The present invention relates to a technique for calculating a crystal orientation distribution of a sample from an X-ray diffraction profile (in the present specification, the X-ray diffraction profile refers to, for example, a list of diffraction angles corresponding to a certain crystal plane and relative intensities thereof obtained by measurement using an X-ray diffraction (XRD) apparatus, a powder diffraction file (PDF) card issued by the International Centre for Diffraction Data (ICCD), numerical calculation, or the like), and is particularly suitable for calculating an orientation degree distribution of a sample treated such that a certain crystal plane of a permanent magnet or the like is oriented in one direction.
Some materials have different characteristics depending on a crystal direction in which the material is constituted, and some materials are used by being treated (oriented) so that the crystal direction in the material is oriented in one direction in order to improve the characteristics of the material.
For example, a permanent magnet has an axis of easy magnetization which is easily magnetized depending on a crystal orientation of a material and an axis of difficult magnetization which is hardly magnetized, and it is important to align all directions of the axes of easy magnetization of powder constituting the magnet in one direction in order to maximize performance of the magnet.
An index for evaluating the degree of orientation includes an orientation degree. As a method of evaluating the orientation degree of a permanent magnet, there are a method of measuring magnetic characteristics and calculating the orientation degree from saturation magnetization and residual magnetization, a method of estimating the orientation degree from an X-ray diffraction profile, and a method of directly observing a crystal orientation by an electron back scatter diffraction patterns (EBSD) method.
In a method of measuring an orientation degree a from magnetic characteristics, a saturation magnetization Js and a residual magnetization Jr of a sample to be measured are measured, and the orientation degree a is determined from Formula (1) below.
However, in this method, in order to obtain an accurate saturation magnetization, a strong magnetic field (hereinafter, stated as being a magnetic field of 2 T or more) must be applied to the sample, and thus, only the average orientation degree of the entire measurement sample can be ascertained.
As a generally widely used method for estimating the orientation degree from the X-ray diffraction profile, there is a Lotgering method (Non Patent Literature 1). Lotgering factor F is obtained by Formulas (2) to (4) below.
Here, ΣI (HKL) and ΣI (hkl) are the sum of the peak intensity of the orientation plane and the sum of the X-ray peak intensity of all the crystal planes of the measurement sample, respectively, and ΣI0 (HKL) and ΣI0 (hkl) are the sum of the peak intensity of the orientation plane and the sum of the X-ray peak intensity of all the crystal planes of a non-orientation sample, respectively. The Lotgering factor of the non-orientation sample is F=0, and the Lotgering factor of a perfect orientation sample is F=1.
In addition, when the orientation degree is obtained using the Lotgering method, a plane other than the orientation plane ((HKL) plane) is treated equally to a plane perpendicular to the orientation plane. Therefore, according to Patent Literature 1, there is a problem in that the orientation degree obtained by the Lotgering method is smaller than the actual orientation degree. According to Patent Literature 1 described above, a method of obtaining an orientation degree close to reality by performing vector correction on diffraction peaks other than the orientation plane has been proposed. However, even when this method is used, it is not possible to calculate the orientation degree distribution with an average orientation degree.
In addition, there is also a problem in that it is difficult to accurately calculate an integral value of all peak intensities in a material having many diffraction peaks and distributed in a wide range of diffraction angles as in a rare earth magnet.
In the above two methods, only the average orientation degree of the entire sample can be evaluated. As a simple evaluation index for controlling the quality of a product, the average orientation degree is an index widely used industrially. However, ascertaining the variation in orientation degree and the existence ratio, which cannot be determined by the average orientation degree and the range of the orientation degree of each portion of the sample is important information for producing a product with a higher orientation degree.
The EBSD method is a method of irradiating a sample with an electron beam and analyzing a crystal orientation from a diffraction pattern of reflected electrons diffracted on a sample surface. By using this method, since the crystal orientation can be directly observed, it is possible to ascertain the orientation degree distribution and the spatial mapping (the spatial mapping of the crystal plane in the present invention refers to a diagram in which the direction of the crystal plane is associated with the position thereof) of the crystal plane. Since the diffracted reflected electrons are emitted from a shallow region of about 50 nm from the sample surface, it is a very surface-sensitive method. Therefore, it is essential that there is almost no damaged layer on the surface of the sample, and when it is necessary to treat the sample surface so as to be very smooth by electrolytic polishing, ion etching, or the like, in particular, when it is necessary to measure a large area, there is a problem in that it takes time to pretreat and measure the sample.
