feature articles
Precise implications for real-space pair distribution function modeling of effects intrinsic to modern time-of-flight neutron diffractometers
aOak Ridge National Laboratory, One Bethel Valley Road, PO Box 2008, MS-6454, Oak Ridge, TN 37831-6454, USA, bCalifornia Institute of Technology, 1200 East California Boulevard, Pasadena, California 91125, USA, and cUniversity of Kentucky, Lexington, Kentucky 40506, USA
*Correspondence e-mail: oldsdp@ornl.gov, pagekl@ornl.gov
Total scattering and pair distribution function (PDF) methods allow for detailed study of local atomic order and disorder, including materials for which Rietveld refinements are not traditionally possible (amorphous materials, liquids, glasses and nanoparticles). With the advent of modern neutron time-of-flight (TOF) instrumentation, total scattering studies are capable of producing PDFs with ranges upwards of 100–200 Å, covering the correlation length scales of interest for many materials under study. Despite this, the d spacing and merging of multiple banks in neutron TOF data as they directly relate to real-space PDF analysis. Suggestions for best practice in analysis of data from modern neutron TOF total scattering instruments when using conventional analysis programs are made, as well as recommendations for improved analysis methods and future instrument design.
and subsequent analysis of data are often limited by confounding factors that are not rigorously accounted for in conventional analysis programs. While many of these artifacts are known and recognized by experts in the field, their effects and any associated mitigation strategies largely exist as passed-down `tribal' knowledge in the community, and have not been concisely demonstrated and compared in a unified presentation. This article aims to explicitly demonstrate, through reviews of previous literature, simulated analysis and real-world case studies, the effects of resolution, binning, bounds, peak shape, peak asymmetry, inconsistent conversion of TOF toKeywords: total scattering; pair distribution function; instrument resolution function; time-of-flight peak shapes.
1. Introduction
Total scattering and pair distribution function (PDF) analysis methods have been evolving rapidly in recent years (Farrow et al., 2007; Billinge & Levin, 2007; Playford et al., 2014; Egami & Billinge, 2012; Keen & Goodwin, 2015; Mancini & Malavasi, 2015) as the advent of faster computers has allowed for increasingly complex modeling programs such as RMCProfile (Tucker et al., 2007), DEBUSSY (Cervellino et al., 2015) and FullRMC (Aoun, 2016), to address longer length-scale correlations. At the same time, the complexity of many modern material studies often involves characterizing the structural correlations and nanoscale ordering at length scales on the order of tens to hundreds of ångströms (Aksel et al., 2013; Coduri et al., 2013; Hill & Allieta, 2013; Usher et al., 2015; Allieta et al., 2015; Checchia et al., 2015; Liu et al., 2016, 2017; Jiang et al., 2017). To take full advantage of the higher-fidelity models, the need to measure reliable, long length-scale spanning, high-resolution PDFs is greater than ever. Neutron total scattering methods in particular present this capability due to a balance between high Q range and resolution, and the absence of atomic form factor damping of the measured scattering pattern. Furthermore, neutron total scattering is the technique of choice for light atomic species (Li/H/C), particularly in the presence of heavy atoms, and through low absorption in complex sample environments.
Modern instrumentation of many neutron total scattering capable beamlines has been based around the time-of-flight (TOF) architecture of spallation sources, such as the NOMAD (Neuefeind et al., 2012) and POWGEN (Huq et al., 2011) beamlines at the Spallation Neutron Source (SNS) at Oak Ridge National Laboratory (ORNL), the NPDF (Proffen et al., 2002) beamline at Los Alamos National Laboratory (LANL), the GEM (Williams et al., 1997) and POLARIS (Hull et al., 1992) beamlines at the ISIS Neutron Source, and the NOVA (Hattori et al., 2010) beamline at the Japan Proton Accelerator Research Complex (J-PARC). Despite the advantages posed by spallation sources for total scattering techniques, in practice the real-space PDF is rarely used to examine structure beyond the short-range local order (<20 Å).
Previous studies have detailed a wide variety of intrinsic reciprocal-space data artifacts which influence the resultant PDF, including the effects of reciprocal-space constant resolution (Howe et al., 1989; Qiu et al., 2004), finite Q range and Q-dependent resolution (Toby & Egami, 1992; Billinge & Egami, 1993; Chung & Thorpe, 1999; Tucker et al., 2001; Qiu et al., 2004; Olds et al., 2015), Nyquist limits (Farrow et al., 2011), combining spectra (Howe et al., 1989), finite size effects (Jeong et al., 2005; Page et al., 2011; Olds et al., 2015), back-to-back exponential peak shapes (Jeong et al., 2005), and ad hoc corrections to optimize a PDF (Peterson et al., 2000, 2003). However, many of these factors can have a similar impact on the PDF, and no previous work has presented a unified review or presentation of the combined repercussions these artifacts have on the resultant PDF.
