Structures of Simple Inorganic Solids

Dr S.J. Heyes

First of Four Lectures in the 1st Year Inorganic Chemistry Course

Michaelmas Term 1999

If you have any comments please contact stephen.heyes@chem.ox.ac.uk 


Lecture 1. Fundamental Aspects of Solids & Sphere Packing.

1. Why Study Solids?

2. Some crystallographic ideas

3. Representations of structures

4. Close-Packing of spheres

5. Structures of metallic elements

6. Interstitial sites in close-packed arrangements

 


Aims of this Lecture

After studying this lecture you should be able to:-

1. Define the Terms

Lattice

Motif

Crystal Structure

Unit Cell

Coordination Number

2. Interpret a Plan or Perspective structure diagram of a Unit Cell & determine

Lattice Type

Number of Atoms in unit cell

Coordination Number/Geometry of atoms

3. For ccp, hcp and bcc structures

Describe the Sphere Packing

Identify symmetry of unit cell

Draw unit cell in plan or perspective

State Coordination Number/Geometry of a sphere & the degree of space-filling

Give some examples of metallic elements which adopt each structure

Draw on a plan or perspective view of the unit cell the positions of any octahedral &/or tetrahedral interstitial holes


Why Study Solids?

 

1. ALL Compounds are Solids under suitable conditions of temperature and pressure. Many exist only as solids.

 

2. Solids are of immense Technological Importance

Appearance

 

3. Solids (especially Crystals) have always been fascinating

Some Historical Landmark Events

Date

X-ray

Date

Landmark Event

ca. 6000 BC

Egyptians mine Turquoise

Antiquity

Gemstones (especially diamond, sapphire, emerald & ruby) are much prized. Indeed some still attribute magical properties, such as healing to crystals!

ca. 350 BC

ca. 2310 BX

Theophrastus describes regular form of Garnet crystals

ca. 30 BC

1976 BX

Strabo names Quartz krystlloz (crystallum in Latin), hence our 'crystal'

1597

315 BX

The alchemist Libavius recognizes that the geometrical habit of crystals is characteristic of the salts concerned

17th C

ca. 302 BX

Boyle, Leeuwenhoek, Kepler, Hooke... make numerous observations with the newly invented microscope

1611

301 BX

Kepler suggests that the hexagonal symmetry of snowflakes is due to "regular packing of the constituent particles"

1665

247 BX

Hooke suggests that crystals are composed of "spheroids"

1669

243 BX

Steno observes that Quartz crystals, whatever their origin or state, always preserve the same characteristic interfacial angles

1780

132 BX

Carangeot invents the Contact Goniometer - measures interfacial angles leading to a great mass of crystallographic detail

1783

129 BX

Bergman's studies of crystal cleavage suggest to him that crystals consist of packed rhombohedral units

1783

129 BX

de l'Isle formulates the law of "Constancy of Interfacial Angle"

1801

111 BX

Haüy substantiates the law of "Rational Indices"

The Fundamental Laws of Crystal Morphology are established

1808

104 BX

Malus observes the polarization of light by certain crystals

1809

103 BX

Wollaston invents the Reflecting Goniometer - this leads to a massive improvement in the accuracy of interfacial angle data

1815

97 BX

Biot discovers laevo- and dextro-rotatory forms of Quartz

1819-22

93 BX

Mitscherlich discovers

Isomorphism (crystals of different composition with the same form)

Polymorphism (different crystal forms with the same chemical composition) [= Allotropy in elements]

1839

73 BX

Miller uses his Miller Indices to designate crystal faces

1848

64 BX

Pasteur discovers enantiomorphic crystals

1880s-90s

32 BX

Sohncke, Federov, Schönflies & Barlow develop theories of internal symmetry of crystals - but still no experimental evidence to support these theories

1906-19

6 BX

Groth's "Chemische Krystallographie" tabulates morphological, optical and other properties of 7000 crystalline substances {but it contains no information about internal structures - no experimental techniques!)