The present invention has been developed in view of the above problems, and an object of the present invention is to provide a method of easily calculating an orientation degree distribution from an X-ray diffraction profile by using an information processing apparatus and a calculation program without requiring complicated pretreatment of a sample as in an EBSD method, and a method of obtaining a spatial mapping of the orientation degree distribution from a plurality of diffraction intensity maps obtained by using micro-focal X-rays.
In order to solve the above problems, the present invention provides an orientation degree distribution analysis method that is a method of calculating an orientation degree distribution from a measurement result of X-ray diffraction and information of a crystal structure using an information processing apparatus including a main storage device and a central processing unit (CPU), the method including:
In addition, the present invention provides an orientation degree distribution analyzer that analyzes an orientation degree distribution from a measurement result of X-ray diffraction and information of a crystal structure using an information processing apparatus including a main storage device and a central processing unit (CPU), the analyzer including:
Furthermore, the present invention provides an orientation degree distribution analysis program for calculating an orientation degree distribution from a measurement result of X-ray diffraction and information of a crystal structure using an information processing apparatus including a main storage device and a central processing unit (CPU), the program causing a computer to execute:
According to the present invention, it is possible to calculate an orientation degree distribution using an information processing apparatus and a calculation program from information of a crystal structure unique to a material and a plurality of diffraction peak intensities obtained by X-ray diffraction. The spatial map of the orientation degree distribution can be created by obtaining a plurality of diffraction intensity maps using a micro-focal X-ray source.
The present invention relates to an orientation degree distribution analysis technique for calculating an orientation degree distribution from crystal structure information of a sample to be measured, an X-ray diffraction profile of a randomly oriented sample, and an X-ray diffraction profile of a sample to be analyzed obtained by measurement using an X-ray diffractometer. Hereinafter, an embodiment of the present invention will be described with reference to the drawings.
(Configuration of Apparatus)
(Crystal Structure Information Acquisition Unit)
A crystal structure information acquisition unit 11 acquires crystal structure information of a material as a calculation target of an orientation degree distribution necessary for calculating an angle (φm) formed by an orientation plane and a crystal plane. The crystal structure information is a crystal lattice and its lattice constant. The acquisition of the crystal structure information by the crystal structure information acquisition unit 11 is realized, for example, by the user reading a file recorded in the auxiliary storage device 4 via the input device 8 to the main storage device 5.
(Angle Calculation Unit for Angle formed by Orientation Plane and Crystal Plane corresponding to Diffraction Peak of Interest)
An angle calculation unit 12 for angle formed by an orientation plane and a crystal plane corresponding to a diffraction peak of interest calculates an angle (φm) formed by the orientation plane and the crystal plane corresponding to the diffraction peak of interest from the crystal structure information acquired by the crystal structure information acquisition unit 11. An angle φm formed by the (h1k1l1) plane and the (h2k2l2) plane is calculated, for example, by
in the case of a hexagonal crystal system, and by
in the case of a tetragonal crystal system, where lattice constants are a, b, and c. Using the above equations, all the diffraction angles used to obtain the orientation degree distribution are calculated using the CPU 3 and stored in the main storage device 5.
(Diffraction Range/Diffraction Sensitivity Acquisition Unit)
The diffraction peak observed in the XRD measurement is ideally observed only when the Bragg condition is satisfied, that is, when the angle of the X-ray incident on the crystal plane is the Bragg angle, but in practice, reflection is observed even at an angle slightly deviated from the Bragg angle (here, stated as an angle of 10° or less therefrom) due to crystallinity of the measurement sample, and thus it is necessary to take this into consideration in the analysis in the present invention. A diffraction range/diffraction sensitivity acquisition unit 13 acquires diffraction intensity information obtained at an angle slightly shifted from a diffraction angle θ corresponding to a certain crystal plane. This information is obtained, for example, by preparing a sample in which a target sample raw material powder is almost completely oriented and measuring the rocking curve of the sample. The acquisition of the diffraction intensity information by the diffraction range/diffraction intensity acquisition unit 13 is realized, for example, by the user reading a file recorded in the auxiliary storage device 4 via the input device 8 to the main storage device 5.
(Weight Function Setting Unit)
A weight function calculation unit 14 determines the weight function w(φm) from the measurement data obtained by the diffraction range/diffraction intensity acquisition unit 13. As the weight function, for example, a case of assuming the Gaussian distribution of Formula (7) will be described as an example.
The determination of the weight function w(φm) by the weight function setting unit 14 is realized by determining a parameter σg that best fits the data acquired by the determined diffraction range/diffraction intensity acquisition unit 13 by calculation using the CPU 3 and storing the obtained parameter in the main storage device 5. An arbitrary function can be used as the weight function, and for example, when a certain angular range is set without performing the rocking curve measurement, another function such as a continuous uniform distribution function may be used.
