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gas hydrate - CCOP

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a<br />

b<br />

100<br />

4<br />

92% of recoverable CH 4 (sII+CO 2 )<br />

Relative moles in <strong>hydrate</strong> phase<br />

3<br />

2<br />

1<br />

CH 4<br />

C 2<br />

H 6<br />

CO 2<br />

0 200 400 600 800 1000 1200 1400 1600<br />

Replacement rate (mol%)<br />

80<br />

60<br />

40<br />

20<br />

85% of recoverable CH 4 (sI+CO 2 +N 2 )<br />

64% of recoverable CH 4 (sI+CO 2 )<br />

0<br />

0 200 400 600 800 1000 1200 1400 1600 1800 2000<br />

t (min)<br />

0<br />

0 200 400 600 800 1000 1200 1400 1600<br />

t (min)<br />

Figure 4. (a) Relative moles in the sII CH 4 + C 2 H 6 <strong>hydrate</strong> replaced with CO 2 measured by<br />

<strong>gas</strong> chromatography. (b) Replacement rate of CH 4 molecules encaged in sI CH 4 <strong>hydrate</strong>s by<br />

N 2 + CO 2 mixture (square) and in sII CH 4 <strong>hydrate</strong> by pure CO 2 (circle). The recovered CH 4 is<br />

85% for the N 2 + CO 2 mixture and 92% for sII CH 4 <strong>hydrate</strong> with CO 2 . The dotted line<br />

represents the 64% recovery rate of CH 4 obtained during swapping process between sI CH 4<br />

<strong>hydrate</strong> and pure CO 2 .<br />

CONCLUSION<br />

First, we focused on the direct sequestration of <strong>gas</strong> mixtures containing CO 2 and N 2 into the<br />

preponderant sI naturally-occurring CH 4 <strong>hydrate</strong> deposits. However, for ocean storage,<br />

recently proposed approaches require that injected CO 2 must be in a pure state, and thus an<br />

appropriate separation procedure of CO 2 from the mixed <strong>gas</strong> must be conducted. A<br />

spectroscopic analysis reveals that the external N 2 molecules specifically attack CH 4<br />

molecules already entrapped in sI-S and play a significant role in substantially increasing the<br />

CH 4 recovery rate. On the contrary, during swapping the sII CH 4 <strong>hydrate</strong> structurally<br />

transforms to sI, which causes CH 4 molecules in sII-S to spontaneously be released through a<br />

continuous reduction of small cage sites. The cage-specific occupation accomplished by direct<br />

invasion of external guest molecules largely depends on their molecular details that appear to<br />

be so complex for visualization, but this mutually interactive pattern of targeted guest-cage<br />

conjugates might possess an important implication on the extensive <strong>hydrate</strong>-based<br />

applications as clearly illustrated in the swapping process between CO 2 stream and CH 4<br />

<strong>hydrate</strong>. However, the swapping rate and total yield of the replacement reaction in actual<br />

natural <strong>gas</strong> <strong>hydrate</strong> deposits will depend on a variety of factors such as particle size and <strong>gas</strong><br />

transport.<br />

New Energy Resources in the <strong>CCOP</strong> Region - Gas Hydrates and Coalbed Methane 103

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