1907

5 BX

Barlow & Pope propose that ions in crystals are hard spheres touching each other

1912

Friedrich, Knipping & von Laue discover X-ray diffraction

1913

1 AX

W.H. & W.L. Bragg use orientation dependence of X-ray diffraction from a single crystal to solve the structure of NaCl (& subsequently diamond etc...)

1913

1 AX

Ewald introduces the concept of the Reciprocal Lattice

1914

2 AX

Debye's theory of Thermal Motion of atoms in solids (hence Debye-Waller factors in X-ray structures)

1916

4 AX

Debye & Scherrer's experiments on diffraction by powders

1924

12 AX

Bernal et al. - structure of Graphite

1926

14 AX

Frenkel's investigations of Point Defects in structures

1926

14 AX

Goldschmidt's spherical atom formulation of structures

1927

15 AX

Pauling's formulation of Goldschmidt's Ionic Model into Pauling's Rules

1929

17 AX

Rotating Anode X-ray generator - allows increased X-ray intensities for better diffraction patterns

1934

22 AX

Patterson Function for structure solution from X-ray diffraction

1934

22 AX

Ruska takes images using the first (transmission) electron microscope

1936

24 AX

Halaban & Preiswerk - diffraction of neutrons by crystals

1941

29 AX

Hughes uses Least-Squares refinement to obtain best possible structures from a diffraction data set

1944

32 AX

Buerger invents the Precession Camera

1948

36 AX

Harker & Kasper - Direct Methods for structure solution from X-ray diffraction data

1950s

ca. 38 AX

Automatic diffractometers and computers dramatically increase the ease of solving crystal structures

1951

39 AX

Bijvoet uses anomalous scattering to determine chirality (absolute configuration)

mid 1950s

ca. 43 AX

Computers first used for Structure solution from X-ray data

1955

43 AX

Principles of Laves - space-filling in crystal structures

1956

44 AX

Menter produces first lattice image from Transmission Electron Microscopy (TEM)

1957

45 AX

Müller - Field-Ion Microsopy visualizes individual atoms in metals

1970

58 AX

Crewe, Wall and Langmore - Darkfield Scanning Electron Microscopy (the first general method for imaging individual heavy atoms)

1971

59 AX

Formanek et al. - the first detection of an individual atom by High Resolution Electron Microscopy (HREM)

1974

62 AX

Iijima - the first observation of point defects in structures by electron microscopy

1980s

ca. 68 AX

Synchrotron Radiation Available - massively increased intensity of X-rays (Laue X-ray patterns of crystals obtained on ms timescale)

1982

70 AX

Area detectors for obtaining X-ray diffraction patterns (massive decrease in time taken to obtain a diffraction pattern)

1982

70 AX

Binnig & Rohrer - Scanning Tunnelling Microscopy (STM) images even light atoms at surfaces

1984

72 AX

Schechtman et al. discover Quasi-Crystals

1984

74 AX

Binnig et al. - Atomic Force Microscopy (AFM) images at surfaces (even easier to obtain than STM)

1990s

ca. 80 AX

>200,000 Crystal structures (internal atom coordinates) stored in databases


Some Basic Definitions

LATTICE = An infinite array of points in space, in which each point has identical surroundings to all others.

CRYSTAL STRUCTURE = The periodic arrangement of atoms in the crystal.

It can be described by associating with each lattice point a group of atoms called the MOTIF (BASIS)

 

UNIT CELL = The smallest component of the crystal, which when stacked together with pure translational repetition reproduces the whole crystal


2D LATTICES

e.g. the fused hexagonal pattern of a single layer of GRAPHITE

Counting Lattice Points/Atoms in 2D Lattices

 

2-Dimensional Lattice Symmetries were famously exploited by the artist Escher in many patterns


Analysing a 3D solid

e.g. Graphite = a staggered arrangement of stacked hexagonal layers

Perspective: Clinographic views of solids

Projection onto a Plane: Plan views of solids

GRAPHITE

Unit Cell Dimensions

a, b and c are the unit cell edge lengths

a, b and g are the angles (a between b and c, etc....)