(Randomly Oriented Sample X-ray Diffraction Profile Acquisition Unit)
A randomly oriented sample X-ray diffraction profile acquisition unit 15 acquires an X-ray diffraction profile of a randomly oriented sample having the same composition and structure as the measurement sample. The acquisition of the randomly oriented sample X-ray profile by the randomly oriented sample X-ray diffraction profile acquisition unit 15 is realized, for example, by the user reading measurement data recorded as a file in the auxiliary storage device 4 via the input device 8 or, for example, an ICCD database or the like to the main storage device 5.
(Existence Ratio Calculation Unit)
An existence ratio calculation unit 16 calculates an existence ratio S0 of the particles whose crystal plane are oriented in the direction corresponding to each diffraction angle of the randomly oriented sample from the following equation using φm calculated by the angle calculation unit formed by the orientation plane and the crystal plane corresponding to the diffraction peak of interest and w(φm) calculated by the weight function calculation unit 14.
[Math. 8]
S0=∫w(φm)sin φmdφm/2π (8)
Using the above equation, all the diffraction angles used to obtain the orientation degree distribution are calculated using the CPU 3 and the result is stored in the main storage device 5.
(X-ray Diffraction Profile/Diffraction Intensity Map Acquisition Unit)
An X-ray diffraction profile/diffraction intensity map acquisition unit 17 acquires, for example, an X-ray diffraction profile of a sample for measuring an orientation degree distribution measured using an X-ray diffraction (XRD) device, or a diffraction intensity map measured using a device capable of irradiating a minute site of the sample with X-rays, such as a micro-focal X-ray source, as an X-ray source. In the present specification, the “diffraction intensity map” refers to an intensity ratio of each diffraction peak obtained by X-ray diffraction measurement in which irradiation position information is added to an X-ray diffraction profile. The acquisition of the X-ray diffraction profile/diffraction intensity map by the X-ray diffraction profile/diffraction intensity map acquisition unit 17 is realized, for example, by the user reading the X-ray diffraction profile recorded as a file in the auxiliary storage device 4 via the input device 7 to the main storage device 5.
(Orientation Degree Distribution Function Setting Unit)
An orientation degree distribution function setting unit 18 sets the orientation degree distribution function f(φm) by assuming the distribution shape of the orientation degree distribution. Setting of the orientation degree distribution function by the orientation degree distribution function setting unit 18 is realized, for example, by reading the orientation degree distribution function recorded in the calculation program stored in the auxiliary storage device 4 to the main storage device 5. An arbitrary equation can be set as the orientation degree distribution function f(φm), but it is desirable to use a distribution function capable of sufficiently simulating an actual orientation degree distribution.
(Orientation Degree Distribution Analysis Unit)
An orientation degree distribution analysis unit 19 calculates the orientation degree distribution using the CPU 3 on the basis of the angle φm formed by the orientation plane recorded in the main storage device 5 and the crystal plane corresponding to the diffraction peak of interest at the diffraction angle θi, the weight function w(φm), the existence ratio Si of the particles facing the direction of the angle φm in the randomly oriented sample, the information on the diffraction angle corresponding to a certain crystal plane and the relative intensity thereof acquired by the X-ray diffraction profile/diffraction intensity map acquisition unit 17, or the information on the diffraction intensity map.
Details of the operation of the orientation degree distribution analysis unit 19 will be described with reference to the flowchart illustrated in
When the data acquired by the X-ray diffraction profile/diffraction intensity map acquisition unit 17 is a diffraction intensity map, a j-th position in the diffraction intensity map is selected and set as Xj in step S100.
Next, in step S110, the auxiliary variable of f(φm) is also provisionally determined, and temporarily stored in the main storage device 5 as a temporary orientation degree distribution function f*(φm).
Next, in step S120, the diffraction angle θi of the i-th peak is selected from the X-ray diffraction profile of the sample to be measured, which is stored in the main storage device 5 by the X-ray diffraction profile/diffraction intensity map acquisition unit 17, and the relative intensity Ii and the existence ratio Si are set.
Next, in step S130, the relative intensity of the randomly oriented sample corresponding to the diffraction angle θi set in step S120 is selected from the data stored in the main storage device 5 by the randomly oriented sample X-ray diffraction profile acquisition unit 15 and the existence ratio calculation unit 16, and is set as I0i and S0i, respectively.
Next, in step S140, φm corresponding to the diffraction angle θi selected in step S120 is selected and set. As φm, a value calculated by the angle calculation unit 12 formed by the orientation plane and the crystal plane corresponding to the diffraction peak of interest and stored in the main storage device 5 is used.
