Statistical Factors Affecting the Intensity of X-Rays Diffracted by Crystalline Powders
- 1 August 1948
- journal article
- research article
- Published by AIP Publishing in Journal of Applied Physics
- Vol. 19 (8) , 742-753
- https://doi.org/10.1063/1.1698200
Abstract
The Laplacian probability equation can be used to predict the reproducibility of the intensities of x-rays diffracted by crystalline powders. If absorption is neglected, and N is the number of particles irradiated, p the proportion of particles which are oriented so as to diffract, and q=1 − p, the relative mean deviation to be expected in repeated intensity measurements is given by Um=0.798 (q/Np)½. When absorption and the actual distribution of particle sizes are taken into account, the expression becomes Um=0.798(qμve/pA)12,where μ is the linear absorption coefficient of the material, ve the effective volume per particle, and A the cross-sectional area of the incident beam. The theory is confirmed by measurements on four size fractions of quartz powder using a Norelco Geiger-counter x-ray spectrometer. For typical experimental conditions and powders of medium absorbing power for x-rays, it is demonstrated that good reproducibility can be expected only if the effective particle dimension is less than approximately five microns.This publication has 7 references indexed in Scilit:
- X-Ray Studies of Surface Layers of CrystalsBell System Technical Journal, 1946
- The Perfection of Quartz and Other Crystals and Its Relation to Surface TreatmentPhysical Review B, 1934
- Absolute X-Ray Reflectivities of Single Crystals of Calcite, Rocksalt, Rochelle Salt and BaritePhysical Review B, 1933
- The Reflecting and Resolving Power of Calcite for X-raysPhysical Review B, 1932
- Structure of α quartzProceedings of the Royal Society of London. Series A, Containing Papers of a Mathematical and Physical Character, 1926
- I. The intensity of reflexion of X-rays by rock-salt.—Part IIJournal of Computers in Education, 1921
- An Experimental Study of the Reflection of X-Rays from CalcitePhysical Review B, 1921