While methods have been developed to address some of these intrinsic artifacts in the PDF, the details of these mitigation strategies are too often employed solely by experts of the technique, or passed down as communal `at-the-beamline' knowledge. For example, MCGRtof (Tucker et al., 2001) is a Fortran program which calculates the PDF from total scattering data via a Monte Carlo approach in order to correct for inherent instrument resolution functions. This program saw little adoption by the greater total scattering community (likely due to relatively long computation times) and, in its current implementation, is unable to address most of the issues presented herein (Tucker, 2017). Given the landscape of newly emerging total scattering beamlines and the complex material challenges they seek to address, it may be time to reassess the reduction and analysis approaches employed by the community, and develop new methods and software to fill the gaps.
This contribution aims to distill and concisely present the cumulative tribal knowledge about artifacts found in neutron TOF-based PDF modeling in a way that is both concise and accessible to novices of the technique. Through simulation, the effects of individual reciprocal-space artifacts are isolated and their effect on the PDF presented. Also discussed are the current methods used in conventional PDF analysis software, such as PDFgui (Farrow et al., 2007), TOPAS (Bruker, 2015) and DISCUS (Proffen & Neder, 1997) to mitigate or model data aberrations. It is demonstrated that many of these methods are insufficient at high r for data from modern TOF-based total scattering instrumentation. Three case studies from neutron TOF instruments are shown (NPDF, NOMAD, POWGEN), which demonstrate real-world examples of the effects of these artifacts on measured data. All simulated and real data presented herein are included as supporting information. Finally, a list of best practices for analyzing neutron PDF data from modern TOF sources is compiled, as well as suggestions for improvements to commonly used analysis programs, and related considerations for future neutron total scattering beamline designs.
2. Simulated study of the effect of data artifacts on the PDF
We begin our presentation with a systematic simulation study of the effects on the PDF due to commonly encountered TOF reciprocal-space artifacts. Although many of these are well known and have been described previously, they are presented here in series to illustrate how similar some of them can be in their alteration of the final PDF and thus emphasize the care in analysis that must be taken when they are present. For these studies, a simulated idealized Si total scattering pattern is utilized. This pattern extends from Q = 0 Å−1 to Q = 50 Å−1 with ΔQ = 0.01 Å−1. The form of the PDF employed in this article is defined by Egami & Billinge (2012) as
where is the atomic pair density and is the average S(Q), via the form
This form of the PDF (often referred to as the reduced pair distribution function) is generated from the measured scattering structure function,2.1. The effect of absolute Q resolution and bounds
The PDF is generated, broadly speaking, through the Fourier transform of the measured scattering data (Bragg and diffuse), which has been normalized such that it oscillates about zero at high Q. If the diffuse component is ignored, and the Bragg peaks are treated as delta functions, the PDF would be constructed through the sum of weighted sine functions, with the set of frequencies and amplitudes defined through the positions and amplitudes of the Bragg peaks. The effect of finite broadening of Bragg peaks, therefore, is to introduce a band of frequencies centered about each peak's maxima. The net effect of this is to damp the PDF, which is discussed in detail in §2.2 of this article.
Viewing the measured scattering data through this lens, it becomes evident that the effect of limiting the bounds used in the generation of the PDF (Qmin/Qmax) is to reduce the available frequencies employed in the construction of the PDF. Because there are fewer neutron counts at high Q on most instruments, measurement noise tends to increase with Q. Selecting a lower Qmax is a commonly employed technique to reduce high-frequency noise in the PDF originating from these components of the data. However, care must be taken in such bound optimization, as limiting the Qmax could potentially remove true high-frequency local structure features in the real-space representation of the data. Similarly, this also explains how removing low-Q peaks (via the Qmin) can result in the absence of slowly oscillating real-space signal (e.g. pore structure) from the PDF. Examples of limiting Qmin/Qmax are shown in Fig. 1.
Beyond the effect of any missing structural signal, abrupt termination of non-zero intensity leads to `termination ripples'. Most PDF analysis programs offer the ability to model the effects of termination at Qmax through a convolution of the calculated PDF with a sinc function. These effects have been demonstrated and explored in detail in many previous studies (Chung & Thorpe, 1999; Farrow & Billinge, 2009; Gagin et al., 2014; Olds et al., 2015). Note that the Qmax value present in typical neutron TOF-produced PDFs does not originate from the physical limits of the instrument, but rather the choice of Qmax employed in the data reduction process.
The bandwidth of Q space employed defines the minimum-frequency () and maximum-frequency () sinusoidal component used in the generation of the PDF, where
and
While real-space resolution () is directly related to (no resolvable feature can exist finer than ), the effect of the is more subtle, as it defines a lower limit on the frequency of sinusoidal, single-component contributions (long wavelength) to the PDF. In general, S(Q) can be extrapolated down to Q = 0; however, if longer length-scale correlations are present in the material (such as the kind that might be expected in small-angle scattering) caution is required as these simple extrapolations may invalidate fully atomistic models that include long length-scale features (Farrow & Billinge, 2009; Gagin et al., 2014; Olds et al., 2015). A particularly disastrous example of using a Qmin value above a Bragg peak is shown in Fig. 1(b).
