Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meaningsLoomis, Frederic Brewster
Science
Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meanings
Loomis, Frederic Brewster
Minerals -- United States; Rocks -- United States
In case these oil-bearing shales have been heavily overburdened and
compressed, the petroleum may have been more or less completely pressed
out of them. Then the droplets uniting have formed a liquid, which has
moved out from the shale, and gone wherever it could find open spaces.
Sandstones have frequently offered their pore space, and as it filled,
have been thus saturated with petroleum. If the sandstones were open to
the air, or if fissures extended from them to the surface, the oil has
escaped to the surface and evaporated into the air. But in those cases
where the sandstone (or other permeable rocks) was covered by an
impervious layer, like a dense shale or clay, the oil was confined below
the covering layer of rock. Crude oil is lighter than water; so that
when natural gas, petroleum and water were all present in the rocks, the
gas lies on top, the petroleum next, and the water underneath. With this
in mind it is easy to see, that in slightly folded or undulating layers
of rock, the gas and petroleum would be caught under upraised folds and
domes. This is the basis of prospecting for oil.
If petroleum-bearing layers are depressed far enough beneath the surface
to be affected by the high temperatures of the earth’s interior, or have
been near volcanic activity, of course the petroleum has been distilled
by natural processes, and at most only the residues, like paraffin or
asphalt, have remained. For this reason it is impossible to find
petroleum in igneous or metamorphic rocks.
Natural gas
Natural gas is the lightest portion of crude oil, and consists mostly of
marsh gas (“fire damp,” CH₄) together with other light hydrocarbons,
like ethane (C₂H₆), ethylene (C₂H₄), and some carbon dioxide and
monoxide. It is colorless, odorless, and burns with a luminous flame.
Mixed with air it is explosive. It is found in sedimentary rocks, mostly
sandstones, either with or without petroleum. Usually it is under
considerable pressure, and escapes with great force wherever a hole
permits. In time the gas all escapes through the hole or well, and then
the well “runs out.” If petroleum is present under the natural gas, the
hole may become an “oil well,” from which petroleum may be pumped, until
it in turn is exhausted. The end of an oil supply is usually indicated
by the appearance of water in the well. Natural gas is mostly associated
with oil districts, as in Pennsylvania, Ohio, Illinois, Texas,
California, etc.
Petroleum Crude Oil
Pl. 61
Petroleum is a mixture of paraffin compounds all the way from the gases,
through gasoline, kerosene, lubricating oils, and vasoline to paraffin.
In some of the crude oils there is also an admixture of compounds from
the benzine series, in which case, when all the volatile compounds have
been distilled off, an asphalt remains. The different components of
petroleum may be separated out by heating the crude oil in closed tanks,
and drawing off the various substances at the proper temperatures.
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