research papers
Analysis of time-of-flight small-angle neutron scattering data on mesoscopic crystals such as magnetic vortex lattices1
aDivision of Synchrotron Radiation Research, Lund University, SE-22100 Lund, Sweden, bHelmholtz-Zentrum Berlin für Materialien und Energie, Hahn-Meitner-Platz 1, D-14109 Berlin, Germany, and cSchool of Physics and Astronomy, University of Birmingham, Birmingham B15 2TT, United Kingdom
*Correspondence e-mail: emma.campillo@sljus.lu.se
Bragg diffracted intensities and q values for crystalline structures with long repeat distances may be obtained by small-angle neutron scattering (SANS) investigations. An account is given of the methods, advantages and disadvantages of obtaining such data by the multichromatic time-of-flight method, compared with the more traditional quasi-monochromatic SANS method. This is illustrated with data obtained from high-magnetic-field measurements on magnetic vortex line lattices in superconductors on the former HFM/EXED instrument at Helmholtz-Zentrum Berlin. The methods have application to other mesoscopic crystalline structures investigated by SANS instruments at pulsed sources.
Keywords: vortex lattices; superconductivity; time-of-flight neutron diffraction; small-angle neutron scattering; SANS.
1. Introduction
Small-angle neutron scattering (SANS) is a very apt technique for measuring large-scale crystalline structures having repeat distances in the tens to thousands of ångströms. et al., 2011), but others include skyrmion lattices (Mühlbauer et al., 2009) and other long-period helical magnetic structures or mesophases formed by nanoparticles in colloidal suspensions (Mühlbauer et al., 2019). Taking the case of Bragg diffraction by vortex lattices, the parameters obtained are the VL structure and spacing and the VL form factors as a function of applied magnetic field and temperature. These data may be analysed in terms of the magnetic and the coherence length of the superconductor. Information about the superconducting energy gap and the nature of the pairing may also be inferred. Traditionally, such measurements have been performed on quasi-monochromatic (Δλ/λ ≃ 10%) SANS instruments, and there has been little published use of the multichromatic time-of-flight (TOF) SANS technique for such measurements (Pautrat et al., 2012; Bannenberg et al., 2018; Li et al., 2019; Campillo, Bartkowiak et al., 2022).
line, or vortex, lattices (VLs) in superconductors are a typical application (EskildsenMany years ago, the Christen formula (Christen et al., 1977) was derived for the quasi-monochromatic case to relate the integrated intensity of a VL Bragg peak at wavevector q [q = (4π/λ)sinθ, where θ is half the scattering angle and λ is the wavelength of the incident radiation] to the magnetic form factor (the spatial Fourier component of the VL magnetic field at that q). Here, we demonstrate how to obtain the same information using TOF SANS. With the increasing availability of pulsed sources, such as the ISIS Neutron and Muon Source (UK), the Spallation Neutron Source (USA), J-PARC (Japan) and soon the European Spallation Source (Sweden), and the reduction in quasi-monochromatic instruments due to the closure of reactor sources, it is important to establish how VL studies may be carried out quantitatively on TOF SANS instruments. The information about VLs is obtained from the integrated intensity, position and q widths of the diffraction spots. The analysis described here may equally be used to obtain crystallographic information about other mesoscopic structures, for example the skyrmions studied by Bannenberg et al. (2018) and Li et al. (2019).
We have carried out several experimental studies (Campillo, Bartkowiak et al., 2022; Campillo, Soda et al., 2022; Cameron et al., 2022) on VLs using the HFM/EXED neutron beamline (no longer in service) at the Helmholtz Zentrum Berlin (Prokhnenko et al., 2015, 2017; Smeibidl et al., 2016). This instrument was a multi-purpose instrument that operated exclusively in TOF mode and had a SANS option. In this paper, we primarily draw on examples from a sample of 98% detwinned YBa2Cu3O7 (Campillo, Bartkowiak et al., 2022) to illustrate our analysis methods. We have also used these methods for high-field VL studies on twinned Y0.85Ca0.15Ba2Cu3O7 (Cameron et al., 2022) crystals and Ba1−xKxFe2As2 (Campillo, Soda et al., 2022). In all three cases, we had results obtained from quasi-monochromatic SANS to compare with. The data reduction on HFM/EXED and subsequent analysis were carried out using the software package Mantid (Arnold et al., 2014).
