Suggested Reading
In Lecture 4 we discussed the energies that that control the state of magnetization within ferromagnetic particles. Particles will tend to find a configuration of internal magnetization directions that minimizes the energies (although meta-stable states with local energy minima or LEMs are a possibility). The longevity of a particular magnetization state has to do with the depth of the energy well that the magnetization is in and the energy available for hopping over energy barriers. We discussed a few basic configurations of the remanent magnetic state: uniform magnetization (single domain; SD), flower (F), vortex (V), and multi-domain (MD) states. We also mentioned the case in which thermal energy dominates: superparamagnetic (SP) particles.
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SP particles have sufficient thermal energy to easily overcome the various anisotropy energies; they come into equilibrium with whatever external field they are in within seconds. Particles with domain walls (multi-domain, or MD particles) also have low stability. It is relatively easy to move a wall around within crystals so the domains grow and shrink depending on the external field.
Quasi-uniformly magnetized (SD and F states) particles have a great deal of resistance to changes in the external field because the magnetization vectors have to jump over high energy barriers to change directions within the crystal. These particles require relatively high magnetic fields to overcome the anisotropy energy and change their magnetizations. Finally, vortex state particles are somewhere in between the extremes of uniformly magnetized particles and those with domain walls.
The ease with which particles can be “coerced” into changing their magnetizations in response to external fields can tell us much about the overall stability of the particles and perhaps also something about their ability to carry a magnetic remanence over the long haul. The concepts of long term stability, incorporated in the concept of relaxation time and the response of the magnetic particles to external magnetic fields are therefore linked through the anisotropy energy constant K (see Lecture 4). In this lecture we will discuss the behavior of magnetic particles in response to external magnetic fields.
Magnetic remanence is the magnetization in the absence of an external magnetic field. If we imagine a particle with a single “easy” axis - a so-called “uniaxial” particle, the magnetization in the absence of a magnetic field will be aligned along one of the directions parallel to the easy axis and
, the angle between the magnetic moment m and the easy axis is zero (see Figure 7.1a). But if there is an external field applied at an angle
to the easy axis, there will be a competition between the anisotropy
energy (tending to keep the magnetization parallel to the easy axis) and the interaction energy (tending to line the magnetization up with the external magnetic field). We showed in Lecture 4 that the total magnetic energy density of such a particle is given by:
| (7.1) |
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The magnetic moment of a uniaxial single domain grain will find the angle
that is associated with the minimum total energy (Emin; see Figure 7.2). For low external fields (e.g., 5 mT; Figure 7.2a),
will be closer to the easy axis and for higher external fields (e.g., 30 mT; Figure 7.2b),
will be closer to the applied field direction (
).
When a magnetic field that is large enough to overcome the anisotropy energy is applied in a direction opposite to the magnetization vector, the moment will jump over the energy barrier and stay in the opposite direction when the field is switched off. The field necessary to accomplish this feat is called the flipping field (Bf) (also sometimes the “switching field”). Stoner and Wohlfarth (1948) showed that the flipping field can be found from the condition that dEt/d
= 0 and d2Et/d
2
= 0. We will call this the “flipping condition”. The necessary equations can be found by differentiating Equation 7.1:
| (7.2) |
and again
| (7.3) |
Solving these two equations for B and using trigonometric trickery we get:
| (7.4) |
where t = tan1 3
. Here we have the derivation for the so-called “intrinsic coercivity” (Bk) when the dominant magnetic anisotropy constant is Ku and
is zero, Bk = 2Ku Ms
(introduced as “coercivity” in Lecture 4 ).
Using the parameters for magnetite (Ku = 1.4 x 104 Jm-3 and Ms = 4.8 x 105 Am-1) we get Bf = 58 mT. We plot the behavior of Equations 7.1 - 7.3 in Figure 7.3. We see that the minimum in Et occurs at an angle of
= 180o and that the first and second derivatives satisfy the flipping criterion by having a common zero crossing. There is no other field for which this is true (see, e.g., the case of a 30 mT field in Figure 7.4).
We show the flipping field Bf versus
in Figure 7.5. For
parallel to the easy axis (zero), Bf is 62 mT as we found before. Bf drops steadily as the angle between the field and the easy axis increases, until an angle of 45o when Bf
starts to increase again. Bf is undefined when
= 90o, so when the field is applied at right angles to the easy axis, there is no field sufficient to flip the moment.
