces between iron nanoparticles have a large effect on the rate of aggregation. The mass transport coefficients are much higher and the aggregation probability increases, which corresponds to our expectations.

A comparison of mass transport coefficients computed by the primary model β, mass transport coefficients computed in distance L_{D} including magnetic forces β_{mg}, and mass transport coefficients computed in distance L_{D} including both magnetic forces and electrostatic forces ${\beta}_{\text{mg}}^{\text{el}}$. The β represents the sum of the mass transport coefficients for Brownian motion, velocity gradient and sedimentation. Computation of L_{D} was performed by averaging of the magnetic forces (11) for particles with ratio L_{D}/R_{0} higher than 15; otherwise, the computation of magnetic forces was performed accurately by summation (10) (for more information, see [20]). Results were computed using the following values: M=570 kA/m; σ=2.5×10^{−5} C/m^{2};and G=50.

Discussion

In future work, the system of grouping of particles according to their size will be derived for the new extended mass transport coefficients including electrostatic and magnetic forces. The groups will represent particles with similar transport properties (small particles are easily transportable, large particles remain in the pores in the ground) and a model of aggregation over time will be developed. The model will be compared with the measuring of aggregation of zero-valent iron nanoparticles in time.

Subsequently, the limit distance should be derived for the equilibrium of all forces acting on particles depending on specific conditions.

Conclusions

In the case of magnetic nanoparticles with non-zero surface charges migrating through the ground, a basic model of interaction between nanoparticles described by the probability of collision due to Brownian motion, velocity gradient, and sedimentation is insufficient. In our previous work, we derived the level of effect of repulsive electrostatic forces between the nanoparticles, and we assessed the level of effect of the attractive magnetic forces between magnetic nanoparticles. In this paper, we summarised the findings and included it into an analytical model of collisions between magnetic nanoparticles. Due to attractive magnetic forces, the rate of aggregation is significantly higher, whereas the repulsive electrostatic forces are almost negligible. One can suppose that with other realistic selections of values of magnetization vector or surface charge, this trend would not change dramatically. This modified model of aggregation can better explain the rapid aggregation of zero-valent iron nanoparticles that is observed. This can help with the simulation of the migration of undissolved particles in groundwater.

Declarations

Acknowledgements

This work was supported by the Ministry of Education of the Czech Republic within the project no. 7822 of the Technical University in Liberec and within the research project FR-TI1/456 ‘Development and implementation of the tools additively modulating soil and water bioremediation’ - Programme MPO-TIP supported by the Ministry of Industry and Trade.

Authors’ Affiliations

(1)

Technical University of Liberec, Institute of Novel Technologies and Applied Informatics

References

Kanchana A, Devarajan S, Rathakrishnan Ayyappan S: Green synthesis and characterization of palladium nanoparticles and its conjugates from Solanum trilobatum leaf extract. Nano-Micro Lett 2010, 2(3):169–176.View Article

Alonso U, Missana T: Role of inorganic colloids generated in a high-level deep geological repository in the migration of radionuclides: open questions. J Iberian Geol 2006, 32: 79–94.

Matsunaga T, Nagao S, Ueno T, Takeda S, Amano H, Tkachenko Y: Association of dissolved radionuclides released by the Chernobyl accident with colloidal materials in surface water. Appl Geochem 2004, 19(10):1581–1599. 10.1016/j.apgeochem.2004.02.002View Article

Li L, Fan M, Brown RC, Van Leeuwen JH, Wang J, Wang W, Song Y, Zhang P: Synthesis, properties, and environmental applications of nanoscale iron-based materials: a review. Crit Rev in Environ Sci Technol 2006, 36(5):405–431. 10.1080/10643380600620387View Article

