Page 545 - Environment: The Science Behind the Stories
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FIGURE 19.7 Coal forms as
                                                                                                 ancient plant matter turns to
                                                                                                 peat and then is compressed
                                                       Time
                                Ancient                                                          underground. Of the four classes
                                forest                                                           of coal, lignite coal forms under the
                                                 Decreasing moisture                             least pressure and heat and retains
                                                                                                 the most moisture. Anthracite
                                                             Increasing heat and pressure        coal is formed under the greatest
                                                                                                 pressure, where temperatures are
                                                                                                 high and moisture content is low.
                                                                                                 Anthracite coal has the densest
                                                                                                 carbon content and so contains
                                                                                                 the most potential energy.










                                          Peat     Lignite   Sub-      Bituminous  Anthracite
                                                           bituminous




                     northeast Alberta. Microorganisms (which are abundant near   Once geologists have identified a promising location for a
                     the  surface  but  absent  at  depth)  began  to  consume  the oil,   deposit of oil or natural gas, a company will typically conduct
                     particularly the lighter components, leaving degraded heavy   exploratory drilling, drilling small holes that descend to great
                     bitumen.                                             depths. If enough oil or gas is encountered, extraction begins. Just
                                                                          as you would squeeze a sponge to remove its liquid, pressure is
                     Oil shale   Oil shale is sedimentary rock filled with kerogen   required to extract oil from porous rock. Oil is typically already
                     that can be processed to produce a liquid form of petroleum   under pressure—from above by rock or trapped gas, from below
                     called shale oil. Oil shale is formed by the same processes   by groundwater, and at times internally from natural gas dis-
                     that form crude oil but occurs when kerogen was not buried   solved in the oil. All these forces are held in check by surrounding
                     deeply enough or subjected to enough heat and pressure to   rock until drilling reaches the deposit, whereupon oil will often
                     form oil.                                            rise to the surface of its own accord. Once pressure is relieved and
                                                                          some oil or gas has risen to the surface, however, the remainder
                     Methane hydrate   Methane hydrate occurs in sediments   becomes more difficult to extract and needs to be pumped out.
                     in the Arctic and on the ocean floor. Also called  methane   Coal is a solid, and so we mine it rather than drilling for
                     clathrate or methane ice, this fossil fuel is an ice-like solid   it. For coal deposits near the surface, we use strip mining, in
                     consisting of molecules of methane embedded in a crystal lat-  which heavy machinery scrapes away huge amounts of earth
                     tice of water molecules. Methane hydrate is stable at tempera-  to expose the coal. For deposits deep underground, we use
                     ture and pressure conditions found in many sediments in the   subsurface mining, digging vertical shafts and blasting out
                     Arctic and on the seafloor. Most methane in these gas hydrates   networks of horizontal tunnels to follow seams, or layers, of
                     formed from bacterial decomposition in anaerobic environ-  coal. (Strip mining and subsurface mining are illustrated in
                     ments, but some resulted from thermogenic formation deeper   Figure 23.6, p. 657.) We are also now mining coal on immense
                     below the surface.                                   scales in the Appalachian Mountains, essentially scraping off
                                                                          entire mountaintops in a process called mountaintop removal
                                                                          mining (pp. 659–663).
                     We mine and drill for fossil fuels                      Oil from oil sands is extracted by two main methods. For
                                                                          deposits near the surface (FIGURE 19.8a), a process akin to strip
                     Because fossil fuels of each type form only under certain   mining for coal or open-pit mining for minerals (p. 658) is
                     conditions, they occur in isolated deposits. For instance,   used. Shovel-trucks peel back layers of peat and soil and then
                     oil and natural gas tend to rise upward through cracks and   dig out vast quantities of bitumen-soaked sand or clay. This
                     fissures in porous rock until meeting a dense impermeable   is mixed with hot water and piped to an extraction facility,
                     rock layer that traps them. As a result, geologists search for   where sand sinks to the bottom of tanks while bitumen floats
                     fossil fuels by drilling cores and conducting ground, air, and   to the top. The bitumen is skimmed off, solvent is added, and
                     seismic surveys to map underground rock formations. With   the mixture is spun in a centrifuge to further purify the bitu-
                     knowledge of underground geology, they can predict where   men, which is then processed into crude oil. Three barrels of
                     fossil fuel deposits might lie (see THE SCIENCE BEHIND THE STORY,    water are required to extract each barrel of oil, and the result-
             544     pp. 548–549).                                        ing toxic wastewater is discharged into vast tailings lakes.







           M19_WITH7428_05_SE_C19.indd   544                                                                                    12/12/14   5:22 PM
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