Name: crystal structure using x-ray diffraction
Uploaded: 2023-04-30T07:02:53.000Z
Duration: 9 min 31 s
Channel: JoVE

K12 Standards

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Ohio’s Learning Standards and Model Curriculum

9-12

Physical Geology

Minerals

Crystallinity (crystal structure)

X-ray Diffraction

The following procedure applies to a specific XRD instrument and its associated software, and there may be some variations when other instruments are used.
<ol>
	<li>We will examine a Ni powder sample on a Panalytical Alpha-1 XRD instrument.</li>
	<li>First, choose the mask to fix the beam size according to your sample diameter. The beam must not have a footprint larger than the sample at the smallest &#952; value (typically ~ 70-100). For a sample of width &#949;, the beam size should be &#60; &#949; sin&#952;.</li>
	<li>Load the sample in the sample spinner stage and lock the sample into position. The sample spinner helps to spatially randomize the exposure of the sample to the X-ray source.</li>
	<li>Choose the angle range for your XRD scan. For example 15-90 degrees is a typical range.</li>
	<li>Choose a step size, i.e. the increment in 2&#952;, and integration (counting) time. Generally a 0.05 degree step size and 4 seconds integration is the default for a wide angle scan.</li>
	<li>Once all the peak positions are determined through this initial scan, subsequent scans can focus on a narrower scan range around specific peaks using a smaller step size in angle if higher resolution data from those peaks are desired.</li>
</ol>

This is a demonstration of a standard XRD experiment. The material examined in this experiment was in a powder form, but XRD works equally well with solid piece of material as long as the sample has a flat surface that can be set parallel to the plane of the sample stage.
XRD is a fairly ubiquitous method for determining the presence (or absence) of crystallographic order in materials. Beyond the standard application of determining the crystal structure, XRD is often used to obtain a variety of other structural information such as:
<ol>
	<li>Whether or not the structure of a material is amorphous (characterized by a broad hump in the diffraction intensity and a lack of discernable crystallographic peaks),</li>
	<li>Whether the sample is a composite material consisting of multiple crystallographic phases and, if so, determine the fraction of each phase,</li>
	<li>Determining whether a material is an amorphous/crystalline composite</li>
	<li>Determining the grain/particle size of the material,</li>
	<li>Determining the degree of texture (preferred orientation of grains) in material.</li>
</ol>

