Natural gas formation - Revision history

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2019-01-04T18:15:20Z

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2dev>Ashley.Sheardown at 19:04, 19 December 2018

2018-12-19T19:04:22Z

← Older revision		Revision as of 19:04, 19 December 2018
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	[[Category:Done 2018-07-20]]		[[Category:Done 2018-12-10]]
	<onlyinclude>Natural gas is a [[fossil fuel]] that is composed mainly of [[methane]] - composed itself of [[carbon]] and [[hydrogen]] - and is thus known as a [[hydrocarbon]].<ref name="RE1">Natural Resources Canada. (May 28, 2015). ''Natural Gas: A Primer'' [Online]. Available: https://www.nrcan.gc.ca/energy/natural-gas/5641</ref> '''Natural gas formation''' (which is a [[gas]]) is essentially the same as the [[oil formation\|formation of oil]] (a [[liquid]]) and thus takes a significant amount of [[~~timescale~~ of the universe\|time]] with natural gas beginning to form millions of years ago.</onlyinclude>		[[Category: Ashley edit]]
			<onlyinclude>Natural gas is a [[fossil fuel]] that is composed mainly of [[methane]] - composed itself of [[carbon]] and [[hydrogen]] - and is thus known as a [[hydrocarbon]].<ref name="RE1">Natural Resources Canada. (May 28, 2015). ''Natural Gas: A Primer'' [Online]. Available: https://www.nrcan.gc.ca/energy/natural-gas/5641</ref> '''Natural gas formation''' (which is a [[gas]]) is essentially the same as the [[oil formation\|formation of oil]] (a [[liquid]]) and thus takes a significant amount of [[time scale of the universe\|time]] with natural gas beginning to form millions of years ago.</onlyinclude>

	The formation of natural gas begins in warm, shallow [[ocean]]s that were present on the Earth millions of years ago. In these oceans, extremely small dead organic [[matter]] - classified as [[plankton]] - falls to the floor of the ocean. This plankton consists of animals, called ''zooplankton'', or plants, called ''phytoplankton''. This material then lands on the ocean floor and mixes with inorganic material that enters the ocean by rivers. It is this [[sediment]] on the ocean floor that then forms [[oil]] and natural gas over many years. The [[energy]] in [[natural gas]] initially comes from the [[Sun]], and is energy from [[sunlight]] trapped by dead plankton.<ref name="wolfson">R. Wolfson. ''Energy, Environment and Climate'', 2nd ed. New York, U.S.A.: Norton, 2012, pp. 96-97</ref>		The formation of natural gas begins in warm, shallow [[ocean]]s that were present on the Earth millions of years ago. In these oceans, extremely small dead organic [[matter]] - classified as [[plankton]] - falls to the floor of the ocean. This plankton consists of animals, called ''zooplankton'', or plants, called ''phytoplankton''. This material then lands on the ocean floor and mixes with inorganic material that enters the ocean by rivers. It is this [[sediment]] on the ocean floor that then forms [[oil]] and natural gas over many years. The [[energy]] in [[natural gas]] initially comes from the [[Sun]], and is energy from [[sunlight]] trapped by dead plankton.<ref name="wolfson">R. Wolfson. ''Energy, Environment and Climate'', 2nd ed. New York, U.S.A.: Norton, 2012, pp. 96-97</ref>
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	The process that creates natural gas is the same as the process that creates oil, and is generally the same in most areas. However, there may be different types of plant and animal debris that falls to the ocean floor and slightly different conditions. To form natural gas, the following steps are followed:<ref name="wolfson"/><ref name="geo">Stephen Marshak. (May 11, 2015). ''Earth: Portrait of a Planet'', 3rd ed. New York, NY, U.S.A:W.W. Norton & Company, 2008</ref>		The process that creates natural gas is the same as the process that creates oil, and is generally the same in most areas. However, there may be different types of plant and animal debris that falls to the ocean floor and slightly different conditions. To form natural gas, the following steps are followed:<ref name="wolfson"/><ref name="geo">Stephen Marshak. (May 11, 2015). ''Earth: Portrait of a Planet'', 3rd ed. New York, NY, U.S.A:W.W. Norton & Company, 2008</ref>

