We humans eat apples and eggplants, but we don’t eat their stems or leaves or roots. Bacteria in water are similarly picky. Even before a plant sinks all the way to the bottom of the ocean, bacteria and other living things are picking off the chemicals they like, either because those chemicals are easier to get or more useful to the bacteria, leaving other chemicals behind. This continues as the plants are buried. Some bacteria in low-oxygen but organic-rich mud make methane, CH4, the main ingredient in natural gas, as described in the Enrichment section More on Oxygen in Water. As more mud accumulates on top, deeper sediments are warmed by the heat of the Earth, “cooking” the dead plants. The result depends on how much cooking occurs, and what the plants were at the beginning.
“Woody” land plants—tree trunks, but also leaves, twigs, roots, etc.—become coal, which is mostly carbon. During the transformation from leaves and twigs to hard, shiny black coal, we change the name, first to peat, and then to coal of different types, lignite, then bituminous, then anthracite. You’ll generally find that as time, heat, and pressure change the organic materials, they also change the rest of the sediment around the coal. Peat occurs in sediments that are not yet hard enough to be called rock, lignite in soft sedimentary rocks, bituminous in harder ones, and anthracite in metamorphic rocks.
Oil is formed from “slimy” water plants (algae, plus things such as cyanobacteria that probably shouldn’t really be called plants, but we’re simplifying a little here). Because oil is primarily made of carbon (C) and hydrogen (H), we sometimes refer to it as a hydrocarbon. Methane is the simplest hydrocarbon, CH4, but oil contains a great range of larger hydrocarbon molecules, such as octane (C8H18). With too much heat, the oil breaks down to make methane. This gas is also produced as coal forms.
Coal, as a solid, mostly sits where it was formed. Eventually, if the rocks above it are eroded so that it is exposed at the Earth’s surface, the coal itself may be eroded away, and either “eaten” by bacteria, or buried in new rocks. And, occasionally, a natural forest fire or a lightning strike may set coal on fire. This burning usually isn’t really fast, because after the coal nearest the surface burns away, oxygen doesn’t get to deeper coal very easily. But, a lot of coal has avoided being eroded or burned, and is sitting in the rocks where it formed.
(Humans have also set coal on fire, releasing mercury and other toxic materials, and burning up a valuable resource. A few percent of China’s annual coal production may be burned in such fires, the town of Centralia in Pennsylvania was abandoned because of one such fire (see the figure below), and other impacts occur.)
Mining coal involves either removing the rocks on top, or tunneling into the Earth along the coal layer. Removing the rocks on top of the coal, called “surface mining” or “strip mining”, requires putting those rocks on top of something else, breaking the coal loose with machines or explosives, hauling the coal away to be burned, and then either putting the rocks back on top or just leaving them. (We’ll revisit some of the implications of this later in the semester.) Digging along the coal is often called “deep mining”, and puts miners in a potentially dangerous place. For more information about mountain removal mining, visit the U.S. Environmental Protection Agency [3] for some good resources, and watch the video at NASA's page on Moutaintop Removal [4].
When mud rocks (shale layers) are heated, the buried dead plants break down into the smaller molecules that make up oil and gas. Initially, these are trapped in the shale. However, because many small molecules take up more space than a few big ones, heating and cooking the rocks raises the pressure inside until the oil and gas seep out, often by cracking the rock. After some oil and gas escape, the pressure drops and the cracks close under the weight of rocks above. This may happen multiple times as more cooking occurs.
After oil and gas have escaped from the shale into sandstone or other rocks with bigger spaces, the oil and gas can move through those spaces. Most sediments are deposited under water, or the spaces in them fill up with water later. Natural gas is gaseous (no surprise there!), oil is liquid and floats on water, and so both tend to move upward through the water-filled spaces. The great majority of oil and gas eventually reach the Earth’s surface as oil or gas seeps. Before the industrial revolution, the amount of fossil fuel being formed, and the amount leaking out of seeps, were probably very similar (we’ll give some numbers soon).