Relationship between diffracted peak positions and crystal structure:
When light waves of sufficiently small wavelength are incident upon a crystal lattice, they diffract from the lattice points. At certain angles of incidence, the diffracted parallel waves constructively interfere and create detectable peaks in intensity. W.H. Bragg identified the relationship illustrated in Figure 1 and derived a corresponding equation:
nλ = 2dhkl sin θ [1]
Here λ is the wavelength of the X-rays used, dhkl is the spacing between a particular set of planes with (hkl) Miller indices*, and θ is the angle of incidence at which a diffraction peak is measured. Finally, n is an integer that represents the 'harmonic order' of the diffraction. At n=1, for example, we have the first harmonic, meaning that the path of X-rays diffracted through the crystal (equivalent to 2dhkl sin ) is exactly 1λ, while at n=2, the diffracted path is 2λ. We can typically assume n=1, and, in general, n=1 for θ &lt; sin-1(2λ/dh'k'l'), where h'k'l' are the Miller indices of the planes that show the first peak (at the lowest 2θ value) in a diffraction experiment. Miller indices are a set of three integers that constitute a notation system for identifying directions and planes within crystals. For directions, the [h k l] Miller indices represent the normalized difference in the respective x, y and z coordinates (in a Cartesian coordinate system) of two points along the direction. For planes, the Miller indices (h k l) of a plane are simply the h k l values of the direction perpendicular to the plane.
In a typical XRD experiment in reflection mode, the X-ray source is fixed in position and the sample is rotated with respect to the X-ray beam over θ. A detector picks up the diffracted beam and has to keep up with the sample rotation by rotating at twice the rate (i.e. for a given sample angle of θ, the detector angle is 2θ). The geometry of the experiment is schematically shown in Figure 1.
<img alt="X-ray diffraction diagram; setup showing Bragg's law, θ angles, crystal lattice, X-ray source/detector." src="/files/ftp_upload/10446/10446fig1v2.jpg" data-altupdatedat="1761830439000" data-alt="Figure 1"> 
Figure 1: Illustration of Bragg's Law.
When a peak in intensity is observed, equation 1 is necessarily satisfied. Consequently, we can calculate d-spacings based on the angles at which these peaks are observed. By calculating the d-spacings of multiple peaks, the crystal class and the crystal structure parameters material sample can be identified using a database such as the Hanawalt Search Manual or database libraries available with the XRD software being used.
We will be assuming that the sample being investigated is not a single crystal. If the sample were a single crystal with a particular (h*k*l*) plane parallel to the sample surface, it would need to be rotated until the Bragg condition for the (h*k*l*) is satisfied in order to see a peak in diffracted intensity (for n=1) with potentially higher harmonic (h*k*l*) peaks (e.g. for n=2) also detectable at higher angles. At all other angles there would be no peaks in a single crystal sample. Instead, let's assume that the sample is either polycrystalline or that it is a powder, with a statistically significant number of crystalline grains or powder particles illuminated by the incident X-ray beam. Under this assumption, the sample consists of randomly oriented grains, with a similar statistical probability for all possible lattice planes to diffract.
The relationships between the dhkl and the unit cell parameters are shown below in Equations 2-7 for the 7 crystal classes, cubic, tetragonal, hexagonal, rhombohedral, orthorhombic, monoclinic and triclinic. The unit cell parameters consist of lengths of (a,b,c) and the angles between (α, β, γ) the edges of the unit cells for the 7 crystal classes (Figure 1x shows the example of one of the crystal classes: the tetragonal structure where a=b≠c, and α=β=γ=900). Using multiple diffracted peak positions (i.e. several distinct dhkl values), the values of the unit cell parameters can be solved uniquely.
<img alt="Orthorhombic crystal system diagram, a≠b≠c, angles α=β=γ=90°, axial dimensions labeled." src="/files/ftp_upload/10446/10446fig2.jpg" data-altupdatedat="1761830439000" data-alt="Figure 2"> 
Figure 2: The tetragonal structure as one of the seven crystal classes.
Cubic (a = b = c; α = β = γ = 900):
<img alt="Crystallography equation, d_hkl formula, lattice spacing calculation formula." src="/files/ftp_upload/10446/10446eq1.jpg" style="opacity: 0.9; font-size: 14px;" data-altupdatedat="1761830439000" data-alt="Equation 1">  [2]
Tetragonal (a = b ≠ c; α = β = γ = 900):
<img alt="Crystallography equation; inverse lattice spacing formula; reciprocal lattice parameters analysis." src="/files/ftp_upload/10446/10446eq2.jpg" style="opacity: 0.9; font-size: 14px;" data-altupdatedat="1761830439000" data-alt="Equation 2">  [3]
Hexagonal (a = b ≠ c; α = β = 900; γ = 1200):
<img alt="Crystallography equation for hexagonal lattice structure, key formula used in X-ray diffraction." src="/files/ftp_upload/10446/10446eq3.jpg" style="opacity: 0.9; font-size: 14px;" data-altupdatedat="1761830439000" data-alt="Equation 3">  [4]
Orthorhombic (a ≠ b ≠ c; α = β = γ = 900):
<img alt="Three-dimensional geometry equation for ellipsoid; mathematical formula exploration." src="/files/ftp_upload/10446/10446eq4.jpg" style="opacity: 0.9; font-size: 14px;" data-altupdatedat="1761830439000" data-alt="Equation 4">  [5]