When a single domain, uniaxial particle is subjected to an increasing magnetic field the magnetization is gradually drawn into the direction of the applied field. If the flipping condition is not met, then the magnetization will return to the original direction when the magnetic field is removed. If the flipping condition is met, then the magnetization undergoes an irreversible change and will be in the opposite direction when the magnetic field is removed.
Now let us consider what happens to single particles when subjected to applied fields in the cycle known as the “hysteresis loop”. Measurements of magnetic moment m as a function of applied field B are made on a variety of instruments, such as a vibrating sample magnetometer (VSM) or alternating gradient force magnetometer (AGFM; see Figure 7.6). In the AGFM, a sample is placed on a thin stalk between pole pieces of a large magnet. There is a probe mounted behind the sample that measures the applied magnetic field. There are small coils on the pole pieces that modulate the gradient of the applied magnetic field (hence alternating gradient force). The sample vibrates in response to changing magnetic fields and the amplitude of the vibration
is proportional to the moment in the axis of the applied field direction. The vibration of the sample stalk is measured and calibrated in terms of magnetic moment. The magnetometer is only sensitive to the induced component of m parallel to the applied field Ho, which is m|| = mcos
(because the off axis terms are squared and very small, hence can be neglected.) In the hysteresis experiment, therefore, the moment parallel to the field m|| is measured as a function
of applied field B.
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Imagine a single domain particle with uniaxial anisotropy. Because the particle is single domain, the magnetization is at saturation and, in the absence of an applied field is constrained to lie along the easy axis. Now suppose we apply a magnetic field in the opposite direction (see track # 1 in Figure 7.7). When B reaches Bf in magnitude, the magnetization flips to the opposite direction (track #2 in Figure 7.7) and will not change regardless of how high the field goes. The field then is decreased to zero and then increased along track #3 in Figure 7.7 until Bf is reached again. The magnetization then flips back to the original direction (track #4 in Figure 7.7).
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Applying fields at arbitrary angles to the easy axis results in loops of various shapes (see Figure 7.8a). As
approaches 90o, the loops become thinner. Remember that the flipping fields for
= 22o and
= 70o
are similar (see Figure 7.5) and are lower than that from
= 0o, but the flipping field for
= 90o is infinite, so that “loop” is closed and completely reversible.
In rocks with an assemblage of randomly oriented particles with uniaxial anisotropy, we would measure the sum of all the millions of tiny individual loops. A specimen from such a rock would yield a loop similar to that shown in Figure 7.8b. If the field is first increased to +Bmax, all the magnetizations are drawn into the field direction and the net magnetization is equal to the sum of all the individual magnetizations and is the saturation magnetization Ms. When the field is reduced to zero, the moments relax back to their individual easy axes, many of which are at a high angle to the direction of the saturating field and cancel each other out. The net remanence after saturation is termed the saturation remanent magnetization Mr. For a random assemblage of single domain uniaxial particles, Mr/Ms = 0.5. The field necessary to reduce the net moment to zero is defined as the coercive field Bc. The coercivity of remanence Bcr is defined as the magnetic field required to irreversibliy flip half the magnetic moments (so the net remanence after application of -Bcr to a saturation remanence is 0). Bcr is always greater than or equal to Bc and the ratio Bcr/Bc for our random assemblage of uniaxial SD particles is 1.09 (Wohlfarth, 1958).
If one were to switch off the field at the point labeled Bcr* in Figure 7.8, the magnetization would follow the dashed line and intersect the origin. For single domain grains, the dashed curve is parallel to the lower curve. So if one only measured the outer loop, one could estimate the coercivity of remanence by simply tracing the curve parallel to the lower curve (dashed line) from the origin to the point of intersection with the upper curve (circled in Figure 7.8). This parameter is here called Bcr*. As we will learn in Lecture 8 , this estimate is only valid for single domain grains.
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In the case of equant grains of magnetite for which magnetocrystalline anisotropy dominates, there are four easy axes, instead of two as in the uniaxial case. The maximum angle
between an easy axis and an applied field direction is 55o. Hence there is no individual loop that goes through the origin (see Figure 7.9). A random assemblage of particles with cubic anisotropy will therefore have a much higher saturation remanence. In fact, the theoretical ratio of Mr/Ms for
such an assemblage is 0.87, as opposed to 0.5 for the uniaxial case (Joffe and Heuberger, 1974). Other theoretical predictions for hysteresis parameters are summarized in Table 7.1.
