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Surface of a sheet may not have the same texture as the bulk

문서에서 Crystalline nature of materials TEXTURE (페이지 32-43)

 Transmission measurements can have a big problem due to

absorption

65 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Thin film – texture; YBCO/STO

Intensity

Omega (deg.)

14 15 16 17 18 19

0.4o

Intensity

0 90 180 270 360

Phi (deg.) fwhm = 1o

Intensity

10 20 30 40 50 60

2 theta (degrees)

002 003

004 005

006

007 STO 001 STO 002

66 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Textured film vs. single crystal

The amount of material properly oriented, in addition to ∆φ

and ∆ω, is needed to describe the degree of texture

67 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Percentage cube texture

111

A B

Collect data

@ A

Collect data

@ B

At each point, I(A) – I(B) 

 I (blue)/ I (blue + yellow) = percentage cube texture

Theta

68 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Inverse pole

figure

69 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Direct pole figure vs. Inverse pole figure

 xyz sample coordinate system

 x’y’z’ crystal coordinate system

 Both are 2-D projections of the 3-D orientation distribution functions (ODF)  cannot completely describe the orientations present. 3-D ODF can do this.

z = ND x= RD

y= TD

x’ = [100] z’ = [001]

Y’ = [010]

z = ND x= RD

y= TD x’ = [100]

z’ = [001]

Y’ = [010]

Pole figure Inverse pole figure

70 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Direct pole figure vs. Inverse pole figure

z = ND x= RD

y= TD

x’ = [100] z’ = [001]

Y’ = [010]

z = ND x= RD

y= TD x’ = [100]

z’ = [001]

Y’ = [010]

Pole figure Inverse pole figure

Dist. of selected xtallographic

direction relative to certain directions in the specimen

Dist. of selected direction in the specimen relative to xtal axes

Dist. of a, b & c relative to RD, TD & ND

Dist. of RD, TD & ND

relative to a, b & c

71 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Pole Figure & Inverse Pole Figure

72 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Inverse pole figure

 Choose a sample direction of

interest, e.g. the Normal Direction (ND or “3”)

 Choose a grain; determine which crystal direction the ND is parallel to; plot the result on a

stereographic projection.

 Repeat for all grains!

 If appropriate (large number of data points), plot contours

 Remember that the unit triangle is the fundamental zone for directions in cubic crystals

Carnegie Mellon Univ.

73 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Inverse pole figure

74 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Inverse PF

 The crystallographic direction // to ND plotted on a stereographic projection with axes // to the edges of the crystal unit cell

 The direction is repeated because, for cubic materials, it could be any one of 48

symmetrically equivalent crystal directions

a cubic crystal unit cell oriented w.r.t. sample axes

the same sample axes oriented w.r.t. the crystal unit cell

75 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Inverse pole figure

The RD and TD inverse pole figures are obtained in a similar way

76 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Inverse pole figure

Negligible fraction of non-<111> fiber

Sample direction 3, or ND Strong <111>//ND Fiber Texture

Carnegie Mellon Univ.

77 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Direct PF vs. Inverse PF

 DPF

 Specify the poles of a specific crystal direction w.r.t. sample coordinate in stereographic projection

 Shows the distribution of a selected crystallographic direction relative to certain directions in the specimen

 IPF

 Specify the poles of sample coordinate system w.r.t. those of crystal coordinate system in stereographic projection

 Shows the distribution of a selected direction in the specimen relative to the crystal axes

78 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Direct PF vs. Inverse PF

 DPF

 A normal PF indicates how likely it is that a specific direction in a grain will adopt some orientation relative to the external features of the sample

 IPF

 An inverse PF indicates how likely it is that some external feature of the sample, (e.g. the fiber axis) will be at some orientation relative to the crystallographic axes of the grains

 shows the distribution of crystallographic directions // to certain sample directions and can show some textures more clearly

79 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Inverse pole figure

 In an inverse PF, the axes of the projection sphere are aligned with crystal directions.

 The directions plotted are the stereographic projection of crystal directions // to either the normal direction (ND), rolling direction (RD) or transverse direction (TD) in the sample.

 The inverse PF can help visualize certain types of textures.

80 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Inverse pole figure

 Indicates the frequencies with which different crystal directions occur in a specified sample direction.

 Plays an important role in the calculation or estimation of physical properties of polyxtalline materials.

 Very informative for fiber samples as we are only interested in how the fiber axis is oriented.

 For sheet samples, it is less informative as we have to worry about the orientation of the sheet normal, the rolling direction and the transverse direction. This requires multiple inverse PFs.

81 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Inverse pole figure of extruded Al rod

 Contours indicate how likely it is that the fiber axis will adopt a given orientation relative to the

crystallographic axes (directions) of a grain.

 IPF shows immediately the

crystallographic “direction” of the scatter.

Cullity 3rdEd. Page 428

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Euler angle

83 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Euler angles

TD(y)

RD(x) ND(z)

Rotation ϕ1about ND (z) axis

Rotation φ about new x axis bring ND to 001

Rotation ϕ2 about new z axis bring RD & TD to 100 & 010

84 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Euler angles

TD(y)

RD(x) sample

crystal

ND(z)

Rotation ϕ1about ND (z) axis

Rotation φabout new x axis bring ND to 001

Rotation ϕ2about new z axis bring RD & TD to 100 & 010

 The orientation between 2 coordinate systems can be defined by a set of 3 successive rotations about specified axes.

 These rotation angles are called the Euler angles ---ϕ1, φ, ϕ2

(

Bunge’s notation).

85 CHAN PARK, MSE, SNU Spring-2019 Crystal Structure Analyses

Euler Angles, Animated

e

1

=X

sample

=RD

문서에서 Crystalline nature of materials TEXTURE (페이지 32-43)

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