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Bitumen

Form of petroleum primarily used in road construction

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Natural formed Bitumen collected at the Dead Sea shore
Daniel Tzvi · Public domain

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Through Viscosity, Petroleum and Engineering

About 70% of annual bitumen production is destined for road construction, its primary use. In this application, bitumen is used to bind aggregate particles, like gravel, and forms a substance referred to as asphalt concrete, which is colloquially termed asphalt. Its other main uses lie in bituminous waterproofing products, such as roofing felt and roof sealant.

In materials science and engineering, the terms asphalt and bitumen are often used interchangeably and refer to both natural and manufactured forms of the substance, although there is regional variation as to which term is most common. Worldwide, geologists tend to favor the term bitumen for the naturally occurring material. For the manufactured material, which is a refined residue from the distillation process of selected crude oils, bitumen is the prevalent term in much of the world; however, in American English, asphalt is more commonly used. To help avoid confusion, the terms "liquid asphalt", "asphalt binder", or "asphalt cement" are used in the U.S. to distinguish it from asphalt concrete. Colloquially, various forms of bitumen are sometimes referred to as tar, as in La Brea Tar Pits, although tar is not the same thing as bitumen.

Naturally occurring bitumen is sometimes specified by the term crude bitumen. Its viscosity is similar to that of cold molasses while the material obtained from the fractional distillation of crude oil boiling at 525 °C (977 °F) is sometimes referred to as refined bitumen. The Canadian province of Alberta has most of the world's reserves of natural bitumen in the Athabasca oil sands, which cover 142,000 square kilometres (55,000 sq mi), an area larger than England.

Terminology

Etymology

The Latin word traces to the Proto-Indo-European root *gʷet- "pitch".

The word "asphalt" is derived from the late Middle English, in turn from French asphalte, based on Late Latin asphaltum, which is the latinisation of the Greek ἄσφαλτος (ásphaltos), a word meaning "asphalt/bitumen/pitch", which perhaps derives from ἀ-, "not, without", i.e. the alpha privative, and σφάλλειν (sphallein), "to cause to fall, baffle, (in passive) err, (in passive) be balked of".

The first use of asphalt by the ancients was as a cement to secure or join various objects, and it thus seems likely that the name itself was expressive of this application. Specifically, Herodotus mentioned that bitumen was brought to Babylon to build its gigantic fortification wall.

In French, the term asphalte is used for naturally occurring asphalt-soaked limestone deposits, and for specialised manufactured products with fewer voids or greater bitumen content than the "asphaltic concrete" used to pave roads.

Modern terminology

Bitumen mixed with clay was usually called "asphaltum", but the term is less commonly used today.

In American English, "asphalt" is equivalent to the British "bitumen". However, "asphalt" is also commonly used as a shortened form of "asphalt concrete" (therefore equivalent to the British "asphalt" or "tarmac").

In Canadian English, the word "bitumen" is used to refer to the vast Canadian deposits of extremely heavy crude oil, while "asphalt" is used for the oil refinery product. Diluted bitumen (diluted with naphtha to make it flow in pipelines) is known as "dilbit" in the Canadian petroleum industry, while bitumen "upgraded" to synthetic crude oil is known as "syncrude", and syncrude blended with bitumen is called "synbit".

"Bitumen" is still the preferred geological term for naturally occurring deposits of the solid or semi-solid form of petroleum. "Bituminous rock" is a form of sandstone impregnated with bitumen. The oil sands of Alberta, Canada are a similar material.

Neither of the terms "asphalt" or "bitumen" should be confused with tar or coal tars. Tar is the thick liquid product of the dry distillation and pyrolysis of organic hydrocarbons primarily sourced from vegetation masses, whether fossilized as with coal, or freshly harvested. The majority of bitumen, on the other hand, was formed naturally when vast quantities of organic animal materials were deposited by water and buried hundreds of metres deep at the diagenetic point, where the disorganized fatty hydrocarbon molecules joined in long chains in the absence of oxygen. Bitumen occurs as a solid or highly viscous liquid. It may even be mixed in with coal deposits. Bitumen, and coal using the Bergius process, can be refined into petrols such as gasoline, and bitumen may be distilled into tar, not the other way around.

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