During typical TOF neutron total scattering measurements, neutron detection events are measured at a much finer granularity (δQ) than is ultimately employed in the generation of the PDF, on the order of δQ = 10−4 ms/(0.3 ms < TOF < 16.6 ms) = 3 × 10−4 to 6 × 10−6. During data reduction, these raw counts are binned linearly in Q space with widths on the order of ΔQ = 0.02 Å−1. Rebinning data into coarser schemes is possible, but the effects of aliasing (Shannon, 1949; Qiu et al., 2004; Farrow et al., 2011) will be present when the PDF is generated to distances larger than
Above Lmax,bin, the calculated PDF will become non-physically periodic, a result of the introduced aliasing (the signal will be reversed and intensity inverted). To demonstrate such an artifact, the data have been rebinned on the scale of ΔQ = 0.05 Å−1, and the PDF calculated out to 200 Å, with the results shown in Fig. 2. In this example, clear aliasing effects are seen at periods of π/0.05 Å = 62.8 Å, which both confound and repeat (non-structurally) the apparent PDF. Note that, in this example, some damping is also seen due to the subtle loss of resolution, discussed in more detail in §2.2.
Usually, the granularity resolution is much finer than the employed Q binning () in order to avoid loss of information. However, since the number of neutrons per bin is proportional to the bin width, smaller ΔQ results in seemingly noisier data in Q space. Although selecting a coarser binning scheme in ΔQ will produce smoother-appearing reciprocal-space data, such rebinning will only result in a PDF with a greater damping rate and more limited length-scale range. Thus, there is no clear benefit for the resultant PDF to rebinning of reciprocal-space data prior to performing the Fourier transformation.
2.2. The effect of symmetric peak shapes
If using a ; Finger et al., 1994), with many contributions to the characteristic width given by instrumentation design (guides, slits, collimators, monochromators etc). Additional sources of peak broadening, due to factors such as detector precision, beam dispersion and sample thickness, will lead to convolutions of additional Gaussian-like effects on the peak shape. These effects broaden the peak shape, but do not change its inherent characteristics. Some of these effects will have a Q dependence, which is addressed in §2.3. Here, the inherent effects of convolving a constant peak shape with the idealized reciprocal-space data are shown on a resultant real-space PDF.
or X-ray synchrotron source, the characteristic shape of the integrated incident radiation at a reflection point can often be well modeled as a Gaussian or Voigt function (Rietveld, 1969Fig. 3 demonstrates the effect of static convolutions for the case of a Gaussian of width 0.01 Å−1 [Fig. 3(a), orange], a Gaussian of width 0.05 Å−1 [Fig. 3(b), red], a Lorentzian of width 0.01 Å−1 [Fig. 3(c), dark green] and a Lorentzian of width 0.05 Å−1 [Fig. 3(d), light green]. In each case, the inset figure highlights the effect of the convolution in compared with the idealized (unconvolved data) at Q = 3.8 Å−1. The primary effect is the damping of the high-r real-space PDF as the reciprocal-space peak is broadened. To first order, this can be considered a resolution feature similar to the effect of discussed in §2.1. However, as this loss in effective resolution has been framed precisely (as convolutions of known functions), it is possible to explicitly address these effects in real space.
Recall the convolution theorem, which states that when two functions, j(r) and k(r), individually Fourier transform into corresponding functions, J(Q) and K(Q), then the product of these two functions in one space will Fourier transform into the convolution of the corresponding pairs in the other space, as described by
In regards to the examples shown in Figs. 3(a) and 3(b), the reciprocal-space data have been convolved by a Gaussian of width . The resultant real-space effect will be the original PDF multiplied by the Fourier transform of the convolving Gaussian, resulting in an associated Gaussian scaling factor, Gdamp, defined as
This damping method is demonstrated in Fig. 4(a) and is seen to correctly address this effect.
The Fourier transform of a Lorentzian function is an exponential function, and thus in Figs. 3(c) and 3(d), where the ideal data have been convolved with a Lorentzian function of peak width , one can see an exponential damping envelope in the PDF, Ldamp, described as
This convolution is demonstrated in Fig. 4(b) and is seen to correctly address this effect.
Several software packages address the effect of instrument resolution on the PDF by utilizing Gaussian damping effects. For instance in PDFgui (Farrow et al., 2007), DISCUS (Proffen & Neder, 1997), and TOPAS (Bruker, 2015) (encoded intrinsically or via defined functions), a so-called Qdamp term can be employed when refining to data, where Qdamp defines the Gaussian-shaped damping in equation (7). However, the value of this is typically fit during of a standard data set, and not explicitly based on inherent instrument characteristics. Note that such a Gaussian implementation of Qdamp can only precisely account for peak-shape effects that are Gaussian in nature, and employing it to account for alternative peak shapes is inherently an approximation.