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In superparamagnetic (SP) particles, Et is balanced by thermal energy kT. This behavior can be modelled using statistical mechanics in a manner similar to that derived for paramagnetic grains in Lecture 3 and summarized in the Appendix. In fact,
| (7.5) |
where
= MsBv kT and N is the number of particles of volume v.
Our end result, (Equation 7.5), is the familiar Langevin function from our discussion of paramagnetic behavior (Lecture 3); hence the term “superparamagnetic” for such particles.
The contribution of SP particles for which the Langevin function is valid with given Ms and d is shown in Figure 7.10a. The field at which the population reaches 90% saturation B90 occurs at
~ 10. Assuming particles of magnetite (Ms = 4.8 x 105 A/m) and room temperature (T = 300oK),
B90 can be evaluated as a function of d (see Figure 7.10b). Because of its inverse cubic dependence on d, B90 rises sharply with decreasing d and is hundreds of tesla for particles a few nanometers in size, approaching paramagnetic values. The maximum size for SP behavior is rather controversial at the moment, but Tauxe et al. (1996) argue that it is ~ 20 nm.
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Moving domain walls around is much easier than flipping the magnetization of an entire particle coherently. The reason for this is the same as the reason that it is easier to move a rug by lifting up a small wrinkle and pushing that through the rug, than to drag the whole rug by the same amount. Because of the greater ease of changing magnetic moments in MD grains, they have lower coercive fields and saturation remanence is also much lower than for uniformly magnetized particles (see Figure 7.10c). For grains large enough to have many walls (say a few microns), we predict that the grains would have no stability and the loop would be nearly indistinguishable from an SP loop. Yet some large grains have rather large coercivities and remanence ratios. The principle mechanism invoked to explain the unexpected stability of some grains is that wall energy is not uniform through-out the grain; some places have substantially lower energies than others and walls get “stuck” in these local energy minima (LEMs).
There are several possible causes of variability in wall energy within a magnetic grain, for example, voids, lattice dislocations, stress, etc. The effect of voids is perhaps the easiest to visualize, so we will consider voids as an example of why wall energy varies as a function of position within the grain. We show a particle with lamellar domain structure and several voids in Figure 7.11. When the void occurs within a uniformly magnetized domain (left of figure), the void sets up a demagnetizing field as a result of the free poles on the surface of the void. There is therefore, a self-energy associated with the void. When the void is traversed by a wall, the free pole area is reduced, reducing the demagnetizing field and the associated self-energy. Therefore, the energy of the void is reduced by having a wall bisect it. Furthermore, the energy of the wall is also reduced, because the area of the wall in which magnetization vectors are tormented by exchange and magnetocrystalline energies is reduced. The wall gets a “free” spot if it bisects a void. The wall energy Ew therefore is lower as a result of the void.
In Figure 7.12, we show a sketch of a hypothetical transect of Ew across a particle. There are four LEMs labelled a-d. Domain walls will distribute themselves through out the grain in order to minimize the net magnetization of the grain and also to try to take advantage of LEMs in wall energy.
Domain walls move in response to external magnetic fields (see Figure 7.13). Starting in the demagnetized state (Figure 7.13a), we apply a magnetic field that increases to saturation (Figure 7.13b). As the field increases, the domain walls move in sudden jerks as each successive local wall energy high is overcome. This process, known as Barkhausen jumps, leads to the stair-step like increases in magnetization (shown in the inset of Figure 7.13). At saturation, all the walls have been flushed out of the crystal and it is uniformly magnetized. When the field decreases again, to say +3 mT (Figure 7.13c), domain walls begin to nucleate, but because the energy of nucleation is larger than the energy of denucleation, the grain is not as effective in cancelling out the net magnetization, hence there is a net saturation remanence (Figure 7.13d). The walls migrate around as a magnetic field is applied in the opposite direction (Figure 7.13e) until there is no net magnetization). The difference in nucleation and denucleation energies was called on by Halgedahl and Fuller (1983) to explain the high stability observed in some large magnetic grains.
Magnetite particles whose remanence states are in a “vortex” structure (see Lecture 4) probably flip using what has been called a “curling” mode. In order to flip its magnetic moment, the particle forms vortices which can zip through the particle. The hysteresis behavior of these particles can be modelled numerically (e.g. Tauxe et al., 2002). Examples of simulations of uniformly distributed assemblages are shown in Figure 7.14.