2. Bragg diffraction in TOF SANS
To generate a VL, a magnetic field must be applied to the superconductor; the
lines then lie parallel to this magnetic field (with vortices of supercurrent around them) and the reciprocal-lattice vectors of the VL are therefore perpendicular to this field. If the magnetic field is aligned nearly parallel to the neutron beam, all of the Bragg reflections from the VL will be experimentally accessible in the SANS geometry.The diffraction condition for a Bragg peak is set by the Bragg equation. In most VL SANS studies using a quasi-monochromatic neutron wavelength, the diffraction condition is met by altering the angle of the sample and magnet together with respect to the incoming neutron beam, and so the measurement is typically referred to as a rocking curve through the Bragg condition. If the relevant diffraction spot is perpendicular to the rotation axis (e.g. a horizontal spot with a vertical rotation axis) then the rocking angle ω moves q perpendicular to the the rocking curve will be centred on the θB, and the intensity integrated over ω and the rocking curve width can be extracted. In the more general case, when the spot is at an angle β to the perpendicular, the rocking will be centred on θB/cosβ; it moves q more slowly through the and the angular width has to be corrected by the `Lorentz factor' cosβ. The width is often reported in terms of angular width but more properly corresponds to a width in the qz direction (z is parallel to the applied field). In the rest of this paper we will use ω to refer to the special case where the rotation axis is perpendicular to the spot.
In the time-of-flight (TOF) case, at a given value of the sample and magnet rotation angle α a range of wavelengths are scattered, and so at each α a range of qz values are sampled. at the appropriate angles by shorter and longer wavelengths therefore corresponds to measuring the signal at different rocking angles in the case of quasi-monochromatic SANS ω (Pautrat et al., 2012). Alternatively, as illustrated schematically in Fig. 1, the neutron wavelength distribution at fixed magnet rotation angle can be regarded as giving the signal over a range of qz. Depending on the range of Bragg angles and the width of the VL rocking curve, it may be necessary to measure in TOF mode at two or three different α values to give complete coverage of the rocking curve.
It is also possible to measure the VL with the field perpendicular to the beam (Laver et al., 2008). In this case the sample has to be rotated so that one of the VL Bragg planes (which are typically 60° apart in this geometry) is at a small angle to the incoming beam (see Fig. 2). In this arrangement, the B direction marked in Fig. 1 corresponds to this Bragg plane and the field direction is perpendicular to the page. This means that the rocking curve or qz width gives information about the orientation of the VL structure around the field direction rather than along B.
3. VL form factor
The VL form factor is the magnitude of a Fourier component of the spatial variation of the magnetic field within the VL. For non-TOF SANS at a neutron wavelength λ, the form factor F(q) for a diffraction spot with wavevector q is related to the integrated intensity I(q) by the following relationship (Christen et al., 1977):
Here, Φ0 (= h/2e, with h the Planck constant and e the electron charge) is the quantum, V is the illuminated sample volume, γ (= 1.91) is the neutron in nuclear magnetons and φ is the neutron (neutrons m−2 s−1) illuminating the sample. The integrated intensity is defined as
where ω is the rocking angle through the diffraction spot. (The angle is measured in radians, around an axis perpendicular to the scattering plane.) I(qx, qy, ω) is the intensity detected at rocking angle ω. This is then summed over the area of the detector containing the diffraction spot, and the integral represents the area under the graph of summed intensity versus qω.
The equivalent equation in TOF mode is obtained by considering the illuminating beam as a distribution φ(λ) over the neutron wavelengths, represented by a histogram with bins of width Δλ centred on wavelengths λj (and corresponding wavevectors kj) having neutron φj = φ(λj)Δλ. This will give rise to a scattered intensity Ij = I(qx, qy, qz, λj)Δλ, with φj appearing in equation (1) and Ij inside the integral in equation (2). Note that Δλ cancels in the ratio Ij/φj, as indeed it does in non-TOF SANS where a single wavelength band is used. However, for a TOF measurement the VL is at a fixed angle to the neutron beam, so a rocking curve measurement is not performed. Instead, as shown in Fig. 1, the distribution of wavelengths corresponds to a range of values of the θB, and hence plays the part of the rocking curve. If the range of wavelengths is not broad enough to cover the whole rocking curve width for a VL, several measurements at different magnet rotation angles may be used; the following analysis applies to each one of these measurements.
