Online Encyclopedia

ASPHALT, or ASPHALTUM

Online Encyclopedia
Originally appearing in Volume V02, Page 768 of the 1911 Encyclopedia Britannica.
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ASPHALT, or ASPHALTUM  . The solid or semi-solid kinds of
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bitumen (q.v.) were termed &r4aXros by the Greeks; and by some ancient classical writers the name of pissasphaltum (irio'o'a, pitch) was also sometimes employed . The asphalt of the Dead Sea (known as Lacus Asphaltites) received considerable
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notice from early travellers, and Diodorus the historian states that the inhabitants of the surrounding parts were accustomed to collect it for use in
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Egypt for embalming . In
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common with other forms of bitumen, asphalt is very widely distributed geographically and occurs in greater or less quantity in rocks of all ages . There is some divergence in the views expressed as to the precise manner of its production, but it may certainly be said that the
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principal asphalt deposits are merely the result of the evaporation and oxidation of liquid petroleum which has escaped from outcropping strata . The celebrated Pitch Lake of
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Trinidad was long regarded as the largest deposit of asphalt in existence, but it is said to be exceeded in
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area, if not in
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depth also, by one in
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Venezuela . The Trinidad " Lake " has an area of 99.3 acres, and is sufficiently
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firm in places to support a team of horses . The deposit is worked with picks to a depth of a
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foot or two, and the excavations soon become filled up by the plastic material flowing in from below and hardening . The depth of the deposit is not accurately known . The
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surface is not level but is composed of irregularly tumescent masses of various sizes, each said to be subject to
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independent motion, whereby the interior of each rises and flows centrifugally towards the edges . As the spaces between them are always Ailed with
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water, these masses are prevented from coalescing . The softer parts of the lake constantly evolve
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gas, which is stated to consist largely of carbon dioxide and sulphuretted hydrogen, and the pitch, which is honey-combed with gas-cavities, continues to exhibit this
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action for some time after its removal from the lake .

The working of the deposit is in the hands of the New Trinidad Asphalt

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Company, who hold the concession up to the
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year 1930 on payment to the government of a minimum royalty of £I0,o0o a year . A circular
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line of
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tramway, supported on palm-leaves, has been laid on the lake to facilitate the removal bf the asphalt . Very large quantities are exported for paving and other purposes, the
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annual shipments amounting to about 130,000 tons from the lake and about 30,000 tons from other properties . The amount of asphalt in the lake has been estimated at 158,400 tons for each foot of depth, and if the
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average depth be taken at 20 ft. this would give a
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total of 3,168,000 tons; but in 1908, though 1,885,600 tons had been removed in the previous
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thirty-five years, there was but little evidence of reduction in the quantity . The Venezuelan deposit already referred to is in the state of
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Bermudez, and the area of it is reported to be more than root) acres . The asphalt of Cuba is a well-known article of commerce, of which 7252 tons was exported to the
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United States in 1902 . The principal deposits are near the harbour of Cardenas (70 ft. thick), in the Pinar del Rio, near Havana (18 ft. thick), at Canas Tomasita (105 ft. thick); and a specially pure variety near Vuelta . The
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comparative composition of Trinidad and Cuba asphalt is given in the following table: Refined Refined Refined Trinidad, Cuba(soft), Cuba(hard), Melting Melting Melting point point point 185° F . I15° F . 16o° F . Water . . .

0.17 0.13 0.11 Volatile bitumen . . 51.81 64'03 8'34

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Sulphur . . . .
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I000 8.35 8.92 Ash (earthy
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matter) . 28.30 19.51 16.6o Fixed carbon 9.72 7.98 66.03
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I00.00 I00.00 I00.00 ASPHODEL The chemical composition of Trinidad asphalt has been given as: 0 . I S . I.40 11.48 — Asphalt in its purest forms is generally black or blackish brown in colour, and is frequently brittle at ordinary temperatures . Apart from its principal use in the manufacture of paving materials, it is largely employed in
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building as a "
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damp-course " and as a water-excluding coating for concrete floors, as well as in the manufacture, of roofing-felt . It also enters largely into the composition of black
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varnish . The material chiefly used in the construction of asphalt roadways is an asphaltic or bituminous
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limestone found in the Val de Travers, canton of Neuchatel; in the neighbourhood of Seyssel, department of
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Ain; at Limmer, near the city of Hanover; and else-where . The proportion of bitumen
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present in asphalt rock usually ranges from 7 to 20 %, but it is found that rock containing more than I I % cannot be satisfactorily used for street pavements, and it is accordingly customary to mix the richer and poorer varieties in
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fine powder in such respective quantities that the proportion of bitumen present is from 9 to 10 % . The richer rock is utilized as a source of asphalt " mastic,” which is employed for footpaths, floors,
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roofs, &c .

Excellent

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foundations ,for steam-hammers, dynamos and high-speed engines are made of asphaltic concrete . (B .

End of Article: ASPHALT, or ASPHALTUM
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