Dj. Stephens et Jn. Dunlevey, Recovery of dispersed clay-sized suspensions for X-ray diffraction mineralanalysis, S AFR J SCI, 95(9), 1999, pp. 390-393
The determination of soil engineering properties is essential for the succe
ssful design of all types of construction projects. However, the testing me
thods required are often time-consuming and expensive. Therefore, approxima
te prediction techniques have been developed to save time and money using s
impler soil tests, such as particle-size distribution, to achieve this purp
ose. The existing methods for such particle identification rely purely on g
rain size analysis and consider all mineral particles with an effective dia
meter of less than two microns to be clays. However, soil mineralogy, geoch
emistry and the differences between predicted and real values indicate that
this is not entirely correct. To establish and quantify the 'true clay fra
ction' for more realistic modelling of soil behaviour, a technique has ther
efore been developed by which the mineral fraction can be recovered in a st
ate that is suitable for X-ray diffraction analysis. The mineralogical data
obtained in this manner can then be used to improve the available evaluati
on parameters and thereby provide a more realistic prediction model of the
soil's behaviour.