To do the TOF equivalent of `integrating over the rocking curve', we have to determine how detector counts translate into q space. We make use of the geometry represented in Fig. 3, where we define the `laboratory' frame, which has the z direction pointing towards the incoming beam.
In the laboratory frame, the scattered q′ = kf − ki. If the magnitude of the neutron wavevectors is kj, then we may write the components of q′ as
This is q′ in the laboratory frame; we wish to have q in the sample/magnet frame, which is rotated from the laboratory frame by a small angle α about the vertical y axis. If the diffraction spot is perpendicular to the magnet rotation axis then α is equivalent to ω, and α = ω = θB brings the spot into the diffraction condition. Otherwise α > θB is required. In our experiments the magnet rotation axis was vertical and the spots were at ∼45° to the horizontal, so α ≃ θB/cos45°. In the sample frame, the VL diffraction spots will lie at qz = 0, perpendicular to the field direction. For small rotation angles and small qz we have, to a good approximation,
Differentiating equation (4) shows that the relationship between pixel space and q space in the xy plane is
At this point, one has to make choices about how to treat the experimental information regarding wavelength and counts and how they are recorded. In our work here we have used Mantid as implemented at EXED, where we must work in q space, and so the rest of our treatment builds on that (see Section 5). However, different choices could be made, for instance in the user-friendly GRASP software (Dewhurst, 2003) work can be done using the appropriate TOF bins associated with each detector pixel.
Of immediate relevance for our discussion of the expression for the form factor is the fact that, when the detector data are assembled by Mantid into pixels of q space, there may be counts from several detector pixels added into one q pixel, and these counts will be normalized by the main beam intensity, summed for the same number of pixels. To calculate the intensity summed over the detector pixels, we have to account for this. If the size in the xy plane of a q pixel is ΔqxΔqy then, using equation (5), the area of the detector contributing to this pixel is ΔxΔy, given by
Hence the number N of detector pixels (of real-space size δxδy as in Fig. 3) included in this q pixel is
This factor has to be included in a sum over q space to convert it into a sum over the detector. We note that the kj2 in the denominator cancels the in the Christen formula for the whole of the wavelength distribution. The Christen formula applies when summing over a real-space detector; when summing over q space the wavelength dependence in the Christen formula disappears. Finally, qdω translates into dqz, so we come to the TOF version of the formula for the form factor,
The area ΔqxΔqy is chosen to contain all the intensity of the diffraction spot. The integral over qz is understood as the area of a Gaussian (or Lorentzian if that is the observed shape) fitted to this intensity as a function of qz. This is analogous to using the area under a rocking curve in the quasi-monochromatic SANS case to establish the integrated intensity.
4. Instrument setup
Our neutron measurements were carried out on the High Magnetic Field Facility for Neutron Scattering (Prokhnenko et al., 2017). This facility is no longer operational, but at the time of our experiments it consisted of the High Field Magnet (HFM) (Smeibidl et al., 2016) and the Extreme Environment Diffractometer (EXED) (Prokhnenko et al., 2015) at the Helmholtz-Zentrum Berlin (HZB). The multi-purpose EXED instrument operated in TOF mode, with a wide range of incident neutron wavelengths, maximizing the volume of that could be observed for a given orientation of the HFM. This was a hybrid solenoid magnet system with a maximum field of 25.9 T, making it the highest continuous magnetic field that was available in the world for neutron scattering experiments. The instrument was used for a wide variety of elastic diffraction or experiments; in this case we used a setup appropriate for elastic small-angle scattering from the vortex lattice (VL), which has a repeat period of ∼100 Å under our conditions. The direction of the horizontal magnetic field, and therefore of the sample, was rotated relative to the incoming beam by a few degrees, so as to satisfy the Bragg scattering condition at a wavelength near the middle of the range for the incoming neutrons.
The neutron beam from the HZB reactor was chopped at a frequency of 10 Hz by two counter-rotating choppers with opening angles of ∼55° situated 53 m before the sample. The gap both opens and closes linearly with time, with a total opening time of 15.2 ms. However, the maximum width of the chopper gap is roughly three times larger than the guide width, so the beam is fully transmitted over the central ∼10.1 ms, giving a flat-topped pulse, as shown in Fig. 4. We use this pulse shape in our resolution calculations later in the paper, where we represent its width by a single number, the root-mean-square (r.m.s.) time width of the intensity distribution.
