_Elutriation of Clayey Soils._—Hilgard found that by churn elutriation
no satisfactory results could be obtained on clay without long boiling
and subsequent kneading of the finer sediments. Osborne examined a
sample of clay by his method after previous boiling for twenty-three
hours. When the sediments were examined by the microscope they were
found to contain many aggregations of particles which broke into dust
under the pressure of the thin glass slide-cover. These sediments were
then gently crushed in the beaker with the help of a soft rubber stopper
with a glass rod for a handle, the grinding together of the particles
being, as much as possible, avoided. This pestling was continued with
clear water as long as it occasioned turbidity. Comparison of the
analyses shows that practically identical results were obtained on this
soil whether it was boiled or not and indicates that the sediments are
reduced to their elements by gentle pestling alone. For such soils,
therefore, it is demonstrated that pestling is a much safer treatment
than boiling. The same remark may be applied to the fertile prairie soil
of Mercer County, Illinois, where boiling proved quite insufficient and
in which the pestling process proved completely successful. The general
conclusions arrived at from the results obtained by Osborne are as
follows:
1. On sands and silts of pure quartz or similar resistant material
Hilgard’s method and beaker elutriation give practically identical
results.
2. With coarse sands and silts upon whose grains finer matter has been
cemented by silicates, etc., and with soils containing soft slaty
detritus, the churn elutriator with preliminary boiling may give results
too low for the coarse and too high for the finer grades. In these cases
beaker elutriation with pestling yields more correct figures.
3. Some loamy soils containing no large amount of clay or of extremely
fine silt, as well as prairie soils rich in humus, cannot be suitably
disintegrated by twenty-four hours’ boiling, but are readily reduced by
pestling.
4. Beaker elutriation preceded by sifting, gives results in five or six
hours with use of two to three gallons of pure water, which, in churn
elutriation, require several days and consume eight to ten gallons of
pure water.
5. Hilgard found that practically 0.25 millimeter is about the lowest
velocity of water current per second available within reasonable limits
of time in his elutriator. Such a current carries over particles up to
0.015 millimeter diameter and hence the silts of less dimensions cannot
be conveniently separated by churn elutriation. In beaker elutriation
there is no difficulty in making good separations at 0.01 millimeter and
at 0.005 millimeter.
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