In Figure 7.14a we show the results from equant particles with widths of about 90 nm. The thin lines are individual loops for a given orientation of the applied field with respect to the crystallographic axes and the average loop is the heavy line. The loop from a uniform assemblage of such particles has a remanence ratio (Mr/Ms) of 0.63 and a coercive field of 14 mT. As mentioned previously, the expected values (Table 7.1) are 0.87 and 10 mT respectively for uniformly magnetized equant (CSD) particles of magnetite, so this flower state assemblage has a magnetization that is “harder”. The lower Mr/Ms ratio stems from the fact that the particles are not at saturation.
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In Figure 7.14b we show a similar set of curves for an assemblage of 70 nm particles with a/b ratios of 2. The remanence ratio of this assemblage is 0.46 and the coercive field is ~38 mT as compared to 0.5 and 69 mT (Table 7.1). These uniaxial, flower state particles therefore have lower coercive fields than expected from a random assemblage of SD grains.
A third example of an assemblage of particles is shown in Figure 7.14c. This is for an assemblage of 115 nm (vortex state) equant particles. The average loop has a squareness of 0.16 and coercive field of 10 mT. Particles with characteristic vortex remanence states therfore have lower coercive fields than SD particles, but higher than a truly MD particle. They also have remanence ratios that are in between SD and MD particles.
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Hysteresis loops can yield a tremendous amount of information yet much of this is lost by simply estimating the set of parameters Mr,Ms,Bcr,Bc,
i,
hf, etc.. Pike et al. (e.g., 1999) popularized the method of Mayergoyz
(1986) or using so-called First Order Reversal Curves or FORCs to represent hysteresis data. In the FORC experiment, a sample is subjected to a saturating field, as in most hysteresis experiments. The field is lowered to some field Ha, then increased again through some value Hb to saturation (see Figure 7.15a). [It is unfortunate that the FORC terminology has chosen to use Ha, yet routinely neglects the necessary
o
to render these field values in tesla...] The magnetization curve between Ha and Hb is a “FORC”. A series of FORCs (see Figure 7.15b) are generated to the desired resolution.
To transform FORC data into some useful form, they are gridded as in the inset in Figure 7.15c. In this example, we take a curve (in red) with its three neighbors on either side (in green), for a smoothing factor of SF = 3. The data in the box are fit with a polynomial surface of the form:
where the ai are fitted coefficients. The coefficient -a6(Ha,Hb) is contoured as in the Figure 7.15b and is a good approximation for the second derivative of the polynomial surface at P (Figure 7.15b). A FORC diagram is the contour plot rotated such that Hc = (Hb -Ha)/2 and Hu = (Ha + Hb)/2. Please note that because Ha < Hb, data are only possible for positive Hc.
Imagine we travel down the descending magnetization curve (dashed line in Figure 7.15a) to a particular field
oHa less than the smallest flipping field in the assemblage. If the particles are single domain, the behavior is reversible and the first FORC will travel back up the descending curve. It is only when |
oHa|
exceeds the flipping field of some of the particles that the FORC will trace a new curve on the inside of the hysteresis loop. In the simple single domain, non-interacting, uniaxial magnetite case, the FORC density in the quadrants where Ha and Hb are of the same sign must be zero. Indeed, FORC densities will only be non-zero for the range of flipping fields because these are the bounds of the flipping field distribution. So the diagram in Figure 7.15c is nearly that of an ideal uniaxial SD distribution.
Consider now the case in which a particle has domain walls. Walls can move much more easily than flipping the moment of an entire grain coherently. In fact, they begin to move in small jumps (from LEM to LEM) as soon as the applied field changes. If a wall nucleates while the field is decreasing and the field is then ramped back up, the magnetization curve will not be reversible, even though the field never changed sign or approached the flipping field for coherent rotation. The resulting FORC for such behavior would have much of the action in the region where Ha is positive. When transformed to Hu and Hc, the diagram will have the highest densities for small Hc but over a range of ±Hu as shown in Figure 7.16.
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FORC diagrams take hours to create while a single hysteresis loop takes minutes. In many cases the the most interesting thing one learns from FORC diagrams is the degree to which there is irreversible behavior when the field is reduced to zero then ramped back up to saturation (see Figure 7.17). Such irreversible behavior in what Yu and Tauxe (2004) call the “Zero FORC” or ZFORC can arise from particle interactions, domain wall jumps or from the formation and destruction of vortex structures in the magnetic grains.