Neutrons over the wavelength range 2.5–9.3 Å could be identified by their time of arrival at the detector, between ∼37 and 137 ms after they had passed through the source choppers. Additional choppers removed neutrons which would have arrived at the edges of this time range or outside it. This avoids `frame overlap' with the next pulse arriving 100 ms later (Prokhnenko et al., 2015). For our first experiment, the data were analysed over the wavelength range 2.55–8.15 Å, ignoring low intensities at the extremes of the range. The incoming beam was collimated by a 30 mm diameter aperture located 5.5 m before the sample and a second 14 mm diameter aperture 1.0 m before the sample, with a sample-to-detector distance of 5.5 m. For the second experiment, the range was 5.0–8.15 Å to reduce background due to double Bragg scattering, first from one twin domain and then from another domain. This is seen only below the Bragg cut-off, i.e. at short wavelengths, and from a sample containing both twin domains. The collimation in this case was 30 mm at 7 m with another 12 mm aperture at 0.65 m and a detector distance of 4.5 m. The sample areas were defined by a 7 × 5 mm hole in a cadmium `window frame' around the mosaics. This gave an angular divergence of the incoming beam of ∼0.20° FWHM in the first experiment and ∼0.17° FWHM in the second.
Two different detectors were used in the two experiments; both consisted of arrays of cylindrical position-sensitive detector tubes. The tube spacing defined their horizontal resolution while the vertical resolution was given by 1% of their length. In the first, the detector is that described by Prokhnenko et al. (2017). This detector was at a fixed position with respect to the laboratory and had pixels of size (δx, δy) = (14, 9) mm. In the second case, the detector was attached to the magnet, and so both rotated with the same angle α. This detector also had larger pixels: (20.8, 24) mm. The first detector had better resolution but was not in a vacuum as it was separate from the magnet, so helium or argon gas was put in the flight path to reduce background due to air scattering. Equation (5) gives the relationship between pixel size and q resolution.
In both experiments, a perforated cadmium beamstop of measured transmission (∼1.5%) was set to intercept most of the incident beam to avoid overloading the detector. The fraction of the beam transmitted by a perforated beamstop also acts as a beam monitor. This gives a measure of the main beam intensity with the same
as the scattered beam and – in TOF mode – with the same time structure. The alternative arrangement of a beam monitor in the incident beam will give a wavelength-dependent efficiency, which in general will be different from that of the detector. In TOF mode, corrections would have to be made for monitor efficiency and the different distance of the monitor from the choppers. In quasi-monochromatic mode, a monitor in the incident beam is not a problem, as long as a perforated attenuator of known transmission is used to measure the main beam intensity. In both cases, one relies on the transmission through the perforations being determined by the fraction of area they occupy, which allows us to make the reasonable assumption that the transmission is wavelength independent.5. Data treatment
The data treatment for obtaining the VL was performed using the software package Mantid (Arnold et al., 2014) using the following procedure.
(i) Before starting the data treatment, we first loaded data files containing information on the position of the direct beam on the detector for each angle of rotation of the magnet at which measurements were taken. These define the centre of our detector, i.e. q = 0.
(ii) We then loaded separately all of the data files, designated as foreground (being studied to see if there is a VL signal) and background (no VL signal possible). Each file was labelled with an identification number, the angle of rotation of the magnet, and the temperature and magnetic field applied during that measurement. Each foreground file had a corresponding background file measured at the same magnet angle of rotation and both should have been measured at the same field. Background files were obtained by measuring above the
of the sample. Each file contained the neutron counts collected during a run (usually around 60 min) assembled into 256 logarithmically spaced time bins for each pixel of the detector.(iii) Next, the data were re-binned from time bins to wavelength bins of width 0.02 Å.
(iv) Each foreground and background file was then divided by the known pixel-dependent efficiency of the detector.
(v) Using the detector centre appropriate for the relevant magnet rotation angle, these files were re-binned from neutron counts versus wavelength in each detector pixel to neutron counts versus wavelength in pixels of the q space of the sample (see Section 3).
(vi) Where files had been measured at the same temperature and magnetic field but at different rotation angles, the files were merged at this point and the counts for all angles were added together into the appropriate q-space pixel and wavelength bins. It is important to note that Mantid conserves the number of neutron counts, adding them to the appropriate bins in the q-space pixels.