	1. Dead plankton - both phytoplankton and zooplankton - as well as ~~[[algae]]~~ and ~~bacteria~~ sink to the bottom of an ancient ocean and mix with inorganic, clay-like materials that enter these oceans from streams and rivers. This creates an organic-rich mud. This mud can only form in still [[water]] environments. This step is shown in Figure 1, panel A.		1. Dead plankton - both phytoplankton (including [[algae]]) and zooplankton - as well as other soft and hard organic matter tissues (including microbes), sink to the bottom of an ancient ocean and mix with inorganic, clay-like materials that enter these oceans from streams and rivers. This creates an organic-rich mud. This mud can only form in still [[water]] environments. This step is shown in Figure 1, panel A.

	2. This mud cannot be exposed to too much [[oxygen]], or else the organic matter in the mud would be decomposed by bacteria and disappear quickly. Therefore environments where natural gas can form are known as anoxic environments. Before this organic matter is destroyed, it is buried by more sediment and ''lithifies'' (becomes [[sedimentary rock]]), creating ''[[shale\|organic shale]]''. This step is shown in Figure 1, panel B.		2. This mud cannot be exposed to too much [[oxygen]], or else the organic matter in the mud would be decomposed by bacteria and disappear quickly. Therefore environments where natural gas can form are known as anoxic environments. Before this organic matter is destroyed, it is buried by more sediment and ''lithifies'' (becomes [[sedimentary rock]]), creating ''[[shale\|organic shale]]''. This step is shown in Figure 1, panel B.
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	*[[Coal formation]]		*[[Coal formation]]
	*[[Hydraulic fracturing]]		*[[Hydraulic fracturing]]
			*Or explore a [[Special:Random\|random page]]

	==References==		==References==
	{{reflist}}		{{reflist}}
	[[Category:Uploaded]]		[[Category:Uploaded]]

Jmdonev: 1 revision imported

2018-07-21T01:13:06Z

1 revision imported

← Older revision	Revision as of 01:13, 21 July 2018
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Jmdonev at 20:18, 19 July 2018

2018-07-19T20:18:59Z

← Older revision		Revision as of 20:18, 19 July 2018
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	[[Category:Done ~~2017~~-07-01]]		[[Category:Done 2018-07-20]]
	<onlyinclude>~~'''~~Natural gas~~'''~~ is a [[fossil fuel]] that is composed mainly of [[methane]] - composed itself of [[carbon]] and [[hydrogen]] - and is thus known as a [[hydrocarbon]].<ref name="RE1">Natural Resources Canada. (May 28, 2015). ''Natural Gas: A Primer'' [Online]. Available: https://www.nrcan.gc.ca/energy/natural-gas/5641</ref> ~~The~~ formation ~~of natural gas~~ (which is a [[gas]]) is essentially the same as the [[oil formation\|formation of oil]] (a [[liquid]]) and thus takes a significant amount of [[timescale of the universe\|time]] with natural gas beginning to form millions of years ago.</onlyinclude>		<onlyinclude>Natural gas is a [[fossil fuel]] that is composed mainly of [[methane]] - composed itself of [[carbon]] and [[hydrogen]] - and is thus known as a [[hydrocarbon]].<ref name="RE1">Natural Resources Canada. (May 28, 2015). ''Natural Gas: A Primer'' [Online]. Available: https://www.nrcan.gc.ca/energy/natural-gas/5641</ref> '''Natural gas formation''' (which is a [[gas]]) is essentially the same as the [[oil formation\|formation of oil]] (a [[liquid]]) and thus takes a significant amount of [[timescale of the universe\|time]] with natural gas beginning to form millions of years ago.</onlyinclude>