 

Counting Atoms in 3D Cells

Atoms in different positions in a cell are shared by differing numbers of unit cells


On combining 7 Crystal Classes with 4 possible unit cell types Symmetry indicates that only 14 3-D lattice types occur

 

The 14 possible BRAVAIS LATTICES

{note that spheres in this picture represent lattice points, not atoms!}

Examine the 14 Bravais Lattices in Detail

Cubic-P, Cubic-I, Cubic-F, Tetragonal-P, Tetragonal-I, Orthorhombic-P, Orthorhombic-I, Orthorhombic-F, Orthorhombic-C, Hexagonal-P, Trigonal-P, Monoclinic-P, Monoclinic-C, Triclinic-P

If you have the Chemscape Chime Plug-in you can manipulate the 14 Bravais lattices at the University of Texas, Austin

Combining these 14 Bravais lattices with all possible symmetry elements

230 different Space Groups

For applications of different geometry lattice theories to simple structures see:-


1926 Goldschmidt proposed atoms could be considered as packing in solids as hard spheres

This reduces the problem of examining the packing of like atoms to that of examining the most efficient packing of any spherical object - e.g. have you noticed how oranges are most effectively packed in displays at your local shop?

 

CLOSE-PACKING OF SPHERES


A single layer of spheres is closest-packed with a HEXAGONAL coordination of each sphere


A second layer of spheres is placed in the indentations left by the first layer

{P = sphere, O = octahedral hole, T+ / T- = tetrahedral holes)


When a third layer of spheres is placed in the indentations of the second layer there are TWO choices


Close-Packed Structures

The most efficient way to fill space with spheres

Is there another way of packing spheres that is more space-efficient?

In 1611 Johannes Kepler asserted that there was no way of packing equivalent spheres at a greater density than that of a face-centred cubic arrangement. This is now known as the Kepler Conjecture.

This assertion has long remained without rigorous proof, but in August 1998 Prof. Thomas Hales of the University of Michigan announced a computer-based solution. This proof is contained in over 250 manuscript pages and relies on over 3 gigabytes of computer files and so it will be some time before it has been checked rigorously by the scientific community to ensure that the Kepler Conjecture is indeed proven!

 

Features of Close-Packing

Simplest Close-Packing Structures

2 atoms in the unit cell (0, 0, 0) (2/3, 1 /3, 1 /2)

View a Quicktime HCP Movie or Quicktime HCP VR scene

4 atoms in the unit cell (0, 0, 0) (0, 1 /2, 1 /2) (1 /2, 0, 1 /2) (1 /2, 1 /2, 0)

View a Quicktime CCP Movie or Quicktime CCP VR scene


The most common close-packed structures are METALS

A NON-CLOSE-PACKED structure adopted by some metals is:-

View a Quicktime BCC Movie or Quicktime BCC VR scene

68% of space is occupied

Coordination Number ?

8 Nearest Neighbours at 0.87a

6 Next-Nearest Neighbours at 1a


 

CrystalMaker file for C60

Further information about Fullerenes


Location of Interstitial Holes in Close-Packed Structures

The HOLES in close-packed arrangements may be filled with atoms of a different sort.

It is therefore important to know:-

The hole positions are shown relative to the unit cells below

The structures possible from filling them are considered in Lecture 2

CCP Octahedral holes------------------------------------------------HCP Octahedral holes

CCP Tetrahedral holes------------------------------------------------HCP Tetrahedral holes


Solids Page Lecture 1 Lecture 2 Lecture 3 Lecture 4 Problems Set Help


© S.J. Heyes, Oxford, 1996-2000