TOPIC 1: Gas Hydrates
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NIVERSITY B41OA December 2018 v3
Reminder-2: Micro-organisms at the top few hundred metres of marine
sediments consume organic materials within the sediments and
produce various gases, mainly methane. The resulting gas is termed as
biogenic gas.
Reminder-3: Organic materials transferred
to higher depths are
decomposed due to high pressure and temperature conditions. The
resulting hydrocarbons migrate upward due to lower density, compared
with that of water in the porous media. This type of hydrocarbon is
called thermogenic.
5. In permafrost regions the ice overburden pressure and pore water
pressure (inside the sediments where temperature
is higher than ice
melting point), combined with low temperature environment, provide
favourable conditions for gas hydrate formation.
The geographic location of gas hydrate deposits are shown in Figure 3:
Figure 3: Locations of Identified Hydrate Deposits (adapted
from Koh
and Sloan, 2008)
6. In offshore drilling, the drilling fluid pressure together with low
temperature conditions in deepwater and arctic
drilling provides the
necessary conditions for gas hydrate formation.
Reminder-4: If a gas kick occurs then the gas influx must be circulated
out of the drill string. If conditions are favourable, then this can lead to
hydrate formation.
TOPIC 1: Gas Hydrates
8
©H
ERIOT
-W
ATT
U
NIVERSITY B41OA December 2018 v3
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