Cheiron School 2011

BL10XU: High Pressure Research
The undulator beamline BL10XU is dedicated for X-ray diffraction experiments at highpressure and low/high temperature using a diamond anvil cells (DAC) (Figure 1) [Ohishi et al.
(2008) High Press. Res., 28, 163.]. The high-resolution monochromatic angle-dispersive X-ray
diffraction patterns obtained at BL10XU allow us to make an accurate determination ofequations of state, precise determination of phase relation, structure refinement by Rietveld
analysis, and charge density distribution analysis in crystals submitted to extreme pressures.
High pressure is possible to change physical, chemical, and structural characteristics ofmaterials through a change of its volume or distance between atoms (or molecules). The
high-pressure properties are drastically different from those known at ambient pressure.
Pressure thus serves as a versatile tool in material research, and it is also important in theinvestigation of the deep interior of the Earth and other planets. To learn high-pressure
phenomena in the BL practice course, in-situ high-pressure X-ray diffraction experiments will
be performed using a combination of synchrotron radiation and a DAC technique.

Figure1. Schematic layout of beamline BL10XU [1].

Diamond anvil cell

Diamond anvil cell is one of high-pressure
generation techniques by static compression. The
sample is placed in a pressure chamber createdbetween the flat parallel faces (culets) of two opposed
diamond anvils and the hole penetrating a hardened
metal foil (the gasket) (Figure 2). Pressure is applied
by forcing the diamonds together. Diamond is thepremier anvil material because of hardest substanceand transparency to electromagnetic radiation over awide spectral range from the infrared to hard X-rays.

Figure 2. Diamond-anvil cellEnergy calibration
Angle dispersive X-ray diffraction (XRD) requires a monochromatic X-ray beam. The
accurate determination of the wavelength for incident X-ray beam and of the distance between
sample and detector of imaging plate (IP) allow to determine precise crystal structures and theunit-cell parameters of materials. In this practice, we use photon energy tuned to 30 keV(0.4133 Å) for the XRD measurement. The calibration of the X-ray wavelength and the distanceis based on the standard material of cerium oxide (celia, CeO2).

– Practice –Observe a structural phase transition of sodium chloride (NaCl) at high pressure and obtain
the parameters of Equation of State (EOS) for NaCl from in-situ X-ray diffraction data.

1) Sample preparation
The sample is set up in a chamber created between the culets of two opposed diamondanvils and the gasket hole. The gasket in anvil devices serves three critical functions: (1)encapsulating the sample, (2) building a gradient from ambient to the peak pressure, and (3)supporting the tip of anvils. Gasket material, hole size of sample chamber, and thickness are
critical for generating high pressure.
In this practice, for efficiency measurement we use a gas-membrane DAC. A sample ofNaCl powder is placed in a chamber hole drilled in a rhenium foil, together with tiny ruby chips
for a pressure marker.

2) XRD data collection at ambient and high pressures
In-situ high-pressure XRD measurements are carried out with the following steps: (1) firstmeasurement at ambient pressure, (2) loading to the desired pressure, (3) pressure determination
with ruby scale, and (4) collection of XRD images with IP. Collect XRD images at pressureintervals of 5 GPa up to 35 GPa.

3) High-pressure generation and pressure measurement
In a gas-membrane DAC, pressure is generated online, smoothly, and remotely throughcontrolling the gas pressure in a membrane.
Pressure in the DAC is determined by ruby pressure scale [Mao et al. (1978) J. Appl. Phys.
49, 3276.]. The ruby scale, which has been calibrated against primary shock-wave experimentson several metals, is commonly used for DACs: the pressure-shift of ruby fluorescencewavelength can be easily probed with a laser beam through the diamond window. Determine thepressure with empirical quasi-linear relationship: P (GPa) = 1904[(λ ⁄λ0)B – 1] ⁄ B, where B = 5
for non-hydrostatic conditions, for the correlation of the measured wavelength shift λ (in nm) of
the R1 line with applied pressure.

4) Data analysis and peak indexing
The basic principle of the X-ray diffraction is the Bragg's law: λ = 2dsinθ, where λ is thewavelength of the X-ray, d the lattice spacing, θ the angle of the incident beam and thediffracting lattice plane. The diffraction peaks are observed when the d-spacing satisfied theBragg's law.
First, convert the X-ray image to conventional one-dimensional X-ray pattern with thesoftware. Next, calculate d-spacing for each peak from 2θ value using the Bragg's law. Then,perform peak indexing. Finally, refine the unit-cell parameter and volume.

Note that sodium chloride (NaCl) has face-centered cubic (fcc) structure with space groupof Fm3m, called B1-type (or NaCl-type) structure. At ambient conditions, the lattice parameterof NaCl is 5.630 Å. Its structure transforms from the B1 to B2 (CsCl) structure at 29.3 GPa.

5) Determination of the EOS parameters
An EOS is the relationships among the thermodynamic parameters volume, pressure, ortemperature. The EOS is useful to describe the properties of solid, fluid, and even the interior ofplanets and stars. In this practice, obtain the EOS parameters of zero-pressure bulk modulus andits pressure derivative for a low-pressure phase of B1-type NaCl from pressure-volume data atroom temperature. Plot the P-V data, and then fit the EOS with the Birch-Murnaghan equation.
Note that the Birch-Murnaghan equation of state is based on the Eulerian strain [Birch(1952) J. Geophys. Res. 57, 227.] and is widely used for mineralogists:
P = 3KT0/2 [(V0/V)7/3 – (V0/V)7/3]{1 – 3/4(4 – K’T0)[ (V0/V)2/3 – 1]}, where P is pressure, KT zero-pressure bulk modulus, K’T its pressure derivative, V the volume
at P, and the subscript “0” refers to ambient pressure conditions.

6) Comparison with other materials
Compare the EOS parameters of NaCl with other materials. The parameters for ionic,covalent, and metal crystals are given in table.
Material
DiamondNaSiAlAuPt
MgO
Al2O3H2NeNaCl

K0 (GPa)
444.5
6.310
97.9
73
167
277
160.2
253
0.162
1.42
23.83

K'0
3.98
3.886
4.16
4.54
5.46
5.08
3.99
4.30
6.813
8.03
5.09

Ref.
[1]
[2]
[3]
[4]
[5]
[4]
[6]
[7]
[8]
[9]
[10]

References: [1] Occelli et al. (2003); [2] Hanfland et al. (2002); [3] Knittle (1995); [4] Dewaele et al. (2004); [5]Takemura (2007); [6] Speziale et al. (2001); [7] Syassen (2008); [8] Loubeyre et al. (1996); [9] Dewaele et al. (2008);[10] Dorogolupets and Dewaele (2007).