Rhombohedral (a = b ≠ c; α = β = γ = 900):
<img alt="Crystallography formula for d-spacing; mathematical equation; X-ray diffraction analysis." src="/files/ftp_upload/10446/10446eq5.jpg" style="opacity: 0.9; font-size: 14px;" data-altupdatedat="1761830439000" data-alt="Equation 5">  [6]
Monoclinic (a ≠ b ≠ c; α = γ = 900 ≠ β):
<img alt="Crystallography formula, reciprocal lattice equation, mathematical derivation, structural analysis." src="/files/ftp_upload/10446/10446eq6.jpg" style="opacity: 0.9; font-size: 14px;" data-altupdatedat="1761830439000" data-alt="Equation 6">  [7]
Triclinic (a ≠ b ≠ c; α ≠ β ≠ γ ≠ 900): 
      <img alt="Crystallography formula diagram; reciprocal lattice vector calculation for X-ray diffraction analysis." src="/files/ftp_upload/10446/10446eq8v2.jpg" data-altupdatedat="1761830439000" data-alt="Equation 7">  [8] 
Relationship between diffracted peak intensities and crystal structure:
Next we examine the factors that contribute to the intensity in an XRD pattern. The factors can be broken down as 1) the contribution to scattering that results directly from the unique structural aspects of the material (the specific types and locations of scattering atoms in the structure) and 2) those that are not specific to the material. In the former, there are two factors: the 'absorption factor' and the 'structure factor'. The absorption factor primarily depends on the ability of the material to absorb X-rays on their way in and out. This factor does not have a θ dependence as long as the samples are not thin (the sample should be &gt; 3 times thicker than the attenuation length of the X-rays). In other words, the contribution by the absorption factor to the intensity of different peaks is constant. The 'structure factor' directly affects the intensity of specific peaks as a direct result of the structure. The remaining factors, the 'multiplicity', which accounts for all the planes that belong to the same family because they are symmetrically related, and the 'Lorentz-Polarization' factor, which comes from the geometry of the XRD experiment, also affect the relative intensity of the peaks but they are not specific to a material and can easily be accounted for with analytical expressions (i.e. XRD analysis software can remove them with analytical functions).
<img alt="Ray optics diagram illustrating light reflection and refraction paths through a prism." src="/files/ftp_upload/10446/10446fig3.jpg" data-altupdatedat="1761830439000" data-alt="Figure 3"> 
Figure 3: Three diffraction ray paths, of which rays 11' and 22' satisfy the Bragg condition, while ray 33' results from scattering by an atom (red circle) at an arbitrary position. 
As the only factor that carries the unique structural contribution of a material to the relative intensities of XRD peaks, the structure factor is very important and requires a closer look. In Figure 2, let us assume that the 1st order Bragg diffraction condition (remember, that this corresponds to n=1) is satisfied between ray11' and ray22' which are scattered on two atomic planes in the h00 direction (using the Miller indices notation described earlier) separated by a distance d. Under this condition, the difference in path length between ray11' and ray22' is δ(22'-11') = SA + AR = λ. The phase shift between the diffracted rays 1 and 2 is, therefore, Φ22'-11' = (δ(22'-11')/λ) 2π = 2π (assuming a cubic symmetry and, therefore, d = a/h in the h00 direction].
With a few steps in analytical geometry, it can be shown that the phase shift, Φ(33'-11'), with ray 3 diffracted by an arbitrary plane of atoms that are spaced an arbitrary distance x, is given by: Φ(33'-11') = 2πhu, where u=x/a (a is the unit cell parameter in the (h00) direction.) Taking the two other orthogonal directions, (0k0) and (00l), and v=y/a and w=z/a as fractional coordinates in the y- and z-directions, the expression for the phase shift extends to Φ = 2π(hu+kv+lw). Now, the X-ray wave scattered by the j-th atom in a unit cell will have a scattering amplitude of fj and a phase of Φj, such that the function describing it is <img alt="Mathematical exponential function formula; physics, engineering calculation; e^phi expression." src="/files/ftp_upload/10446/10446eq8.jpg" style="opacity: 0.9; font-size: 14px;" data-altupdatedat="1761830439000" data-alt="Equation 8">. The structure factor we seek, therefore, is the sum of all the scattering functions due to all the unique atoms in a unit cell. This structure factor, F, is given as:
<img alt="Crystallography equation, Fourier transform formula, mathematical notation in scientific research." src="/files/ftp_upload/10446/10446eq9v2.jpg" data-altupdatedat="1761830439000" data-alt="Equation 9">  [9]
and the intensity factor contributed by the structure factor is I = F2.
Based on the positions (u,v,w) of atoms on particular planes (h,k,l), there is the possibility of interference between scattered waves that is constructive, destructive, or in-between, and this interference directly affects the amplitude of the XRD peaks representing the (hkl) planes.
Now, a plot of intensity, I, versus 2θ is what is measured in an XRD experiment. The determination of the of crystal type and the associated unit cell parameters (a, b, c, α, β, and γ) can be arrived at analytically by observing systematic presence/absence of peaks, using the equations 2-9, comparing values against databases, using deduction and a process of elimination. Nowadays, this is process is fairly automated by a variety of software linked to crystal structure databases.

