American Rural HighwaysAgg, T. R. (Thomas Radford)
Science
American Rural Highways
Agg, T. R. (Thomas Radford)
Roads -- United States
The sand-clay road surface consists of a natural or artificial mixture
of sand and clay, in which the amount of clay is somewhat greater than
sufficient to fill the voids in the dry sand. It may be assumed that
the sand contains 40 per cent of voids and that at least 45 per cent
of clay is required to fill the voids and bind the sand grains
together, because the clay spreads the sand grains apart during the
mixing, thus having the effect of increasing the voids. As a matter of
experiment, it is found to be impractical to secure by available
construction methods mixtures of sufficient uniformity to render it
necessary to exercise great exactness in proportioning the components,
but reasonable care in proportioning the materials is desirable.
Successful utilization of this type of surface requires considerable
study of available materials and investigations of their behavior when
combined. Extensive and exhaustive experiments have been conducted
with sand-clay mixtures in various places where they are widely used
for road surfaces and the following general principles have been
deduced.
=The Binder.=--In the sand-clay road, stability is obtained by
utilizing the bonding properties possessed to some degree by all
soils. Naturally this characteristic may be expected to vary widely
with the several types of soil. It is generally considered to be a
common property of clay, but the term clay is a general one that is
often applied to soils differing greatly in physical characteristics
and the term therefore loses its significance in this connection.
Those soils that are properly and technically called clay are
decidedly sticky when wet and are the best materials for sand-clay
construction. Of the clays, those that produce a tough sticky mud are
best. This can be tested by mixing a small quantity into a stiff mud
and molding it into a ball and immersing in water. If the ball retains
its shape for some little time, it is likely to prove a very
satisfactory binder, but, if it becomes plastic and loses its shape,
it will be an inferior binder, as a general rule. The ball clay, as
the former is called, may be of any color common to soils, not
necessarily yellow or reddish as is sometimes supposed. Likewise,
balls of mixtures containing varying percentages of sand and the
binder to be used may be made up and immersed in water. The mixture
that holds its shape longest is of course the best combination of the
materials and indicates the mixture to use in the construction.
An ideal, or even a fairly satisfactory soil for a binder may not
exist in the vicinity of a proposed improvement, and consequently an
inferior binder is frequently the only material available.
Sometimes deposits of clay or gravel contain a considerable percentage
of gypsum which serves as a binder and is particularly effective when
used in combination with clay and sand or gravel.
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