Abstract--Lattice spacings of layer silicates, particularly clay minerals, may exceed 20 A. The errors in measuring lattice spacings increase rapidly for spacings greater than about 10 A and diffraction angles 20 tess than about 10 ~ Long-chain organic compounds, such as normal alcohols, ClcC2o, and normal alkancs (paraffins), Cz6-C3o, provide useful calibrations for lattice spacings in the range 10-50 A. The basal spacings of the calibrating substances are determined from their higher order reflections in the angular range where reflections from quartz and silicon are used as standards.
INTRODU(.qI'IONThe measurement of lattice spacings greater than about 10A. in layer silicates, particularly in clay minerals, is subject to several sources of error, of which some arise in the conventional use of diffractometers, and others are related to the nature of the diffracting materials and the diffraction process itself. Kittrick (1960) emphasized that when X-ray diffractometers are adjusted by observing reflections from silicon or quartz powders, any lack of perfection in the adjustment or in the instrument itself becomes greatly magnified when measurements are made at small angles. If To improve the accuracy of long spacing measurements, Kittrick (1960) recommended that diffractometers be adjusted with respect to an accurately known long spacing reflection and showed that the strong (010) reflection from cholesterol could be so used. Cholesterol has d(010)= 33"6 ~ I = 100, and d(020) = 16.8 A., I = 12, (see X-Ray Powder Data File,