2.3. The effect of asymmetric peak shapes
Up until now, the effects presented have been exclusively due to symmetric peak-shape profiles. For TOF neutron sources, the inherent nature of the pulse shape as it is emitted from the moderator will produce asymmetric peak shapes, with a sharp rise at lower TOF (corresponding to the onset of the neutron pulse), followed by a much longer decay tail. To first order, this pulse shape is often treated in et al., 1982; Jeong et al., 2005; Avdeev et al., 2007). Jeong et al. have shown that simulated TOF peaks can lead to r-dependent artifacts in PDF data (Jeong et al., 2005). To examine how the degree of asymmetry in a peak profile affects a PDF, it is convenient to define an asymmetric Gaussian function,
as a back-to-back exponential and has been explained in detail previously (Von Dreelewhere α and β are different widths and Hc is the Heaviside function, defined as 1 when and 0 when . This peak may be numerically recentered such that the centroid position (at x = 0) is defined by half the total integrated area under the curve, . Although non-standard for fitting TOF reciprocal-space peak shapes (where a back-to-back exponential is typical), by demonstrating the effects of this asymmetric Gaussian peak profile on the PDF, it is possible to isolate those artifacts introduced solely due to characteristic asymmetry.
Here, convolutions of the recentered asymmetric Gaussian function have been applied to the idealized Si pattern for the case of , and compared against data corresponding to symmetric Gaussian functions with equivalent area, . The resultant PDFs from these convoluted data sets are shown in Fig. 5(a).
Performing boxcar-style refinements on these PDFs, where the r but at increasingly higher rmin and rmax bounds, it is clear that in the case of the asymmetric peak, the as-fit lattice constant [Fig. 5(b), top] displays an r-dependent contraction (consistent with data shifted to higher Q). The overall ability to fit the PDF from the asymmetric case decreases at higher r, as surmised by the increase in the weighted residual, Rwp [Fig. 5(b), bottom], defined as
is performed iteratively for a fixed width inwhere Gd(r) is the observed PDF and Gf(r) is the calculated model PDF, and w(r) is the associated weighting function (Dinnebier, 2008), taken as unity in these simulations.
Conventional approaches to resolution-dependent damping of the PDF with a Gaussian function are found to poorly fit the asymmetric peak-induced damping behaviour at high r. Despite the overall area under the convolution peaks being equivalent in these two cases, the damping of the PDF in the case of the symmetric peak is occurring faster than in the case of the asymmetric peak. The r-dependent contraction of the PDF becomes significant at higher r values and thus data are not quantitatively reliable above 40 Å in this example. As the artifact introduced to the PDF from asymmetric peak shapes is cumulative in r, low-r data in a measured PDF (below approximately 20 Å for typical measurements) will not be dramatically affected by asymmetric peak shape.
2.4. The effect of Q-dependent resolution
Typically, neutron TOF instrument resolution drops as a function of Q, such that the width of measured diffraction peaks increases as a function of Q. Variation in modern TOF neutron detector bank resolution is often addressed by invoking a or correction term. Here, the implication of constantly varying reciprocal-space is demonstrated by convolving the ideal Si data set with a Gaussian of linearly varying width, .
Fig. 6(a) demonstrates the difference in applying constant versus Q-dependent resolution functions, as they relate to the PDF. The ideal Si S(Q) pattern was convolved by a Gaussian of either static (black and purple) or linearly changing (blue) width. The resultant PDF from the linearly varying width () case is effectively being convolved by a Gaussian with a width varying as = 0.01. This effect is the basis of the so-called `Qbroad' term in PDF refinements, which acts to linearly increase the real-space as a function of r (Toby & Egami, 1992; Billinge & Egami, 1993; Qiu et al., 2004). Although directly attributed to instrument resolution effects, any linearly dependent peak-broadening effect can be modeled in this way. In Fig. 6(b) the PDF resulting from convolving the reciprocal-space data by (blue) is seen to be essentially identical to that resulting from convolving the ideal PDF with (green). Those differences remaining (offset gray) can be attributed to termination errors in the method of the convolution applied to the ideal PDF.
One is cautioned that if Q-dependent broadening displays non-linearity (for instance, if above a threshold the broadening becomes constant), these simple Qbroad corrections will no longer address the full effect. This concept is explored in detail in §3.2 of this article.
2.5. The effect of inconsistent TOF-to-d conversion
The natural units for data from TOF neutron instruments are, explicitly, the measured time of flight (ms). Raw data are `time-focused' to a single effective energy and then converted from TOF to d (where d is the interplanar distance) most commonly through a quadratic equation, with diffractometer constants (DIFC, DIFA and T0) as defined in the software suite General Structure Analysis System (GSAS) (Larson & Von Dreele, 1994). Solving the quadratic form of this equation, d values can be expressed in TOF as
In the limit where DIFA tends to zero, the relationship simplifies to
In principle, DIFC is the only constant required to convert TOF data to Q or d spacing. In practice, T0 corrects for any delay in moderator emission time or detector and DIFA acts as a second-order correction term accounting for shifts in the center of scattering, such as those attributed to sample misalignment and wavelength-dependent absorption. During it is common to initially refine these terms to a known standard, although there can be cases where these values are refined during the fitting of data. This is because a wide variety of variations between the measured standard and the measured samples can cause subtle changes in the apparent TOF value, such as sample placement, sample thickness relative to calibrant, detector tube drift, changes in detector tube temperature, moderator changes etc. The value of DIFC, although physically defined based on the diffractometer geometry, is often numerically fit during calibration procedures on the instrument. If multiple banks of data are being merged, there exists the possibility that inconsistent TOF-to-d conversion routines are being used to generate the unified S(Q). During PDF refinements, these diffractometer constants are rarely exposed, forcing the user into a `what you see is what you get' reality. Here, the effect of slight inaccuracies in the employed DIFC parameter on the resultant PDF is explored. Note that slight variation in DIFA or T0 would have a potentially similar effect.