(vii) A separate workspace was then created to allocate the main-beam wavelength distribution information to every detector pixel. The main-beam information was obtained from the counts passing through the perforated beamstop, corrected by its q space in the same manner as the foreground and background files. This process assigned the number of main-beam counts that could have given rise to the scattered intensity in each q-space pixel and wavelength bin.
These data were also rebinned to(viii) After this re-binning the separate foreground and background files containing the scattered counts were normalized by the main-beam intensity. The normalized intensities were then summed over wavelength bins as in equation (8) for each q-space pixel.
(ix) The normalized background was subtracted from the normalized foreground to give the diffraction signal – from the VL in our case. For our VL data, this was concentrated near the plane perpendicular to the magnetic field (defined as the qz = 0 plane) in diffraction spots from the VL at q = (qx, qy).
(x) We note that determining the integrated intensity from any mesoscopic
investigated by SANS would require a similar analysis procedure. In the case of a skyrmion lattice, this would give the form factor of the spatially varying magnetization perpendicular to the scattering vector.Figs. 5(a) and 5(b) provide examples of foreground and background raw data taken on the 98% detwinned YBa2Cu3O7 sample at 23 T. These display the intensity per pixel of the detector, summed over all neutron wavelengths. The bright spot is the direct beam. Fig. 5(c) shows the corresponding subtraction. In both foreground and background there are four spots of intensity forming a square pattern around the direct beam (note that the detector pixels are not square). These spots are the results of a double diffraction process, firstly from the majority twin and then from the minority twin, or vice versa. They are not related to the VL. This occurs at a specific wavelength controlled by the Bragg condition for the crystal planes in question. The actual VL diffraction signal is spread out over a range of distances from the main beam as it appears at all wavelengths, and it is most clearly seen after converting from detector pixels to q space. To see the signal clearly in the detector panel output prior to the rest of the analysis required at least 4 h of counting time for both foreground and background.
To extract the integrated intensity of the Bragg reflection, a sum over qx, qy and an integration over qz must be carried out, as described in the text following equation (8). Fig. 6 shows an example of the data prior to this integration. Firstly, the signal versus qx and then versus qy is plotted in Fig. 7. In each case, the quantity plotted has been summed over the spot area in the other two dimensions of q space. This gives the position and width of the spot, which determine the area of qx and qy over which to sum the signal. Finally the qz integration is done to give the total integrated intensity. As shown in Fig. 7, all of the fits were Gaussians with the background level constrained to be zero. From the fits, the FWHM in a given direction can also be extracted; this is discussed in more detail in the following section. The dimensions of the qxqy area used to sum the signal shown in Fig. 7(c) were set to be ±3× the Gaussian widths of Figs. 7(a) and 7(b).
We have checked our analysis by comparison with quasi-monochromatic measurements and find excellent quantitative agreement in the measured form factor for YBa2Cu3O7 as a function of field (Campillo, Bartkowiak et al., 2022) when using the first detector setup. For the detector setup in the second experiment, we consistently recorded an integrated intensity lower than that obtained in the first experiment or quasi-monochromatic measurements on three different samples. The measured form factor from the second setup had to be multiplied by 1.5 to match the values measured by other setups. We do not know the exact reason for this but the most likely cause would be a problem with correctly establishing the main beam intensity.
6. General considerations
In a TOF experiment, there is often a choice of the range of wavelengths to be used, which will give rise to a range of qz at the diffraction spot. However, a wide range may not give much extra information, because the intensity of the beam will fall off at long wavelengths and the reflectivity of the sample falls off at short wavelengths as λ2. Also, short wavelengths may diffract from the main as well as from the long-period structure to be examined. This can give unwanted background, as observed in YBa2Cu3O7 near the main beam in Fig. 5. This was much more important in our Y0.85Ca0.15Ba2Cu3O7 sample, because it had equal populations of both twin domains, giving much stronger double Bragg scattering. In this case, as described in Section 4, the short-wavelength data had to be removed from the analysis to reduce the background.