	The formation of natural gas begins in warm, shallow [[ocean]]s that were present on the Earth millions of years ago. In these oceans, extremely small dead organic [[matter]] - classified as [[plankton]] - falls to the floor of the ocean. This plankton consists of animals, called ''zooplankton'', or plants, called ''phytoplankton''. This material then lands on the ocean floor and mixes with inorganic material that enters the ocean by rivers. It is this [[sediment]] on the ocean floor that then forms oil and natural gas over many years. The [[energy]] in [[natural gas]] initially comes from the [[Sun]], and is energy from [[sunlight]] trapped by dead plankton.<ref name="wolfson">R. Wolfson. ''Energy, Environment and Climate'', 2nd ed. New York, U.S.A.: Norton, 2012, pp. 96-97</ref>		The formation of natural gas begins in warm, shallow [[ocean]]s that were present on the Earth millions of years ago. In these oceans, extremely small dead organic [[matter]] - classified as [[plankton]] - falls to the floor of the ocean. This plankton consists of animals, called ''zooplankton'', or plants, called ''phytoplankton''. This material then lands on the ocean floor and mixes with inorganic material that enters the ocean by rivers. It is this [[sediment]] on the ocean floor that then forms [[oil]] and natural gas over many years. The [[energy]] in [[natural gas]] initially comes from the [[Sun]], and is energy from [[sunlight]] trapped by dead plankton.<ref name="wolfson">R. Wolfson. ''Energy, Environment and Climate'', 2nd ed. New York, U.S.A.: Norton, 2012, pp. 96-97</ref>

	==Formation Process==		==Formation Process==
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	==Unconventional Sources==		==Unconventional Sources==
	The process above describes the formation of natural gas in a traditional, [[Conventional vs unconventional resource\|conventional deposit]]. However, [[Unconventional resource\|unconventional deposits]] such as [[shale gas]] and [[coal bed methane]] are also sources of natural gas. In these deposits, natural gas is stored differently and is also more difficult to access than with traditional deposits.		The process above describes the formation of natural gas in a traditional, [[Conventional vs unconventional resource\|conventional deposit]]. However, [[Unconventional resource\|unconventional deposits]] such as [[tight gas]], [[shale gas]] and [[coal bed methane]] are also sources of natural gas. In these deposits, natural gas is stored differently and is also more difficult to access than with traditional deposits.

			==For further reading==
			*[[Tight gas]]
			*[[Shale gas]]
			*[[Coal formation]]
			*[[Hydraulic fracturing]]

	==References==		==References==
	{{reflist}}		{{reflist}}
	[[Category:Uploaded]]		[[Category:Uploaded]]

Jmdonev: 1 revision imported

2017-08-29T01:46:44Z

1 revision imported

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Jmdonev at 17:30, 14 July 2017

2017-07-14T17:30:16Z

← Older revision		Revision as of 17:30, 14 July 2017
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	[[Category:Done ~~2015~~-06-11]]		[[Category:Done 2017-07-01]]
	<onlyinclude>'''Natural gas''' is a [[fossil fuel]] that is composed mainly of [[methane]] - composed itself of [[carbon]] and [[hydrogen]] - and is thus known as a [[hydrocarbon]].<ref name="RE1">Natural Resources Canada. (May 28, 2015). ''Natural Gas: A Primer'' [Online]. Available: https://www.nrcan.gc.ca/energy/natural-gas/5641</ref> The formation of gas is essentially the same as the [[oil formation\|formation of oil]] and thus takes a significant amount of [[timescale of the universe\|time]] with natural gas beginning to form millions of years ago.</onlyinclude>		<onlyinclude>'''Natural gas''' is a [[fossil fuel]] that is composed mainly of [[methane]] - composed itself of [[carbon]] and [[hydrogen]] - and is thus known as a [[hydrocarbon]].<ref name="RE1">Natural Resources Canada. (May 28, 2015). ''Natural Gas: A Primer'' [Online]. Available: https://www.nrcan.gc.ca/energy/natural-gas/5641</ref> The formation of natural gas (which is a [[gas]]) is essentially the same as the [[oil formation\|formation of oil]] (a [[liquid]]) and thus takes a significant amount of [[timescale of the universe\|time]] with natural gas beginning to form millions of years ago.</onlyinclude>