Fig. 7 demonstrates the effect of overestimating the true DIFC value (which for this idealized data set was approximately 10 000) by values of 1 (Fig. 7a), 5 (Fig. 7b) and 10 (Fig. 7c). Although these are very subtle shifts in the apparent DIFC values (0.01%, 0.05% and 0.1%), one can observe that the net effect on the PDF can be dramatic. The cumulative Rwp values are calculated against the ideal PDF, shown in Fig. 7(d). The net effect from such a shift in DIFC will be a fixed offset in the as-fit lattice constant. This was verified by performing boxcar-style refinements of the `miscalibrated' data, in which the as-fit lattice constant was found to be decreased by a scale factor matching the degree of miscalibration (e.g. the fit lattice constant is 0.05% smaller than ideal when the DIFC value was 0.05% larger). While such a miscalibration in DIFC would alter the interpretation of the real-space PDF, the effect will be isolated to a fixed apparent offset of the lattice constant, and not introduce any r-dependent artifacts in the PDF. Such differences in lattice parameters are often observed in real- versus reciprocal-space analyis.
If the degree of miscalibration is not constant in Q, the implication for the PDF is far more complicated and ultimately uncorrectable during analysis. To demonstrate this, the PDF resulting from data which have an incorrect DIFC value of 0.05% above Q = 5.5 Å−1 (but nominal value below) is calculated. This would be similar to the effect of combining data from two detectors which had inconsistent calibration of DIFC values. The resultant PDFs are shown in Fig. 8(a). Fitting this resultant data set in PDFgui produced lower-quality fits when compared with the constant offset and ideal cases, as demonstrated by the resultant Rwp as a function of rmax, Fig. 8(b). It is also clear that the effect of this distortion on the apparent lattice parameter is complex and intractable. There are no conventionally available corrections for instrument characteristics in the PDF due to the merging of two inconsistently calibrated `banks' of data.
Certain types of inconsistent TOF-to-d conversion across multiple banks are likely random in nature (e.g. tube drift). To simulate such a condition, a modeled effect of random drift in collected reciprocal-space data is employed. Beginning with no offset at Q = 0, each Q value is assigned a random offset drift which is the sum of the previous random offsets and a uniformly distributed random value between and .
The effect of three such random drift patterns is shown in Fig. 9, which demonstrates the resultant PDF compared with the idealized case. Even though the degree of total offset is much less than the constant offset cases discussed previously, the overall effect is more detrimental to modeling as there is no overarching motif uniformly shifting the data.
Although this degree of random drift in real calibrations would hopefully be avoided through careful instrumentation, calibration and reduction procedures, this demonstrates that even a small deviation, such as the case shown in Fig. 9(a), would result in PDFs that cannot be fit well at high r. It is noteworthy that below r = 20 Å the PDF is affected very little by this sort of random drift.
3. TOF powder diffraction instrument case studies
In this section, data from a standard reference material [Si-SRM 640 (Mendenhall, 2016)] that have been measured on three modern neutron TOF powder diffractometers, NOMAD (SNS ORNL), POWGEN (SNS ORNL) and NPDF (Lujan Center LANL, no longer openly available) are presented and explored. The goodness of fit on this standard material using conventional (PDFgui) real-space is presented, with a focus on any aberrations found and how they link to the fundamental principles of PDF generation on TOF neutron diffraction instruments.
3.1. NPDF
Although presently not available in an open user program, the NPDF diffractometer at the Lujan Neutron Scattering Center (LANL) (Proffen et al., 2002) was previously a dedicated neutron total scattering beamline for disordered crystalline materials (Qiu et al., 2005; Page et al., 2008; Jeong et al., 2008; Božin et al., 2010; Harrington et al., 2011; Ramezanipour et al., 2012). Four distinct detector banks on NPDF (centered at 45, 90, 119 and 148° 2θ) were typically weighted according to neutron counts and combined to form the merged total scattering S(Q).
Data from Si-SRM (640c) were collected on NPDF in a 3/8 inch (9.525 mm)-diameter vanadium sample canister, measured with a beam size of 1 × 4 cm for 1 h on the NPDF diffractometer. TOF-to-d calibration was performed with NXproc (Proffen, 2015), with bank-merging and the generation of the PDF carried out using the PDFgetN program (Peterson et al., 2000). The as-fit data and refined lattice constant are shown in Fig. 10 (details of the can be found in the supporting information).