x-ray diffraction

Source: Faisal Alamgir, School of Materials Science and Engineering, Georgia Institute of Technology, Atlanta, GA
X-ray diffraction (XRD) is a technique used in materials science for determining the atomic and molecular structure of a material. This is done by irradiating a sample of the material with incident X-rays and then measuring the intensities and scattering angles of the X-rays that are scattered by the material. The intensity of the scattered X-rays are plotted as a function of the scattering angle, and the structure of the material is determined from the analysis of the location, in angle, and the intensities of scattered intensity peaks. Beyond being able to measure the average positions of the atoms in the crystal, information on how the actual structure deviates from the ideal one, resulting for example from internal stress or from defects, can be determined.
The diffraction of the X-rays, that is central to the XRD method, is a subset of the general X-ray scattering phenomena. XRD, which is generally used to mean can wide-angle X-ray diffraction (WAXD), falls under several methods that use the elastically scattered X-ray waves. Other elastic scattering based X-ray techniques include small angle X-ray scattering (SAXS), where the X-rays are incident on the sample over the small angular range of 0.1-100 typically). SAXS measures structural correlations of the scale of several nanometers or larger (such as crystal superstructures), and X-ray reflectivity that measures the thickness, roughness, and density of thin films. WAXD covers an angular range beyond 100.

In Figure 4 we see the XRD peaks for the Ni powder sample. Note that the peaks that are observed (e.g. {111}, {200}) are for those that have either all even or all odd combinations of h, k, and l. Ni is face-centered cubic (FCC), and in all FCC structures, the peaks corresponding to {hkl} planes where h, k, and l are mixtures of even and odd integers, are absent due to the destructive interference of the scattered X-rays. Peaks corresponding to planes, such as {210} and {211} are missing. This phenomenon is called the systematic presence and absence rules, and they provide an analytical tool for assessing the crystal structure of the sample.
<img alt="X-ray diffraction pattern, intensity vs. 2-theta, crystal structure analysis, peak identification." class="xfigimg" src="/files/ftp_upload/10446/10446fig4.jpg" data-altupdatedat="1761830439000" data-alt="Figure 4"> 
Figure 4: An XRD scan of Ni with a face-centered cubic structure is shown.

Source: Faisal Alamgir, School of Materials Science and Engineering, Georgia Institute of Technology, Atlanta, GA
X-ray diffraction (XRD) is a technique ...