Next, in step S150, from the temporary orientation degree distribution function f*(φm) stored in the main storage device 5 in step S110, a particle existence ratio S*i at which the angle formed by the orientation plane and the crystal plane corresponding to the diffraction peak of interest is φm is calculated from the following equation and stored in the main storage device 5.
[Math. 9]
Si*=∫w(φm)f(φm)dφm (9)
Next, in step S160, the peak intensity I*i at f*(φm) is calculated from the following equation using S*i, S0i, and I0i calculated in steps S130 and S150.
In step S170, it is determined whether the calculations in steps S120 to S160 have been performed for the peak data of all diffraction angles input to the orientation degree distribution analyzer 1, and if all the calculations have been performed, step S180 is performed, and if not, step S120 is performed.
For the peak data of all diffraction angles, the peak intensity I*i predicted from the temporary orientation degree distribution function f*(φm) is calculated, and then, in step S180, a degree of the similarity between the predicted peak intensity group (I*i, I*2, I*3, . . . , I*n) and the actually measured peak intensity group (I1, I2, I3, . . . , In) is calculated. For example, the following normalized residual sum of squares (SSR) can be used to calculate the degree of the similarity.
Subsequently, in step S190, it is determined whether or not the degree of the similarity calculated in S180 has reached a specified value, and when the similarity has reached the specified value, the orientation degree distribution function f*(φm) assumed at that time is used as the orientation degree distribution. In this case, it is considered that the difference between the peak intensity values is sufficiently small. In a case where the SSR is used for calculating the degree of the similarity, for example, a value of about 5×10−3 to 5×10−6 can be used as the specified value. The specified value is desirably set according to necessary calculation accuracy.
In a case where the data acquired by the X-ray diffraction profile/diffraction intensity map acquisition unit 17 is a diffraction intensity map, it is determined in step S200 whether calculation has been performed for all the positions, and in a case where calculation has not been performed for all the positions, step S100 is performed.
When there are a plurality of compositions (having different crystal structures) for which the orientation degree distribution is to be measured in the sample, the above calculation is repeated for each composition to determine the orientation degree distribution function f(φm).
(Orientation Degree Distribution/Average Orientation Degree/Orientation Degree Space Map Output Unit)
An orientation degree distribution/average orientation degree/orientation degree space map output unit 20 displays the orientation degree distribution analyzed by the orientation degree distribution analysis unit 19 on the X-ray diffraction profile, and when the data stored in the main storage device 5 in the diffraction intensity map acquisition unit 17 is the diffraction intensity map, the orientation degree spatial map on the output device 10 such as a display. In the present specification, the “spatial map of orientation degree distribution” refers to a diagram in which the orientation degree and the position thereof are associated with each other. The orientation degree distribution/average orientation degree/orientation degree space map output unit 20 is realized when the CPU 3 performs processing of reading the analysis result of the orientation degree distribution function f(φm) from the auxiliary storage device 4 or the like and displaying the analysis result on the output device 10 such as a display, and the display displays the analysis data.
An example in which the orientation degree distribution calculation of the Sm2Fe17N3 bonded magnet is performed using the above orientation degree distribution calculation method will be described.
(Calculation of Angle φm Formed by Orientation Plane and Crystal Plane Corresponding to Diffraction Peak of Interest)
According to a PDF card of Sm2Fe17N3; (ICDD Card No.: 00-048-1790) (hereinafter, referred to as Non Patent Literature 2), the crystal structure of Sm2Fe17N3 is a rhombohedral crystal system, and the lattice constants are a=8.74 and c=12.66, respectively. From this data, Table 1 shows the results of calculating the angle (φm) formed by the orientation plane (in the case of this example, the (001) plane orthogonal to the c-axis which is the axis of easy magnetization) calculated using Formula (5) and the crystal plane corresponding to the diffraction peak of interest. In Table 1, calculation results for only peaks between diffraction angles of 30 to 60 degrees among certain diffraction peaks described in the PDF card are described.
(Determination of Weight Function w(φm))
In addition, in order to determine the weight function w(φm), rocking curve measurement was performed in this example. A commercially available Sm2Fe17N3 fine powder (average particle diameter: about 2 μm) was mixed with an epoxy resin and then filled in a nonmagnetic mold, and then cured in a static magnetic field of 2.2 T to prepare a bonded magnet in which the Sm2Fe17N3 fine powder was oriented substantially parallel to the magnetic field direction.