It is clear that the modeled Uiso) and lattice constant (other parameters were held fixed to values refined from the initial fit). The as-fit lattice constant is shown in Fig. 10(b), which demonstrates an r-dependent contraction of the data. This apparent r-dependent lattice contraction can be fit to the form a = ao(1+r)p, for which the values fit were ao = 5.43965 and p = -0.000263, shown as the orange line in Fig. 10(b). Although the as-fit lattice constant is gradually approaching the expected average value [shown as a dashed line in Fig. 10(b)], the offset coupled with the r-dependent behavior are evidence of artifacts or miscalibration in the data.
matches the measured PDF to a high degree; however, there are observable systematic offsets between the as-refined model and the measured PDF. Boxcar-style refinements, performed with a constant width of 5 Å, were completed while refining only the scale, isotropic atomic displacement parameter (To better understand the origin of this artifact, it is useful to examine the reciprocal-space data from the separate solid-angle detector banks of NPDF, prior to merging the data in PDFgetN. The four banks of data from NPDF are shown in Fig. 11 (left), with insets focused on two of the peaks. It is immediately clear that, in this data set, the calibration is more consistent between the four banks at low Q (seen in the peak at 3.37 Å−1) than high Q (seen in the peak at 8.26 Å−1). To further quantify this degree of misalignment, the offset between the measured positions of the 18 largest peaks in the Si data from each bank compared with their known positions is shown in Fig. 11 (right). One can see that the higher-resolution banks (3 and 4) are more consistently calibrated than the lower-resolution banks (1 and 2). When merged together, not only will this introduce a Q-dependent varying degree of misalignment, it will also introduce a gradually varying peak shape. The lower-Q data, where calibration was more consistent between banks, will merge to more Gaussian-like peak shapes, whereas the higher-Q data will merge to a more asymmetric shape with the peak maxima shifted to the right of the centroid.
As demonstrated through simulation in §2.5, inconsistent TOF-to-d conversion in can be a source of intractable behavior in the real-space PDF. In this case, any number of factors could have led to a miscalibration of the NPDF data, such as incorrect sample positioning, inadequate calibration procedure and short measurement time resulting in low statistics. Because measured data from a set of detectors with different characteristic peak profiles (and apparently, quality of calibration) were merged to generate the PDF shown in Fig. 10(a), the net effect on the PDF is not easy to track down ex post facto, and thus it is difficult to derive an analytical correction (in the manner of Qdamp or Qbroad) which can properly model the observed artifacts in real space. Note that higher-quality data were more typical on NPDF; however, this presented atypical data set (from a short collection time) is included to demonstrate the effects of a miscalibration on the resultant PDF.
3.2. NOMAD
The NOMAD diffractometer at the SNS (ORNL) is a dedicated neutron total scattering instrument (Neuefeind et al., 2012), with unparalleled and a wide simultaneously accessible Q range (0.1–50 Å−1). Data from NOMAD's six detector banks (centered at 6, 15, 31, 67, 122 and 154° 2θ) are weighted according to neutron counts and combined to form the merged total scattering S(Q). The instrument was developed with a dual purpose: for liquids and amorphous materials (Skinner et al., 2014; Lan et al., 2014; Yang et al., 2016; Wang et al., 2017), and for disordered crystalline materials (Shamblin et al., 2016; Charles et al., 2017; Fabini et al., 2017). NOMAD trades some resolution for high and a wide Q range, being the lowest-resolution diffractometer of the three case studies here, but is essential for many in situ and in operando total scattering studies (Wang et al., 2013; Ushakov et al., 2015; Hillis et al., 2016; Olds et al., 2017; Wu et al., 2017).
Data from a Si-SRM (640d) were collected on NOMAD in a 6 mm-diameter vanadium sample canister, with a beam size of diameter 1.5 cm for 6 h. Data were reduced using standard data reduction protocols, which include TOF-to-d calibration, merging of banks and generation of the PDF with custom IDL code available at the instrument (Neuefeind et al., 2012). The data, and resultant fit, are shown in Fig. 12(a) (detailed parameters can be found in the supporting information).
Compared with NPDF data, the lower average reciprocal-space resolution damps the NOMAD PDF significantly faster, and the overall fit from 0 to 100 Å is markedly worse. However, examining the difference curve between PDFs in Fig. 12(a) shows that the majority of the weighted residual occurs above r = 20 Å. If the is carried out solely below r = 20 Å, the resultant Rwp of the is 0.055, as opposed to 0.161. This is an indication that the artifacts which contribute to corrupting the NOMAD data set are, like many of the demonstrated artifacts, cumulative in their effect on the real-space PDF. Just as with the NPDF data set, one can examine the reciprocal-space data in a bank-by-bank manner to better understand the origin of the aberrations. Fig. 12(b) shows a small Q range where all six banks overlap, where the as-shown scattered intensity has been rescaled for visual comparison, and plotted concurrently with the merged S(Q) in black in each panel. In each bank, the peak profiles are seen to vary considerably from the final, merged profile. The highest-resolution bank (154°) exhibits significantly finer resolved peaks than the merged data set, while the lower-resolution banks exhibit more broad peak shapes, which also vary as a function of Q.
Whether the data from the banks are merged in an overlapping or non-overlapping (such that no two banks contribute to the same Q value) manner, the inherent peak profile varies from Gaussian-like at low Q to asymmetric back-to-back exponential-like at high Q. The inability to match the damping profile of the PDF here with the straightforward application of a standard Gaussian `Qdamp' correction is testament to the non-Gaussian nature of the peak shape in some detector banks, as well as differences in resolution between banks.