X-Ray diffraction is a technique used to determine the atomic and molecular structure of materials. Solids have a crystalline structure, which corresponds to a microscopic arrangement of atoms that is repeated periodically. By staking planes, a 3-D structure of specific symmetry can be formed.These structural arrangements result in a specific packing geometry that dictates the physical and chemical properties of the material. Such as magnetization, thermal conductivity, or malleability. Reflecting x-rays off of materials can reveal the inner details of their structure.This video will illustrate the general principles of x-ray diffraction on a material and how this phenomenon is used in the laboratory to determine the structure and chemical composition of materials.To begin, let's have a closer look at a crystal. It is formed of atomic lattices disposed in planes periodically separated by a distance dhkl of a few angstroms. H, k, l are Miller indices, a set of three integers the constitute a notation system for identifying directions and planes within crystals. The smallest repeating structure in a crystal is called the unit cell. Different angles, alpha, beta, gamma, and lengths a, b, c, of a unit cell forming the lattice will give rise to different symmetries. There are seven crystal systems. Cubic, tetragonal, orthorhombic, rhombohedral, monoclinic, triclinic, and hexagonal.The relationship between the unit cell parameters and the Miller indices can be calculated for each crystal class. Electromagnetic of wavelength lambda can have similar dimensions with the differences between planes within the crystal's lattice. These correspond to wavelengths in the x-ray spectral range. When x-ray light waves irradiate a crystal at an incident angle theta, they propagate through the crystal and encounter lattice points from which they defract. Bragg's Law relates these parameters where n is an integer that represents the harmonic order of the diffraction. For a given lambda, only specific angles theta give rise to diffraction. This is the unique signature of a crystalline structure.In an experiment, the sample is rotated and the detector that collects the scattered x-rays records peaks in intensity when reaching these characteristic angles. One can then extract the lattice spacing DHKL for each angle satisfying the Bragg's Law. Using multiple diffracted peak positions corresponding to several distinct DHKL values, the parameters of the unit cell can be solved uniquely.Two main factors contribute to the relative intensity of the peaks. First, there are the non-structural contributions, which include the ability of the material to absorb x-ray light, and the geometry of the XRD experiment. These can be taken into account in the post-processing of the experimental data. Second, and most importantly, the structural contribution of the material is carried to the relative intensities of XRD. Each diffraction peak is in fact the sum of all the scattered amplitudes from multiple ray paths diffracted by all the unique atoms in a unit cell. If scattered lights are in phase, there is constructed interference. While if they are out of phase, there is destructed interference. These interferences directly affect the amplitude of the XRD peaks, representing the HKL planes of the crystal.We will now see how these principles apply in an actual x-ray diffraction experiment.Before starting, carefully inspect the XRD instrument and assess its status and safety. XRD users must be trained in basic radiation safety before having access to the instrument. Then proceed with sample preparation. In this experiment, we use a nickel powder sample in the form of a pressed pellet.It is important that the sample is not thin and it should be at least three times thicker than the attenuation length of the x-rays. Note that the following procedure applies to a specific XRD instrument and its associated software and there may be some variations when other instruments are used.Load the sample in the sample spinner stage and lock the sample into position, making sure the irradiated side of the sample is parallel to the sample stage. Use a mask to adjust the x-ray beam size of the instrument according to the sample diameter. At the smallest incident angle, the beam must have a footprint smaller than the sample width.Now it is time to choose the acquisition parameters. First, select the angle range for the XRD scan. Typically, the range goes from 15 to 90 degrees. Then, select the degree step size as well as the integration time at each angle scanned.Next, proceed to the data acquisition. After the scan, a graph of the intensity as a function of the angle to theta is obtained. From this initial scan, select specific peaks and determine peak positions.Repeat the acquisition and focus this time on a narrower scan range around specific peaks. Using a smaller step size in angle to obtain higher resolution data. Once the data acquisition is finished, data can be analyzed to identify the structure of the material.Using the instrument software and database library, each peak of the spectrum is identified and associated to a specific symmetry of crystal arrangement. In this particular case of the nickel powder sample, the spectrum shows a first peak corresponding to a one one one symmetry.The second peak is associated to a two zero zero symmetry and so on. Then the software determines that this specific combination of symmetries corresponds to a face centered cubic structure and it identifies that the sample is a nickel powder.X-ray diffraction is a standard method for determining the presence or absence of crystallographic order in materials. It is often used to obtain a variety of other structural information regarding internal stress and defects in a crystal, or multiple crystallographic phases in composite materials. XRD technique is also used in biology to determine the structure and spatial orientation of biological macromolecules such as proteins and nucleic acids.In particular, this is how the double helix structure of DNA has been discovered, leading to the Nobel Prize in Physiology or Medicine in 1962. The study of the geochemistry of minerals either for mining purposes or even for planetary exploration also makes use of XRD technique. Think of the Rover Curiosity on Mars that has amongst its ten scientific instruments an XRD detector to analyze the composition of the martian soil.You've just watched Jove's introduction to x-ray diffraction. You should now understand the crystalline structure of a solid and the principles of x-ray diffraction. You should also know how the XRD technique is used in the laboratory to obtain the structure and chemical composition of materials.Thanks for watching!

