Appletons' Popular Science Monthly, March 1900: Vol. 56, Nov. 1899 to April, 1900Various
History
Appletons' Popular Science Monthly, March 1900: Vol. 56, Nov. 1899 to April, 1900
Various
Science -- Periodicals; Technology -- Periodicals
The asphaltic cement and sand are heated separately to about 300° F.
The stone dust is then added to and mixed with the hot sand in the
proportion of from five to eighty in the case of fine, well-graduated
sand, to fifteen to sixty-seven for coarse sands, having less variation
in size. The asphaltic cement is then added, and the materials are
mixed to a homogeneous mass, which is ready to be taken to the street.
It should reach there at a temperature not less than 250°, and is
spread with hot iron rakes so as to give usually a thickness of two
inches after consolidation. After spreading, it is rolled with a hand
roller, after which a small amount of hydraulic cement is swept over
the surface, and it is thoroughly rolled with a steam roller of not
less than ten tons, the rolling to be continued as long as the roller
makes any impression on the surface.
The foundation is usually of cement concrete about six inches thick,
though asphalt pavements are often laid over old stone pavements.
Between the foundation and the wearing surface there is generally laid
what is called a binder course, one inch thick and formed of small
broken stone, to which has been added asphaltic cement, the same as is
used in making the wearing surface. Five or six pints of this cement
are used to each cubic foot of stone.
[Illustration: KING'S HIGHWAY, BROOKLYN; SIXTEEN FEET IN CENTER OF ROAD
MACADAMIZED.]
The pavement just described is made from Trinidad asphalt, the material
from which nearly all the earlier artificial asphalt pavements in this
country were made, and which was used almost exclusively until within
the last half dozen years.
Within that time, however, it has been discovered that there are a
number of other deposits of asphalt well adapted to use for street
pavements. A very large deposit containing a high percentage of bitumen
and very little mineral matter is located near the coast in the State
of Bermudez, in Venezuela. Large deposits have been found in several
places in California, and in Utah, Kentucky, and Texas, and a number
of other places. The Kentucky product is classed as a natural rock
asphalt, as it is a sandstone impregnated with bitumen. It has been
mixed with about an equal portion of German rock asphalt and used
with very satisfactory results in Buffalo. These asphalts are quite
different in their composition, and each requires somewhat different
treatment. The Bermudez, being richer in bitumen and softer, requires
the addition of very little flux. The California deposits furnish their
own flux in a liquid asphalt or maltha, which is almost absolutely
pure bitumen, and the use of petroleum residuum is thereby avoided
altogether.
[Illustration: ASPHALT PAVEMENT ON CLINTON AVENUE, BROOKLYN.]
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