| Historically, conventional
natural gas deposits have been the most practical, and
easiest, deposits to mine. However, as technology and
geological knowledge advances, unconventional natural
gas deposits are beginning to make up an increasingly
larger percent of the supply picture.
So what exactly is unconventional gas? A precise answer
to that question is hard to find. What was unconventional
yesterday, may through some technological advance, or
ingenious new process, become conventional tomorrow.
In the broadest sense, unconventional natural gas is
gas that is more difficult, and less economically sound,
to extract, usually because the technology to reach
it has not been developed fully, or is too expensive.
For example, prior to 1978, natural gas that had been
discovered buried deep underground in the Anadarko basin
was virtually untouched. It simply wasn't economical,
or possible, to extract this natural gas. It was unconventional
natural gas. However, deregulation of the area (and
particularly the passage of the Natural
Gas Policy Act, which provided incentives towards
searching and extracting unconventional natural gas),
spurred investment into deep exploration and development
drilling, making much of the deep gas in the basin conventionally
extractable.
Therefore, what is really considered unconventional
natural gas changes over time, and from deposit to deposit.
The economics of extraction play a role in determining
whether or not a particular deposit may be unconventional,
or simply to costly to extract. Essentially, however, there are six main categories
of unconventional natural gas. These are deep gas, tight
gas, gas-containing shales, coalbed methane, geopressurized
zones, and Arctic and sub-sea hydrates.
Deep Natural Gas
Deep natural gas is exactly what it sounds like - natural
gas that exists in deposits very far underground, beyond
'conventional' drilling depths. This gas is typically
15,000 feet or deeper underground, quite a bit deeper
than conventional gas deposits, which are traditionally
only a few thousand feet deep, at most.
Deep gas has, in recent years, become more conventional.
Deep drilling, exploration, and extraction techniques
have substantially improved, making drilling for deep
gas economical. However, deep gas is still more expensive
to produce than conventional natural gas, and as such,
economic conditions have to be such that it is profitable
for the industry to extract from these sources.
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| Source: Gas Technology
Institute |
Tight Natural Gas
Another form of unconventional natural gas is referred
to as tight gas. This is gas that is stuck in a very
tight formation underground, trapped in unusually impermeable,
hard rock, or in a sandstone or limestone formation
that is unusually impermeable and non-porous (tight
sand). Here is a graphical depiction, provided by the
USGS, of a cross section of a normal
reservoir, and a tight
gas formation. In a conventional natural gas deposit,
once drilled, the gas can usually be extracted quite
readily, and easily. A great deal more effort has to
be put into extracting gas from a tight formation. Several
techniques exist that allow natural gas to be extracted,
including fracturing and acidizing. However, these techniques
are also very costly. Like all unconventional natural
gas, the economic incentive must be there to incite
companies to extract this costly gas instead of more
easily obtainable, conventional natural gas. Tight gas
makes up a significant portion of the nation's natural
gas resource base, with the Energy
Information Administration (EIA) estimating that,
as of January 2009, 309.58 Tcf of technically recoverable
tight natural gas exists in the U.S. This represents
over 17% of the total recoverable natural gas
in the United States, and is an extremely important
portion of natural gas resources.
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| Source: EIA |
Shale Gas
Natural gas can also exist in shale deposits.
Devonian shales are formed from the mud of shallow seas
that existed about 350 million years ago (during the
Devonian period of the Paleozoic era). Shale is a very
fine-grained sedimentary rock, which is easily breakable
into thin, parallel layers. It is a very soft rock,
but does not disintegrate when it becomes wet. These
shales can contain natural gas, usually when two thick,
black shale deposits 'sandwich' a thinner area of shale.