	The formation of natural gas begins in warm, shallow ~~oceans~~ that were present on the Earth millions of years ago. In these oceans, extremely small dead organic matter - classified as plankton - falls to the floor of the ocean. This plankton consists of animals, called ''zooplankton'', or plants, called ''phytoplankton''. This material then lands on the ocean floor and mixes with inorganic material that enters the ocean by rivers. It is this sediment on the ocean floor that then forms oil and natural gas over many years. The energy in [[natural gas]] initially comes from the [[Sun]], and is energy from sunlight trapped by dead plankton.<ref name="wolfson">R. Wolfson. ''Energy, Environment and Climate'', 2nd ed. New York, U.S.A.: Norton, 2012, pp. 96-97</ref>		The formation of natural gas begins in warm, shallow [[ocean]]s that were present on the Earth millions of years ago. In these oceans, extremely small dead organic [[matter]] - classified as [[plankton]] - falls to the floor of the ocean. This plankton consists of animals, called ''zooplankton'', or plants, called ''phytoplankton''. This material then lands on the ocean floor and mixes with inorganic material that enters the ocean by rivers. It is this [[sediment]] on the ocean floor that then forms oil and natural gas over many years. The [[energy]] in [[natural gas]] initially comes from the [[Sun]], and is energy from [[sunlight]] trapped by dead plankton.<ref name="wolfson">R. Wolfson. ''Energy, Environment and Climate'', 2nd ed. New York, U.S.A.: Norton, 2012, pp. 96-97</ref>

	==Formation Process==		==Formation Process==
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	The process that creates natural gas is the same as the process that creates oil, and is generally the same in most areas. However, there may be different types of plant and animal debris that falls to the ocean floor and slightly different conditions. To form natural gas, the following steps are followed:<ref name="wolfson"/><ref name="geo">Stephen Marshak. (May 11, 2015). ''Earth: Portrait of a Planet'', 3rd ed. New York, NY, U.S.A:W.W. Norton & Company, 2008</ref>		The process that creates natural gas is the same as the process that creates oil, and is generally the same in most areas. However, there may be different types of plant and animal debris that falls to the ocean floor and slightly different conditions. To form natural gas, the following steps are followed:<ref name="wolfson"/><ref name="geo">Stephen Marshak. (May 11, 2015). ''Earth: Portrait of a Planet'', 3rd ed. New York, NY, U.S.A:W.W. Norton & Company, 2008</ref>

	1. Dead plankton - both phytoplankton and zooplankton - as well as [[algae]] and bacteria sink to the bottom of an ancient ocean and mix with inorganic, clay-like materials that enter these oceans from streams and rivers. This creates an organic-rich mud. This mud can only form in still water environments. This step is shown in Figure 1, panel A.		1. Dead plankton - both phytoplankton and zooplankton - as well as [[algae]] and bacteria sink to the bottom of an ancient ocean and mix with inorganic, clay-like materials that enter these oceans from streams and rivers. This creates an organic-rich mud. This mud can only form in still [[water]] environments. This step is shown in Figure 1, panel A.

	2. This mud cannot be exposed to too much [[oxygen]], or else the organic matter in the mud would be decomposed by bacteria and disappear quickly. Therefore environments where natural gas can form are known as anoxic environments. Before this organic matter is destroyed, it is buried by more sediment and ''lithifies'' (becomes sedimentary rock), creating ''organic shale''. This step is shown in Figure 1, panel B.		2. This mud cannot be exposed to too much [[oxygen]], or else the organic matter in the mud would be decomposed by bacteria and disappear quickly. Therefore environments where natural gas can form are known as anoxic environments. Before this organic matter is destroyed, it is buried by more sediment and ''lithifies'' (becomes [[sedimentary rock]]), creating ''[[shale\|organic shale]]''. This step is shown in Figure 1, panel B.