The rotation angle of the sample and the range of wavelengths determine the region of q space covered. A slice in the qxqz plane is represented in Fig. 8. The shape of this region means that some parts of q space have little or no scattered signal and also little or no main beam to serve for normalization. If the data are normalized by the main beam, this results in large uncertainties or even divide-by-zero errors in regions near to or outside the edge of the region covered. These effects can be seen in the plots in Fig. 7, particularly in Fig. 7(c). Taking data at other magnet angles will increase the volume of q space that is covered but does not necessarily increase the quantity of useful data about the diffraction spot itself. This is illustrated in Fig. 9. A good way of dealing with this problem would be to use a Bayesian method of analysis (Holmes, 2014) which gives little weight to data that have large fractional uncertainties.
Another consideration in SANS measurements is the qz width of the diffraction spot in the TOF method – or equivalently, the width of the rocking curve in quasi-monochromatic SANS. In the latter case, the width for a new and uninvestigated sample is immediately revealed by a rocking scan. In the TOF case, the range of wavelengths may be too large or too small to obtain efficiently the required data at a single magnet rotation angle. Consider first the situation with a small q and a short z-axis correlation length, i.e. a large qz width of the signal. Because of the small q, the range of qz covered by the range of wavelengths will also be small (see Fig. 1) and a set of different sample rotation angles will be required to give sufficient qz coverage. Conversely, if the sample exhibits a well ordered structure at a large value of q, the `rocking curve' given by the TOF technique may be too wide, with many of the data giving background instead of signal. The most challenging situation for SANS by any technique is a weak signal at low q with large qz width, where efficiently setting the required measurement conditions is somewhat more involved for the TOF technique.
7. Instrument resolution and VL perfection
In this section, we discuss the questions of instrument resolution and measurement of the perfection of the structure being investigated within the context of VL diffraction. However, the results can equally be applied to other mesoscopic structures to relate the coherence of these structures in the x, y and z directions to the spot widths in q space. The width of a diffraction spot in qx, qy and qz will be determined partly by the instrument resolution (which is highest in the z direction) and partly by the perfection of the VL. A simple approach in the quasi-monochromatic case is described by Cubitt et al. (1992).2 This analysis was carried out not in q space but in terms of the widths of distributions over angles, including any spread in the It showed how the effects of the angular spread and wavelength spread of the incoming beam combine with any imperfection of the VL to give the widths of the diffraction spot on the detector and of its rocking curve. In equation (3) of Cubitt et al. (1992), the intensity of a diffraction spot is given as a function of two variables, both treated as pointing radially from the main beam through the diffraction spot: (i) the angle φ of the scattered beam measured relative to the ideal Bragg 2θB of the spot, and (ii) the rocking angle ω measured relative to the ideal Bragg θB. We extend slightly the treatment of Cubitt et al. (1992) to derive the instrument qz resolution, which was not explicitly derived there, and to calculate the qxqy resolution for the TOF case. In a quasi-monochromatic SANS experiment, the contributions of the instrument to the resolution are given by the instrument setup, and the contributions of the sample may be extracted from the data as angular widths. The outputs obtained from the analysis of TOF data are in q space, and so to use the results of Cubitt et al. (1992) it is convenient to convert values from TOF observations into angles. The radial width σφ of a spot in the plane of the detector is related to the observed radial width σq by σφ = σq/kj (see Fig. 10). However, because of the range of wavelengths used in TOF, we can only apply this expression approximately, using a value in the middle of the wavelength range. The equivalent of the rocking curve width σω is given in terms of the observed width by . Note that this implies that, for a rocking curve measured by quasi-monochromatic SANS to have an angular width which is independent of field, this would correspond to a qz width which increases with q and therefore with field.
Cubitt et al. (1992) used the following symbols: a is the angular width of the incoming collimation, b is the mosaic spread of the VL crystal and c is the spread of Bragg angles. To calculate the rocking curve width for a spot, we have to integrate equation (3) of Cubitt et al. (1992) over φ to obtain the total intensity of the spot as a function of ω. This was not done explicitly by Cubitt et al. The result is
This simple addition of the three widths applies in both quasi-monochromatic and TOF setups. However, for the spot size different expressions may need to be used. If in a quasi-monochromatic experiment the spot width is measured at fixed ω = 0, the following expression applies:
However, in a TOF experiment, we are effectively sampling a range of ω values so we have to integrate equation (3) of Cubitt et al. (1992) over ω, obtaining the much simpler expression
This result [not given by Cubitt et al. (1992)] may also be used in the quasi-monochromatic case if the spot width is measured on a sum over a rocking curve. We note that equation (11) shows that the spot size does not depend on the mosaic spread b of the sample. In the quasi-monochromatic case, the ω = 0 spot size in equation (10) does give information about b. Furthermore, as discussed by Cubitt et al. (1992), a different expression containing a, b and c may be obtained from the slight shift in spot position as a function of rocking angle ω. To obtain similar information from TOF data, one would have to analyse thin slices of the wavelength distribution to obtain quasi-monochromatic data.
