1. mass absorption coefficient for lead, m/r = 230 cm2/g
g = 1.54Å
r = 11.3g
I(g) = 10
Io(g) = 108
Equation for X-Ray absorption I(g)/Io(g) = exp{-(m/r)grx}
This rearranges to x = ln (I(g)/Io(g)) / --(m/r)grr
Substituting the figures into the equation gives
x = 0.00620cm
The extra thickness is used in common practise to reduce the intensity of the CuKb radiation and maintain a good intensity of the CuKa.
2. a) Using a laboratory diffractometer, the use of deep sample holders (if there is plenty of material) or a sample holder that doesn't detract from the intensity of the radiation. The use of Soller slits will prevent angular divergence, keeping the x-rays within the q/2q plane. A beam catcher will also help to minimise any interference caused by non-monochromatic x-rays. The use of a silicon crystal sample holder, leading to a negligible background scatter will aslo help to get a better diffraction pattern.
b) The use of a 'well focussed 'transmission geometry set-up is a good way of collecting data on organic materials with low absorption. This setup utilises a Debye-Scherrer camera to collect data over 360o. this lead to good lattice parameters from very high angle reflection. The set-up uses an incident beam collimator that reduces air scatter at the penalty of focussing the radiation. Curved silicon monochromators can be used to focus the divergent beam and lead to a narrower peaks
3. Constant parameters
g1 = 0.7Å
Minor comment: More conventional to use l for wavelengthg2 = 0.65Å
n = 1
d = 3.136Å
Equation 1
q1 = sin-1 ((ng1)/2d)
q1 = sin-1 (0.7/(2x3.316))
q1 = 6.408o
Equation 2
q2 = sin-1 ((ng2)/2d)
q2 = sin-1 (0.65/(2x3.316))
q2 = 5.949o
Difference in angles, Dq = q1 - q2
Dq = 0.459o
4. Constant parameters
E1 = 20 KeV
E2 = 100KeV
n = 1
q = 3.5o
Error: This value represents 2qEquation 1
E1 = 12.398/g
g = 12.398/E1 but ng = 2dsinq \ d = (12.398/E1)/2sinq
Hence, d = (12.398/20)/2sin3.5
d = 5.074Å
Equation 2
E2 = 12.398/g g = 12.398/E2 but ng = 2dsinq \ d = (12.398/E2)/2sinq
Hence, d = (12.398/100)/2sin3.5
d = 1.015Å
d-spacing ranging between 1.015Å and 5.074Å can be measures by the detector.
4 Marks
5. I) x, y, -z.
Minor comment: The "–" will not work with all browsers. In general, do be aware of non-standard Microsoft-specific features being incorporated when using their products to create/write/edit HTML files1 MarkThis is a 2-fold rotation axis parallel to the y direction.
Y will not change, and x and z indicate a 180o rotation in those axes. The origin is (0,0,0)
II) ½+x, ½+y, ½+z
This is a point of inversion through (-¼, -¼, -¼)
Comment: Point of inversion at -1/4,-1/4,-1/4 has the symmetry operator -1/2-x,-1/2-y,-1/2-zConsidering three points -Tx, -Ty, and -Tz as the centre of origin. The distance to the points, x,y,z. By considering the x-coordinate, the difference between x and the starting position Tx will be (x--Tx) which is x+ Tx. Once a symmetry operation has taken place, the distance to the new position will similarly be x+ Tx. Therefore, the x co-ordinate of the atom once it has moved will equal x-2(x+Tx) = x-2x-2Tx = -x-2Tx multiplying by 1 to make x a positive starting point and this gives 2Tx+x Using the same logic for the y and z coordinates gives the coordinates of the atom after the symmetry operation as (2Tx+x, 2Ty+y, 2Tz+z) If Tx = ¼ , Ty = ¼ , Tz = ¼ , then the equation becomes (½+x,½+y,½+z) with the origin being -Tx, -Ty, and -Tz, then the symmetry element will be a point of inversion, where all three coordinates are subject to change providing the origin is located at (-¼,-¼,-¼).
III) x, -y, -z
This is a point of inversion through (0,0,0)
All three coordinates are inverted by the symmetry operation
IV) x, -y, ½+z
This is a point of inversion through (0,0,-¼)
½+z follows the logic expressed in II) and the negative signs on the x and y direction show that all three coordinates will be affected by the symmetry, leading to the point of inversion
V) x, y, -z
This is a mirror in the z-direction
Only reflection occurs via the z-direction, which will lead to a mirror image since x and y will not be affected
VI) ½+x, -y, z
This is a two fold-rotation parallel to the z-direction with the origin (-¼,0,0)
The origin coordinate for x follow the reasoning in II), Only x and y are affected by the symmetry operation, therefore, rotation will occur in parallel to the unchnged coordinate direction, which is z in this case.
VII) ½+x, -y, -z
This is a point of inversion through (-¼,0,0)
All three coordinates are inverted by the symmetry operation and the origin is determined for the x axis by the same logic as II)
VIII) ½+x, ½+y, z
This is a two-fold rotation parallel to the z-direction with the origin(-¼,-¼,0)
z remains unchanged and x and y will change with respect to the reasoning given in II), leading to a 2-fold rotation.
IX) ½-x, ½-y, z
This is a two-fold rotation parallel to the z-direction with the origin (¼,¼,0)
Considering three points Tx,Ty and z as the centre of origin. The distance to the points, x,y,z. By considering the x-coordinate, the difference between x and the starting position Tx will be x-Tx. Once a symmetry operation has taken place, the distance to the new position will similarly be x+Tx. Therefore, the x co-ordinate of the atom once it has moved will equal x-2(x-Tx) = 2Tx-x Using the same logic for the y coordinate gives the coordinates of the atom after the symmetry operation as (2Tx+x, 2Ty+y, z) If Tx= ¼ , Ty = ¼ , then the symmetry operator becomes (½-x,½-y,z) providing the origin is (¼,¼,0)
X) x, ½-y, z
Minor error: Plane is at (x, plus 1/4,z)This is a mirror plane in the y axis with the origin (0,-¼,0)
x and z remain unchanged, whilst y will change according to the logic applied in II), resulting in a mirror image in the y-direction via the new origin
General comment: This seems to be your weakest answer. If you have any problems in understanding the model answers, please ask me for more detailed explanations