Crystals
Everyone has noticed that table salt comes in little cubes.
This orderly outside arises from an orderly inside— the way the atoms lie is also cubical, these cubes stack in neat rows and columns, and the salt faces tend to be just an outer layer of cubes. One cube of atoms is shown below. Salt is sodium chloride and the small spheres shown are sodium while the big ones are chloride. To simplify the view, it only shows the sodiums and chlorides on the front, top, and right.
The specks of salt that we see above have many repetitions of this fundamental unit. A solid, such as table salt, with a regular internal structure is a crystal.
We can restrict our attention to the front face. There we have a square repeated many times giving a lattice of atoms.
The distance along the sides of each square cell is about Ångstroms (an Ångstrom is meters). When we want to refer to atoms in the lattice that number is unwieldy, and so we take the square’s side length as a unit. That is, we naturally adopt this basis.
Now we can describe, say, the atom in the upper right of the lattice picture above as , instead of Ångstroms over and up.
Another crystal from everyday experience is pencil lead. It is graphite, formed from carbon atoms arranged in this shape.
This is a single plane of graphite, called graphene. A piece of graphite consists of many of these planes, layered. The chemical bonds between the planes are much weaker than the bonds inside the planes, which explains why pencils write—the graphite can be sheared so that the planes slide off and are left on the paper.
We can get a convenient unit of length by decomposing the hexagonal ring into three regions that are rotations of this unit cell.
The vectors that form the sides of that unit cell make a convenient basis. The distance along the bottom and slant is Ångstroms, so this
is a good basis.
Another familiar crystal formed from carbon is diamond. Like table salt it is built from cubes but the structure inside each cube is more complicated. In addition to carbons at each corner,
there are carbons in the middle of each face.
(To show the new face carbons clearly, the corner carbons are reduced to dots.) There are also four more carbons inside the cube, two that are a quarter of the way up from the bottom and two that are a quarter of the way down from the top.
(As before, carbons shown earlier are reduced here to dots.) The distance along any edge of the cube is Ångstroms. Thus, a natural basis for describing the locations of the carbons and the bonds between them, is this.
The examples here show that the structures of crystals is complicated enough to need some organized system to give the locations of the atoms and how they are chemically bound. One tool for that organization is a convenient basis. This application of bases is simple but it shows a science context where the idea arises naturally.
Exercises
Exercise 1 Worked answer
How many fundamental regions are there in one face of a speck of salt? (With a ruler, we can estimate that face is a square that is cm on a side.)
Answer. Each fundamental unit is cm, so there are about such units. That gives , so there are something like (three hundred million) regions.
Exercise 2 Worked answer
In the graphite picture, imagine that we are interested in a point Ångstroms over and Ångstroms up from the origin.
Express that point in terms of the basis given for graphite.
How many hexagonal shapes away is this point from the origin?
Express that point in terms of a second basis, where the first basis vector is the same, but the second is perpendicular to the first (going up the plane) and of the same length.
Answer.
We solve
to get and .
Here is the point located in the lattice. In the picture on the left, superimposed on the unit cell are the two basis vectors and , and a box showing the offset of . The picture on the right shows where that appears inside of the crystal lattice, taking as the origin the lower left corner of the hexagon in the lower left.
So this point is two columns of hexagons over and one hexagon up.
This second basis
makes the computation easier
(we get and ), but it doesn’t seem to have to do much with the physical structure that we are studying.
Exercise 3 Worked answer
Give the locations of the atoms in the diamond cube both in terms of the basis, and in Ångstroms.
Answer. In terms of the basis the locations of the corner atoms are , , …, . The locations of the face atoms are , , , , , and . The locations of the atoms a quarter of the way down from the top are and . The atoms a quarter of the way up from the bottom are at and . Converting to Ångstroms is easy.
Exercise 4 Worked answer
This illustrates how we could compute the dimensions of a unit cell from the shape in which a substance crystallizes ([Ebbing], p. 462).
Recall that there are atoms in a mole (this is Avogadro’s number). From that, and the fact that platinum has a mass of grams per mole, calculate the mass of each atom.
Platinum crystallizes in a face-centered cubic lattice with atoms at each lattice point, that is, it looks like the middle picture given above for the diamond crystal. Find the number of platinum’s per unit cell (hint: sum the fractions of platinum’s that are inside of a single cell).
From that, find the mass of a unit cell.
Platinum crystal has a density of grams per cubic centimeter. From this, and the mass of a unit cell, calculate the volume of a unit cell.
Find the length of each edge.
Describe a natural three-dimensional basis.
Answer.
Each platinum atom in the middle of each face is split between two cubes, so that is atoms so far. Each atom at a corner is split among eight cubes, so that makes an additional atom, so the total is .
cubic centimeters
centimeters.
References cited in this section
Ebbing
Darrell D. Ebbing, General Chemistry, fourth edition, Houghton Mifflin, 1993.