Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Methane clathrate
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
==Structure and composition== [[File:Gas_Hydrate_Crystals.jpg|thumb|microscope image]] The nominal methane clathrate hydrate composition is (CH<sub>4</sub>)<sub>4</sub>(H<sub>2</sub>O)<sub>23</sub>, or 1 [[mole (unit)|mole]] of methane for every 5.75 moles of water, corresponding to 13.4% methane by mass, although the actual composition is dependent on how many methane molecules fit into the various cage structures of the water [[Crystal structure|lattice]]. The observed density is around 0.9 g/cm<sup>3</sup>, which means that methane hydrate will float to the surface of the sea or of a lake unless it is bound in place by being formed in or anchored to sediment.<ref name=Max>{{Cite book |last=Max |first=Michael D. |title=Natural Gas Hydrate in Oceanic and Permafrost Environments |publisher=Kluwer Academic Publishers |year=2003 |page=62 |url=https://books.google.com/books?id=fd8QFKwcSskC |isbn=978-0-7923-6606-5}}</ref> One litre of fully saturated methane clathrate solid would therefore contain about 120 grams of methane (or around 169 litres of methane gas at 0 Β°C and 1 atm),{{#tag:ref|The average methane clathrate hydrate composition is 1 [[mole (unit)|mole]] of methane for every 5.75 moles of water. The observed density is around 0.9 g/cm<sup>3</sup>.<ref name=Max/> For one mole of methane, which has a molar mass of about 16.043 g (see [[Methane]]), we have 5.75 moles of water, with a molar mass of about 18.015 g (see [[Properties of water]]), so together for each mole of methane the clathrate complex has a mass of {{nowrap|16.043 g + 5.75 Γ 18.015 g}} β 119.631 g. The fractional contribution of methane to the mass is then equal to {{nowrap|16.043 g / 119.631 g}} β 0.1341. The density is around 0.9 g/cm<sup>3</sup>, so one litre of methane clathrate has a mass of around 0.9 kg, and the mass of the methane contained therein is then about {{nowrap|0.1341 Γ 0.9 kg}} β 0.1207 kg. At a density as a gas of 0.716 kg/m<sup>3</sup> (at 0 Β°C; see the info box at [[Methane]]), this comes to a volume of {{nowrap|0.1207 / 0.716 m<sup>3</sup>}} = 0.1686 m<sup>3</sup> = 168.6 L.|group="nb"}} or one cubic metre of methane clathrate releases about 160 cubic metres of gas.<ref name=BBCMay17 /> Methane forms a "structure-I" hydrate with two [[dodecahedron|dodecahedral]] (12 vertices, thus 12 water molecules) and six [[tetradecahedron|tetradecahedral]] (14 water molecules) water cages per unit cell. (Because of sharing of water molecules between cages, there are only 46 water molecules per unit cell.) This compares with a [[hydration number]] of 20 for methane in aqueous solution.<ref name="Dec 2005">{{Cite journal |title=Direct Measure of the Hydration Number of Aqueous Methane |journal=[[Journal of the American Chemical Society|J. Am. Chem. Soc.]] |year=2006 |volume=128 |issue=2 |pages=414β415 |doi=10.1021/ja055283f |pmid=16402820 |last1=Dec |first1=Steven F. |last2=Bowler |first2=Kristin E. |last3=Stadterman |first3=Laura L. |last4=Koh |first4=Carolyn A. |last5=Sloan |first5=E. Dendy}} Note: the number 20 is called a [[magic number (chemistry)|magic number]] equal to the number found for the amount of water molecules surrounding a [[hydronium ion]].</ref> A methane clathrate [[Magic angle spinning|MAS NMR]] spectrum recorded at 275 [[kelvin|K]] and 3.1 [[Pascal (unit)|MPa]] shows a peak for each cage type and a separate peak for [[gas phase]] methane.{{Citation needed|date=September 2010}} In 2003, a clay-methane hydrate intercalate was synthesized in which a methane hydrate complex was introduced at the interlayer of a sodium-rich [[montmorillonite]] clay. The upper temperature stability of this phase is similar to that of structure-I hydrate.<ref name="Guggenheim 2003">{{Cite journal |last=Guggenheim |first=S |author2=Koster van Groos AF |year=2003 |title=New gas-hydrate phase: Synthesis and stability of clay-methane hydrate intercalate |journal=[[Geology (journal)|Geology]] |volume=31 |issue=7 |pages=653β656 |doi=10.1130/0091-7613(2003)031<0653:NGPSAS>2.0.CO;2 |bibcode=2003Geo....31..653G}}</ref> [[File:Methane Hydrate phase diagram.jpg|thumb|Methane hydrate phase diagram. The horizontal axis shows temperature from -15 to 33 Celsius, the vertical axis shows pressure from 0 to 120,000 kilopascals (0 to 1,184 atmospheres). Hydrate forms above the line. For example, at 4 Celsius hydrate forms above a pressure of about 50 atm/5000 kPa, found at about 500m sea depth.]]
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)