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crystal structure using x-ray diffraction

X-ray diffraction is a materials science method for finding crystal structure. It uses incident X-rays that strike a sample and scatter from its atoms and molecules. The scattered X-rays are measured by their intensity and scattering angle.

The results are plotted as intensity versus angle. Scientists then analyze the position of the peaks and their strength to determine the structure of the material. This method can also show how a real crystal differs from an ideal one. It can reveal effects such as internal stress and defects.

X-ray diffraction is part of a broader group of X-ray scattering methods. It is often used to mean wide-angle X-ray diffraction, or WAXD. WAXD covers scattering at angles above 10 degrees.

Other elastic scattering methods include small angle X-ray scattering, or SAXS, and X-ray reflectivity. SAXS uses a small angular range of about 0.1 to 10 degrees and measures structural correlations on the scale of several nanometers or larger, such as crystal superstructures. X-ray reflectivity is used to measure the thickness, roughness, and density of thin films.

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This collection features cutting-edge methods for analysis and characterization of materials, and introduces a range of advanced materials and processes for new technologies and applications.

Learn how X-ray diffraction uses scattered X-rays to identify crystal structure, detect defects, and distinguish WAXD, SAXS, and X-ray reflectivity.

Crystal Structure Using X-ray Diffraction | JoVE K12

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Criteria of a mineral (crystalline solid, occurs in nature, inorganic, defined chemical composition)

Virginia  Standards of Learning

HIgh School

Earth Science

ES.4

ES.4.c

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Motion and Stability: Forces and Interactions

C-PS2-6.

Faisal Alamgir

School of Materials Science and Engineering

Georgia Institute of Technology

Overview

Principles of X-ray Diffraction

Instrument, Sample and Beam Parameters

Selection of the Parameters for the Acquisition

Acquisition and Analysis

Results

Applications

Summary

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Physical Properties Of Minerals II: Polymineralic Analysis

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Physical Properties Of Minerals I: Crystals and Cleavage

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The physical properties of minerals comprise various measurable and discernible ...

Atoms and elements

Content elaboration: This unit builds upon the Earth and Space Science strand in grade 6, where common minerals are defined, tested and classified. It also incorporates knowledge of mineral properties and crystalline structures (chemical compositions and bonding) included in the chemistry sections of other high school courses. The emphasis in this course is to relate the chemical and physical components of minerals to the properties of the minerals. This requires extensive mineral testing, investigations, experimentation, observation, use of technology and models/modeling. The focus is on learning the ways to research, test and evaluate minerals, not in memorization of mineral names or types. Properties such as cleavage and hardness are connected to the chemical structure and bonding of the mineral. In addition, the environment in which minerals form should be part of the classification of the mineral, using mineral data to help interpret the environmental conditions that existed during the formation of the mineral.

