Difference between revisions of "Team:UiOslo Norway/Overview"

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<a href="https://2015.igem.org/Team:UiOslo_Norway" class="tooltip">  
 
<a href="https://2015.igem.org/Team:UiOslo_Norway" class="tooltip">  
 
paddy fields  
 
paddy fields  
<span>  Bacteria in the soil that produce methane). </span> </a>  
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<span>  Bacteria in the soil that produce methane. </span> </a>  
  
 
(rice fields). Natural methane emission places are for example  
 
(rice fields). Natural methane emission places are for example  
  
wetlands
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<a href="https://2015.igem.org/Team:UiOslo_Norway" class="tooltip">
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wetlands
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<span>  land areas saturated with water in which methane producing bacteria reside. </span> </a>
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or
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<a href="https://2015.igem.org/Team:UiOslo_Norway" class="tooltip">
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gas hydrates
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<span>  Gas hydrates are trapped ice-like crystals of gas that are only stable in a specific temperature and pressure range. Found on continental shelves and under permafrost. </span> </a>
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To minimize the leakage of methane in these or other places one would want to breakdown methane locally. Or even better, one could convert methane to methanol or biomass so it can be more easily transported and used as a bio-fuel instead of being discarded of. The current technology doesn't allow this kind of small scale local breakdown of methane, because this process requires high pressure and very high temperatures to break the strong bonds within one methane molecule.6⁠ An attractive alternative is bio-conversion of methane.
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<a href="https://2015.igem.org/Team:UiOslo_Norway" class="tooltip">
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Methanotrophs
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<span>  single-cell organisms that metabolise methane. </span> </a>
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can naturally breakdown methane and use it as their sole carbon and energy sourse. Even better, the enzyme
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<a href="https://2015.igem.org/Team:UiOslo_Norway" class="tooltip">
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methane monooxygenase (MMO)
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<span>  link to more info </span> </a>
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that these methanotrophs use can breakdown methane at ambient temperatures and pressure.6–9⁠
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</p>
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<p>
  
 
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Revision as of 10:19, 4 August 2015

Project overview

Methane is a potent greenhouse gas, and is leaked into the atmosphere at different natural and industrial places. A big part of the industrial methane emission is in the agricultural sector in places like barns, Bacteria in the rumen of cows and other cattle produce methane. ⁠or paddy fields Bacteria in the soil that produce methane. (rice fields). Natural methane emission places are for example wetlands land areas saturated with water in which methane producing bacteria reside. or gas hydrates Gas hydrates are trapped ice-like crystals of gas that are only stable in a specific temperature and pressure range. Found on continental shelves and under permafrost. To minimize the leakage of methane in these or other places one would want to breakdown methane locally. Or even better, one could convert methane to methanol or biomass so it can be more easily transported and used as a bio-fuel instead of being discarded of. The current technology doesn't allow this kind of small scale local breakdown of methane, because this process requires high pressure and very high temperatures to break the strong bonds within one methane molecule.6⁠ An attractive alternative is bio-conversion of methane. Methanotrophs single-cell organisms that metabolise methane. can naturally breakdown methane and use it as their sole carbon and energy sourse. Even better, the enzyme methane monooxygenase (MMO) link to more info that these methanotrophs use can breakdown methane at ambient temperatures and pressure.6–9⁠