However, recall that fluids have more difficulty moving through smaller spaces. If oil and gas are rising through spaces in rock, their motion may be blocked by another shale layer. Especially if the shale has been bent by movements in the Earth associated with mountain-building, so that the oil and gas rise into a “trap”, the fossil fuels may sit there for a long time (see the figure below).
For over a century, exploration for oil and gas—finding the next big field full of valuable fossil fuels—has involved locating oil and gas traps and drilling into them. Most commonly, this has involved “seismic” exploration (see the figure and explanation below). Nature figured out how to use this technique long before humans did. For example, a bat flying around in the dark “looking” for a moth to eat will make a noise, and listen to the echo off the moth, using the time and direction to locate the flying dinner. Dolphins can find their food the same way.
Oil explorers make noises, and listen to the reflections from layers in the Earth, using the time and direction to locate the oil-and-gas-filled traps. Then, drillers drill into the traps, and pump the oil and gas out. (Sometimes, the pressure is so high in the trap at the start that the oil comes out of the hole without being pumped, as a “gusher,” see figures below.)
But, soon, the pressure down there is reduced, and a pump is needed. Occasionally, a gusher catches on fire, with sometimes disastrous consequences, see the figure below.
Increasingly, a new technique is being used to recover oil and gas. Shale layers often have a lot of hydrocarbon left in them that did not escape in the past. Drillers have learned how to bore down to a shale layer, then turn the drill and bore along in the layer. When the hole is long enough, the drillers pump fluids at high pressure into the hole, breaking the shale in a process called “fracking” (from “fracturing”) that mimics the natural process by which oil and gas escaped the shale. Human use of this process was apparently first invented by a veteran of the US Civil War, Col. Edward Roberts, who saw the fractures in the ground caused by an exploding Confederate shell, and went on to patent the technique of using explosives to fracture rocks and allow more flow into wells. The technique has been improved in many ways since.
In many ways, fracking is not revolutionary but evolutionary from older techniques for recovering oil and gas. Under best practices, fracking probably isn’t inherently more risky or dangerous than those other methods. The biggest difference is that fracking is used to recover oil and gas that are spread out over large areas rather than having a large quantity concentrated in one place. So, fracking takes lots more drilling and pumping and installing pipelines in more places. Fracking is more likely to be in someone’s backyard, or near it, so there are more people seeing it and hearing it and complaining about it.
The more drilling there is, the more chances there are for mistakes to be made, contaminating groundwater or otherwise causing problems for neighbors. The drilling can also bring other problems, including lots of traffic. For example, back on Sept. 23, 2011, an article by Cliff White in the Centre Daily Times, State College, PA noted “A review of inspections performed by state police on commercial motor vehicles used in support of Marcellus Shale gas drilling operations in 2010 revealed 56 percent resulted in either the vehicle or driver being placed out of service for serious safety violations” but that “Thanks to heavy enforcement, the noncompliance rate has dropped to about 45 percent in the most recent study.” And, in the same article, “…a trooper in gas-rich Bradford County, said during the initial ramp-up of activity in that area a few years ago, almost all of the vehicles used for gas drilling-related purposes that he stopped had “some degree” of noncompliance.”)
Fracking is done with high-pressure fluids to which certain chemicals have been added, as noted above, and some of those chemicals may be dangerous to humans. The fracking fluids plus salty brines from the rocks “flow back” out of the wells, and these flowback fluids must be disposed of in some way. Much of that disposal recently has involved injecting the flowback fluids into the Earth in special deep wells. This has caused numerous earthquakes, some of them damaging. (See, for example, USGS: Induced Earthquakes [9].) Fluid injection for other reasons also has caused earthquakes; fracking is especially important in this only because it generates so much fluid that is being injected. Note that while fracking has probably triggered a few small earthquakes directly, the main cause of earthquakes is this injection of flowback fluids.
Fracking is likely to be with us for a long time. And, it is likely to remain at least somewhat controversial.