Atoms and elements

Types of Chemical Bonds

Chemical bonding theories were pioneered by American chemist Gilbert&#xA0;N. Lewis. He developed a model called the Lewis model to explain the type and ...

Ionic Bonds

When atoms gain or lose electrons to achieve a more stable electron configuration they form ions. Ionic bonds are electrostatic attractions between ions ...

Ionic Bonding and Electron Transfer

Ions are atoms or molecules bearing an electrical charge. A cation (a positive ion) forms when a neutral atom loses one or more electrons from its valence ...

Lewis Symbols and the Octet Rule

Chemical bonds are complex interactions between two or more atoms or ions, which reduce the potential energy of the molecule. Gilbert N. Lewis developed a ...

Chemical Bonds


Atoms participate in a chemical bond formation&#160;to acquire a completed valence-shell electron configuration similar to that of the noble gas nearest ...

Covalent Bonding and Lewis Structures

Compared to ionic bonds, which results from the transfer of electrons between metallic and nonmetallic atoms, covalent bonds result from the mutual ...

Bonding in Metals

Metallic bonds are formed between two metal atoms. A simplified model to describe metallic bonding has been developed by Paul Dr&#xFC;de called the ...

soil-nutrient-analysis-nitrogen-phosphorus-and-potassium

Soil Nutrient Analysis: Nitrogen, Phosphorus, and Potassium

Source: Laboratories of Margaret Workman and Kimberly Frye - Depaul University
In this experiment, three soil macronutrients are chemically extracted, ...

Chemical bonding (ionic, covalent, metallic)

Content elaboration: This unit builds upon the Earth and Space Science strand in grade 6, where common minerals are defined, tested and classified. It also incorporates knowledge of mineral properties and crystalline structures (chemical compositions and bonding) included in the chemistry sections of other high school courses. The emphasis in this course is to relate the chemical and physical components of minerals to the properties of the minerals. This requires extensive mineral testing, investigations, experimentation, observation, use of technology and models/modeling. The focus is on learning the ways to research, test and evaluate minerals, not in memorization of mineral names or types. Properties such as cleavage and hardness are connected to the chemical structure and bonding of the mineral. In addition, the environment in which minerals form should be part of the classification of the mineral, using mineral data to help interpret the environmental conditions that existed during the formation of the mineral.

Chemical bonding (ionic, covalent, metallic)

Structures of Solids

Solids in which the atoms, ions, or molecules are arranged in a definite repeating pattern are known as crystalline solids. Metals and ionic compounds ...

Ionic Crystal Structures

Ionic crystals consist of two or more different kinds of ions that usually have different sizes. The packing of these ions into a crystal structure is ...

X-ray Crystallography

The size of the unit cell and the arrangement of atoms in a crystal may be determined from measurements of the diffraction of X-rays by the crystal, ...

Classifying Matter by Composition

Matter: Pure Substances and Mixtures
According to its composition, the matter can be classified into two broad categories &mdash; pure substances and ...

Optical Materialography Part 2: Image Analysis

Source: Faisal Alamgir, School of Materials Science and Engineering, Georgia Institute of Technology, Atlanta, GA
The imaging of microscopic structures of ...

X-ray Photoelectron Spectroscopy

Source: Faisal Alamgir, School of Materials Science and Engineering, Georgia Institute of Technology, Atlanta, GA
X-ray photoelectron spectroscopy (XPS) ...