Nurmi JT, Tratnyek PG, Sarathy V, Baer DR, Amonette JE, Pecher K, Wang C, Linehan JC, Matson DW, Penn RL, Driessen MD: Characterization and properties of metallic iron nanoparticles: spectroscopy, electrochemistry, and kinetics. Environ Sci Technol 2005, 39(5):1221–1230. 10.1021/es049190uView Article

Filip J, Zboril R, Schneeweiss O, Zeman J, Cernik M, Kvapil P, Otyepka M: Environmental applications of chemically pure natural ferrihydrite. Environ Sci Technol 2007, 41(12):4367–4374. 10.1021/es062312tView Article

Zhang WX: Nanoscale iron particles for environmental remediation: an overview. J Nanopart Res 2003, 5(3):323–332. 10.1023/A:1025520116015View Article

Camp TR: Velocity Gradients in Internal Work in Fluid Motion. Cambridge: MIT; 1943.

Smoluchowski M: Versuch einer mathematischen Theorie der Koagulationskinetik kolloider Lösungen. Z Phys Chem 1917, 92: 129–168.

Buffle J, van Leeuwen HP: Environmental Particles. Chelsea: Lewis Publishers; 1992.

Somasundaran P, Runkana V: Modeling flocculation of colloidal mineral suspensions using population balances. Int J Mineral Process 2003, 72(1–4):33–55.View Article

Sun Y, Li Xq, Cao J, Zhang Wx, Wang HP: Characterization of zero-valent iron nanoparticles. Adv Colloid Interface Sci 2006, 120(1–3):47–56.View Article

Horak D, Petrovsky E, Kapicka A, Frederichs T: Synthesis and characterization of magnetic poly(glycidyl methacrylate) microspheres. J Magn Magn Mater 2007, 311(2):500–506. 10.1016/j.jmmm.2006.08.006View Article

Masheva V, Grigorova M, Nihtianova D, Schmidt JE, Mikhov M: Magnetization processes of small gamma-Fe2O3 particles in non-magnetic matrix. J Phys D: Appl Phys 1999, 32(14):1595–1599. 10.1088/0022-3727/32/14/308View Article

Phenrat T, Saleh N, Sirk K, Tilton RD, Lowry GV: Aggregation and sedimentation of aqueous nanoscale zerovalent iron dispersions. Environ Sci Technol 2007, 41: 284–290. 10.1021/es061349aView Article

Wang J, Wei LM, Liu P, Wei H, Zhang YF: Synthesis of Ni nanowires via a hydrazine reduction route in aqueous ethanol solutions assisted by external magnetic fields. NanoMicro Lett 2010, 1: 49–52.

Einstein A: On the movement of small particles suspended in stationary liquids required by the molecular-kinetic theory of heat. Annalen der Physik 1905, 17: 549–560.View Article

Votruba V, Muzikar C: Teorie Elektromagnetickeho Pole. Praha: Akademia Karolinum; 1958.

Rosicka D, Sembera J: Assessment of influence of magnetic forces on aggregation of zero-valent iron nanoparticles. Nanoscale Res Lett 2010, 6: 10.

Sembera J, Rosicka D: Computational methods for assessment of magnetic forces between iron nanoparticles and their influence on aggregation. Adv Sci Eng Med 2011, 3(1,2):149–154.View Article

Rosicka D, Sembera J: Influence of structure of iron nanoparticles in aggregates on their magnetic properties. Nanoscale Res Lett 2011, 6: 527. 10.1186/1556-276X-6-527View Article

Stumm W, Morgan JJ: Aquatic Chemistry: Chemical Equilibria and Rates in Natural Waters. New York: Wiley; 1996.

Dzombak DA, Morel FMM: Surface Complexation Modeling: Hydrous Ferric Oxide. 1st edition. New York: Wiley-Interscience; 1990.

Lyklema J: Fundamentals of Interface and Colloid Science. Amsterdam: Academic Press; 2005.

Sedlak B, Stoll I, Man O: Elektrina a magnetismus. Praha: Academia Karolinum; 1993.

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