	3. If this shale is buried between 2 and 4 kilometers, its temperature increases due to its location in the [[Cross section of the Earth\|Earths interior]]. This increasing [[pressure]] and [[temperature]] of the shale transforms it into a waxy material known as '''[[kerogen]]'''. Shale that contains this material is known as '''oil shale'''.		3. If this [[shale]] is buried between 2 and 4 kilometers, its temperature increases due to its location in the [[Cross section of the Earth\|Earths interior]]. This increasing [[pressure]] and [[temperature]] of the shale transforms it into a waxy material known as '''[[kerogen]]'''. Shale that contains this material is known as '''[[oil shale]]'''.

	4. If temperatures of the kerogen are ''greater'' than [[Celsius\|90°C]] but lower than 160°C, the kerogen is transformed into [[oil]] and natural gas. At temperatures greater than 90°C, the only product is natural gas or graphite.		4. If temperatures of the kerogen are ''greater'' than [[Celsius\|90°C]] but lower than 160°C, the kerogen is transformed into [[oil]] and natural gas. At temperatures greater than 90°C, the only product is natural gas or [[graphite]].

	5. Natural gas and oil are both lighter than water, so as they escape from the source oil shale the products rise through pores in rocks, displacing water. Rock bodies that contain significant amounts of oil or natural gas are known as [[Oil and gas reservoir\|reservoir]] rocks. For the gas to remain trapped in the reservoir, there must be some sort of thick, impermeable layer of rock to seal the reservoir. If this seal exists, then oil, gas, and water are trapped beneath and can be drilled into to obtain the oil.<ref name="canada">Canadian Federation of Earth Sciences. (May 11, 2015). ''Four Billion Years and Counting: Canada's Geological Heritage'', 1st ed. Toronto, ON, Canada.: Nimbus Publishing, 2014</ref>		5. Natural gas and oil are both lighter than water, so as they escape from the source oil shale the products rise through pores in rocks, displacing water. Rock bodies that contain significant amounts of oil or natural gas are known as [[Oil and gas reservoir\|reservoir]] rocks. For the gas to remain trapped in the reservoir, there must be some sort of thick, impermeable layer of rock to seal the reservoir. If this seal exists, then oil, gas, and water are trapped beneath and can be drilled into to obtain the oil.<ref name="canada">Canadian Federation of Earth Sciences. (May 11, 2015). ''Four Billion Years and Counting: Canada's Geological Heritage'', 1st ed. Toronto, ON, Canada.: Nimbus Publishing, 2014</ref>
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	==Unconventional Sources==		==Unconventional Sources==
	The process above describes the formation of natural gas in a traditional, conventional deposit. However, unconventional deposits such as [[shale gas]] and [[coal bed methane]] are also sources of natural gas. In these deposits, natural gas is stored differently and is also more difficult to access than with traditional deposits.		The process above describes the formation of natural gas in a traditional, [[Conventional vs unconventional resource\|conventional deposit]]. However, [[Unconventional resource\|unconventional deposits]] such as [[shale gas]] and [[coal bed methane]] are also sources of natural gas. In these deposits, natural gas is stored differently and is also more difficult to access than with traditional deposits.

	==References==		==References==
	{{reflist}}		{{reflist}}
	[[Category:Uploaded]]		[[Category:Uploaded]]

J.williams: 1 revision imported

2015-08-26T21:31:24Z

1 revision imported

← Older revision	Revision as of 21:31, 26 August 2015
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J.williams at 16:57, 12 August 2015

2015-08-12T16:57:04Z

New page

[[Category:Done 2015-06-11]]
<onlyinclude>'''Natural gas''' is a [[fossil fuel]] that is composed mainly of [[methane]] - composed itself of [[carbon]] and [[hydrogen]] - and is thus known as a [[hydrocarbon]].<ref name="RE1">Natural Resources Canada. (May 28, 2015). ''Natural Gas: A Primer'' [Online]. Available: https://www.nrcan.gc.ca/energy/natural-gas/5641</ref> The formation of gas is essentially the same as the [[oil formation|formation of oil]] and thus takes a significant amount of [[timescale of the universe|time]] with natural gas beginning to form millions of years ago.</onlyinclude>