These NOMAD data confirm what the simulations in §2.5 demonstrate: combining banks of data must be performed very carefully, and differences between banks in can lead to unexpected and cumulative artifacts in real space. As was the case for the NPDF data, deriving an analytical real-space correction to account for the artifacts which have been introduced in is very challenging.
3.3. POWGEN
POWGEN is a third-generation high-resolution powder diffractometer at the Spallation Neutron Source (Huq et al., 2011), which, although not designed for total scattering, has the capability to produce PDFs (Liu et al., 2016). Through the use of a novel guide design and detector placement, POWGEN is able to maintain a much more constant reciprocal-space resolution relative to other cases.
Data from Si-SRM (640d) were collected in a 6 mm-diameter vanadium canister measured with a 1 × 3 cm beam size for 4 h total across two separate histograms with wavelength centers of 0.533 and 4.797 Å, which were then combined to span the desired Q range to generate the PDF. TOF-to-d calibration was performed using the Mantid software framework (Arnold et al., 2014), with bank-merging and the generation of the PDF carried out using the PDFgetN program (Peterson et al., 2000). The resultant total scattering structure function and PDF are shown in Figs. 13(a) and 13(c), respectively.
The higher resolution available on POWGEN is plainly visible when comparing the reciprocal-space data in Fig. 13(a). This results in a reduced damping rate of the associated PDFs, shown in Fig. 13(d). It is worth noting that at low r in Fig. 13(c), the PDFs from the three instruments are very similar.
3.4. Comparison of instruments
A summary of the fits from the three instruments is given in the supporting information. To further explore the differences in resolution between NOMAD, NPDF and POWGEN, Gaussian peak fits were performed of the largest, first 18 peaks in the measured pattern up to 18 Å−1. In Fig. 13(b), the resultant full width at half-maxima (FWHM) of the as-fit peaks are shown. This plot can help explain a majority of the differences in the PDFs of the three instruments. In the case of POWGEN, not only is a significantly smaller FWHM observed, but the value of the FWHM remains much more consistent over the full reciprocal-space pattern. This results in a PDF which has relatively little damping or real-space broadening present. Although the POWGEN peak-width behavior is not ideal for the generation of PDFs (for which one would desire a constant dQ/Q profile), the overall lower value of the FWHM means there is less of a need for Qdamp and Qbroad terms in order to model the PDF behavior.
In the NPDF data, significantly more variation in the FWHM of the Si peaks is observed than in the POWGEN data. However, the FWHM behavior follows a much more linear trend. Thus, despite the significant broadening and damping of the NPDF PDF at high r, the trends are readily modeled by the conventional correction of Qbroad (which assumes linear dQ/Q).
The NOMAD FWHM displays significant deviations from these two behaviors. The slope of the apparent dQ/Q effect is negative from Q = 0 to 5 Å−1, and then increasing. This can be attributed to the onset of the high-resolution detector bank, which begins contributing to the total measured pattern at approximately 5 Å−1. The resultant NOMAD PDF will be far less broadened at high r, compared with the NPDF PDF. However, the quality of the of the NOMAD PDF is greatly reduced since the particular reciprocal-space aberrations are not well handled by available corrections. Also, because the overall peak shape of NOMAD reciprocal-space data is more broad than for the POWGEN data, the damping function effect is more severe.
4. Best practices and looking forward
Many details of reciprocal-space data which are directly addressed in Rietveld refinements, such as peak shape and individual bank resolution characteristics, are not commonly addressed by most conventional PDF analysis programs. Yet, as can be seen from the presented simulations and case studies, these artifacts can have important effects on the resultant PDF, primarily at high r. The inherent asymmetry and non-Gaussian nature of the merged reciprocal-space data from modern TOF neutron powder diffraction instruments are not well addressed with the simple models for Gaussian peak shapes and constant dQ/Q behavior commonly employed in fitting PDF data from other sources. Regardless of their origin, asymmetric peak shapes like those shown in §2.3 will always introduce aberrations that will result in a changing lattice constant as a function of real space during data fitting.
Furthermore, the need for accurate calibrations, data merging algorithms and consistent sample positioning cannot be understated, particularly when combining multiple banks of data into a unified reciprocal-space pattern. If improper peak shapes are used in the procedures generating the TOF-to-d conversion (such as using peak centroid positions instead of true peak centers), it is possible that the instrument calibration will be adversely affected. Any misalignment of the sample or other pixel-to-d spacing offsets will produce artifacts in the PDF such as those shown in §2.5, which are intractable and likely irreversible during data analysis in real space. Although not presently possible, future methods similar to those in the MCGRtof program (Tucker et al., 2001) may be capable of addressing some or all of these effects and work in this area is ongoing (Tucker, 2017). The data sets available in the supporting information are provided in part with the hope that they will aid the community in developing solutions to the demonstrated problems.