Earth: The Operators' Manual
If you want to see a little more on fracking, much of the clip is relevant, but the first 3 minutes and 40 seconds especially fit here.
You may also hear about oil shales and tar sands (see image below). These are sometimes called unconventional petroleum or unconventional oil, or something similar, and represent opposite ends of a spectrum: oil shales haven’t been cooked enough to make oil yet, and tar sands are the leftovers after cooking and dining.
Tar sands, such as the huge deposits of Alberta, Canada (see images above), are like the much smaller tar deposits in the pits at La Brea, mentioned earlier. Oil contains many different types of molecules. When oil seeps to the surface, the smaller ones tend to evaporate, or to be used preferentially by bacteria, leaving the larger molecules behind. These larger ones don’t flow as easily, so the result is a thick, almost solid mass of “tar” (technically called “bitumen”). Native Americans were waterproofing their birch-bark canoes with Alberta’s bitumen when the first Europeans arrived, probably with no knowledge that early peoples of the Fertile Crescent of Mesopotamia also used bitumen to waterproof boats.
Because the bitumen is so “thick” (viscous), normal drill-and-pump techniques don’t work well. Many techniques are in use or being tested to separate oil from the sand or gravel in which it occurs. For shallow deposits, the tar-soaked sands can be surface-mined and then heated or mixed with appropriate chemicals to free the oil from the sand. For deeper deposits, injection of steam or hot air or other hot fluids can warm the bitumen enough that it will flow. Oil companies are even experimenting with setting small fires in wells, to make heat and gases that drive liquid hydrocarbon to other wells. All of these techniques have associated costs, including water and energy use. For now, much more energy is obtained from the oil recovered than is used in recovery, but the ratio is not as good as for “normal” oil, and is likely to get worse as the easier-to-recover tar sands are used up.
In contrast to the tar-sand “leftovers” from normal oil after bacteria have eaten a lot, oil shales are undercooked not-yet-oil. In many places, dead plants and mud accumulated, but without being buried deeply enough to get hot enough to break down the dead plants and make oil. The dead plants have typically been changed enough to get a new name (“kerogen”), but not to make oil that can be pumped out easily. This sort of deposit is called oil shale (Figures 13-15). (The names are NOT the easiest to deal with. Oil pumped out of shale may be called shale oil, but the shale from which that oil is pumped is generally not called oil shale. Instead, that shale is an oil source rock. The name “oil shale” is saved for those shales that haven’t been heated enough to make oil, but that could be in the future. Given our choice, most of us who work in these areas would pick clearer names, but no one asked us!)
Oil shale can be burned as-is, but the organic matter is diluted by the clay in the shale, so just burning doesn’t work really well. Most plans for future use involve speeding up the natural process, heating the rock to “pyrolyze” the organic matter, releasing oil and gas while leaving some organic material behind in the rock. This may be done in the ground, or after mining the shale. Because energy is needed to heat the rock, costs tend to be higher, and energy recovered lower, than for conventional oil in which the heat of the Earth acting over millions of years did the cooking for us.
Links
[1] http://pubs.usgs.gov/fs/2009/3084/
[2] http://www.loc.gov/item/cmns001287#about-this-item
[3] https://www.epa.gov/sc-mining
[4] http://earthobservatory.nasa.gov/Features/WorldOfChange/hobet.php
[5] https://www.e-education.psu.edu/geosc10/node/1834
[6] http://www.loc.gov/pictures/item/2006678003/
[7] http://www.loc.gov/pictures/item/2003678396/
[8] http://www.loc.gov/pictures/item/97514401/
[9] https://www.usgs.gov/search?keywords=fracking+induced+earthquakes
[10] http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2866701/#!po=50.0000
[11] http://ostseis.anl.gov/guide/tarsands/index.cfm
[12] https://www.blm.gov/
[13] http://energy.gov/fe/services/petroleum-reserves/naval-petroleum-reserves/oil-shale-and-other-unconventional-fuels
[14] http://ostseis.anl.gov/guide/photos/index.cfm