To use these expressions we must calculate the parameters. First we consider the spread of Bragg angles, which can arise either from wavelength spread or from variation in the d spacing of the VL or other mesoscopic crystal. For a VL, it is usually the case that the magnetic field is extremely uniform, so c tends to be dominated by the wavelength spread. The data from a TOF instrument will be collected into bins with arrival time t for each pixel of the detector, but if these bins are chosen correctly they will not determine the wavelength resolution of the instrument. This is instead controlled by the pulse width of the incoming beam, often set by input chopper(s).
In our case, the pulse shape shown in Fig. 4 gives a 2 × r.m.s. width of δt = 7.3 ms. The wavelength resolution arising from the width of the incoming neutron pulse is given by Δλ/λ = Δt/t, and in our case varied from 2 × r.m.s. ∼22% at 2.55 Å to ∼7% at 8.15 Å. This may also be expressed by stating that Δλ ∝ Δt is independent of λ and in our experiment was equal to ∼0.55 Å. Pautrat et al. (2012) reduced Δt using choppers to improve the wavelength resolution in their TOF experiment on the VL in niobium. This has a side effect of reducing the flux.
The other contributions to the resolution of the instrument are the input collimation and the detector pixel size. In the first experiment setup, the ∼0.20° input-beam divergence projected to a ∼19 mm FWHM spot size on the detector at 5.5 m, which had a pixel size (δx, δy) = (14, 9) mm. For the second setup, with a detector less suitable for SANS located 4.5 m from the sample, the calculated spot size was ∼13 mm FWHM, compared with (δx, δy) = (20.8, 24) mm. Thus in the first case the resolution in the detector plane was limited by input collimation, and in the second by pixel size.
We calculate only for the first setup, relating to the data shown in Figs. 11 and 12, and demonstrate the method for B = 20 T and a wavelength of 6 Å in the middle of the TOF range. We have a = 0.20° and calculate c = 0.16° from the instrumental wavelength spread. (The spread of the δθB ≃ δλ/2d, with δλ ≃ 0.55 Å and d ≃ 100 Å at 20 T.) Using equation (9) we calculate the FWHM of σω = 0.27° due to just these two terms. However, with ≃ 10−3 Å−1 from Fig. 11, we calculate (using ) a much larger σω ≃ 0.9°. This indicates that, in the qz direction, the VL mosaic b (or alternatively the z correlation length of the VL) dominates the observed qz width, which is much larger than the instrument resolution due to input collimation and wavelength spread denoted by a and c.
Now we turn to the size of the spots in the qxqy plane. At 20 T, equation (11) gives σφ ≃ 0.42°, and hence σq ≃ 8 × 10−3 Å−1. The calculated radial q resolution is comparable to the qx, qy widths observed in Fig. 12, so the circular spot that we see is resolution limited. This only confirms that the spread of Bragg angles c, which is the only quantity in equation (11) possibly depending on VL properties, is dominated by wavelength resolution and cannot give information about any spread in the VL d spacing.
8. Summary
We have shown how to extract quantitative information from VLs and other long-period structures, such as skyrmions, using a TOF instrument. The range of wavelengths is equivalent to sampling a range of rocking angles at once. However, sometimes using a large range of wavelengths can give additional background. The choice of magnet angles at which to collect data is very important and is challenging to determine in advance of the measurement, especially if the VL structure or sample quality is not already known. The strategies presented here will be useful for the high-flux TOF SANS instruments at pulsed sources.
Footnotes
1This article is part of a virtual special issue on Magnetic small-angle neutron scattering – from nanoscale magnetism to long-range magnetic structures.
2There is a misprint in equation (2) of Cubitt et al. (1992), where integration over ω should be over ν, but the following results are correct.
Funding information
Funding for this research was provided by Lunds Universitet (studentship to EC).
References
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