Because of some of the properties of these shales, the
extraction of natural gas from shale formations is more
difficult (and thus expensive!) than extraction of conventional
natural gas. Most of the natural gas containing Devonian
shale in the U.S. is located around the Appalachian
Basin. Although estimates of the amount of natural gas
contained in these shales are high, it is expected that
only about 10 percent of the gas is recoverable. However,
their potential as a natural gas supply is still very
promising, given an adequate technological and economic
environment. As of November 2008, FERC estimated that there are 742
Tcf of technically recoverable shale gas in the United
States, representing a large and growing share of total recoverable
resources.
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| Source: Gas Technology
Institute |
Coalbed Methane
Coal, another fossil fuel, is formed underground under
similar geologic conditions as natural gas and oil.
These coal deposits are commonly found as seams that
run underground, and are mined by digging into the seam
and removing the coal. Many coal seams also contain
natural gas, either within the seam itself or the surrounding
rock. This coalbed methane is trapped underground, and
is generally not released into the atmosphere until
coal mining activities unleash it. Historically, coalbed
methane has been considered a nuisance in the coal mining
industry. Once a mine is built, and coal is extracted,
the methane contained in the seam usually leaks out
into the coal mine itself. This poses a safety threat,
as too high a concentration of methane in the well create
dangerous conditions for coal miners. In the past, the
methane that accumulated in a coal mine was intentionally
vented into the atmosphere. Today, however, coalbed
methane has become a popular unconventional form of
natural gas. This methane can be extracted and injected
into natural gas pipelines for resale, used as an industrial
feedstock, or used for heating and electricity generation.
The Potential Gas Committee estimates that 163.0 Tcf of technically recoverable
coalbed methane exists in the United States, making
up 7.8% of the total natural gas resource
base.
What was once a by-product of the coal industry is
becoming an increasingly important source of methane
and natural gas. For more information on coalbed methane,
visit the Environmental
Protection Agency.
Geopressurized Zones
Geopressurized zones are natural underground formations
that are under unusually high pressure for their depth.
These areas are formed by layers of clay that are deposited
and compacted very quickly on top of more porous, absorbent
material such as sand or silt. Water and natural gas
that is present in this clay is squeezed out by the
rapid compression of the clay, and enters the more porous
sand or silt deposits. This natural gas, due to the
compression of the clay, is deposited in this sand or
silt under very high pressure (hence the term 'geopressure').
In addition to having these properties, geopressurized
zones are typically located at great depths, usually
10,000-25,000 feet below the surface of the earth. The
combination of all of these factors makes the extraction
of natural gas in geopressurized zones quite complicated.
However, of all of the unconventional sources of natural
gas, geopressurized zones are estimated to hold the
greatest amount of gas. Most of the geopressurized natural
gas in the U.S. is located in the Gulf Coast region.
The amount of natural gas in these geopressurized zones
is uncertain. However, experts estimate that anywhere
from 5,000 to 49,000 Tcf of natural gas may exist in
these areas! Given the current technically recoverable
resources are around 1,100 Tcf, geopressurized zones
offer an incredible opportunity for increasing the nation's
natural gas supply.
Methane Hydrates
Methane hydrates are the most recent form of unconventional
natural gas to be discovered and researched. These interesting
formations are made up of a lattice of frozen water,
which forms a sort of 'cage' around molecules of methane.
These hydrates look like melting snow and were first
discovered in permafrost regions of the Arctic. Research into methane hydrates has revealed that they
may be much more plentiful than first expected. Estimates
range anywhere from 7,000 Tcf to over 73,000 Tcf! In
fact, the USGS estimates that methane hydrates may contain
more organic carbon than the world's coal, oil, and
conventional natural gas - combined! However, research into methane hydrates is still in its infancy. It is
not known what kind of effects the extraction of methane
hydrates may have on the natural carbon cycle.
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A
Methane Hydrate Molecule
Source: USGS |
Unconventional natural gas constitutes a large proportion
of the natural gas that is left to be extracted in North
America, and is playing an ever-increasing role in supplementing
the nation's natural gas supply. As technology advances
and new methods of extracting and using this natural
gas are developed, the resource potential of unconventional
natural gas is enormous!
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