Crystallinity (crystal structure)

Content elaboration: This unit builds upon the Earth and Space Science strand in grade 6, where common minerals are defined, tested and classified. It also incorporates knowledge of mineral properties and crystalline structures (chemical compositions and bonding) included in the chemistry sections of other high school courses. The emphasis in this course is to relate the chemical and physical components of minerals to the properties of the minerals. This requires extensive mineral testing, investigations, experimentation, observation, use of technology and models/modeling. The focus is on learning the ways to research, test and evaluate minerals, not in memorization of mineral names or types. Properties such as cleavage and hardness are connected to the chemical structure and bonding of the mineral. In addition, the environment in which minerals form should be part of the classification of the mineral, using mineral data to help interpret the environmental conditions that existed during the formation of the mineral.

single-crystal-and-powder-x-ray-diffraction

Single Crystal and Powder X-ray Diffraction

Source: Tamara M. Powers, Department of Chemistry, Texas A&#38;M University&#160;
X-ray crystallography is a technique that uses X-rays to study the ...

determining-the-solubility-rules-of-ionic-compounds

Determining the Solubility Rules of Ionic Compounds

Source: Laboratory of Dr. Neal Abrams &#8212; SUNY College of Environmental Science and Forestry
An ionic compound&#39;s solubility can be determined via ...

Criteria of a mineral (crystalline solid, occurs in nature, inorganic, defined chemical composition)

Content elaboration: This unit builds upon the Earth and Space Science strand in grade 6, where common minerals are defined, tested and classified. It also incorporates knowledge of mineral properties and crystalline structures (chemical compositions and bonding) included in the chemistry sections of other high school courses. The emphasis in this course is to relate the chemical and physical components of minerals to the properties of the minerals. This requires extensive mineral testing, investigations, experimentation, observation, use of technology and models/modeling. The focus is on learning the ways to research, test and evaluate minerals, not in memorization of mineral names or types. Properties such as cleavage and hardness are connected to the chemical structure and bonding of the mineral. In addition, the environment in which minerals form should be part of the classification of the mineral, using mineral data to help interpret the environmental conditions that existed during the formation of the mineral.

physical-and-chemical-properties-of-matter

Physical and Chemical Properties of Matter

The characteristics that enable us to distinguish one substance from another are called properties.

Physical Properties of Matter

A physical property is ...

Metallic Solids

Metallic solids such as crystals of copper, aluminum, and iron are formed by metal atoms. The structure of metallic crystals is often described as a ...

Properties of Transition Metals

Transition metals are defined as those elements that have partially filled d orbitals. As shown in Figure 1, the d-block elements in groups 3&#8211;12 are ...

stress-strain-characteristics-of-aluminum

Stress-Strain Characteristics of Aluminum

Source:&#160;Roberto Leon, Department of Civil and Environmental Engineering, Virginia Tech, Blacksburg, VA
Aluminum is one of the most abundant materials ...

an-overview-of-bgdgt-biomarker-analysis-for-paleoclimatology

An Overview of bGDGT Biomarker Analysis for Paleoclimatology

Source: Laboratory of Jeff Salacup&#160;- University of Massachusetts Amherst
Throughout this series of videos, natural samples were extracted and ...

an-overview-of-alkenone-biomarker-analysis-for-paleothermometry

An Overview of Alkenone Biomarker Analysis for Paleothermometry

Properties of minerals (hardness, luster, cleavage, streak, crystal shape, fluorescence, flammability, density/specific gravity, malleability)

Content elaboration: This unit builds upon the Earth and Space Science strand in grade 6, where common minerals are defined, tested and classified. It also incorporates knowledge of mineral properties and crystalline structures (chemical compositions and bonding) included in the chemistry sections of other high school courses. The emphasis in this course is to relate the chemical and physical components of minerals to the properties of the minerals. This requires extensive mineral testing, investigations, experimentation, observation, use of technology and models/modeling. The focus is on learning the ways to research, test and evaluate minerals, not in memorization of mineral names or types. Properties such as cleavage and hardness are connected to the chemical structure and bonding of the mineral. In addition, the environment in which minerals form should be part of the classification of the mineral, using mineral data to help interpret the environmental conditions that existed during the formation of the mineral.

properties-minerals-hardness-luster-cleavage-streak-crystal-shape

Crystal Structure Using X-ray Diffraction

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