It is important to note that, as seen in both the simulations and the case studies, the PDF is surprisingly resilient in maintaining an accurate representation of local structure up to approximately 20 Å, almost independent of any corrupting or complicating factors in the reciprocal-space data presented here. Also, for in situ studies, where a local feature of interest is being tracked or relative comparisons are being made between samples measured under the same conditions, these concerns are somewhat mitigated as many unaccounted for artifacts or aberrations in the data (e.g. lattice contractions, damping) will be the same among all the measured data.
What can be said of fits above 20 Å in real space? With available analysis programs, the authors recommend the following best practices for neutron TOF total scattering studies. A known standard should always be measured concurrently with samples of interest, and used to derive any Qdamp- and Qbroad-like terms, which should then be fixed for subsequent refinements of experimental samples. Furthermore, if the overall goodness of fit to standard data worsens as the rmax is increased (as is the case in all examples presented herein), this is a clear indication that data should not be quantitatively refined above that length scale. When possible, the results of Rietveld refinements should be compared with the results of fits to the PDF, with attention paid to the cases where the refined values deviate. If using flexible software such as TOPAS, DISCUS or Diffpy-CMI for PDF refinements, explicit damping and broadening terms can be defined beyond the standard single Gaussian. In initial testing, it has been found that simply allowing the refined damping term to be a sum of two Gaussians, where widths are independent variables, greatly improves the quality of NOMAD data refinements. A full analysis of best practices for refining NOMAD data is beyond the scope of this article, and will be presented elsewhere.
To be clear, the long-term solution would be to derive precisely how the peak shape of a given instrument directly impacts the as-calculated PDF. These suggested numerical corrections would allow a path forward in the same manner as the currently used Gaussian Qdamp and Qbroad corrections, without major modifications to available code bases.
Given the average computing power of a desktop computer is roughly 500 times greater than it was the year PDFfit was initially published (Proffen & Billinge, 1999), as well as the broad availability of massively parallel computing resources, it is perhaps not unreasonable to re-examine and re-define the approach employed in analysis of total scattering data. With a seemingly small addition, the ability to model Qmin, Qmax, and ΔQ effects, one could fit PDFs generated from a narrowly defined range in even though the PDF itself could span as wide a real-space length scale as desired. Although such narrow-bandwidth PDFs would be visually abstracted, this approach would allow the real-space data to be broken apart into different principal components. The net sum of these separate PDFs would still reproduce the conventional PDF. The advantage here is that a narrowly defined band of may be selected where the resolution and peak-shape profile are well defined and consistent, allowing for straightforward application of the analytically defined real-space corrections. In much the same way that Rietveld refinements are performed simultaneously on different banks of reciprocal-space data, PDF refinements could be performed on a single model applied to multiple PDFs (high-resolution, low-resolution, different Q ranges, different degrees of signal to noise etc).
It is entirely possible that the most accurate way of modeling total scattering data will ultimately involve, as is presently possible in RMCProfile and TOPAS, calculating both the real- and reciprocal-space data from a unified model, applying various corrections in whatever space is most appropriate (e.g. peak shape applied in nanoparticle shape effects in real space) and fitting directly to measured data.
The importance of minimizing intractable detector tube drift or variation in TOF-to-d conversion was illustrated in §2.5, and should be considered in future instrument design. Note that wider Q coverage does not necessarily result in higher-quality PDFs, especially if these banks have greatly varying resolution functions. In principle, a complex geometry of detector banks could be accounted for during analysis through the methods just proposed, although solving a problem with a hardware solution may avoid complex mitigation algorithms in software. Conventional requirements for high-quality measurements of diffuse scattering data still very much apply (low and consistent background), and detailed implications for factors such as absorption and multiple scattering must be considered. However, prioritizing constancy in the resolution functions, or keeping this behavior linear, could greatly simplify the modeling of real-space data for neutron TOF-derived PDFs.
Supporting information
Library of messed-up data. DOI: https://doi.org/10.1107/S2053273318003224/ib5055sup1.zip
Comparisons of fits on three neutron TOF diffractometers, detailed comparison of symmetric versus asymmetric reciprocal peak-shape effects and details of the simulated Si data-set generation. DOI: https://doi.org/10.1107/S2053273318003224/ib5055sup2.pdf
Acknowledgements
The authors acknowledge Ashfia Huq, Matthew G. Tucker, Peter F. Peterson and Ramya Deshpande for their helpful discussions related to this article.
Funding information
This work was supported under the Department of Energy Office of Basic Energy Sciences Laboratory Directed Research and Development (LDRD) Program at Oak Ridge National Laboratory LDRD No. 8420 (simulation and analysis) and the BES Early Career Award: Exploiting Small Signatures: Quantifying Nanoscale Structure and Behavior KC04062. Research conducted at the NOMAD and POWGEN beamlines at ORNL's Spallation Neutron Source was sponsored by the Scientific User Facilities Division, Office of Basic Sciences, US Department of Energy under contract No. DE-AC05-00OR22725 with UT-Battelle, LLC. Research conducted on NPDF at the Lujan Center was funded by DOE Office of Basic Energy Sciences. LANL is operated by Los Alamos National Security LLC under DOE contract No. DE-AC52-06NA25396.
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