(Existence Ratio of Particles Whose Crystal Planes are Oriented in Direction Corresponding to Diffraction Angle θ in Randomly Oriented Sample)
The existence ratio S of the particles whose crystal planes are oriented in the direction corresponding to the diffraction angle θ in the randomly oriented sample is calculated as shown in Table 2 from Formula (8) using the data of Non Patent Literature 2 described above.
(Determination of Orientation Degree Distribution Function f(φm))
For f(φm), the orientation degree distribution can be calculated with high accuracy by using a distribution function capable of sufficiently simulating the orientation degree distribution of the sample to be measured. However, when an attempt is made to experimentally determine the functional form of the orientation degree distribution function, it is necessary to examine the crystal orientation of all the crystal grains constituting the magnet with respect to the magnet having various orientation degrees, and the number of crystal grains to be measured is too large, which is extremely difficult in practice. Therefore, as a method for examining the orientation directions of all the crystal grains constituting the magnet having various orientation degrees, in this example, the distribution of the orientation directions of the particles was analyzed using discrete element method simulation.
However, since the orientation directions of the crystal grains inside the magnet are always distributed between 0 degrees and 90 degrees, it is not possible to sufficiently simulate the actual orientation degree distribution if the orientation degree distribution function is assumed to be normal distribution and lognormal distribution in which a definition range is from −∞ to +∞ and from 0 to +∞.
Therefore, in the present embodiment, the truncated log-normal distribution represented by the following formula is assumed as a functional form that has a definition range of 0 degrees to 90 degrees and can sufficiently simulate all orientation degree distributions obtained by numerical calculation of the orientation magnet.
Here, the auxiliary variables μ and σ are distributed between φl≤φm≤φu with a scale parameter and a shape parameter, respectively. The functions erf and ln are respectively an error function and a natural logarithm. The result of approximation of the distribution in the orientation direction by Formula (12) is the solid line shown in
(Analysis of Orientation Degree Distribution)
Since diffraction peaks other than the (006) plane are observed in all the samples, the samples are not completely oriented. Sample A has the highest diffraction intensity of the (006) plane and the lowest intensity of the other peaks as compared with the other samples, and thus has the highest orientation degree among the samples used for the measurement this time. Conversely, Sample C is estimated to have the lowest orientation degree because the diffraction intensity of the (006) plane is the lowest and the intensities of the other peaks are high.
A case where the same Sm2Fe17N3 bonded magnet as that prepared in Example 1 is used as a measurement target, a diffraction intensity map is acquired using a micro-focal X-ray source, and spatial mapping of the orientation degree is performed will be described.
The measured sample was the same sample as Sample A in
The focusing lens is obtained by bundling several millions of glass capillaries each having a diameter of about 5 micrometers with light from an X-ray point light source, and is a device capable of obtaining a pseudo-parallel X-ray beam having a spot diameter of about 50 micrometers by guiding X-rays while totally reflecting the X-rays inside. The measured area was about 4 mm3, and the measurement area was divided into 50 μm squares for measurement. The number of measurement points is 63 points in the vertical direction and 25 points in the horizontal direction, that is, a total of 1575 points.
This indicates that a guideline for improving the orientation degree can be obtained by visualizing the orientation degree map using the present invention.
Note that the above examples merely show specific examples for calculating the orientation degree distribution and the orientation degree map according to the present invention, and the technical scope of the present invention should not be interpreted in a limited manner by these examples. The present invention can be implemented in various forms without departing from the technical idea or the main features thereof.
According to the orientation distribution calculation method of the present invention, since the orientation degree distribution and the orientation degree map can be easily calculated from the X-ray diffraction profile of the sample to be measured, the X-ray diffraction profile of the non-oriented sample, and the crystal structure information of the sample to be measured, the method is effective for various materials in which properties such as electrical and thermal conductivity, magnetic properties, piezoelectricity, optical transparency, and magnetic properties change depending on the crystal orientation. Therefore, it can be expected to be applied to a wide range of fields such as various magnetic materials such as permanent magnet materials, high-frequency materials, and soft magnetic materials, various ceramic materials whose characteristics change due to crystal orientation, such as honeycomb ceramics for automobile exhaust gas, and fiber-reinforced plastics.
Number | Date | Country | Kind |
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2019-158868 | Aug 2019 | JP | national |
Filing Document | Filing Date | Country | Kind |
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PCT/JP2020/030586 | 8/11/2020 | WO |
Publishing Document | Publishing Date | Country | Kind |
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WO2021/039379 | 3/4/2021 | WO | A |
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2006-258616 | Sep 2006 | JP |
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Number | Date | Country | |
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20220291153 A1 | Sep 2022 | US |