Fabian (2003) defined a parameter called “transient hysteresis” which is the area between the ascending and descending loops of a ZFORC (shaded area in Figure 7.17). This is defined as:
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Transient hysteresis is thought to result from self demagnetization, for example shifting of domain walls or the formation and destruction of vortex structures. An example of what might be causing transient hysteresis at the macro scale is shown for micromagnetic modelling of a single particle in Figure 7.18 (Yu and Tauxe, 2004). The ZFORC starts and ends at saturation. On the descending loop, a vortex structure suddenly forms, at the point on the hysteresis loop labelled a), sharply reducing the magnetization. The magnetization state just before the jump is shown as snapshot labelled “descending branch”. The vortex remains along the ascending branch until much higher fields (see snapshot labelled “ascending branch”). The irreversible behavior of millions of particles with different sizes and shapes leads to the total transient hysteresis of the macro specimen. In general, Tauxe and Yu (2004) showed that the larger the particle, the greater the transient hysteresis, until truly multi-domain behavior essentially closed the loop, precluding the observation of TH (or of a FORC diagram for that matter).
Much of the character of hysteresis loops is frequently attributed to interaction between particles, something that is extremely difficult to model and up until recently impossible to observe. A new technique for imaging of both the composition and the magnetization of particles on a nanoscale (e.g., Harrison et al. 2002) allows a glimpse at the magnetization structure of tiny, interacting particles. In Figure 7.19, we show an example of the mapping of iron and titanium (top panel) and the magnetic structure inferred from “off-axis electron holography” from Harrison et al. (2002). The figure shows both uniform magnetization and vortex structures within particles and super vortex structures from magnetostratic interaction fields between particles.
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The derivation of superparamagnetism follows closely that of paramagnetism whereby the probability of finding a magnetization vector an angle
away from the direction of the applied field is give by:
| (A1) |
The total magnetization contributed by the N moments is:
| (A2) |
Combining ( A1) and ( A2) we get
| (A3) |
and finally
| (A4) |
where
= MsBv kT and N is the number of particles of volume v.
Butler, R. F. (1992), Paleomagnetism: Magnetic Domains to Geologic Terranes, Blackwell Scientific Publications.
Fabian, K. (2003), ‘Some additional parameters to estimate domain state from isothermal magnetization measurements’, Earth and Planetary Science Letters 213(3-4), 337-345.
Halgedahl, S. & Fuller, M. (1983), ‘The dependence of magnetic domain structure upon magnetization state with emphasis upon nucleation as a mechanism for pseudo-single domain behavior’, J. Geophys. Res. 88, 6505-6522.
Joffe, I. & Heuberger, R. (1974), ‘Hysteresis properties of distributions of cubic single-domain ferromagnetic particles’, Phil. Mag. 314, 1051-1059.
Mayergoyz, I. (1986), ‘Mathematical models of hysteresis’, IEEE Trans. Magn. MAG-22, 603-608.
O’Reilly, W. (1984), Rock and Mineral Magnetism, Blackie.
Pike, C. R., Roberts, A. P., Dekkers, M. J. & Verosub, K. L. (2001), ‘An investigation of multi-domain hysteresis mechanisms using FORC diagrams’, Physics of The Earth and Planetary Interiors 126(1-2), 11-25.
Pike, C., Roberts, A. & Verosub, K. (1999), ‘Characterizing interactions in fine magnetic particle systems using first order reversal curves’, J. Appl. Phys. 85, 6660-6667.
Stoner, E, C. & Wohlfarth, W. P. (1948), ‘A mechanism of magnetic hysteresis in heterogeneous alloys’, Phil. Trans. Roy. Soc. Lond. A240, 599-642.
Tauxe, L., Bertram, H. & Seberino, C. (2002), ‘Physical interpretation of hysteresis loops: Micromagnetic modelling of fine particle magnetite’, Geochem., Geophys., Geosyst. 3, DOI 10.1029/ 2001GC000280.
Tauxe, L., Mullender, T. A. T. & Pick, T. (1996), ‘Potbellies, wasp-waists, and superparamagnetism in magnetic hysteresis’, Jour. Geophys. Res. 101, 571-583.
Wohlfarth, E. P. (1958), ‘Relations between different modes of acquisition of the remanent magnetisation of ferromagnetic particles’, J.of App. Phys. 29, 595-596.
Yu, Y. & Tauxe, L. (2004), ‘On the use of magnetic transient hysteresis in paleomagnetism for granulometry’, Geochem., Geophys., Geosyst. 6, Q01H14; doi: 10.1029/2004GC000839.
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