The formation of natural gas begins in warm, shallow oceans that were present on the Earth millions of years ago. In these oceans, extremely small dead organic matter - classified as plankton - falls to the floor of the ocean. This plankton consists of animals, called ''zooplankton'', or plants, called ''phytoplankton''. This material then lands on the ocean floor and mixes with inorganic material that enters the ocean by rivers. It is this sediment on the ocean floor that then forms oil and natural gas over many years. The energy in [[natural gas]] initially comes from the [[Sun]], and is energy from sunlight trapped by dead plankton.<ref name="wolfson">R. Wolfson. ''Energy, Environment and Climate'', 2nd ed. New York, U.S.A.: Norton, 2012, pp. 96-97</ref>

==Formation Process==
[[File:oilgasformation2.png|400px|center|framed]]
The process that creates natural gas is the same as the process that creates oil, and is generally the same in most areas. However, there may be different types of plant and animal debris that falls to the ocean floor and slightly different conditions. To form natural gas, the following steps are followed:<ref name="wolfson"/><ref name="geo">Stephen Marshak. (May 11, 2015). ''Earth: Portrait of a Planet'', 3rd ed. New York, NY, U.S.A:W.W. Norton & Company, 2008</ref>

1. Dead plankton - both phytoplankton and zooplankton - as well as [[algae]] and bacteria sink to the bottom of an ancient ocean and mix with inorganic, clay-like materials that enter these oceans from streams and rivers. This creates an organic-rich mud. This mud can only form in still water environments. This step is shown in Figure 1, panel A.

2. This mud cannot be exposed to too much [[oxygen]], or else the organic matter in the mud would be decomposed by bacteria and disappear quickly. Therefore environments where natural gas can form are known as anoxic environments. Before this organic matter is destroyed, it is buried by more sediment and ''lithifies'' (becomes sedimentary rock), creating ''organic shale''. This step is shown in Figure 1, panel B.

3. If this shale is buried between 2 and 4 kilometers, its temperature increases due to its location in the [[Cross section of the Earth|Earths interior]]. This increasing [[pressure]] and [[temperature]] of the shale transforms it into a waxy material known as '''[[kerogen]]'''. Shale that contains this material is known as '''oil shale'''.

4. If temperatures of the kerogen are ''greater'' than [[Celsius|90°C]] but lower than 160°C, the kerogen is transformed into [[oil]] and natural gas. At temperatures greater than 90°C, the only product is natural gas or graphite.

5. Natural gas and oil are both lighter than water, so as they escape from the source oil shale the products rise through pores in rocks, displacing water. Rock bodies that contain significant amounts of oil or natural gas are known as [[Oil and gas reservoir|reservoir]] rocks. For the gas to remain trapped in the reservoir, there must be some sort of thick, impermeable layer of rock to seal the reservoir. If this seal exists, then oil, gas, and water are trapped beneath and can be drilled into to obtain the oil.<ref name="canada">Canadian Federation of Earth Sciences. (May 11, 2015). ''Four Billion Years and Counting: Canada's Geological Heritage'', 1st ed. Toronto, ON, Canada.: Nimbus Publishing, 2014</ref>

6. Geological changes in the Earth's crust bring these deposits up closer to the surface, making them somewhat easier to access.<ref>J. Kraushaar, R. Ristinen. (May 11, 2015).Energy and the Environment, 2nd ed. Hoboken, NJ, U.S.A.: John Wiley & Sons, 2006, pp. 54</ref> This step is shown in Figure 1, panel C.

==Unconventional Sources==
The process above describes the formation of natural gas in a traditional, conventional deposit. However, unconventional deposits such as [[shale gas]] and [[coal bed methane]] are also sources of natural gas. In these deposits, natural gas is stored differently and is also more difficult to access than with traditional deposits.

==References==
{{reflist}}
[[Category:Uploaded]]